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		<id>https://soil.evs.buffalo.edu/index.php?title=Fungal_farming&amp;diff=6639</id>
		<title>Fungal farming</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Fungal_farming&amp;diff=6639"/>
		<updated>2021-05-05T04:01:27Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
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&lt;div&gt;Fungus farming is a form of symbiosis between fungi and fungi-growing organism in which a species facilitates the growth of a fungal species in order to create a stable food supply. This mutualistic behavior is an example of how two species can co-evolve over time through interactions that are mutually beneficial and often results in obligate relationships.[1] [[File:Screenshot (15).png|thumb|Leaf cutter ants carrying leaves to feed their fungus crop.]]&lt;br /&gt;
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Fungus farming is thought to have originated some 30-60 million years ago and evolved in three different insects, specifically ants, beetles, and termites.[2] While it was previously thought to be exclusive to insects, recent findings has uncovered this behavior in a species of snail which indicates that this phenomenon may be more common than previously thought. &amp;lt;!--I think this sentence could read &amp;quot;while it was previously thought to be exclusive to insects, recent findings has uncovered this behavior in a species of snail. (done)&amp;quot; --&amp;gt;  &lt;br /&gt;
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== &#039;&#039;&#039;Farming Process&#039;&#039;&#039; ==&lt;br /&gt;
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Similar to human agriculture, fungus farmers must go through a process to prepare and care for their crops. In order to culture fungi, farmers must prepare the substrate and inoculate their crop in prime growing conditions. Growers must also tend to their crop as it grows to ensure the success of the crop. Tending to crops can be in the form of fertilization or as protection from competition, pests, and pathogens. Once the crop is fully grown the farmers can harvest and consume the fungi.[1][3] Subsisting on farmed fungus over time creates a nutritional dependency.[2] Fungus farming relationships are obligate mutualisms because both the fungus and farmer rely on each other due to generations of the dependency.[4] &lt;br /&gt;
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The exact process a fungus farmer goes through to cultivate their crop can vary among species of farmers, as well as species of fungi. Fungus cultivation can be characterized as either high-level food production or low-level food production.[5] Low-level food production consists of altering the environment to promote or protect the fungus. High-level fungus production involves more complicated steps such as transporting and planting the fungus, fertilization, and protecting the crops physically or chemically.[5][3]&lt;br /&gt;
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===&#039;&#039;&#039;Terrestrial Systems&#039;&#039;&#039;=== &lt;br /&gt;
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The majority of fungus farming mutualisms are found in terrestrial systems because this relationship evolved in 3 distinct insect lineages, ants(&#039;&#039;Formicidae&#039;&#039;), termites(&#039;&#039;Isoptera&#039;&#039;), and beetles(&#039;&#039;[[Coleoptera]]&#039;&#039;).  These mutualisms evolved independently in each of the 3 [[insects]] resulting in unique farming practices between the various farmers.[2]  &lt;br /&gt;
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====&#039;&#039;&#039;Ants&#039;&#039;&#039;====&lt;br /&gt;
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Fungus-growing ants are a monophyletic group that is a part of the Formicidae family and grouped together into a tribe known as Attina. Attine ants are thought to have originated around 40-60 million years ago in the tropical forests of South America.[6][7] Currently there are more than 200 known species of attine ants, including the well-known leaf-cutter ants, and they are all found in the western hemisphere, in tropical rainforests.[5] It is currently unknown how these farming relationships started, but there have been 2 models put forward to try and explain its origins.[7] The “consumption first” model states that the cultured fungi began as part of the ant’s diet and overtime the ants started to grow the fungi which then lead to the transferring and spread of the crop.[7] The opposing model is called the “transmission first” model which states the fungi could have been dispersed by the ants before they became part of their diet.[7] &lt;br /&gt;
[[File:Atta colombica queen.jpg|thumb|An &#039;&#039;Atta colombica&#039;&#039; queen and workers standing in their fungal farm. &#039;&#039;Atta colombica&#039;&#039; is a species of leafcutter ants.]]&lt;br /&gt;
The farming process begins when a young female leaves the mother colony to find her own. The founding ant brings with her some fugus from the parent colony to start the farm for the new colony. The farms are grown in enclosed, often subterranean burrows and the ants must collect some type of growth material and substrate to propagate their crop. Most attine farmers grow [[Basidiomycota]] fungi, with a majority of fungi belonging to the Leucocoprinus genus.[8] While the crops grow the ants must tend to their crop and this can include fertilization with organic and fecal material or weeding of unwanted invaders or predators. [1] While the general process of fungal farming is relatively similar between different species of attine ants, there are some unique differences. Throughout the history of the fungus farming ants there have been five agriculture systems that have been observed. The five agriculture systems of attine ants are 1) Lower agriculture, 2) Coral-fungal agriculture, 3) Yeast agriculture, 4) Generalized higher agriculture, and 5) Leafcutter agriculture.[8]&lt;br /&gt;
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Lower agriculture refers to the simplest and oldest form of fungal farming. Ants belonging to this system culture Leucocoprinus fungi and employ a number of different substrate types including bits of grasses, fruit flesh, seeds, insect waste, wood, flower parts, and other organic materials.[8] &lt;br /&gt;
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Coral-fungal agriculture differs from the other systems because this agricultural system grows Pterulaceae fungi instead of fungi belonging to the Leucocoprineae. This system is poorly studied but some of the substrates that have been found are insect frass, seeds, detritus material, wood, and even [[arthropod]] parts.[8]&lt;br /&gt;
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Yeast agriculture is where the attine ants grow yeats-like fungi that are closely related to Leucocoprineae. In this system the fungi are grown as unicellular nodules rather than a multicellular phase.[8] The substrate that is typically used for this system is arthropod waste, but there have been some species that reguritate nectar and sap onto the crops to promote its growth.[8]&lt;br /&gt;
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Generalized higher agriculutre is characterized by domesticated fungi that are not considered free-living. These domesticated fungi prodcue nutrient righ hyphal tips, called “gongylidia”.[8] Ants that utlize this system use similar substrates as the previous systems, but also collect live and fresh plant matter to use as substrate, such as plant shoots, flower petals, and leaves.[8]&lt;br /&gt;
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Leafcutter agriculture is the final and most complex system of fungus farming. This system differs from generalized higher agriculutre mainly because leafcutter agriculutre primarily use cut plant matreial as growth substrate.[8] The well-known Leafcutter ants belong to this agriculutre system, hence the name. Leafcutter ants not only physically cut plant material from living plants for substrate use, but also tend to their crop by weeding out unwanted microfungi.[9]  &lt;br /&gt;
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====&#039;&#039;&#039;Termites&#039;&#039;&#039;====&lt;br /&gt;
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Around the same time ants began to develop their mutualistic relationships with fungus, termites were also developing their own farming techniques. Fungus-growing termites, Macrotermitinae, belong to the Termitidae family and are thought to have originated around 30 million years ago in African rainforest.[10] Today there are around 300 species of termites that cultivate fungi and they can be found throughout Africa, Asia, and Europe. [2] A defining characteristic of Macrotermitinae are the complex mounds that these termites make that house the termites and the fungus farms. Inside of these mounds there are specialized burrows that are known as combs that are used to cultivate their fungi.[2]&lt;br /&gt;
[[File:Termite fungus farm.jpg|thumb|An exposed termite mound shows one of their hidden fungal farms.]]&lt;br /&gt;
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Once the comb burrow has been dug out the termites prepare the combs by depositing feces. The feces is nutrient rich and mixed with semi-digested plant material such as leaves, grass, and wood.[2] The termites grow a specific fungus known as Termitomyces, which belong to the Basidiomycota. These fungi can survive the digestion of the termites when consumed and this allows the termites to deposit both the fungal spores and fecal matter together in the combs. [2] Depositing the spores and feces allows the termites to plant their crop but also fertilize it at the same time. Unlike the attine ants, the fungi planted by termites grow until they form fruiting bodies and spores.[11] The farmers then harvest and consume the fungi, but since the spores can survive the gut of the termite the cycle can continue.&lt;br /&gt;
          &lt;br /&gt;
====&#039;&#039;&#039;Beetles&#039;&#039;&#039;====&lt;br /&gt;
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Beetles are a type of insect that make up the Coleoptera and include some beetles that have been found to cultivate fungi. The beetles that are found to grow fungi are considered weevils, a subfamily of Coleopterans. These beetles create burrows in host trees and the fungal farms are found inside some of these burrows. This symbiosis between beetles and fungi are thought to have originated around 60 million years ago.[12] Fungal farming in ants and termites evolved only once but this mutualism is believed to have evolved at least 7 times in beetles. [1] Beetles that engage in fungus faming are known as Ambrosia beetles because they found to exclusively grow ambrosia fungi.[13] Presently there are over 3000 known beetles that farm fungus and majority of them are found in tropical forests, there are a few species that are found in temperate systems.[12] The reason for the greater abundance of fungal farming beetles in the tropics is because temperate habitats are typically drier and may not have enough moisture to support fungal cultivation.[12]&lt;br /&gt;
[[File:Xylosandrus_crassiusculus_galleryR.jpg|thumb|The larvae of &#039;&#039;Xylosandrus crassiusculus&#039;&#039;, a species of ambrosia beetles surrounded by a black fungus farm.]]&lt;br /&gt;
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To begin the farming process the beetles will burrow into living, and sometimes dead, trees and create elaborate tunnels. Once the tunnels are complete the beetles can start to inoculate their crop. Beetles employ a unique method to acquire their crops. The beetles have a morphological structure known as a “mycangia” which is simply a pocket on the beetle that is specifically used to transport fungi.[12] Using their mycangia, beetles collect fungus spores and bring them back to the host tree which harbors the beetle colony and begin to plant their crop.[12] The fungi are planted within the walls of the tunnels and left to grow into the host plants xylem and phloem, which further promotes their growth.[12] Once the crop grows to maturity the fungus will form a layer of hyphae on the walls of the burrow known as “ambrosia”.[14] Both adult and larvae feed on these fungi and when it is time for a beetle to leave the colony it will bring spores with it in its mycangia to ensure the success of the future farm.        &lt;br /&gt;
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===&#039;&#039;&#039;Aquatic Systems&#039;&#039;&#039;===&lt;br /&gt;
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While the majority of fungus farmers are found in terrestrial systems that does not mean that fungus farming is exclusive to those systems. A study in 2003 found the first evidence of fungal farming in an aquatic system and outside of the insect family. &lt;br /&gt;
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====&#039;&#039;&#039;Marine snail&#039;&#039;&#039;====  &lt;br /&gt;
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The Periwinkle snail, &#039;&#039;Littoraria irrorata&#039;&#039;, is the first observed example of fungal farming that is not associated with terrestrial systems or insects. This snail is a grazer that is typically found on marsh cordgrasses, such as &#039;&#039;Spartina alterniflora&#039;&#039;. [1] While it was previously though that these snails were [[detritivores]], researchers discovered that the snail is an active grazer of these grasses. [1] This grazing is a key part of the fungal farming process. &lt;br /&gt;
[[File:Marsh_periwinkle_001.jpg|thumb|&#039;&#039;Littoraria irrorata&#039;&#039; on marsh grasses where their fungal farms are located]]&lt;br /&gt;
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The first step in the farming process of these snails is preparing the substrate. To prepare the substrate the snail uses its radulae to cut openings in the leaf surface. This activity is mainly to promote the growth of fungi because the snails do not feed on the cut plant material. [1] The wounds expose the inner plant material which is a nutritious food source for [[ascomycete]] fungi and these fungi populate around these wounds. To increase the success of their farming efforts, the snail will deposit fecal pellets that are rich in nitrogen and hyphae onto the open wounds where the fungi have invaded. [1] These fecal pellets act as a fertilizer for the fungi and may also increase propagules due to the hyphae, although it is unknown whether the hyphae are vital. [1] Some unique aspects of the fungal farming process of these snails is that they do not inoculate their crop or weed out unwanted invaders. [1] The spores of these fungi are rather abundant in the system so snails do not need to find spores because they already present. [1] Even though the fungi are the preferred food of the snails, this relationship is facultative for both species. [1]&lt;br /&gt;
&amp;lt;!--Overall I think youve done a really good job at presenting and structuring your page! I would only suggest altering some sentences for them to sound more formal.--&amp;gt;&lt;br /&gt;
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==References==&lt;br /&gt;
[1] Silliman, B.R., Newell, S.Y., 2003. Fungal farming in a snail. Proc. Natl. Acad. Sci. U. S. A. 100, 15643–15648. https://doi.org/10.1073/pnas.2535227100&lt;br /&gt;
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[2] Mueller, U.G., Gerardo, N., 2002. Fungus-farming insects: Multiple origins and diverse evolutionary histories. Proc. Natl. Acad. Sci. U. S. A. 99, 15247–15249. https://doi.org/10.1073/pnas.242594799&lt;br /&gt;
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[3] Wang, L., Feng, Y., Tian, J., Xiang, M., Sun, J., Ding, J., Yin, W.B., Stadler, M., Che, Y., Liu, X., 2015. Farming of a defensive fungal mutualist by an attelabid weevil. ISME J. 9, 1793–1801. https://doi.org/10.1038/ismej.2014.263&lt;br /&gt;
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[4] Toki, W., Tanahashi, M., Togashi, K., Fukatsu, T., 2012. Fungal farming in a non-social beetle. PLoS One 7. https://doi.org/10.1371/journal.pone.0041893&lt;br /&gt;
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[5] Rehner, S. a, 2005. Phyllogenetics of the insect pathogenic genus Beauveria, Insect-fungal associations: [[ecology]] and evolution.&lt;br /&gt;
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[6] Branstetter, M.G., Ješovnik, A., Sosa-Calvo, J., Lloyd, M.W., Faircloth, B.C., Brady, S.G., Schultz, T.R., 2017. Dry habitats were crucibles of domestication in the evolution of agriculture in ants. Proc. R. Soc. B Biol. Sci. 284. https://doi.org/10.1098/rspb.2017.0095&lt;br /&gt;
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[7] Mueller, U.G., Schultz, T.R., Currie, C.R., Adams, R.M.M., Schultz, R., 2001. The Origin of the Attine Ant-Fungus Mutualism David Malloch Source : The Quarterly Review of Biology , Vol . 76 , No . 2 ( Jun ., 2001 ), pp . 169-197 Published by : The University of Chicago Press Stable URL : http://www.jstor.org/stable/2664003 . The Un 76, 169–197.&lt;br /&gt;
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[8] Mehdiabadi, N.J., Schultz, T.R., 2009. Natural histroy and phylogeny of the fungus-farming ants ([[Hymenoptera]]: Formicidae: Myrmicinae: Attini). Myrmecological News 13, 37–55 &lt;br /&gt;
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[9] Rodrigues, A., Bacci, M., Mueller, U.G., Ortiz, A., Pagnocca, F.C., 2008. Microfungal “weeds” in the leafcutter ant symbiosis. Microb. Ecol. 56, 604–614. https://doi.org/10.1007/s00248-008-9380-0&lt;br /&gt;
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[10] Aanen, D.K., Eggleton, P., 2005. Fungus-growing termites originated in African rain forest. Curr. Biol. 15, 851–855. https://doi.org/10.1016/j.cub.2005.03.04 &lt;br /&gt;
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[11] Aanen, D.K., Eggleton, P., Rouland-Lefèvre, C., Guldberg-Frøslev, T., Rosendahl, S., Boomsma, J.J., 2002. The evolution of fungus-growing termites and their mutualistic fungal symbionts. Proc. Natl. Acad. Sci. U. S. A. 99, 14887–14892. https://doi.org/10.1073/pnas.222313099&lt;br /&gt;
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[12] Farrell, B.D., Sequeira, A.S., O’Meara, B.C., Normark, B.B., Chung, J.H., Jordal, B.H., 2001. The evolution of agriculture in beetles (Curculionidae: Scolytinae and Platypodinae). Evolution (N. Y). 55, 2011–2027. https://doi.org/10.1111/j.0014-3820.2001.tb01318.x&lt;br /&gt;
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[13] Hulcr, J., Atkinson, T.H., Cognato, A.I., Jordal, B.H., McKenna, D.D., 2015. Morphology, Taxonomy, and Phylogenetics of Bark Beetles, Bark Beetles: Biology and Ecology of Native and Invasive Species. https://doi.org/10.1016/B978-0-12-417156-5.00002-2&lt;br /&gt;
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[14] BEAVER, R.A., 1989. Insect–Fungus Relationships in the Bark and Ambrosia Beetles. Insect-fungus Interact. 121–143. https://doi.org/10.1016/b978-0-12-751800-8.50011-2&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=File:Screenshot_(15).png&amp;diff=6638</id>
		<title>File:Screenshot (15).png</title>
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		<updated>2021-05-05T04:00:12Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: Leaf cutter ants carrying leaves to feed their fungus crop. 
Thomas Janisch / Getty Images
From: https://www.treehugger.com/crazy-facts-leaf-cutter-ants-4864484&lt;/p&gt;
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&lt;div&gt;Leaf cutter ants carrying leaves to feed their fungus crop. &lt;br /&gt;
Thomas Janisch / Getty Images&lt;br /&gt;
From: https://www.treehugger.com/crazy-facts-leaf-cutter-ants-4864484&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6632</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6632"/>
		<updated>2021-05-05T03:44:51Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
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&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
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Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes.]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
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While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
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Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
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==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
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The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils.[[File:Desert Grassland Landscape.jpg|thumb|320px|A desert biome (Left) and a grassland biome (Right).]]&lt;br /&gt;
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====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
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====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes: [[File:Amazon soil.jpg|right|thumb|Soil profile of an eroded hill in a tropical forest biome. A majority of the soil is nutrient poor (Light color soil) with a small amount of fertile soil (dark color soil).]]&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7][[File:Permafrost layers.png|right|thumb|320px|Diagram of a tundra biome soil layer showing permafrost.]] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]&lt;br /&gt;
&lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
[[File:Freshwater.jpg|thumb|A lake at Acadia National Park, ME. Lakes are classified as freshwater biomes.]]&lt;br /&gt;
&lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
[[File:Deforestation.jpg|thumb|A forest biome that has been cut down to make room for agriculture.]]&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
[[File:Garbage pactch.jpg|thumb|A patch of garbage and plastics floating in the ocean.]]&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25] Runoff is a major source of pollution, specifically chemicals and excess nutrients, for both marine and freshwater systems.[26][27]&lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;br /&gt;
&lt;br /&gt;
[26] National Geographic Society. Marine pollution. https://www.nationalgeographic.org/encyclopedia/marine-pollution/#:~:text=Marine%20pollution%20is%20a%20combination,and%20to%20economic%20structures%20worldwide.&lt;br /&gt;
&lt;br /&gt;
[27] Pollution Issues. Water pollution: freshwater. http://www.pollutionissues.com/Ve-Z/Water-Pollution-Freshwater.html#:~:text=Freshwater%20pollution%20is%20the%20contamination,sediment%2C%20or%20even%20heated%20discharges.&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6631</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6631"/>
		<updated>2021-05-05T03:23:46Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: /* Aquatic */&lt;/p&gt;
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&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes.]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils.[[File:Desert Grassland Landscape.jpg|thumb|320px|A desert biome (Left) and a grassland biome (Right).]]&lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes: [[File:Amazon soil.jpg|right|thumb|Soil profile of an eroded hill in a tropical forest biome. A majority of the soil is nutrient poor (Light color soil) with a small amount of fertile soil (dark color soil).]]&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7][[File:Permafrost layers.png|right|thumb|320px|Diagram of a tundra biome soil layer showing permafrost.]] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]&lt;br /&gt;
&lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
[[File:Freshwater.jpg|thumb|A lake at Acadia National Park, ME. Lakes are classified as freshwater biomes.]]&lt;br /&gt;
&lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
[[File:Deforestation.jpg|thumb|A forest biome that has been cut down to make room for agriculture.]]&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
[[File:Garbage pactch.jpg|thumb|A patch of garbage and plastics floating in the ocean.]]&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6630</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6630"/>
		<updated>2021-05-05T03:21:12Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes.]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils.[[File:Desert Grassland Landscape.jpg|thumb|320px|A desert biome (Left) and a grassland biome (Right).]]&lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes: [[File:Amazon soil.jpg|right|thumb|Soil profile of an eroded hill in a tropical forest biome. A majority of the soil is nutrient poor (Light color soil) with a small amount of fertile soil (dark color soil).]]&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7][[File:Permafrost layers.png|right|thumb|320px|Diagram of a tundra biome soil layer showing permafrost.]] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]&lt;br /&gt;
&lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
[[File:Freshwater.jpg|thumb|A lake at Acadia National Park, ME. Lakes are classified as freshwater biomes.]]&lt;br /&gt;
&lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
[[File:Deforestation.jpg|thumb|A forest biome that has been cut down to make room for agriculture.]]&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
[[File:Garbage pactch|thumb|A patch of garbage and plastics floating in the ocean.]]&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=File:Garbage_pactch.jpg&amp;diff=6629</id>
		<title>File:Garbage pactch.jpg</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=File:Garbage_pactch.jpg&amp;diff=6629"/>
		<updated>2021-05-05T03:19:49Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: A patch of garbage and plastics floating in an ocean.
© SHAUNL
From: https://www.conservation.org/stories/ocean-pollution-11-facts-you-need-to-know&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;A patch of garbage and plastics floating in an ocean.&lt;br /&gt;
© SHAUNL&lt;br /&gt;
From: https://www.conservation.org/stories/ocean-pollution-11-facts-you-need-to-know&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6549</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6549"/>
		<updated>2021-05-04T22:00:10Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: /* Marine */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes.]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils.[[File:Desert Grassland Landscape.jpg|thumb|320px|A desert biome (Left) and a grassland biome (Right).]]&lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes: [[File:Amazon soil.jpg|right|thumb|Soil profile of an eroded hill in a tropical forest biome. A majority of the soil is nutrient poor (Light color soil) with a small amount of fertile soil (dark color soil).]]&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7][[File:Permafrost layers.png|right|thumb|320px|Diagram of a tundra biome soil layer showing permafrost.]] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]&lt;br /&gt;
&lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
[[File:Freshwater.jpg|thumb|A lake at Acadia National Park, ME. Lakes are classified as freshwater biomes.]]&lt;br /&gt;
&lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
[[File:Deforestation.jpg|thumb|A forest biome that has been cut down to make room for agriculture.]]&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6548</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6548"/>
		<updated>2021-05-04T21:59:53Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes.]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils.[[File:Desert Grassland Landscape.jpg|thumb|320px|A desert biome (Left) and a grassland biome (Right).]]&lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes: [[File:Amazon soil.jpg|right|thumb|Soil profile of an eroded hill in a tropical forest biome. A majority of the soil is nutrient poor (Light color soil) with a small amount of fertile soil (dark color soil).]]&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7][[File:Permafrost layers.png|right|thumb|320px|Diagram of a tundra biome soil layer showing permafrost.]] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]&lt;br /&gt;
&lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
[File:Freshwater.jpg|thumb|A lake at Acadia National Park, ME. Lakes are classified as freshwater biomes.]]&lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
[[File:Deforestation.jpg|thumb|A forest biome that has been cut down to make room for agriculture.]]&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6547</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6547"/>
		<updated>2021-05-04T21:59:00Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes.]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils.[[File:Desert Grassland Landscape.jpg|thumb|320px|A desert biome (Left) and a grassland biome (Right).]]&lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes: [[File:Amazon soil.jpg|right|thumb|Soil profile of an eroded hill in a tropical forest biome. A majority of the soil is nutrient poor (Light color soil) with a small amount of fertile soil (dark color soil).]]&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7][[File:Permafrost layers.png|right|thumb|320px|Diagram of a tundra biome soil layer showing permafrost.]] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]&lt;br /&gt;
&lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
[File:Freshwater.jpg|right|thumb|320px|A lake at Acadia National Park, ME. Lakes are classified as freshwater biomes.]]&lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
[[File:Deforestation.jpg|thumb|A forest biome that has been cut down to make room for agriculture.]]&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=File:Freshwater.jpg&amp;diff=6546</id>
		<title>File:Freshwater.jpg</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=File:Freshwater.jpg&amp;diff=6546"/>
		<updated>2021-05-04T21:57:46Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: A lake at Acadia National Park, ME. Lakes are classified as freshwater biomes.
Image: University of California, Berkley
From:https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;A lake at Acadia National Park, ME. Lakes are classified as freshwater biomes.&lt;br /&gt;
Image: University of California, Berkley&lt;br /&gt;
From:https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6542</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6542"/>
		<updated>2021-05-04T21:41:19Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes.]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils.[[File:Desert Grassland Landscape.jpg|thumb|320px|A desert biome (Left) and a grassland biome (Right).]]&lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes: [[File:Amazon soil.jpg|right|thumb|Soil profile of an eroded hill in a tropical forest biome. A majority of the soil is nutrient poor (Light color soil) with a small amount of fertile soil (dark color soil).]]&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7][[File:Permafrost layers.png|right|thumb|320px|Diagram of a tundra biome soil layer showing permafrost.]] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]&lt;br /&gt;
&lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
[[File:Deforestation.jpg|thumb|A forest biome that has been cut down to make room for agriculture.]]&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=File:Deforestation.jpg&amp;diff=6540</id>
		<title>File:Deforestation.jpg</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=File:Deforestation.jpg&amp;diff=6540"/>
		<updated>2021-05-04T21:39:45Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: A forest biome that has been cut down to make room for agriculture 
Image: Rich Carey/ShutterStock.com
From: https://www.activewild.com/forest-biome/&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;A forest biome that has been cut down to make room for agriculture &lt;br /&gt;
Image: Rich Carey/ShutterStock.com&lt;br /&gt;
From: https://www.activewild.com/forest-biome/&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6533</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6533"/>
		<updated>2021-05-04T21:30:59Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes.]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils.[[File:Desert Grassland Landscape.jpg|thumb|320px|A desert biome (Left) and a grassland biome (Right).]]&lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes: [[File:Amazon soil.jpg|right|thumb|Soil profile of an eroded hill in a tropical forest biome. A majority of the soil is nutrient poor (Light color soil) with a small amount of fertile soil (dark color soil).]]&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7][[File:Permafrost layers.png|right|thumb|320px|Diagram of a tundra biome soil layer showing permafrost.]] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]&lt;br /&gt;
&lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6529</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6529"/>
		<updated>2021-05-04T21:29:47Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes.]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils.[[File:Desert Grassland Landscape.jpg|thumb|A desert biome (Left) and a grassland biome (Right) .]]&lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes: [[File:Amazon soil.jpg|right|thumb|Soil profile of an eroded hill in a tropical forest biome. A majority of the soil is nutrient poor (Light color soil) with a small amount of fertile soil (dark color soil).]]&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
[[File:Permafrost layers.png|right|thumb|320px|Diagram of a tundra biome soil layer showing permafrost.]]&lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7][[File:Permafrost layers.png|right|thumb|320px|Diagram of a tundra biome soil layer showing permafrost.]] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]&lt;br /&gt;
&lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=File:Amazon_soil.jpg&amp;diff=6523</id>
		<title>File:Amazon soil.jpg</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=File:Amazon_soil.jpg&amp;diff=6523"/>
		<updated>2021-05-04T21:27:16Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: Soil profile of an eroded hill in a tropical forest biome. A majority of the soil is nutrient poor (Light color soil) with a small amount of fertile soil (darker color soil)
Photograph ©2007 Guenter Fischer and World of Stock.
From: https://earthobser...&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;Soil profile of an eroded hill in a tropical forest biome. A majority of the soil is nutrient poor (Light color soil) with a small amount of fertile soil (darker color soil)&lt;br /&gt;
Photograph ©2007 Guenter Fischer and World of Stock.&lt;br /&gt;
From: https://earthobservatory.nasa.gov/features/Deforestation&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6517</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6517"/>
		<updated>2021-05-04T21:15:16Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes.]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils.[[File:Desert Grassland Landscape.jpg|thumb|A desert biome (Left) and a grassland biome (Right) .]]&lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
[[File:Permafrost layers.png|right|thumb|320px|Diagram of a tundra biome soil layer showing permafrost.]]&lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]&lt;br /&gt;
&lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6515</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6515"/>
		<updated>2021-05-04T21:14:36Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes.]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
[[File:Desert Grassland Landscape.jpg|thumb|A desert biome (Left) and a grassland biome (Right) .]]&lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
[[File:Permafrost layers.png|right|thumb|320px|Diagram of a tundra biome soil layer showing permafrost.]]&lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]&lt;br /&gt;
&lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=File:Desert_Grassland_Landscape.jpg&amp;diff=6512</id>
		<title>File:Desert Grassland Landscape.jpg</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=File:Desert_Grassland_Landscape.jpg&amp;diff=6512"/>
		<updated>2021-05-04T21:10:33Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: A desert biome (Left) and a grassland biome (Right)
Images by Bob Protus and Bkell.
From:https://askabiologist.asu.edu/explore/biomes&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;A desert biome (Left) and a grassland biome (Right)&lt;br /&gt;
Images by Bob Protus and Bkell.&lt;br /&gt;
From:https://askabiologist.asu.edu/explore/biomes&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6504</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6504"/>
		<updated>2021-05-04T20:59:12Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: /* Tundra */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
[[File:Permafrost layers.png|right|thumb|320px|Diagram of a tundra biome soil layer showing permafrost.]]&lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]&lt;br /&gt;
&lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6503</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6503"/>
		<updated>2021-05-04T20:58:41Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
[[File:Permafrost layers.png|right|thumb|320px|Diagram of a tundra biome soil layer showing permafrost.]]&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]&lt;br /&gt;
&lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
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==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6501</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6501"/>
		<updated>2021-05-04T20:57:15Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
[[File:Permafrost layers.png|right|320px|Diagram of a tundra biome soil layer showing permafrost.]]&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]&lt;br /&gt;
&lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6497</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6497"/>
		<updated>2021-05-04T20:53:35Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: /* Tundra */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
[[File:Permafrost layers.png|320px|Diagram of a tundra biome soil layer showing permafrost.]]&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]&lt;br /&gt;
&lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6496</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6496"/>
		<updated>2021-05-04T20:53:07Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
[[File:Permafrost layers.png|100px|Diagram of a tundra biome soil layer showing permafrost.]]&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6494</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6494"/>
		<updated>2021-05-04T20:51:57Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
[[File:Permafrost layers.png|320×240|Diagram of a tundra biome soil layer showing permafrost.]]&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6486</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6486"/>
		<updated>2021-05-04T20:50:44Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
[[File:Permafrost layers.png|upright=320×240|Diagram of a tundra biome soil layer showing permafrost.]]&lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6483</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6483"/>
		<updated>2021-05-04T20:49:30Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
[[File:Permafrost layers.png|upright=0.5|Diagram of a tundra biome soil layer showing permafrost.]]&lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6481</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6481"/>
		<updated>2021-05-04T20:48:45Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra  &lt;br /&gt;
[[File:Permafrost layers.png|Diagram of a tundra biome soil layer showing permafrost.]]&lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=File:Permafrost_layers.png&amp;diff=6478</id>
		<title>File:Permafrost layers.png</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=File:Permafrost_layers.png&amp;diff=6478"/>
		<updated>2021-05-04T20:43:58Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: Diagram of tundra soils and permafrost 
Credit: Benjamin Jones, USGS.
From: https://climatekids.nasa.gov/permafrost/#:~:text=and%20South%20Poles.-,Permafrost%20is%20any%20ground%20that%20remains%20completely%20frozen%E2%80%9432%C2%B0,large%20regions%20...&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;Diagram of tundra soils and permafrost &lt;br /&gt;
Credit: Benjamin Jones, USGS.&lt;br /&gt;
From: https://climatekids.nasa.gov/permafrost/#:~:text=and%20South%20Poles.-,Permafrost%20is%20any%20ground%20that%20remains%20completely%20frozen%E2%80%9432%C2%B0,large%20regions%20of%20the%20Earth.&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6377</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6377"/>
		<updated>2021-05-04T04:57:03Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.75|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra         &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
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==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6376</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6376"/>
		<updated>2021-05-04T04:56:43Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|upright=1.5|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra         &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6375</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6375"/>
		<updated>2021-05-04T04:55:51Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|upright=2.7|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra         &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6374</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6374"/>
		<updated>2021-05-04T04:53:53Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
[[File:Map of biomes.png|thumb|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra         &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6373</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6373"/>
		<updated>2021-05-04T04:53:30Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&#039;&#039;&#039;Definition&#039;&#039;&#039;&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra         &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6372</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6372"/>
		<updated>2021-05-04T04:52:34Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;[[File:Map of biomes.png|thumb|Map of biomes around the world.]]&lt;br /&gt;
==&#039;&#039;&#039;Definition&#039;&#039;&#039; == &lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra         &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=File:Map_of_biomes.png&amp;diff=6371</id>
		<title>File:Map of biomes.png</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=File:Map_of_biomes.png&amp;diff=6371"/>
		<updated>2021-05-04T04:50:51Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: Map of biomes 
From: Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America.
Author: Meghan Sindelar
Photos: USDA-NRCS, ARS, istock 
https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;Map of biomes &lt;br /&gt;
From: Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America.&lt;br /&gt;
Author: Meghan Sindelar&lt;br /&gt;
Photos: USDA-NRCS, ARS, istock &lt;br /&gt;
https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6370</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6370"/>
		<updated>2021-05-04T04:45:06Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: /* Determining Factors */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==&#039;&#039;&#039;Definition&#039;&#039;&#039; == &lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra         &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6369</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6369"/>
		<updated>2021-05-04T04:44:16Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==&#039;&#039;&#039;Definition&#039;&#039;&#039; == &lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
[[File:Climate influence on terrestrial biome.PNG|thumb|Graph showing different temperature and precipitation conditions of various biomes..]]&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.  &lt;br /&gt;
    &lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra         &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=File:Climate_influence_on_terrestrial_biome.PNG&amp;diff=6368</id>
		<title>File:Climate influence on terrestrial biome.PNG</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=File:Climate_influence_on_terrestrial_biome.PNG&amp;diff=6368"/>
		<updated>2021-05-04T04:43:48Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: Graph showing different temperature and precipitation conditions of various biomes.
By Navarras - Own work, CC0, https://commons.wikimedia.org/w/index.php?curid=61120531&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;Graph showing different temperature and precipitation conditions of various biomes.&lt;br /&gt;
By Navarras - Own work, CC0, https://commons.wikimedia.org/w/index.php?curid=61120531&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6363</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6363"/>
		<updated>2021-05-04T04:31:49Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==&#039;&#039;&#039;Definition&#039;&#039;&#039; == &lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.  &lt;br /&gt;
    &lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra         &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6362</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6362"/>
		<updated>2021-05-04T04:29:30Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==&#039;&#039;&#039;Definition&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.  &lt;br /&gt;
    &lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra         &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
===Deserts===&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
&lt;br /&gt;
===Grasslands===&lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
===Forests===&lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
===Tundra===&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
===Aquatic===&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
-------------------------------------------------------------------------------------------------------------------------------------    &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6361</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6361"/>
		<updated>2021-05-04T04:26:50Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==&#039;&#039;&#039;Definition&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.  &lt;br /&gt;
    &lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
*Hot and dry deserts &lt;br /&gt;
*Semiarid deserts &lt;br /&gt;
*Coastal deserts &lt;br /&gt;
*Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
*Tropical grasslands (Savannahs)&lt;br /&gt;
*Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
*Tropical forests&lt;br /&gt;
*Temperate forests &lt;br /&gt;
*Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
*Artic tundra &lt;br /&gt;
*Alpine tundra         &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
*Oceans &lt;br /&gt;
*Coral reefs &lt;br /&gt;
*Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
*Lakes and ponds&lt;br /&gt;
*Rivers and streams &lt;br /&gt;
*Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
     &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6360</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6360"/>
		<updated>2021-05-04T04:23:10Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==&#039;&#039;&#039;Definition&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Determining Factors&#039;&#039;&#039; ==&lt;br /&gt;
&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.  &lt;br /&gt;
    &lt;br /&gt;
==&#039;&#039;&#039;Biomes of the World&#039;&#039;&#039; == &lt;br /&gt;
&lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .  &lt;br /&gt;
 &lt;br /&gt;
===&#039;&#039;&#039;Terrestrial Biomes&#039;&#039;&#039;===&lt;br /&gt;
====Desert==== &lt;br /&gt;
desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
-	Hot and dry deserts &lt;br /&gt;
-	Semiarid deserts &lt;br /&gt;
-	Coastal deserts &lt;br /&gt;
-	Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
&lt;br /&gt;
====Grasslands====&lt;br /&gt;
Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
-	Tropical grasslands (Savannahs)&lt;br /&gt;
-	Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
&lt;br /&gt;
====Forests==== &lt;br /&gt;
Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
-	Tropical forests&lt;br /&gt;
-	Temperate forests &lt;br /&gt;
-	Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14] &lt;br /&gt;
 &lt;br /&gt;
====Tundra==== &lt;br /&gt;
The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
-	Artic tundra &lt;br /&gt;
-	Alpine tundra         &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]  &lt;br /&gt;
  &lt;br /&gt;
===Aquatic biomes=== &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
&lt;br /&gt;
====Marine====&lt;br /&gt;
Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
-	Oceans &lt;br /&gt;
-	Coral reefs &lt;br /&gt;
-	Estuaries   &lt;br /&gt;
====Freshwater==== &lt;br /&gt;
Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
-	Lakes and ponds&lt;br /&gt;
-	Rivers and streams &lt;br /&gt;
-	Wetlands   &lt;br /&gt;
&lt;br /&gt;
==Human Influence &amp;amp; Global Change==   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
&lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]&lt;br /&gt;
   &lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
&lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]  &lt;br /&gt;
     &lt;br /&gt;
==References==&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6359</id>
		<title>Biomes</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Biomes&amp;diff=6359"/>
		<updated>2021-05-04T04:13:52Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;Definition &lt;br /&gt;
Biomes (bai-owmz), also known as major life zones, are divisions of Earth’s terrestrial and aquatic environments. A biome is a large community of plants and [[animals]] living in specific abiotic conditions, like climate and [[soil]] conditions.[1] Biomes are made up of various communities of flora and fauna but are classified based on the dominant vegetation of the area.[2][3] The five main types of biomes are deserts, grasslands, forests, tundra, and aquatic, but these biome types can be further broken down to represent more specific characteristics and conditions.[1] All the biomes on Earth make up the biosphere.[5]&lt;br /&gt;
&lt;br /&gt;
Determining Factors&lt;br /&gt;
While biomes are typically classified based on the predominant vegetation of the area, vegetation is not the only factor that determines a biome. There are a number of different abiotic factors that can have an influence on the biome type, but the main determining factor is the climate, specifically the temperature and precipitation of an area.[4] Temperature and precipitation play an important role in dictating the animals and plants that are in a specific area.[4] Variations in the precipitation and temperature conditions can lead to substantial differences in the vegetation  which results in all the unique biomes we see today. &lt;br /&gt;
&lt;br /&gt;
While climate has a major influence on the biomes, it is not the only abiotic factor that plays a role in determining the type of biome. Another important factor that determines biome type is the latitudinal  location of the biome.[6] Latitudinal location and climate are interconnected drivers because the amount of sunlight varies with latitude which effects the temperature, precipitation, and by extension the type of life that can inhabit that location.[6] For example biomes found in lower latitudes are typically characterized by higher temperatures and higher precipitation.[6] &lt;br /&gt;
&lt;br /&gt;
Biomes are complex systems that have many other factors that have an influence on them. Some of these other factors include, but not limited to, soil moisture, nutrients, water availability, disturbances, and length of growing season.[5][6] All of these abiotic conditions dictate what [[organisms]] will persist in those conditions, which defines the specific biome.  &lt;br /&gt;
    &lt;br /&gt;
Biomes of the World &lt;br /&gt;
The term “biome” has had many different definitions and classifications since its first use in 1916 by Fredrick Clements.[5][7] Over the years the term has changed, being both expanded and refined, leading to different classifications and specific biome types.[7] Below are the 6 major types of biomes which can be further divided into more specific biomes that represent more specific conditions, including temperature, precipitation, seasonality, and soil condition .   &lt;br /&gt;
Terrestrial Biomes&lt;br /&gt;
Desert: desert biomes are characterized by low precipitation and extreme temperatures, both hot and cold temperatures, and cover about 20% of earth’s surface.[1] The rainfall in desert biomes are typically lower than 50 cm per year.[1][8] Both plants and animals in this biome are adapted to the low precipitation and extreme temperatures. The predominant vegetation in desert biomes are typically low, ground-hugging shrubs and grasses which are able to thrive in the low water environment.[8] There are four types of desert biomes which share these general characteristics but also have certain aspects that distinguish them.[8] the four types of desert are:&lt;br /&gt;
-	Hot and dry deserts &lt;br /&gt;
-	Semiarid deserts &lt;br /&gt;
-	Coastal deserts &lt;br /&gt;
-	Cold deserts  &lt;br /&gt;
Soils in desert biomes can be sandy, stony, or consist of gravel depending on the specific type of desert.[12] The lack of available water plays an important part in the soils of desert biomes. Desert soils are not abundant in nutrients because the dry environment limits the amount of weathering which breaks down soil particles into essential nutrients and minerals.[13] Deserts also do not have a large amount of organic matter in the soils because of the lack of productivity from the limited plant community.[8] These factors result in the poor and unproductive conditions of desert soils. &lt;br /&gt;
Grassland: Grassland biomes are widespread and found on almost every continent, excluding Antarctica.[7] This biome is described as open and flat land that is dominated by grasses with little to no trees.[7] The climate of grassland biomes are typically characterized by warmer temperatures and increased precipitation, compared to desert biomes.[9] another defining characteristic of grasslands is seasonal droughts and disturbances, such as fires, which promote the growth and success of grasses and benefits biodiversity.[9] Grasslands can be divided into two categories:&lt;br /&gt;
-	Tropical grasslands (Savannahs)&lt;br /&gt;
-	Temperate grasslands (includes parries and steppes)  &lt;br /&gt;
The two distinct groups of grassland biomes, tropical grasslands and temperate grasslands, have widely different soil conditions. The soils of tropical grasslands are porous and experiences a lot of leaching due to the increased precipitation rates.[9] The porous soil contributes to the lack of nutrients and organic matter found in the soil because the precipitation moves through the soil with ease and takes the nutrients along with it, resulting in low nutrients and a small organic layer in the soil.[9] Temperate grassland soils differ from tropical grasslands and are described as deep, dark-colored, nutrient rich soils with the upper soil layers being extremely fertile.[9] Temperate grasslands receive less precipitation than tropical ones which reduces the amount of nutrients that are leached through the soil. [[Decomposition]] also plays an important role in the differences between grassland soils. Tropical forests experience partial decomposition while temperate ones have higher decomposition which contributes to the higher nutrient content of temperate grassland soils.[9]  &lt;br /&gt;
Forests: Forest biomes constitutes about 1/3 of the earth’s surface and hosts majority of the biodiversity found in terrestrial biomes.[1][10] All forest biomes share the same dominant vegetation which is made up of trees and other woody plants, although forests have a wide range of climate conditions in which they can be found in. Forests can be found in the warm, moist tropics, moderate climate conditions of temperate environments, and even in cold and snowy northern latitudes.[10] The difference in environmental conditions of the various forests allows for forests to be categorized in a number of different ways, such as latitude, temperature and precipitation, and seasonality.[10] Below are the three major types of forests, categorized by latitude, but each of these forest types can be diverged into more specific classes:&lt;br /&gt;
-	Tropical forests&lt;br /&gt;
-	Temperate forests &lt;br /&gt;
-	Boreal forests (Taiga) &lt;br /&gt;
Forest biomes have a wide distribution and inhabit a range of unique environmental conditions, including soil conditions. Tropical forests have soils that are nutrient-poor and acidic, both which are results of intense precipitation.[10] The rain leaches through the soil and deprives the soil of nutrients and the loss of nutrients leads to the acidic nature of the soils. Tropical forests also have a fast decomposition rates which prevents organic matter and nutrients from building up in the soil, leaving it nutrient poor.[10] Conversely, temperate forests have nutrient rich soils which comes from the decomposition of organic material and plant litter.[10] The seasonality of temperate forests contributes to the rich soils because many of the trees loose their leaves for the winter, which provides decomposers with a food source that is broken down into soil nutrients. The soil of boreal forests have its own unique characteristics that separates it from tropical and temperate forests. Boreal forest soils are lacking in nutrients, acidic, and relatively thin.[10] The cold temperatures causes lower decomposition rates which limits the amount of nutrients in the soil. The leaves from the predominant vegetation of boreal forests, needle-leaf conifers, fall and the acidic compounds leaches into the soil and changes the pH to be more acidic. [14]  &lt;br /&gt;
Tundra: The tundra biome is coldest and least diverse of all the major biomes.[11] The tundra biome is characterized by extremely low annual temperatures, lower than any other biome, and low precipitation, producing a cold, dry, and inhospitable environment.[1] These intense conditions limit the kinds of life that can occupy the tundra because only species that are adapted to the extreme cold, dry conditions, and short growing seasons.[7] Although the tundra is known for its lack of biodiversity there are still organisms that call this biome home. There is not many different types of vegetation in this biome, due to the harsh growing conditions, but the vegetation that does reside here are rather simple, including mosses, lichens, grasses, and some shrubs.[1] There are two types of tundra biomes that are found on Earth:&lt;br /&gt;
-	Artic tundra &lt;br /&gt;
-	Alpine tundra         &lt;br /&gt;
Tundra biomes do not have great soil conditions which also contributes to the low biodiversity. Tundra soils are defined by the lack of soil nutrients and the frozen layer of soil known as permafrost.[11] the lack of soil nutrients, notably nitrogen and phosphorus, leads to poor soil conditions which limits the vegetation that can grow there.[11] the frozen layer of permafrost also contributes to the poor soil conditions by locking up vital nutrients and organic matter which prevents vegetation from reaching these essential components.[11]    &lt;br /&gt;
Aquatic biomes &lt;br /&gt;
While terrestrial biomes are typically categorized by their dominant plant life, aquatic biomes are not defined by the dominant vegetation, which is much harder to find in aquatic ecosystems, and thus leads to aquatic biomes being classified by other components, such as salinity, depth, temperature, sunlight, and more.[7] &lt;br /&gt;
Marine: Marine biomes are very diverse and unique systems that make up about three fourths of Earth’s total surface.[15] One of the defining factors of marine biomes is the salt content. Marine biomes have a higher salt content than freshwater biomes.[7] The marine biome is extremely important because not only does it act as a sink for atmospheric carbon, but marine algae are responsible for producing a large amount of the world oxygen supply.[15] Marine biomes can be further broken down into:&lt;br /&gt;
-	Oceans &lt;br /&gt;
-	Coral reefs &lt;br /&gt;
-	Estuaries   &lt;br /&gt;
Freshwater: Freshwater biomes are aquatic systems that are surrounded by land and contain on average less than 1% salt content.[16] Freshwater biomes can be either standing water or running water. The close proximity of freshwater biomes to terrestrial biomes means that these systems are connected by similar biotic and abiotic factors and can influence one another.[4] Types of freshwater biomes include:&lt;br /&gt;
-	Lakes and ponds&lt;br /&gt;
-	Rivers and streams &lt;br /&gt;
-	Wetlands   &lt;br /&gt;
Human Influence &amp;amp; Global Change   &lt;br /&gt;
Human activities can have a major influence on the distribution and environmental conditions of both terrestrial and aquatic biomes. Biomes have been disturbed, reduced, and altered over the course of human history. Humans have altered natural biomes so significantly that the term “anthromes” has been used to describe human created biomes, such as agricultural farmlands and urban environments.[17]  In addition to directly disturbing biomes, human-driven climate change is going to alter temperature, precipitation, and other climatic conditions around the world impacting vegetation and entire biomes. Biomes are expected to shift in response to changing climatic conditions, such as temperature and precipitation.[19] &lt;br /&gt;
Desert biomes are expected to expand in response to climate change and human activities. [[Desertification]] describes the encroachment of desert environments into other biomes and is driven by a number of different factors, including deforestation, overgrazing, harmful agricultural practices, and changing climates.[20] variations in precipitation and temperatures can lead to a reduction in plant life, drying and erosion of soils, and droughts which drives the expansion of deserts.[20] &lt;br /&gt;
Grassland biomes have been significantly affected by humans in a number of ways. Human expansion and the development of urban and agricultural areas has changed the landscape and altered the biotic communities resulting in reductions to the extent of grassland biomes.[18] Climate change is going to dramatically shift grassland biomes toward the poles as grasses follow hospitable climate conditions.[19]   &lt;br /&gt;
Forest biomes have experience extreme pressure from humans in the form of deforestation, which decimates large portions of forest for a number of reasons including resources and agricultural expansion.[ 21] Climate change will have significant effects on forest biomes. Trees that make up the various forest biomes will shift towards more favorable climates, shifting biomes toward the poles, and extreme weather events like droughts and flooding will impact forests.[22] Invasive species and pests are other issues that can weaken forests and reduce the extent of forest biomes.[22]  &lt;br /&gt;
Tundra biomes are extremely sensitive to both climate change and human activities. One of the greatest threats to tundra biomes is the increase in temperatures and melting of permafrost due to anthropogenic climate change.[23] thawing of permafrost releases methane and other greenhouse gases that creates a positive feedback loop, perpetuating the rise in temperatures.[23] The plant and animals that inhabit tundra biomes are specifically adapted to colder weather and thus an increase in temperatures can destabilize the tundra communities and force the organisms to adapt or die out. Tundra biomes take a long to repair themselves from disturbances which also highlights the sensitivity of this biome to perturbations and environmental changes.[23]&lt;br /&gt;
Aquatic biomes have their own set of disturbances that threaten the stability and functioning of the biomes. Both freshwater and marine biomes are at risk of severe impacts from humans and climate change alike, although the exact impacts will vary due to the unique conditions of each aquatic biome. The threats towards marine biomes include ocean acidification and rising sea temperatures which can impact the marine life due to changing environmental conditions.[24] This impact is especially seen in coral reef environments in which corals are bleaching and dying at an alarming rate because they cannot cope with the changing conditions. Freshwater biomes are also expected to be influenced by climate change. Increased temperatures and precipitation can lead to both droughts and floods which directly impact the entire biome.[25] The effect humans have on these aquatic biomes include pollution, overuse, and harmful invasive species.[24][25] Pollution and overfishing are two major impacts from humans that can significantly affect the dynamics of these biomes.[24][25]       &lt;br /&gt;
References:&lt;br /&gt;
[1] National Geographic Society. (2020) Biome. https://www.nationalgeographic.org/encyclopedia/biome/&lt;br /&gt;
[2] UC Museum of Paleontology (2019) The world’s biomes. University of California, Berkley. https://ucmp.berkeley.edu/exhibits/biomes/index.php&lt;br /&gt;
[3] Augustyn, Adam. &amp;quot;Biome&amp;quot;. Encyclopedia Britannica, 18 Feb. 2020, https://www.britannica.com/science/biome. Accessed 1 May 2021.&lt;br /&gt;
[4] Carter, S. Introductions to Biomes. Lumen Learning. https://courses.lumenlearning.com/suny-wmopen-biology2/chapter/biomes/&lt;br /&gt;
[5] Mucina, L. 2019. Biome: evolution of a crucial ecological and biogeographical concept. New Phytologist 222:97–114.&lt;br /&gt;
[6] Hain, T. (2019). The link between biomes and climate. The Thought Co. https://www.thoughtco.com/what-are-biomes-1435312&lt;br /&gt;
[7] National Geographic Society. (2019). What makes a biome?  https://www.nationalgeographic.org/article/what-makes-biome/?utm_source=BibblioRCM_Row&lt;br /&gt;
[8] UC Museum of Paleontology (2019). The desert biome. https://ucmp.berkeley.edu/exhibits/biomes/deserts.php&lt;br /&gt;
[9] UC Museum of Paleontology (2019). The grassland biome. https://ucmp.berkeley.edu/exhibits/biomes/grasslands.php&lt;br /&gt;
[10] UC Museum of Paleontology (2019). The forest biome. https://ucmp.berkeley.edu/exhibits/biomes/forests.php&lt;br /&gt;
[11] UC Museum of Paleontology (2019) The tundra biome. https://ucmp.berkeley.edu/exhibits/biomes/tundra.php&lt;br /&gt;
[12] National Geographic Society. (2020). Desert biome. https://www.nationalgeographic.org/encyclopedia/desert-biome/#:~:text=This%20biome%20has%20a%20layer,have%20adaptations%20to%20conserve%20water.&lt;br /&gt;
[13] Sindelar, M. (2015). soils protect the natual enviroment. Soil Science Society of America. https://www.soils.org/files/sssa/iys/september-soils-overview.pdf&lt;br /&gt;
[14] Regional Aquatics Monitoring Program. The physical environment. http://www.ramp-alberta.org/river/boreal/canada/physical+environment.aspx#:~:text=Soils%20in%20the%20boreal%20forest,acidic%2C%20and%20poor%20in%20nutrients.&lt;br /&gt;
[15] UC Museum of Paleontology (2019). The marine biome. https://ucmp.berkeley.edu/exhibits/biomes/marine.php&lt;br /&gt;
[16] UC Museum of Paleontology (2019). The freshwater biome. https://ucmp.berkeley.edu/exhibits/biomes/freshwater.php&lt;br /&gt;
[17] Ellis, E.C. &amp;amp; Ramankutty, N. (2008) Putting people in the map: anthropogenic biomes of the world. Frontiers in [[Ecology]] and the Environment, 6, 439–447&lt;br /&gt;
[18] Carr, K. (2018). What Are the Impacts of Humans on Grassland Biomes? Sciencing. https://sciencing.com/effects-of-land-clearing-13406919.html&lt;br /&gt;
[19] Buis, A. (2011). Climate change may bring big ecosystem changes. NASA. https://climate.nasa.gov/news/645/climate-change-may-bring-big-ecosystem-changes/&lt;br /&gt;
[20] McSweeny, R. (2019). Explainer: ‘Desertification’ and the role of climate change. https://www.carbonbrief.org/explainer-desertification-and-the-role-of-climate-change&lt;br /&gt;
[21] Understanding the different types of biomes. Kent State University. https://onlinedegrees.kent.edu/geography/geographic-information-science/community/biomes-types-and-human-impact#:~:text=The%20forest%20biome%20most%20at,already%20contributed%20to%20global%20warming.&lt;br /&gt;
[22] Climate impacts on forests. (2017). United States Environmental Protection Agency. https://19january2017snapshot.epa.gov/climate-impacts/climate-impacts-forests_.html&lt;br /&gt;
[23] Nunez, C. (2020). Tundra threat explained. National Geographic Society.  https://www.nationalgeographic.org/article/tundra-threats-explained/#:~:text=Air%20pollution%20affects%20tundra%20environments%20in%20different%20ways.&amp;amp;text=And%20toxic%20mercury%2C%20sent%20into,important%20food%20source%20of%20lichen.&lt;br /&gt;
[24] National Geographic Society. Ocean threats. https://www.nationalgeographic.com/environment/article/ocean-threats#:~:text=Global%20warming%20is%20causing%20sea,kills%20marine%20plants%20and%20shellfish.&lt;br /&gt;
[25] National Geographic Society. Freshwater threats. https://www.nationalgeographic.com/environment/article/freshwater-threats&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Red_wiggler_worms&amp;diff=5904</id>
		<title>Red wiggler worms</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Red_wiggler_worms&amp;diff=5904"/>
		<updated>2021-04-29T03:29:10Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: Peer review editing&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;==Overview==&lt;br /&gt;
Red wiggler worms, scientifically known as &#039;&#039;&#039;&#039;&#039;Eisenia fetida&#039;&#039;&#039;&#039;&#039;, are classified as &#039;&#039;[[Annelids]]&#039;&#039;. They go by various other common names such as the manure worm, dung worm, tiger worm, etc. They are widely known for their use in [[compost]] and as fish bait&amp;lt;sup&amp;gt;[4]&amp;lt;/sup&amp;gt;. &amp;lt;!--This seems a little light, is there anything else you can tell us about what it is and what it does?--&amp;gt;&lt;br /&gt;
&lt;br /&gt;
----&lt;br /&gt;
==Classification==&lt;br /&gt;
[[File:Eisenia.png|200px|thumb|right|A red wiggler worm&amp;lt;sup&amp;gt;[2]&amp;lt;/sup&amp;gt;]]&lt;br /&gt;
&#039;&#039;&#039;Domain&#039;&#039;&#039;: Eukarya&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Kingdom&#039;&#039;&#039;: Animalia&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Phylum&#039;&#039;&#039;: Annelida&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Class&#039;&#039;&#039;: Oligochaeta&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Order&#039;&#039;&#039;: Hapliotaxida&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Family&#039;&#039;&#039;: Lumbricidae&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Genus&#039;&#039;&#039;: Eisenia&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Species&#039;&#039;&#039;: Eisenia Fetida&lt;br /&gt;
&lt;br /&gt;
----&lt;br /&gt;
==Habitat==&lt;br /&gt;
&lt;br /&gt;
Red wiggler worms are [[Epigeic Earthworms ]], meaning they live on the upper surface of the [[soil]] or in the soil litter&amp;lt;sup&amp;gt;[4]&amp;lt;/sup&amp;gt;. Red wiggler worms prefer moist, organic-rich environments&amp;lt;sup&amp;gt;[6]&amp;lt;/sup&amp;gt;. Manure or compost provides a great environment for them. The species originated from Europe, but because it is a commercial species and used as fish bait and in vermicomposting, it can be found all across the world&amp;lt;sup&amp;gt;[4]&amp;lt;/sup&amp;gt;. &amp;lt;!--are they found in any specific ecosystems/biomes?--&amp;gt;&lt;br /&gt;
&lt;br /&gt;
----&lt;br /&gt;
&lt;br /&gt;
==Life Cycle and Reproduction==&lt;br /&gt;
[[File:Life-cycle.jpg|200px|thumb|right|Eisenia fetida life cycle&amp;lt;sup&amp;gt;[1]&amp;lt;/sup&amp;gt;]]&lt;br /&gt;
Venter and Reinecke (1988) found that, in favorable conditions, red wiggler worms have a better reproductive ability than other composting worms, so using these worms in vermicomposting will produce a faster working compost. After four days of mating, a cocoon forms where hatchlings will emerge from after an average of 23 days. Usually 2-3 hatchlings are produced, however sometimes more. After around 40-60 days hatchlings mature and reproduce&amp;lt;sup&amp;gt;[5]&amp;lt;/sup&amp;gt;. Red wiggler worms, as well as all earthworms, are hermaphroditic, but no self-fertilization has been documented. Juvenile red wiggler worms do not yet have a clitellum that is used in reproduction&amp;lt;sup&amp;gt;[4]&amp;lt;/sup&amp;gt;.&amp;lt;!--I feel as though this didn&#039;t tell me much about their life cycle/reproduction.--&amp;gt;&lt;br /&gt;
[[File:red-wiggler.png|200px|thumb|left|The clitellum&amp;lt;sup&amp;gt;[3]&amp;lt;/sup&amp;gt;]]&lt;br /&gt;
&lt;br /&gt;
----&lt;br /&gt;
==Vermicomposting==&lt;br /&gt;
Composting is a great way to make use out of food and other organic waste. Worms can be used as a compost method called vermicomposting. Vermicomposting bins can be bought, but when homemade, it is important that they are dark in color (earthworms are sensitive to light), have holes for aeration, and a drainage system. Bedding, such as shredded paper or other soft absorbent material, is needed for worms to thrive. The environment needs to be kept moist, but an abundance of water should never be added, or the worms will drown. The compost does not need to be turned like other compost methods, and should be avoided or worms may perish. Eisenia Fetida can consume 25-35% of their body weight per day, so this type of composting works quite fast. Compost bins should begin with about a thousand (1 lb.) red wiggler worms&amp;lt;sup&amp;gt;[6]&amp;lt;/sup&amp;gt;. Other worms can be used for vermicomposting, but red wiggler worms are the most efficient in composting&amp;lt;sup&amp;gt;[5]&amp;lt;/sup&amp;gt;. Bins must have a drainage system because the worms create castings which is the excrement from red wigglers and provides great nutrients to plants.&lt;br /&gt;
----&lt;br /&gt;
&amp;lt;!--Great page! some more specific details about the life of these worms would really strengthen this page --&amp;gt;&lt;br /&gt;
==References==&lt;br /&gt;
[1]Edwards, C. A., and N. Q. Arancon. (n.d.). THE SCIENCE OF VERMICULTURE: THE USE OF EARTHWORMS IN ORGANIC WASTE MANAGEMENT:25.&lt;br /&gt;
&lt;br /&gt;
[2]Eisenia andrei specimen during the experiment. Credit: photo courtesy... | Download Scientific Diagram. (n.d.). . https://www.researchgate.net/figure/Eisenia-andrei-specimen-during-the-experiment-Credit-photo-courtesy-of-Elaine-van-Ommen_fig1_265518697.&lt;br /&gt;
&lt;br /&gt;
[3]Red Wiggler Reproduction. 2013, August 31. . https://www.solanacenter.org/news/blog/red-wiggler-reproduction.&lt;br /&gt;
&lt;br /&gt;
[4]UWL Website. (n.d.). . http://bioweb.uwlax.edu/bio203/2010/yard_jose/habitat.htm.&lt;br /&gt;
&lt;br /&gt;
[5]Venter, J. M., and A. J. Reinecke. 1988. The life-cycle of the compost worm Eisenia fetida (Oligochaeta). South African Journal of Zoology 23:161–165.&lt;br /&gt;
&lt;br /&gt;
[6]Wormy FACTS and Interesting Tidbits (By Rhonda Sherman). (n.d.). . https://composting.ces.ncsu.edu/vermicomposting-2/wormy-facts-and-interesting-tidbits/.&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Hymenoptera&amp;diff=5903</id>
		<title>Hymenoptera</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Hymenoptera&amp;diff=5903"/>
		<updated>2021-04-29T03:09:36Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: Peer review editing&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;&lt;br /&gt;
== Definition  ==&lt;br /&gt;
&lt;br /&gt;
The Hymenoptera is a large order of [[organisms]] within the phylum [[Arthropoda]], which contains [[insects]] like, bees, wasps, sawflies, and ants. The name is derived from the greek words &amp;quot;Hymen&amp;quot; or &amp;quot;membrane&amp;quot; and &amp;quot;Ptera&amp;quot; or &amp;quot;wings&amp;quot;, which is perfectly describing the fact that their wings are connected into one point called the &amp;quot;Hamuli&amp;quot;, and the membraneous tissue it is formed. Like most insects, these appeared at an early stage of earth&#039;s history, which according to a study done by D.A. Grimaldi, M.S. Engel et al [11], have been around since 281 million years ago (Triassic Period).&lt;br /&gt;
The Hymenopteran who have evolved into a societal way of living(Cretaceous Period), similar to pre-historical humans, created a very well adapted form of resilience for the succession of its offspring. However, many different species still live solitarily, requiring others only for mating. The organisms, who have a social life, live in a nest (ants) or a hive (bees, wasps), which are all descendants of one queen. When the hive or nest is established by a queen in early spring, it begins producing its offspring that will work in their pre-assigned roles, depending on their gender. &amp;lt;!--Great section. maybe give a few examples of solitary living species--&amp;gt;&lt;br /&gt;
&lt;br /&gt;
== Classification ==&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Domain&#039;&#039;&#039;: Eukarya&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Kingdom&#039;&#039;&#039;: Animalia&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Phylum&#039;&#039;&#039;: Arthropoda&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Class&#039;&#039;&#039;: Insecta&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Superorder&#039;&#039;&#039;: Hymenopterida&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Order&#039;&#039;&#039;: Hymenoptera&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Suborder&#039;&#039;&#039;: Apocrita - Ants, Bees, Wasps&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Suborder&#039;&#039;&#039;: Symphyta - Sawflies, some wasps&lt;br /&gt;
&lt;br /&gt;
== Anatomy ==&lt;br /&gt;
[[File:Bee-anatomy-worker.jpeg|200px|thumb|right|Bee&#039;s anatomy]]&lt;br /&gt;
[[File:ANATOMY-OF-A-WASP-min.png|200px|right|thumb|Wasp&#039;s anatomy]]&lt;br /&gt;
&lt;br /&gt;
The anatomy of hymenopterans are very similar to other insects. The ones who fly, usually have two pairs of wings. Their mouths can have two forms, just mandibles used for chewing, or with the addition of the proboscis used for drinking liquids, such as nectar. They have two larger compound eyes, used to differentiate brightness and color, and also three smaller eyes called &amp;quot;ocelli&amp;quot; that are much simpler. Flying insects have their hind wings with hooked bristles called &amp;quot;hamuli&amp;quot; that holds both the fore wings and hind wings together. The number of hamuli vary between species and their sizes, with wasps having more than the usual two to three hamuli present in smaller species. Like most insects, their bodies are divided into three sections, head, thorax and abdomen. &lt;br /&gt;
&lt;br /&gt;
The hymenoptera have an ovipositor, that in older species evolved into a blade-like structure used for slicing plant tissues. However, many today use them for piercing. In some species, we see today an ovipositor that evolved into a stinger in which the tip is used to inject venom and their eggs are laid from the base of the structure. The stinger is usually used to immobilize prey, that could be used to insert their eggs inside, but we see many bees and wasps using for self defense.&lt;br /&gt;
&lt;br /&gt;
The larvae of the hymenoptera have a head region, three thoracic segments, and nine or ten abdominal segments. The hymenoptera, is further divided into the Symphyta and Apocrita. The former includes sawflies, whose larvae feed on leaves, have large mandibles for chewing; six thoracic limbs, and six to eight abdominal prolegs. However, their prolegs do not have spines, and their antennae are reduced to just stubs. Furthermore, the larvae that lives on wood or stem borers have no abdominal prolegs and the thoracic legs are smaller than the non-borers.&lt;br /&gt;
&lt;br /&gt;
The Apocrita, whose species are wasps and bees, however, cannot live freely. The lack of legs, and their shape resembling a maggot, requires them to be taken care either by the solitary wasp who laid them, or by the workers and queen in a beehive. If the larvae was laid by a wasp, it will most likely be living inside of the immobilized insect it captured, where the offspring can feed off of the prey. The larvae laid in the insect have some morphological differences, the head is reduced into the prothorax, the compound eyes are poorly developed, with no ocelli; very small or absent antennae and toothlike mandibles. It also lacks the ability to defecate, since their digestive system is not completed, to avoid contamination in the environment they live. The larvae that has a stinger, generally has ten spiracles, for breathing, while the parasitic form usually has nine. &amp;lt;!--Sub-headings would help break up this paragraph heavy section--&amp;gt;&lt;br /&gt;
&lt;br /&gt;
== Reproduction ==&lt;br /&gt;
&#039;&#039;&#039;Haplodiploid sex-determination system&#039;&#039;&#039;&lt;br /&gt;
In the order Hymenoptera, reproduction uses the Haplodiploid sex-determination system, in which the number of chromosomes determines their gender. If the eggs are fertilized by both parent&#039;s gametes, the individual is diploid and develops into a female. [[File:1920px-Haplodiploid Sex Determination in Honey Bees.svg.png|200px|thumb|right|Haplodiploid system diagram]] However, if the egg is not fertilized by two sets of gametes, the zygote is haploid, and develops into a male. The important factor in this system is that the female is under total control of which gender her offspring will be, depending on what the nest or hive needs in the moment. &lt;br /&gt;
&lt;br /&gt;
Although this system seems very simple to understand, it actually is much more complex than only the number of chromosomes present. In many hymenopterans, the gender is determined in a single gene locus with many alleles. In these organisms, males are haploid and females are diploid heterozygous at the sex locus. However, a diploid organism could be homozygous which develops into a male. This is more likely to happen when we have parents who were siblings reproducing. Diploid males are known for being produced by inbreeding, in many ant, bee, and wasp species. These males organisms, usually are infertile but you can find some species with fertile diploid males.&lt;br /&gt;
&lt;br /&gt;
A problem that appears due to this reproduction system is that females on average have more genes in common with their sisters than with their daughters. Therefore, cooperation among kindred females may be unusually advantageous, which contributed to the multiple origins of eusociality within this order. In many colonies, we see the removal of eggs laid by other workers due to the increase in relatedness to direct siblings, a behavior called worker policing. &lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Thelytoky&#039;&#039;&#039; [[File:Central fusion and terminal fusion automixis.svg.png|200px|thumb|right|Thelitoky Diagram]]&lt;br /&gt;
&lt;br /&gt;
Some hymenopterans also use a type of parthenogenesis, which is the production of an embryo without fertilization, to produce other females. Through the process of thelytoky, a female is produced from the fusion of two haploid proto-eggs in the same meiosis, producing a diploid zygote. This method of reproduction tends to maintain heterozygosity of the genome of the mother to the daughter. Many ant species use this method, some of them are: desert ant &#039;&#039;Cataglyphis cursor&#039;&#039;, the clonal raider ant &#039;&#039;Cerapachys biroi&#039;&#039;, the predaceous ant &#039;&#039;Platythyrea punctata&#039;&#039;, and the electric ant (little fire ant) &#039;&#039;Wasmannia auropunctata&#039;&#039;. It also occurs in the Cape honey bee &#039;&#039;Apis mellifera capensis&#039;&#039;.&lt;br /&gt;
&lt;br /&gt;
== Major Families == &lt;br /&gt;
&amp;lt;!--Love this idea--&amp;gt;&lt;br /&gt;
According to the NCSU Department of Entomology [4]&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Sawflies&#039;&#039;&#039;: Larvae feed on leaves, or burrow into plant tissues&lt;br /&gt;
&lt;br /&gt;
1)&#039;&#039;Diprionidae&#039;&#039;: Conifer sawflies&lt;br /&gt;
&lt;br /&gt;
2)&#039;&#039;Tenthredinidae&#039;&#039;: Common sawflies&lt;br /&gt;
&lt;br /&gt;
3)&#039;&#039;Cephidae&#039;&#039;: Stem sawflies&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Horntails&#039;&#039;&#039;: Larvae are wood borers&lt;br /&gt;
&lt;br /&gt;
1)&#039;&#039;Siricidae&#039;&#039;: Wood or Horntail wasp&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Parasitic Wasps&#039;&#039;&#039;: Larvae are parasitoid of other insects&lt;br /&gt;
&lt;br /&gt;
1)&#039;&#039;Ichneumonidae&#039;&#039;: Largest family, parasitoids of spiders&lt;br /&gt;
&lt;br /&gt;
2)&#039;&#039;Braconidae&#039;&#039;: mostly parasitoid of &#039;&#039;lepidopterous&#039;&#039; larvae&lt;br /&gt;
&lt;br /&gt;
3)&#039;&#039;Encyrtidae&#039;&#039;: mostly parasitoid of &#039;&#039;aphids&#039;&#039; and scale insects&lt;br /&gt;
&lt;br /&gt;
4)&#039;&#039;Eulophidae&#039;&#039;: parasitoid of beetles, moths, and other insects&lt;br /&gt;
&lt;br /&gt;
5)&#039;&#039;Trichogrammatidae&#039;&#039;: egg parasites&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Gall Wasps&#039;&#039;&#039;: Larvae are herbivores which induce the formation of plant galls and live in or on these tissues&lt;br /&gt;
&lt;br /&gt;
1)&#039;&#039;Cynipidae&#039;&#039;: most species live on oak trees&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Predatory Wasps&#039;&#039;&#039;: Adults provision nest sites with prey that they catch and paralyze by stinging &lt;br /&gt;
&lt;br /&gt;
1)&#039;&#039;Sphecidae&#039;&#039;: prey on caterpillars and spiders&lt;br /&gt;
&lt;br /&gt;
2)&#039;&#039;Pompilidae&#039;&#039;: prey on spiders&lt;br /&gt;
&lt;br /&gt;
3)&#039;&#039;Tiphiidae&#039;&#039;: prey on beetle larvae&lt;br /&gt;
&lt;br /&gt;
4)&#039;&#039;Scoliidae&#039;&#039;: prey on beetle larvae&lt;br /&gt;
&lt;br /&gt;
5)&#039;&#039;Vespidae&#039;&#039;: prey on caterpillars&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Social Wasps&#039;&#039;&#039;: The nests are tended by sterile female workers&lt;br /&gt;
&lt;br /&gt;
1)&#039;&#039;Vespidae&#039;&#039;: yellowjackets, hornets, paper wasps&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Ants&#039;&#039;&#039;: True social insects. Wingless workers forage for resources&lt;br /&gt;
&lt;br /&gt;
1)&#039;&#039;Formicidae&#039;&#039;: Ants&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Solitary Bees&#039;&#039;&#039;: Adults build their individual nests and provision them with plant material (nectar or pollen)&lt;br /&gt;
&lt;br /&gt;
1)&#039;&#039;Halictidae&#039;&#039;: Sweat bees&lt;br /&gt;
&lt;br /&gt;
2)&#039;&#039;Megachilidae&#039;&#039;: Leafcutting bees&lt;br /&gt;
&lt;br /&gt;
3)&#039;&#039;Anthophoridae&#039;&#039;: Carpenter bees&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Social Bees&#039;&#039;&#039;: True social insects. Communities are found in nests in the [[soil]] (Bumble Bees) or in cavities (Honey Bees). Sterile female workers forage for resources such as nectar or pollen&lt;br /&gt;
&lt;br /&gt;
1)&#039;&#039;Apidae&#039;&#039;: Bumble bees and Honey bees&lt;br /&gt;
&lt;br /&gt;
== Ecology ==&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Eusociality&#039;&#039;&#039;:[[File:Melissodes desponsa, f, face, Maine, Du Clos 2015-12-01-17.37 (24469964305).jpg|200px|thumb|right|Melissodes desponsa bee body covered in pollen]]&lt;br /&gt;
&lt;br /&gt;
According to C.J.A. Bradshaw, C.R. McMahon [1], is an advanced social system where colonies of organisms are created for the succession of its offspring. This system exists when the adults belong to two or more overlapping generations, they take care cooperatively for the offspring, and are divided into reproductive and non-reproductive castes. This division of labor means that some females give up the ability to have offspring to facilitate reproduction by other individuals in the same colony.&lt;br /&gt;
&lt;br /&gt;
According to Norman F. Johnson [9], the beginning of such society is after a virgin queen from a colony mates with one or several males. Then, the queen builds her nest, which could be in the soil, a natural cavity, or out in the open. The colony founding can be sometimes cooperative, and determining which individual will become the primary reproducer is established through behavioral interactions among the founders. Males are only needed for insemination of the new queens, which soon after will die. The eggs produced by the new queen, will develop into the first female worker generation, which usually cannot reproduce. These workers have many functions, they take care of the offspring, forage for resources, defend the nest and the queen. These functions are sometimes divided by workers, and sometimes by morphological differences in their bodies. Once well established, more males and females are produced to continue the growth of the colony.&lt;br /&gt;
&lt;br /&gt;
&#039;&#039;&#039;Pollination&#039;&#039;&#039;:[[File:Pollen grains observed in aeroplankton of South Europe.png|200px|thumb|right|Pollen Particles]][[File:European honey bee extracts nectar.jpg|200px|thumb|right|European honey bee drinking nectar of a flower]]&lt;br /&gt;
&lt;br /&gt;
Pollination is the transfer of pollen, which can be via wind, water, insects, from the male structure (Anthers) of a flower to the female structure (Stigma) of either the same flower (Monoecious) or another (Dioecious) of the same species. This phenomena is what makes hymenopterans so important for the ecosystem they are present, since most plants rely on them for fertilization. Therefore, plants have evolved a symbiotic relationship with them, in which the plants produce the sweet nectar these insects require in their diet, and the hymenopterans while in search of the nectar carry particles of pollen in their bodies and pollinate other flowers. &amp;lt;!--A brief explanation of why this an important would strengthen this paragraph--&amp;gt;&lt;br /&gt;
&amp;lt;!--Great page and awesome content! my one suggestion would be to try and make it more formal sounding, like using &amp;quot;we&amp;quot; less--&amp;gt;&lt;br /&gt;
== References ==&lt;br /&gt;
&lt;br /&gt;
[1]Bradshaw, C. J. A., and C. R. McMahon. 2008. Fecundity. Encyclopedia of [[Ecology]]:1535–1543. &lt;br /&gt;
&lt;br /&gt;
[2]Contributors, W. 2021, April 22. Wasp. Wikipedia, The Free Encyclopedia. https://en.wikipedia.org/wiki/Wasp. &lt;br /&gt;
&lt;br /&gt;
[3]Contributors, W. 2021, March 12. Hymenoptera. Wikipedia, The Free Encyclopedia. https://en.wikipedia.org/wiki/Hymenoptera. &lt;br /&gt;
&lt;br /&gt;
[4]Department of Entomology. 2015. Hymenoptera. NC State Agriculture and Life Sciences. https://genent.cals.ncsu.edu/insect-identification/hymenoptera/. &lt;br /&gt;
&lt;br /&gt;
[5]The Editors of Encyclopaedia Britannica. 1999. Wasp. Encyclopædia Britannica, inc. https://www.britannica.com/animal/wasp. &lt;br /&gt;
&lt;br /&gt;
[6]Greenwood, D. 2019, May 30. Bee Larvae. https://beehivehero.com/bee-larvae/. &lt;br /&gt;
&lt;br /&gt;
[7]Institution Archives, S. (n.d.). Wasps, Ants, and Bees (Hymenoptera). Department of Systematic Biology, Entomology Section, National Museum of Natural History, in cooperation with Public Inquiry Services,  Smithsonian Institution. https://www.si.edu/spotlight/buginfo/hymenoptera. &lt;br /&gt;
&lt;br /&gt;
[8]Jernigan, C. M. 2017, June 13. Bee Anatomy. Arizona State University School of Life Sciences Ask A Biologist. https://askabiologist.asu.edu/honey-bee-anatomy. &lt;br /&gt;
&lt;br /&gt;
[9]Johnson, N. F. 2001. Hymenoptera. Encyclopedia of Biodiversity:417–426. &lt;br /&gt;
&lt;br /&gt;
[10]Lindauer, M. 1999. Hymenopteran. Encyclopædia Britannica, inc. https://www.britannica.com/animal/hymenopteran/Natural-history#ref39798. &lt;br /&gt;
&lt;br /&gt;
[11]Peters, R. S., L. Krogmann, C. Mayer, A. Donath, S. Gunkel, K. Meusemann, A. Kozlov, L. Podsiadlowski, M. Petersen, R. Lanfear, P. A. Diez, J. Heraty, K. M. Kjer, S. Klopfstein, R. Meier, C. Polidori, T. Schmitt, S. Liu, X. Zhou, T. Wappler, J. Rust, B. Misof, and O. Niehuis. 2017. Evolutionary History of the Hymenoptera. Current Biology 27:1013–1018.&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Fern&amp;diff=5811</id>
		<title>Fern</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Fern&amp;diff=5811"/>
		<updated>2021-04-27T04:14:59Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: /* Reproduction */&lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;Ferns are a type of a vascular plant characterized by spores, complex leaves, and the lack of seeds and flowers.  Ferns belong to a class of plants known as Polypodiopsida, which is further divided into 4 extant subclasses; Equisetidae, Marattiidae, Ophioglossidae, and Polypodiidae.[1] Ferns are thought to have originated some 359 million years ago during the Devonian period, but it is possible that this group of vascular plants is even older.[2] There is a wide range of sizes that ferns can grow to, some of the smallest ferns can be 1-2 cm in height, while the some of the tallest ferns (tree ferns) can grow anywhere from 10-25 meters.[2]&lt;br /&gt;
[[File:Tree-fern.jpg|thumb|A group of tree ferns (Cyathea medullaris), one of the tallest species of ferns.]]&lt;br /&gt;
== &#039;&#039;&#039;Classification&#039;&#039;&#039; ==&lt;br /&gt;
Ferns are an ancient group of vascular plants that are considered to be one of the earliest plants to move onto land.[3] The oldest known ferns are found to be from the late Devonian period around 360 million years ago, but many modern fern families and species are thought to have started appearing in the Cretaceous period, 145-66 million years ago.[4] This diversification of fern families is referred to as the “great fern radiation”.[4] Today there are 4 living sub-classes ferns, but throughout their history there has been 4 sub-classes that have gone extinct. Below are descriptions of the 4 extent sub-classes:&lt;br /&gt;
*Equisetidae: This sub-class consists of vascular plants called horsetails. These are close relatives to true ferns and also reproduce via spores and characterized by a whorl of branch-like leaves.[1]&lt;br /&gt;
*Marattiidae: This sub-class separated from the other fern groups early on in their evolutionary history and is made up of about 100 species. These ferns are known for their extremely large leaves and fleshy rootstocks.[1] &lt;br /&gt;
*Ophioglossidae: This sub-class is not as diverse as the other sub-classes The members of this sub-group are known as the whisk ferns, grape ferns, adder&#039;s-tongues and moonworts.[1]&lt;br /&gt;
*Polypodiidae: these ferns are referred to as leptosporangiate ferns and are the largest of the 4 sub-classes with around 11,000 species. This is the most diverse sub-class of ferns and contains many of the wellknown ferns.[1]   &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Morphology&#039;&#039;&#039;==&lt;br /&gt;
&lt;br /&gt;
===&#039;&#039;&#039;Leaves&#039;&#039;&#039;===&lt;br /&gt;
[[File:fern leaf diagram.jpg|thumb|A Diagram showing the different parts of a fern leaf.]]&lt;br /&gt;
Ferns are an extremely diverse group, and this diversity results in a plethora of unique shapes and sizes. Even though there is a large degree of variability in the leaves of ferns, many ferns share some general morphological similarities.[5] The leaves of ferns are typically referred to as “fronds”.[6] Fronds consist of two parts; the stem (stalk) which is referred to as the “petiole” and the “leaf blade” which is the vegetative organs that extend laterally from the petiole.[5] The leaf blade is often separated into individual segments called “pinnae” which is made up of several leaflets known as “pinna”.[6] Despite the variation in leaf morphology, fern leaves play an important role in the growth, survival, and reproduction of the fern. Photosynthesis takes place in the leaves of the fern and is vital to the survival of the plant, but the leaves can also help to disperse spores for reproduction, house nitrogen-fixing bacteria, allow the fern to reproduce vegetatively, and collect falling nutrients/organic matter that fall from above the leaves.[5]  &lt;br /&gt;
===&#039;&#039;&#039;Stems&#039;&#039;&#039;===&lt;br /&gt;
[[File:Fern stem and root diagram.jpg|thumb|A Diagram showing the difference between the stem and the roots of a fern.]]&lt;br /&gt;
The stems of ferns are called “rhizomes” and are usually found underneath the fern, buried under some type of substrate, most commonly soils and mosses.[6] The rhizomes can extend either laterally or vertically and serves as the connection between the aboveground leaves and the underground roots.[6] In ferns there are two types of stems: long-creeping stems and short-creeping stems. Long-creeping stems have a longer length which allows the fronds to be more spaced out, while short-creeping stems are shorter and tend to have the fronds closer together.[6] &lt;br /&gt;
===&#039;&#039;&#039;Roots&#039;&#039;&#039;===&lt;br /&gt;
The roots of ferns are not entirely different from the roots of seed-producing plants and serve many of the same functions. Roots grow out of the rhizomes (stem) of the fern and extend deeper and further into the growth substrate.[6] Fern roots are thin and spread out in order to provide structural integrity to the fern. The roots are an important structure that assists with the uptake of water and various soil nutrients which are essential elements the fern needs to thrive.[6]     &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Distribution&#039;&#039;&#039;==&lt;br /&gt;
Today it is estimated that a total of 10,500 distinct species of ferns exist, but there could potentially be more than 15,000 species because new species are continuously being found in unexplored areas and some groups of ferns are poorly understood.[2] The diversity of ferns results in a wide distribution that spans multiple continents and biomes. Ferns can be found on every continent on earth except Antarctica. The greatest distribution of ferns is found in tropical areas, specifically tropical rain forests where its possible to find over 100 different species in just a few hectares.[2] Even though the greatest richness of ferns is found in the tropics that does not mean that is the only place they are found. Ferns can also be found in temperate and some artic environments.[2] Generally fern diversity and abundance decreases as one goes from the equator to the poles with the least number of ferns found in artic environments. &lt;br /&gt;
  &lt;br /&gt;
==&#039;&#039;&#039;Habitat&#039;&#039;&#039;==&lt;br /&gt;
Similar to its distribution, ferns can inhabit a wide range of habitats. While a majority of ferns prefer moist tropical forests,  they can also be found high in elevation on mountains, in deserts growing in/on rocks, open/abandoned fields, and even in wetlands and bodies of water.[2]  The most common habitat  for the majority of ferns are damp and warm areas, which makes tropical rain forests a prime habitat for a number of different fern species, but certain species have adapted to a variety of abiotic conditions, such as temperature, precipitation, sunlight, and substrate type. Ferns are often considered an important plant for succession because they are able to colonize such a wide range of different habitats.[2]  Some ferns have even been observed to be epiphytes and grow on other plant species, such as trees.[2] &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Reproduction&#039;&#039;&#039;==&lt;br /&gt;
[[File:Spores under leaf.jpg|thumb|Reproductive spores on the underside of a fern frond.]]&lt;br /&gt;
Unlike seed plants, ferns utilize tiny, microscopic spores that are contained in a specialized structure called the sporangia (plural: sporangium), typically on the underside of leaves.[2][3] The spores are dispersed mainly by wind and water and can be carried long distances from the parent plant.[3] Spores that happen to land in suitable habitats will crack and begin to germinate, growing into a gametophyte.[3] The gametophyte is a structure that houses the reproductive organs of the plant: the antheridium and the archegonium.[3] The sperm swims from the antheridium to the archegonium where the egg is located, although water is required for this to happen which stresses the need for a relatively moist environment.[3] Once the sperm finds the egg the fern begins its life and starts to grow back into the sporophyte.[3]&lt;br /&gt;
&lt;br /&gt;
Some ferns can reproduce asexually through a reproductive strategy known as vegetative reproduction. Vegetative reproduction is essentially growing a new plant from a removed part of the parent plant.[7] In some ferns this is achieved through specialized bulbs that fall off the fern and begins to grow into a new plant, but this may also work with fragments from the parent plant such as leaves.[8] This reproductive method does not disperse the offspring very far from the parent.[2]&lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Influence on Soil&#039;&#039;&#039;==&lt;br /&gt;
Ferns can have a significant effect on the soil they grow on and play an important role in the carbon concentration in the soil.[9] Being an understory plant ferns can catch falling organic matter for higher up in the canopy.[10] The material caught by the ferns resulted in an increase in decomposition rate because the ferns had more efficient decomposers than the soil did.[10] A study in 2019 looked at how using ferns for restoration efforts could affect soil carbon (C). The results of this study showed that the presence of ferns contributed anywhere between 54% and 61% of the total soil C, mostly from leaf litter and dead root material.[9] This study also showed ferns influenced nutrient retention by reducing the loss of nutrients, like nitrogen, and increasing soil carbon storage.[9]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
[1] Smith, A. R., K. M. Pryer, E. Schuettpelz, P. Korall, H. Schneider, and P. G. Wolf. 2006. A classification for extant ferns. Taxon 55:705–731.&lt;br /&gt;
&lt;br /&gt;
[2] Wagner, Warren H. , Walker, Warren F. , Mickel, John T. , Yatskievych, George and Gifford, Ernest M.. &amp;quot;Fern&amp;quot;. Encyclopedia Britannica, 12 Jun. 2020, https://www.britannica.com/plant/fern.&lt;br /&gt;
&lt;br /&gt;
[3] Hill, T. 2015. Ferns. Organismal Diversity, Ohio State University. https://u.osu.edu/eeob3320/2015/03/06/ferns/#:~:text=The%20%E2%80%9Cgreat%20fern%20radiation%E2%80%9D%20is,period%20(Bhattacharya%2C%202009).&amp;amp;text=During%20the%20Carboniferous%20period%2C%20giant,to%2012%20meters%20in%20height.&lt;br /&gt;
&lt;br /&gt;
[4] Plant Evolution II: Ferns. Cortland University. http://cortland.edu/waldbauer-trail/11-plant%20evolution-II.html#:~:text=The%20ferns%20and%20their%20relatives,to%2066%20million%20years%20ago. &lt;br /&gt;
&lt;br /&gt;
[5] Vasco, A., R. C. Moran, and B. A. Ambrose. 2013. The evolution, morphology, and development of fern leaves. Frontiers in Plant Science 4:1–16.&lt;br /&gt;
&lt;br /&gt;
[6] Fern Structure. US Forest Service, United States Department of Agriculture. https://www.fs.fed.us/wildflowers/beauty/ferns/structure.shtml#:~:text=The%20leaves%20of%20ferns%20are,and%20petiole%20(leaf%20stalk).&amp;amp;text=The%20midrib%20is%20the%20main,pinnae%3B%20single%20leaflets%20are%20pinna. &lt;br /&gt;
&lt;br /&gt;
[7] Britannica, The Editors of Encyclopaedia. &amp;quot;Vegetative reproduction&amp;quot;. Encyclopedia Britannica, 9 Aug. 2017, https://www.britannica.com/science/vegetative-reproduction. &lt;br /&gt;
&lt;br /&gt;
[8] Fern Reproduction. US Forest Service, United States Department of Agriculture. https://www.fs.fed.us/wildflowers/beauty/ferns/reproduction.shtml&lt;br /&gt;
&lt;br /&gt;
[9] Lyu, M., J. Xie, C. P. Giardina, M. A. Vadeboncoeur, X. Feng, M. Wang, L. Ukonmaanaho, T. C. Lin, Y. Kuzyakov, and Y. Yang. 2019. Understory ferns alter soil carbon chemistry and increase carbon storage during reforestation with native pine on previously degraded sites. Soil Biology and Biochemistry 132:80–92.&lt;br /&gt;
&lt;br /&gt;
[10] Dearden, F. M., and D. A. Wardle. 2008. The potential for forest canopy litterfall interception by a dense fern understorey, and the consequences for litter decomposition. Oikos 117:83–92.&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Fern&amp;diff=5810</id>
		<title>Fern</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Fern&amp;diff=5810"/>
		<updated>2021-04-27T04:11:33Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;Ferns are a type of a vascular plant characterized by spores, complex leaves, and the lack of seeds and flowers.  Ferns belong to a class of plants known as Polypodiopsida, which is further divided into 4 extant subclasses; Equisetidae, Marattiidae, Ophioglossidae, and Polypodiidae.[1] Ferns are thought to have originated some 359 million years ago during the Devonian period, but it is possible that this group of vascular plants is even older.[2] There is a wide range of sizes that ferns can grow to, some of the smallest ferns can be 1-2 cm in height, while the some of the tallest ferns (tree ferns) can grow anywhere from 10-25 meters.[2]&lt;br /&gt;
[[File:Tree-fern.jpg|thumb|A group of tree ferns (Cyathea medullaris), one of the tallest species of ferns.]]&lt;br /&gt;
== &#039;&#039;&#039;Classification&#039;&#039;&#039; ==&lt;br /&gt;
Ferns are an ancient group of vascular plants that are considered to be one of the earliest plants to move onto land.[3] The oldest known ferns are found to be from the late Devonian period around 360 million years ago, but many modern fern families and species are thought to have started appearing in the Cretaceous period, 145-66 million years ago.[4] This diversification of fern families is referred to as the “great fern radiation”.[4] Today there are 4 living sub-classes ferns, but throughout their history there has been 4 sub-classes that have gone extinct. Below are descriptions of the 4 extent sub-classes:&lt;br /&gt;
*Equisetidae: This sub-class consists of vascular plants called horsetails. These are close relatives to true ferns and also reproduce via spores and characterized by a whorl of branch-like leaves.[1]&lt;br /&gt;
*Marattiidae: This sub-class separated from the other fern groups early on in their evolutionary history and is made up of about 100 species. These ferns are known for their extremely large leaves and fleshy rootstocks.[1] &lt;br /&gt;
*Ophioglossidae: This sub-class is not as diverse as the other sub-classes The members of this sub-group are known as the whisk ferns, grape ferns, adder&#039;s-tongues and moonworts.[1]&lt;br /&gt;
*Polypodiidae: these ferns are referred to as leptosporangiate ferns and are the largest of the 4 sub-classes with around 11,000 species. This is the most diverse sub-class of ferns and contains many of the wellknown ferns.[1]   &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Morphology&#039;&#039;&#039;==&lt;br /&gt;
&lt;br /&gt;
===&#039;&#039;&#039;Leaves&#039;&#039;&#039;===&lt;br /&gt;
[[File:fern leaf diagram.jpg|thumb|A Diagram showing the different parts of a fern leaf.]]&lt;br /&gt;
Ferns are an extremely diverse group, and this diversity results in a plethora of unique shapes and sizes. Even though there is a large degree of variability in the leaves of ferns, many ferns share some general morphological similarities.[5] The leaves of ferns are typically referred to as “fronds”.[6] Fronds consist of two parts; the stem (stalk) which is referred to as the “petiole” and the “leaf blade” which is the vegetative organs that extend laterally from the petiole.[5] The leaf blade is often separated into individual segments called “pinnae” which is made up of several leaflets known as “pinna”.[6] Despite the variation in leaf morphology, fern leaves play an important role in the growth, survival, and reproduction of the fern. Photosynthesis takes place in the leaves of the fern and is vital to the survival of the plant, but the leaves can also help to disperse spores for reproduction, house nitrogen-fixing bacteria, allow the fern to reproduce vegetatively, and collect falling nutrients/organic matter that fall from above the leaves.[5]  &lt;br /&gt;
===&#039;&#039;&#039;Stems&#039;&#039;&#039;===&lt;br /&gt;
[[File:Fern stem and root diagram.jpg|thumb|A Diagram showing the difference between the stem and the roots of a fern.]]&lt;br /&gt;
The stems of ferns are called “rhizomes” and are usually found underneath the fern, buried under some type of substrate, most commonly soils and mosses.[6] The rhizomes can extend either laterally or vertically and serves as the connection between the aboveground leaves and the underground roots.[6] In ferns there are two types of stems: long-creeping stems and short-creeping stems. Long-creeping stems have a longer length which allows the fronds to be more spaced out, while short-creeping stems are shorter and tend to have the fronds closer together.[6] &lt;br /&gt;
===&#039;&#039;&#039;Roots&#039;&#039;&#039;===&lt;br /&gt;
The roots of ferns are not entirely different from the roots of seed-producing plants and serve many of the same functions. Roots grow out of the rhizomes (stem) of the fern and extend deeper and further into the growth substrate.[6] Fern roots are thin and spread out in order to provide structural integrity to the fern. The roots are an important structure that assists with the uptake of water and various soil nutrients which are essential elements the fern needs to thrive.[6]     &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Distribution&#039;&#039;&#039;==&lt;br /&gt;
Today it is estimated that a total of 10,500 distinct species of ferns exist, but there could potentially be more than 15,000 species because new species are continuously being found in unexplored areas and some groups of ferns are poorly understood.[2] The diversity of ferns results in a wide distribution that spans multiple continents and biomes. Ferns can be found on every continent on earth except Antarctica. The greatest distribution of ferns is found in tropical areas, specifically tropical rain forests where its possible to find over 100 different species in just a few hectares.[2] Even though the greatest richness of ferns is found in the tropics that does not mean that is the only place they are found. Ferns can also be found in temperate and some artic environments.[2] Generally fern diversity and abundance decreases as one goes from the equator to the poles with the least number of ferns found in artic environments. &lt;br /&gt;
  &lt;br /&gt;
==&#039;&#039;&#039;Habitat&#039;&#039;&#039;==&lt;br /&gt;
Similar to its distribution, ferns can inhabit a wide range of habitats. While a majority of ferns prefer moist tropical forests,  they can also be found high in elevation on mountains, in deserts growing in/on rocks, open/abandoned fields, and even in wetlands and bodies of water.[2]  The most common habitat  for the majority of ferns are damp and warm areas, which makes tropical rain forests a prime habitat for a number of different fern species, but certain species have adapted to a variety of abiotic conditions, such as temperature, precipitation, sunlight, and substrate type. Ferns are often considered an important plant for succession because they are able to colonize such a wide range of different habitats.[2]  Some ferns have even been observed to be epiphytes and grow on other plant species, such as trees.[2] &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Reproduction&#039;&#039;&#039;==&lt;br /&gt;
[[File:Spores under leaf.jpg|thumb|Reproductive spores on the underside of a fern frond.]]&lt;br /&gt;
Unlike seed plants, ferns utilize tiny, microscopic spores that are contained in a specialized structure called the sporangia (plural: sporangium), typically on the underside of leaves.[2][3] The spores are dispersed mainly by wind and water and can be carried long distances from the parent plant.[3] Spores that happen to land in suitable habitats will crack and begin to germinate, growing into a gametophyte.[3] The gametophyte is a structure that houses the reproductive organs of the plant: the antheridium and the archegonium.[3] The sperm swims from the antheridium to the archegonium where the egg is located, although water is required for this to happen which stresses the need for a relatively moist environment.[3] Once the sperm finds the egg the fern begins its life and starts to grow back into the sporophyte.[3]&lt;br /&gt;
Some ferns can reproduce asexually through a reproductive strategy known as vegetative reproduction. Vegetative reproduction is essentially growing a new plant from a removed part of the parent plant.[7] In some ferns this is achieved through specialized bulbs that fall off the fern and begins to grow into a new plant, but this may also work with fragments from the parent plant such as leaves.[8] This reproductive method does not disperse the offspring very far from the parent.[2] &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Influence on Soil&#039;&#039;&#039;==&lt;br /&gt;
Ferns can have a significant effect on the soil they grow on and play an important role in the carbon concentration in the soil.[9] Being an understory plant ferns can catch falling organic matter for higher up in the canopy.[10] The material caught by the ferns resulted in an increase in decomposition rate because the ferns had more efficient decomposers than the soil did.[10] A study in 2019 looked at how using ferns for restoration efforts could affect soil carbon (C). The results of this study showed that the presence of ferns contributed anywhere between 54% and 61% of the total soil C, mostly from leaf litter and dead root material.[9] This study also showed ferns influenced nutrient retention by reducing the loss of nutrients, like nitrogen, and increasing soil carbon storage.[9]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
[1] Smith, A. R., K. M. Pryer, E. Schuettpelz, P. Korall, H. Schneider, and P. G. Wolf. 2006. A classification for extant ferns. Taxon 55:705–731.&lt;br /&gt;
&lt;br /&gt;
[2] Wagner, Warren H. , Walker, Warren F. , Mickel, John T. , Yatskievych, George and Gifford, Ernest M.. &amp;quot;Fern&amp;quot;. Encyclopedia Britannica, 12 Jun. 2020, https://www.britannica.com/plant/fern.&lt;br /&gt;
&lt;br /&gt;
[3] Hill, T. 2015. Ferns. Organismal Diversity, Ohio State University. https://u.osu.edu/eeob3320/2015/03/06/ferns/#:~:text=The%20%E2%80%9Cgreat%20fern%20radiation%E2%80%9D%20is,period%20(Bhattacharya%2C%202009).&amp;amp;text=During%20the%20Carboniferous%20period%2C%20giant,to%2012%20meters%20in%20height.&lt;br /&gt;
&lt;br /&gt;
[4] Plant Evolution II: Ferns. Cortland University. http://cortland.edu/waldbauer-trail/11-plant%20evolution-II.html#:~:text=The%20ferns%20and%20their%20relatives,to%2066%20million%20years%20ago. &lt;br /&gt;
&lt;br /&gt;
[5] Vasco, A., R. C. Moran, and B. A. Ambrose. 2013. The evolution, morphology, and development of fern leaves. Frontiers in Plant Science 4:1–16.&lt;br /&gt;
&lt;br /&gt;
[6] Fern Structure. US Forest Service, United States Department of Agriculture. https://www.fs.fed.us/wildflowers/beauty/ferns/structure.shtml#:~:text=The%20leaves%20of%20ferns%20are,and%20petiole%20(leaf%20stalk).&amp;amp;text=The%20midrib%20is%20the%20main,pinnae%3B%20single%20leaflets%20are%20pinna. &lt;br /&gt;
&lt;br /&gt;
[7] Britannica, The Editors of Encyclopaedia. &amp;quot;Vegetative reproduction&amp;quot;. Encyclopedia Britannica, 9 Aug. 2017, https://www.britannica.com/science/vegetative-reproduction. &lt;br /&gt;
&lt;br /&gt;
[8] Fern Reproduction. US Forest Service, United States Department of Agriculture. https://www.fs.fed.us/wildflowers/beauty/ferns/reproduction.shtml&lt;br /&gt;
&lt;br /&gt;
[9] Lyu, M., J. Xie, C. P. Giardina, M. A. Vadeboncoeur, X. Feng, M. Wang, L. Ukonmaanaho, T. C. Lin, Y. Kuzyakov, and Y. Yang. 2019. Understory ferns alter soil carbon chemistry and increase carbon storage during reforestation with native pine on previously degraded sites. Soil Biology and Biochemistry 132:80–92.&lt;br /&gt;
&lt;br /&gt;
[10] Dearden, F. M., and D. A. Wardle. 2008. The potential for forest canopy litterfall interception by a dense fern understorey, and the consequences for litter decomposition. Oikos 117:83–92.&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Fern&amp;diff=5809</id>
		<title>Fern</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Fern&amp;diff=5809"/>
		<updated>2021-04-27T04:10:44Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;Ferns are a type of a vascular plant characterized by spores, complex leaves, and the lack of seeds and flowers.  Ferns belong to a class of plants known as Polypodiopsida, which is further divided into 4 extant subclasses; Equisetidae, Marattiidae, Ophioglossidae, and Polypodiidae.[1] Ferns are thought to have originated some 359 million years ago during the Devonian period, but it is possible that this group of vascular plants is even older.[2] There is a wide range of sizes that ferns can grow to, some of the smallest ferns can be 1-2 cm in height, while the some of the tallest ferns (tree ferns) can grow anywhere from 10-25 meters.[2]&lt;br /&gt;
[[File:Tree-fern.jpg|thumb|A group of tree ferns (Cyathea medullaris), one of the tallest species of ferns.]]&lt;br /&gt;
== &#039;&#039;&#039;Classification&#039;&#039;&#039; ==&lt;br /&gt;
Ferns are an ancient group of vascular plants that are considered to be one of the earliest plants to move onto land.[3] The oldest known ferns are found to be from the late Devonian period around 360 million years ago, but many modern fern families and species are thought to have started appearing in the Cretaceous period, 145-66 million years ago.[4] This diversification of fern families is referred to as the “great fern radiation”.[4] Today there are 4 living sub-classes ferns, but throughout their history there has been 4 sub-classes that have gone extinct. Below are descriptions of the 4 extent sub-classes:&lt;br /&gt;
*Equisetidae: This sub-class consists of vascular plants called horsetails. These are close relatives to true ferns and also reproduce via spores and characterized by a whorl of branch-like leaves.[1]&lt;br /&gt;
*Marattiidae: This sub-class separated from the other fern groups early on in their evolutionary history and is made up of about 100 species. These ferns are known for their extremely large leaves and fleshy rootstocks.[1] &lt;br /&gt;
*Ophioglossidae: This sub-class is not as diverse as the other sub-classes The members of this sub-group are known as the whisk ferns, grape ferns, adder&#039;s-tongues and moonworts.[1]&lt;br /&gt;
*Polypodiidae: these ferns are referred to as leptosporangiate ferns and are the largest of the 4 sub-classes with around 11,000 species. This is the most diverse sub-class of ferns and contains many of the wellknown ferns.[1]   &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Morphology&#039;&#039;&#039;==&lt;br /&gt;
&lt;br /&gt;
===&#039;&#039;&#039;Leaves&#039;&#039;&#039;===&lt;br /&gt;
[[File:fern leaf diagram.jpg|thumb|A Diagram showing the different parts of a fern leaf.]]&lt;br /&gt;
Ferns are an extremely diverse group, and this diversity results in a plethora of unique shapes and sizes. Even though there is a large degree of variability in the leaves of ferns, many ferns share some general morphological similarities.[5] The leaves of ferns are typically referred to as “fronds”.[6] Fronds consist of two parts; the stem (stalk) which is referred to as the “petiole” and the “leaf blade” which is the vegetative organs that extend laterally from the petiole.[5] The leaf blade is often separated into individual segments called “pinnae” which is made up of several leaflets known as “pinna”.[6] Despite the variation in leaf morphology, fern leaves play an important role in the growth, survival, and reproduction of the fern. Photosynthesis takes place in the leaves of the fern and is vital to the survival of the plant, but the leaves can also help to disperse spores for reproduction, house nitrogen-fixing bacteria, allow the fern to reproduce vegetatively, and collect falling nutrients/organic matter that fall from above the leaves.[5]  &lt;br /&gt;
===&#039;&#039;&#039;Stems&#039;&#039;&#039;===&lt;br /&gt;
[[File:Fern stem and root diagram.jpg|thumb|A Diagram showing the difference between the stem and the roots of a fern.]]&lt;br /&gt;
The stems of ferns are called “rhizomes” and are usually found underneath the fern, buried under some type of substrate, most commonly soils and mosses.[6] The rhizomes can extend either laterally or vertically and serves as the connection between the aboveground leaves and the underground roots.[6] In ferns there are two types of stems: long-creeping stems and short-creeping stems. Long-creeping stems have a longer length which allows the fronds to be more spaced out, while short-creeping stems are shorter and tend to have the fronds closer together.[6] &lt;br /&gt;
===&#039;&#039;&#039;Roots&#039;&#039;&#039;===&lt;br /&gt;
The roots of ferns are not entirely different from the roots of seed-producing plants and serve many of the same functions. Roots grow out of the rhizomes (stem) of the fern and extend deeper and further into the growth substrate.[6] Fern roots are thin and spread out in order to provide structural integrity to the fern. The roots are an important structure that assists with the uptake of water and various soil nutrients which are essential elements the fern needs to thrive.[6]     &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Distribution&#039;&#039;&#039;==&lt;br /&gt;
Today it is estimated that a total of 10,500 distinct species of ferns exist, but there could potentially be more than 15,000 species because new species are continuously being found in unexplored areas and some groups of ferns are poorly understood.[2] The diversity of ferns results in a wide distribution that spans multiple continents and biomes. Ferns can be found on every continent on earth except Antarctica. The greatest distribution of ferns is found in tropical areas, specifically tropical rain forests where its possible to find over 100 different species in just a few hectares.[2] Even though the greatest richness of ferns is found in the tropics that does not mean that is the only place they are found. Ferns can also be found in temperate and some artic environments.[2] Generally fern diversity and abundance decreases as one goes from the equator to the poles with the least number of ferns found in artic environments. &lt;br /&gt;
  &lt;br /&gt;
==&#039;&#039;&#039;Habitat&#039;&#039;&#039;==&lt;br /&gt;
Similar to its distribution, ferns can inhabit a wide range of habitats. While a majority of ferns prefer moist tropical forests,  they can also be found high in elevation on mountains, in deserts growing in/on rocks, open/abandoned fields, and even in wetlands and bodies of water.[2]  The most common habitat  for the majority of ferns are damp and warm areas, which makes tropical rain forests a prime habitat for a number of different fern species, but certain species have adapted to a variety of abiotic conditions, such as temperature, precipitation, sunlight, and substrate type. Ferns are often considered an important plant for succession because they are able to colonize such a wide range of different habitats.[2]  Some ferns have even been observed to be epiphytes and grow on other plant species, such as trees.[2] &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Reproduction&#039;&#039;&#039;==&lt;br /&gt;
[[File:Spores under leaf.jpg|thumb|Reproductive spores on the underside of a fern frond.]]&lt;br /&gt;
Unlike seed plants, ferns utilize tiny, microscopic spores that are contained in a specialized structure called the sporangia (plural: sporangium), typically on the underside of leaves.[2][3] The spores are dispersed mainly by wind and water and can be carried long distances from the parent plant.[3] Spores that happen to land in suitable habitats will crack and begin to germinate, growing into a gametophyte.[3] The gametophyte is a structure that houses the reproductive organs of the plant: the antheridium and the archegonium.[3] The sperm swims from the antheridium to the archegonium where the egg is located, although water is required for this to happen which stresses the need for a relatively moist environment.[3] Once the sperm finds the egg the fern begins its life and starts to grow back into the sporophyte.[3]&lt;br /&gt;
Some ferns can reproduce asexually through a reproductive strategy known as vegetative reproduction. Vegetative reproduction is essentially growing a new plant from a removed part of the parent plant.[7] In some ferns this is achieved through specialized bulbs that fall off the fern and begins to grow into a new plant, but this may also work with fragments from the parent plant such as leaves.[8] This reproductive method does not disperse the offspring very far from the parent.[2] &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Influence on Soil&#039;&#039;&#039;==&lt;br /&gt;
Ferns can have a significant effect on the soil they grow on and play an important role in the carbon concentration in the soil.[9] Being an understory plant ferns can catch falling organic matter for higher up in the canopy.[10] The material caught by the ferns resulted in an increase in decomposition rate because the ferns had more efficient decomposers than the soil did.[10] A study in 2019 looked at how using ferns for restoration efforts could affect soil carbon (C). The results of this study showed that the presence of ferns contributed anywhere between 54% and 61% of the total soil C, mostly from leaf litter and dead root material.[9] This study also showed ferns influenced nutrient retention by reducing the loss of nutrients, like nitrogen, and increasing soil carbon storage.[9]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
[1] Smith, A. R., K. M. Pryer, E. Schuettpelz, P. Korall, H. Schneider, and P. G. Wolf. 2006. A classification for extant ferns. Taxon 55:705–731.&lt;br /&gt;
[2] Wagner, Warren H. , Walker, Warren F. , Mickel, John T. , Yatskievych, George and Gifford, Ernest M.. &amp;quot;Fern&amp;quot;. Encyclopedia Britannica, 12 Jun. 2020, https://www.britannica.com/plant/fern.&lt;br /&gt;
[3] Hill, T. 2015. Ferns. Organismal Diversity, Ohio State University. https://u.osu.edu/eeob3320/2015/03/06/ferns/#:~:text=The%20%E2%80%9Cgreat%20fern%20radiation%E2%80%9D%20is,period%20(Bhattacharya%2C%202009).&amp;amp;text=During%20the%20Carboniferous%20period%2C%20giant,to%2012%20meters%20in%20height.&lt;br /&gt;
[4] Plant Evolution II: Ferns. Cortland University. http://cortland.edu/waldbauer-trail/11-plant%20evolution-II.html#:~:text=The%20ferns%20and%20their%20relatives,to%2066%20million%20years%20ago. &lt;br /&gt;
[5] Vasco, A., R. C. Moran, and B. A. Ambrose. 2013. The evolution, morphology, and development of fern leaves. Frontiers in Plant Science 4:1–16.&lt;br /&gt;
[6] Fern Structure. US Forest Service, United States Department of Agriculture. https://www.fs.fed.us/wildflowers/beauty/ferns/structure.shtml#:~:text=The%20leaves%20of%20ferns%20are,and%20petiole%20(leaf%20stalk).&amp;amp;text=The%20midrib%20is%20the%20main,pinnae%3B%20single%20leaflets%20are%20pinna. &lt;br /&gt;
[7] Britannica, The Editors of Encyclopaedia. &amp;quot;Vegetative reproduction&amp;quot;. Encyclopedia Britannica, 9 Aug. 2017, https://www.britannica.com/science/vegetative-reproduction. &lt;br /&gt;
[8] Fern Reproduction. US Forest Service, United States Department of Agriculture. https://www.fs.fed.us/wildflowers/beauty/ferns/reproduction.shtml&lt;br /&gt;
[9] Lyu, M., J. Xie, C. P. Giardina, M. A. Vadeboncoeur, X. Feng, M. Wang, L. Ukonmaanaho, T. C. Lin, Y. Kuzyakov, and Y. Yang. 2019. Understory ferns alter soil carbon chemistry and increase carbon storage during reforestation with native pine on previously degraded sites. Soil Biology and Biochemistry 132:80–92.&lt;br /&gt;
[10] Dearden, F. M., and D. A. Wardle. 2008. The potential for forest canopy litterfall interception by a dense fern understorey, and the consequences for litter decomposition. Oikos 117:83–92.&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Fern&amp;diff=5808</id>
		<title>Fern</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Fern&amp;diff=5808"/>
		<updated>2021-04-27T04:10:06Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;Ferns are a type of a vascular plant characterized by spores, complex leaves, and the lack of seeds and flowers.  Ferns belong to a class of plants known as Polypodiopsida, which is further divided into 4 extant subclasses; Equisetidae, Marattiidae, Ophioglossidae, and Polypodiidae.[1] Ferns are thought to have originated some 359 million years ago during the Devonian period, but it is possible that this group of vascular plants is even older.[2] There is a wide range of sizes that ferns can grow to, some of the smallest ferns can be 1-2 cm in height, while the some of the tallest ferns (tree ferns) can grow anywhere from 10-25 meters.[2]&lt;br /&gt;
[[Tree-fern.jpg|thumb|A group of tree ferns (Cyathea medullaris), one of the tallest species of ferns.]]&lt;br /&gt;
== &#039;&#039;&#039;Classification&#039;&#039;&#039; ==&lt;br /&gt;
Ferns are an ancient group of vascular plants that are considered to be one of the earliest plants to move onto land.[3] The oldest known ferns are found to be from the late Devonian period around 360 million years ago, but many modern fern families and species are thought to have started appearing in the Cretaceous period, 145-66 million years ago.[4] This diversification of fern families is referred to as the “great fern radiation”.[4] Today there are 4 living sub-classes ferns, but throughout their history there has been 4 sub-classes that have gone extinct. Below are descriptions of the 4 extent sub-classes:&lt;br /&gt;
*Equisetidae: This sub-class consists of vascular plants called horsetails. These are close relatives to true ferns and also reproduce via spores and characterized by a whorl of branch-like leaves.[1]&lt;br /&gt;
*Marattiidae: This sub-class separated from the other fern groups early on in their evolutionary history and is made up of about 100 species. These ferns are known for their extremely large leaves and fleshy rootstocks.[1] &lt;br /&gt;
*Ophioglossidae: This sub-class is not as diverse as the other sub-classes The members of this sub-group are known as the whisk ferns, grape ferns, adder&#039;s-tongues and moonworts.[1]&lt;br /&gt;
*Polypodiidae: these ferns are referred to as leptosporangiate ferns and are the largest of the 4 sub-classes with around 11,000 species. This is the most diverse sub-class of ferns and contains many of the wellknown ferns.[1]   &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Morphology&#039;&#039;&#039;==&lt;br /&gt;
&lt;br /&gt;
===&#039;&#039;&#039;Leaves&#039;&#039;&#039;===&lt;br /&gt;
[[File:fern leaf diagram.jpg|thumb|A Diagram showing the different parts of a fern leaf.]]&lt;br /&gt;
Ferns are an extremely diverse group, and this diversity results in a plethora of unique shapes and sizes. Even though there is a large degree of variability in the leaves of ferns, many ferns share some general morphological similarities.[5] The leaves of ferns are typically referred to as “fronds”.[6] Fronds consist of two parts; the stem (stalk) which is referred to as the “petiole” and the “leaf blade” which is the vegetative organs that extend laterally from the petiole.[5] The leaf blade is often separated into individual segments called “pinnae” which is made up of several leaflets known as “pinna”.[6] Despite the variation in leaf morphology, fern leaves play an important role in the growth, survival, and reproduction of the fern. Photosynthesis takes place in the leaves of the fern and is vital to the survival of the plant, but the leaves can also help to disperse spores for reproduction, house nitrogen-fixing bacteria, allow the fern to reproduce vegetatively, and collect falling nutrients/organic matter that fall from above the leaves.[5]  &lt;br /&gt;
===&#039;&#039;&#039;Stems&#039;&#039;&#039;===&lt;br /&gt;
[[File:Fern stem and root diagram.jpg|thumb|A Diagram showing the difference between the stem and the roots of a fern.]]&lt;br /&gt;
The stems of ferns are called “rhizomes” and are usually found underneath the fern, buried under some type of substrate, most commonly soils and mosses.[6] The rhizomes can extend either laterally or vertically and serves as the connection between the aboveground leaves and the underground roots.[6] In ferns there are two types of stems: long-creeping stems and short-creeping stems. Long-creeping stems have a longer length which allows the fronds to be more spaced out, while short-creeping stems are shorter and tend to have the fronds closer together.[6] &lt;br /&gt;
===&#039;&#039;&#039;Roots&#039;&#039;&#039;===&lt;br /&gt;
The roots of ferns are not entirely different from the roots of seed-producing plants and serve many of the same functions. Roots grow out of the rhizomes (stem) of the fern and extend deeper and further into the growth substrate.[6] Fern roots are thin and spread out in order to provide structural integrity to the fern. The roots are an important structure that assists with the uptake of water and various soil nutrients which are essential elements the fern needs to thrive.[6]     &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Distribution&#039;&#039;&#039;==&lt;br /&gt;
Today it is estimated that a total of 10,500 distinct species of ferns exist, but there could potentially be more than 15,000 species because new species are continuously being found in unexplored areas and some groups of ferns are poorly understood.[2] The diversity of ferns results in a wide distribution that spans multiple continents and biomes. Ferns can be found on every continent on earth except Antarctica. The greatest distribution of ferns is found in tropical areas, specifically tropical rain forests where its possible to find over 100 different species in just a few hectares.[2] Even though the greatest richness of ferns is found in the tropics that does not mean that is the only place they are found. Ferns can also be found in temperate and some artic environments.[2] Generally fern diversity and abundance decreases as one goes from the equator to the poles with the least number of ferns found in artic environments. &lt;br /&gt;
  &lt;br /&gt;
==&#039;&#039;&#039;Habitat&#039;&#039;&#039;==&lt;br /&gt;
Similar to its distribution, ferns can inhabit a wide range of habitats. While a majority of ferns prefer moist tropical forests,  they can also be found high in elevation on mountains, in deserts growing in/on rocks, open/abandoned fields, and even in wetlands and bodies of water.[2]  The most common habitat  for the majority of ferns are damp and warm areas, which makes tropical rain forests a prime habitat for a number of different fern species, but certain species have adapted to a variety of abiotic conditions, such as temperature, precipitation, sunlight, and substrate type. Ferns are often considered an important plant for succession because they are able to colonize such a wide range of different habitats.[2]  Some ferns have even been observed to be epiphytes and grow on other plant species, such as trees.[2] &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Reproduction&#039;&#039;&#039;==&lt;br /&gt;
[[File:Spores under leaf.jpg|thumb|Reproductive spores on the underside of a fern frond.]]&lt;br /&gt;
Unlike seed plants, ferns utilize tiny, microscopic spores that are contained in a specialized structure called the sporangia (plural: sporangium), typically on the underside of leaves.[2][3] The spores are dispersed mainly by wind and water and can be carried long distances from the parent plant.[3] Spores that happen to land in suitable habitats will crack and begin to germinate, growing into a gametophyte.[3] The gametophyte is a structure that houses the reproductive organs of the plant: the antheridium and the archegonium.[3] The sperm swims from the antheridium to the archegonium where the egg is located, although water is required for this to happen which stresses the need for a relatively moist environment.[3] Once the sperm finds the egg the fern begins its life and starts to grow back into the sporophyte.[3]&lt;br /&gt;
Some ferns can reproduce asexually through a reproductive strategy known as vegetative reproduction. Vegetative reproduction is essentially growing a new plant from a removed part of the parent plant.[7] In some ferns this is achieved through specialized bulbs that fall off the fern and begins to grow into a new plant, but this may also work with fragments from the parent plant such as leaves.[8] This reproductive method does not disperse the offspring very far from the parent.[2] &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Influence on Soil&#039;&#039;&#039;==&lt;br /&gt;
Ferns can have a significant effect on the soil they grow on and play an important role in the carbon concentration in the soil.[9] Being an understory plant ferns can catch falling organic matter for higher up in the canopy.[10] The material caught by the ferns resulted in an increase in decomposition rate because the ferns had more efficient decomposers than the soil did.[10] A study in 2019 looked at how using ferns for restoration efforts could affect soil carbon (C). The results of this study showed that the presence of ferns contributed anywhere between 54% and 61% of the total soil C, mostly from leaf litter and dead root material.[9] This study also showed ferns influenced nutrient retention by reducing the loss of nutrients, like nitrogen, and increasing soil carbon storage.[9]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
[1] Smith, A. R., K. M. Pryer, E. Schuettpelz, P. Korall, H. Schneider, and P. G. Wolf. 2006. A classification for extant ferns. Taxon 55:705–731.&lt;br /&gt;
[2] Wagner, Warren H. , Walker, Warren F. , Mickel, John T. , Yatskievych, George and Gifford, Ernest M.. &amp;quot;Fern&amp;quot;. Encyclopedia Britannica, 12 Jun. 2020, https://www.britannica.com/plant/fern.&lt;br /&gt;
[3] Hill, T. 2015. Ferns. Organismal Diversity, Ohio State University. https://u.osu.edu/eeob3320/2015/03/06/ferns/#:~:text=The%20%E2%80%9Cgreat%20fern%20radiation%E2%80%9D%20is,period%20(Bhattacharya%2C%202009).&amp;amp;text=During%20the%20Carboniferous%20period%2C%20giant,to%2012%20meters%20in%20height.&lt;br /&gt;
[4] Plant Evolution II: Ferns. Cortland University. http://cortland.edu/waldbauer-trail/11-plant%20evolution-II.html#:~:text=The%20ferns%20and%20their%20relatives,to%2066%20million%20years%20ago. &lt;br /&gt;
[5] Vasco, A., R. C. Moran, and B. A. Ambrose. 2013. The evolution, morphology, and development of fern leaves. Frontiers in Plant Science 4:1–16.&lt;br /&gt;
[6] Fern Structure. US Forest Service, United States Department of Agriculture. https://www.fs.fed.us/wildflowers/beauty/ferns/structure.shtml#:~:text=The%20leaves%20of%20ferns%20are,and%20petiole%20(leaf%20stalk).&amp;amp;text=The%20midrib%20is%20the%20main,pinnae%3B%20single%20leaflets%20are%20pinna. &lt;br /&gt;
[7] Britannica, The Editors of Encyclopaedia. &amp;quot;Vegetative reproduction&amp;quot;. Encyclopedia Britannica, 9 Aug. 2017, https://www.britannica.com/science/vegetative-reproduction. &lt;br /&gt;
[8] Fern Reproduction. US Forest Service, United States Department of Agriculture. https://www.fs.fed.us/wildflowers/beauty/ferns/reproduction.shtml&lt;br /&gt;
[9] Lyu, M., J. Xie, C. P. Giardina, M. A. Vadeboncoeur, X. Feng, M. Wang, L. Ukonmaanaho, T. C. Lin, Y. Kuzyakov, and Y. Yang. 2019. Understory ferns alter soil carbon chemistry and increase carbon storage during reforestation with native pine on previously degraded sites. Soil Biology and Biochemistry 132:80–92.&lt;br /&gt;
[10] Dearden, F. M., and D. A. Wardle. 2008. The potential for forest canopy litterfall interception by a dense fern understorey, and the consequences for litter decomposition. Oikos 117:83–92.&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
	<entry>
		<id>https://soil.evs.buffalo.edu/index.php?title=Fern&amp;diff=5807</id>
		<title>Fern</title>
		<link rel="alternate" type="text/html" href="https://soil.evs.buffalo.edu/index.php?title=Fern&amp;diff=5807"/>
		<updated>2021-04-27T04:09:17Z</updated>

		<summary type="html">&lt;p&gt;Ddietric: &lt;/p&gt;
&lt;hr /&gt;
&lt;div&gt;Ferns are a type of a vascular plant characterized by spores, complex leaves, and the lack of seeds and flowers.  Ferns belong to a class of plants known as Polypodiopsida, which is further divided into 4 extant subclasses; Equisetidae, Marattiidae, Ophioglossidae, and Polypodiidae.[1] Ferns are thought to have originated some 359 million years ago during the Devonian period, but it is possible that this group of vascular plants is even older.[2] There is a wide range of sizes that ferns can grow to, some of the smallest ferns can be 1-2 cm in height, while the some of the tallest ferns (tree ferns) can grow anywhere from 10-25 meters.[2]&lt;br /&gt;
[[Tree-fern.jpg|thumb|A group of tree ferns (Cyathea medullaris), one of the tallest species of ferns.]]&lt;br /&gt;
== &#039;&#039;&#039;Classification&#039;&#039;&#039; ==&lt;br /&gt;
Ferns are an ancient group of vascular plants that are considered to be one of the earliest plants to move onto land.[3] The oldest known ferns are found to be from the late Devonian period around 360 million years ago, but many modern fern families and species are thought to have started appearing in the Cretaceous period, 145-66 million years ago.[4] This diversification of fern families is referred to as the “great fern radiation”.[4] Today there are 4 living sub-classes ferns, but throughout their history there has been 4 sub-classes that have gone extinct. Below are descriptions of the 4 extent sub-classes:&lt;br /&gt;
*Equisetidae: This sub-class consists of vascular plants called horsetails. These are close relatives to true ferns and also reproduce via spores and characterized by a whorl of branch-like leaves.[1]&lt;br /&gt;
*Marattiidae: This sub-class separated from the other fern groups early on in their evolutionary history and is made up of about 100 species. These ferns are known for their extremely large leaves and fleshy rootstocks.[1] &lt;br /&gt;
*Ophioglossidae: This sub-class is not as diverse as the other sub-classes The members of this sub-group are known as the whisk ferns, grape ferns, adder&#039;s-tongues and moonworts.[1]&lt;br /&gt;
*Polypodiidae: these ferns are referred to as leptosporangiate ferns and are the largest of the 4 sub-classes with around 11,000 species. This is the most diverse sub-class of ferns and contains many of the wellknown ferns.[1]   &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Morphology&#039;&#039;&#039;==&lt;br /&gt;
&lt;br /&gt;
===&#039;&#039;&#039;Leaves&#039;&#039;&#039;===&lt;br /&gt;
[[File:fern leaf diagram.jpg|thumb|A Diagram showing the different parts of a fern leaf.]]&lt;br /&gt;
Ferns are an extremely diverse group, and this diversity results in a plethora of unique shapes and sizes. Even though there is a large degree of variability in the leaves of ferns, many ferns share some general morphological similarities.[5] The leaves of ferns are typically referred to as “fronds”.[6] Fronds consist of two parts; the stem (stalk) which is referred to as the “petiole” and the “leaf blade” which is the vegetative organs that extend laterally from the petiole.[5] The leaf blade is often separated into individual segments called “pinnae” which is made up of several leaflets known as “pinna”.[6] Despite the variation in leaf morphology, fern leaves play an important role in the growth, survival, and reproduction of the fern. Photosynthesis takes place in the leaves of the fern and is vital to the survival of the plant, but the leaves can also help to disperse spores for reproduction, house nitrogen-fixing bacteria, allow the fern to reproduce vegetatively, and collect falling nutrients/organic matter that fall from above the leaves.[5]  &lt;br /&gt;
===&#039;&#039;&#039;Stems&#039;&#039;&#039;===&lt;br /&gt;
[[File:Fern stem and root diagram.jpg|thumb|A Diagram showing the difference between the stem and the roots of a fern.]]&lt;br /&gt;
The stems of ferns are called “rhizomes” and are usually found underneath the fern, buried under some type of substrate, most commonly soils and mosses.[6] The rhizomes can extend either laterally or vertically and serves as the connection between the aboveground leaves and the underground roots.[6] In ferns there are two types of stems: long-creeping stems and short-creeping stems. Long-creeping stems have a longer length which allows the fronds to be more spaced out, while short-creeping stems are shorter and tend to have the fronds closer together.[6] &lt;br /&gt;
===&#039;&#039;&#039;Roots&#039;&#039;&#039;===&lt;br /&gt;
The roots of ferns are not entirely different from the roots of seed-producing plants and serve many of the same functions. Roots grow out of the rhizomes (stem) of the fern and extend deeper and further into the growth substrate.[6] Fern roots are thin and spread out in order to provide structural integrity to the fern. The roots are an important structure that assists with the uptake of water and various soil nutrients which are essential elements the fern needs to thrive.[6]     &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Distribution&#039;&#039;&#039;==&lt;br /&gt;
Today it is estimated that a total of 10,500 distinct species of ferns exist, but there could potentially be more than 15,000 species because new species are continuously being found in unexplored areas and some groups of ferns are poorly understood.[2] The diversity of ferns results in a wide distribution that spans multiple continents and biomes. Ferns can be found on every continent on earth except Antarctica. The greatest distribution of ferns is found in tropical areas, specifically tropical rain forests where its possible to find over 100 different species in just a few hectares.[2] Even though the greatest richness of ferns is found in the tropics that does not mean that is the only place they are found. Ferns can also be found in temperate and some artic environments.[2] Generally fern diversity and abundance decreases as one goes from the equator to the poles with the least number of ferns found in artic environments. &lt;br /&gt;
  &lt;br /&gt;
==&#039;&#039;&#039;Habitat&#039;&#039;&#039;==&lt;br /&gt;
Similar to its distribution, ferns can inhabit a wide range of habitats. While a majority of ferns prefer moist tropical forests,  they can also be found high in elevation on mountains, in deserts growing in/on rocks, open/abandoned fields, and even in wetlands and bodies of water.[2]  The most common habitat  for the majority of ferns are damp and warm areas, which makes tropical rain forests a prime habitat for a number of different fern species, but certain species have adapted to a variety of abiotic conditions, such as temperature, precipitation, sunlight, and substrate type. Ferns are often considered an important plant for succession because they are able to colonize such a wide range of different habitats.[2]  Some ferns have even been observed to be epiphytes and grow on other plant species, such as trees.[2] &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Reproduction&#039;&#039;&#039;==&lt;br /&gt;
Unlike seed plants, ferns utilize tiny, microscopic spores that are contained in a specialized structure called the sporangia (plural: sporangium), typically on the underside of leaves.[2][3] The spores are dispersed mainly by wind and water and can be carried long distances from the parent plant.[3] Spores that happen to land in suitable habitats will crack and begin to germinate, growing into a gametophyte.[3] The gametophyte is a structure that houses the reproductive organs of the plant: the antheridium and the archegonium.[3] The sperm swims from the antheridium to the archegonium where the egg is located, although water is required for this to happen which stresses the need for a relatively moist environment.[3] Once the sperm finds the egg the fern begins its life and starts to grow back into the sporophyte.[3]&lt;br /&gt;
[[File:Spores under leaf.jpg|thumb|Reproductive spores on the underside of a fern frond.]]&lt;br /&gt;
Some ferns can reproduce asexually through a reproductive strategy known as vegetative reproduction. Vegetative reproduction is essentially growing a new plant from a removed part of the parent plant.[7] In some ferns this is achieved through specialized bulbs that fall off the fern and begins to grow into a new plant, but this may also work with fragments from the parent plant such as leaves.[8] This reproductive method does not disperse the offspring very far from the parent.[2] &lt;br /&gt;
&lt;br /&gt;
==&#039;&#039;&#039;Influence on Soil&#039;&#039;&#039;==&lt;br /&gt;
Ferns can have a significant effect on the soil they grow on and play an important role in the carbon concentration in the soil.[9] Being an understory plant ferns can catch falling organic matter for higher up in the canopy.[10] The material caught by the ferns resulted in an increase in decomposition rate because the ferns had more efficient decomposers than the soil did.[10] A study in 2019 looked at how using ferns for restoration efforts could affect soil carbon (C). The results of this study showed that the presence of ferns contributed anywhere between 54% and 61% of the total soil C, mostly from leaf litter and dead root material.[9] This study also showed ferns influenced nutrient retention by reducing the loss of nutrients, like nitrogen, and increasing soil carbon storage.[9]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
[1] Smith, A. R., K. M. Pryer, E. Schuettpelz, P. Korall, H. Schneider, and P. G. Wolf. 2006. A classification for extant ferns. Taxon 55:705–731.&lt;br /&gt;
[2] Wagner, Warren H. , Walker, Warren F. , Mickel, John T. , Yatskievych, George and Gifford, Ernest M.. &amp;quot;Fern&amp;quot;. Encyclopedia Britannica, 12 Jun. 2020, https://www.britannica.com/plant/fern.&lt;br /&gt;
[3] Hill, T. 2015. Ferns. Organismal Diversity, Ohio State University. https://u.osu.edu/eeob3320/2015/03/06/ferns/#:~:text=The%20%E2%80%9Cgreat%20fern%20radiation%E2%80%9D%20is,period%20(Bhattacharya%2C%202009).&amp;amp;text=During%20the%20Carboniferous%20period%2C%20giant,to%2012%20meters%20in%20height.&lt;br /&gt;
[4] Plant Evolution II: Ferns. Cortland University. http://cortland.edu/waldbauer-trail/11-plant%20evolution-II.html#:~:text=The%20ferns%20and%20their%20relatives,to%2066%20million%20years%20ago. &lt;br /&gt;
[5] Vasco, A., R. C. Moran, and B. A. Ambrose. 2013. The evolution, morphology, and development of fern leaves. Frontiers in Plant Science 4:1–16.&lt;br /&gt;
[6] Fern Structure. US Forest Service, United States Department of Agriculture. https://www.fs.fed.us/wildflowers/beauty/ferns/structure.shtml#:~:text=The%20leaves%20of%20ferns%20are,and%20petiole%20(leaf%20stalk).&amp;amp;text=The%20midrib%20is%20the%20main,pinnae%3B%20single%20leaflets%20are%20pinna. &lt;br /&gt;
[7] Britannica, The Editors of Encyclopaedia. &amp;quot;Vegetative reproduction&amp;quot;. Encyclopedia Britannica, 9 Aug. 2017, https://www.britannica.com/science/vegetative-reproduction. &lt;br /&gt;
[8] Fern Reproduction. US Forest Service, United States Department of Agriculture. https://www.fs.fed.us/wildflowers/beauty/ferns/reproduction.shtml&lt;br /&gt;
[9] Lyu, M., J. Xie, C. P. Giardina, M. A. Vadeboncoeur, X. Feng, M. Wang, L. Ukonmaanaho, T. C. Lin, Y. Kuzyakov, and Y. Yang. 2019. Understory ferns alter soil carbon chemistry and increase carbon storage during reforestation with native pine on previously degraded sites. Soil Biology and Biochemistry 132:80–92.&lt;br /&gt;
[10] Dearden, F. M., and D. A. Wardle. 2008. The potential for forest canopy litterfall interception by a dense fern understorey, and the consequences for litter decomposition. Oikos 117:83–92.&lt;/div&gt;</summary>
		<author><name>Ddietric</name></author>
	</entry>
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