k Coccolithophore, SEM Coccolithophore. Coloured scanning electron micrograph SEM of Emiliana huxleyi. This small algal organism is a calcareous phytoplankton and is surrounded by a skeleton coccosphere of calcium carbonate plates coccoliths. When the organism dies, the plates separate and sink to the ocean floor. Coccolithophores are of particular interest to those studying global climate change because as ocean acidity increases, their coccoliths may become even more important as a carbon sink absorb carbon dioxide. Individual plates have been found in vast numbers and can make up the major component of a particular rock, such as the chalk of England. E. huxleyi an important part of the planktonic base of a large proportion of marine food webs. Magnification x15000 when printed at 10 centimetres wide. Specimen courtesy of Mike Allen, Plymouth Marine Laboratory. Stock Photo - Afloimages
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Coccolithophore, SEM Coccolithophore. Coloured scanning electron micrograph  SEM  of Emiliana huxleyi. This small algal organism is a calcareous phytoplankton and is surrounded by a skeleton  coccosphere  of calcium carbonate plates  coccoliths . When the organism dies, the plates separate and sink to the ocean floor. Coccolithophores are of particular interest to those studying global climate change because as ocean acidity increases, their coccoliths may become even more important as a carbon sink  absorb carbon dioxide . Individual plates have been found in vast numbers and can make up the major component of a particular rock, such as the chalk of England. E. huxleyi an important part of the planktonic base of a large proportion of marine food webs. Magnification: x15000 when printed at 10 centimetres wide. Specimen courtesy of Mike Allen, Plymouth Marine Laboratory.
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Coccolithophore, SEM

Coccolithophore. Coloured scanning electron micrograph (SEM) of Emiliana huxleyi. This small algal organism is a calcareous phytoplankton and is surrounded by a skeleton (coccosphere) of calcium carbonate plates (coccoliths). When the organism dies, the plates separate and sink to the ocean floor. Coccolithophores are of particular interest to those studying global climate change because as ocean acidity increases, their coccoliths may become even more important as a carbon sink (absorb carbon dioxide). Individual plates have been found in vast numbers and can make up the major component of a particular rock, such as the chalk of England. E. huxleyi an important part of the planktonic base of a large proportion of marine food webs. Magnification: x15000 when printed at 10 centimetres wide. Specimen courtesy of Mike Allen, Plymouth Marine Laboratory.

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