Emiliania huxleyi: Difference between revisions
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Some possible explanations for the migration pattern could be decreasing pH near the equator due to ocean acidification and generally rising oceanwater temperature. [3] This migration will have effects on both the ecosystems they leave behind and the new ecosystems they settle into at the more northern/southern latitude destination. | Some possible explanations for the migration pattern could be decreasing pH near the equator due to ocean acidification and generally rising oceanwater temperature. [3] This migration will have effects on both the ecosystems they leave behind and the new ecosystems they settle into at the more northern/southern latitude destination. | ||
==Role in cloud formation== | Ehux is made up of unique plates that are called coccoliths. These coccoliths consist of calcium carbonate (Ca CO<sub>3</sub>). Therefore the formation of Ehux's coccoliths release CO<sub>2</sub>, acting as a carbon source. However they can also act as a carbon sink when they photosynthesize and take away CO<sub>2</sub>. Because of this, Ehux has an effect on the climate.<sup>[]</sup> | ||
==The E. huxleyi Virus (EhV)== | |||
===Role in cloud formation=== | |||
Revision as of 23:10, 3 May 2021
Emiliania huxleyi is a species of unicellular, eukaryotic phytoplankton, (also known as a coccolithophore), and is found in nearly all oceanic ecosystems outside of polar regions. [1] Emiliania huxleyi is the most common coccolithophore. [4] Named after Thomas Henry Huxley, Emiliania huxleyi, (also abbreviated Ehux) plays an important role in all ecosystems in which it is found.
Classification
Domain: Eukaryota
(unranked): Haptophyta
Class: Prymnesiophyceae
Order: Isochrysidales
Family: Noelaerhabdaceae
Genus: Emiliania
Species: E. huxleyi
Scientific interest in Ehux
Emiliania huxleyi is tremendously successful at converting inorganic carbon into products used in photosynthesis and biomineralization. [2] E. huxleyi, like many other phytoplankton, is very important to the ecosystems it inhabits. Blooms of Ehux can be seen as large turquoise patches in the water through satellite imagery, covering hundreds of thousands of square meters of ocean. [2] A study of E. huxleyi populations in 2014 discovered a poleward migration path by the phytoplankton. [1] This indicates that, over time, conditions near the poles have become more favorable for Ehux survival.
Some possible explanations for the migration pattern could be decreasing pH near the equator due to ocean acidification and generally rising oceanwater temperature. [3] This migration will have effects on both the ecosystems they leave behind and the new ecosystems they settle into at the more northern/southern latitude destination.
Ehux is made up of unique plates that are called coccoliths. These coccoliths consist of calcium carbonate (Ca CO3). Therefore the formation of Ehux's coccoliths release CO2, acting as a carbon source. However they can also act as a carbon sink when they photosynthesize and take away CO2. Because of this, Ehux has an effect on the climate.[]
The E. huxleyi Virus (EhV)
Role in cloud formation
References
[1] Winter, Amos, et al. “Poleward Expansion of the Coccolithophore Emiliania Huxleyi.” Journal of Plankton Research, vol. 36, no. 2, 2013, pp. 316–325., doi:10.1093/plankt/fbt110.
[2] Read, Betsy A., et al. “Pan Genome of the Phytoplankton Emiliania Underpins Its Global Distribution.” Nature, vol. 499, no. 7457, Dec. 2013, pp. 209–213., doi:10.1038/nature12221.
[3] Gerald Langer, G. Nehrke, Ian Probert, J. Ly, P. Ziveri. Strain-specific responses of Emiliania huxleyi to changing seawater carbonate chemistry . Biogeosciences, European Geosciences Union, 2009, 6 (11), pp.2637-2646. <10.5194/bg-6-2637-2009>. <hal-01258266>
[4] Hay, W.W.; Mohler, H.P.; Roth, P.H.; Schmidt, R.R.; Boudreaux, J.E. (1967), "Calcareous nannoplankton zonation of the Cenozoic of the Gulf Coast and Caribbean-Antillean area, and transoceanic correlation", Transactions of the Gulf Coast Association of Geological Societies, 17: 428–480.