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Coccolithophore
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Coccolithophores (also called coccolithophorids) are single-celled algae, protists and phytoplankton belonging to the division haptophytes. They are distinguished by special calcium carbonate plates (or scales) of uncertain function called coccoliths (calcareous nannoplankton), which are important microfossils. Coccolithophores are almost exclusively marine and are found in large numbers throughout the surface euphotic zone of the ocean. An example of a globally-significant coccolithophore is Emiliania huxleyi.
The arrangement of coccolithophores are as spherical cells about 15-100 micrometres across, enclosed by calcareous plates, coccoliths, about 2-25 micrometres across.

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Encyclopedia
Coccolithophores (also called coccolithophorids) are single-celled algae, protists and phytoplankton belonging to the division haptophytes. They are distinguished by special calcium carbonate plates (or scales) of uncertain function called coccoliths (calcareous nannoplankton), which are important microfossils. Coccolithophores are almost exclusively marine and are found in large numbers throughout the surface euphotic zone of the ocean. An example of a globally-significant coccolithophore is Emiliania huxleyi.
The arrangement of coccolithophores are as spherical cells about 15-100 micrometres across, enclosed by calcareous plates, coccoliths, about 2-25 micrometres across. Coccolithophores that are alive today have two golden-brown shaded pigment marks in their cell with the nucleus located between them. The pigments are home to the chlorophyll which carry out photosynthesis. In order to obtain the sunlight needed for photosynthesis, coccolithophores live near the surface of the ocean. Although they have the capability to swim, coccolithophores generally float in the ocean currents. But, they may swim in order to keep a stable position within the water column to soak up sunlight and remain in a nutrient rich environment.
Due to their microscopic size and the broad distribution of many of their taxa, coccoliths have become very important as index fossils for solving various stratigraphic problems. Microfossils are sensitive indicators of changes in the temperature and salinity of the ocean and sea surface water. The quantitative analysis of calcareous nannoplankton assemblages is being employed to reveal such changes. They also produce alkenones, biomarkers of great utility in reconstructing ancient temperatures.
Coccolithophores have long been thought to respond to increased ocean acidity, caused by increasing levels, by becoming less calcified. Scientists were recently surprised to learn that in fact the opposite can happen in at least some circumstances, with the model species E. huxleyi becoming 40% heavier, and more abundant, in waters of higher CO2 content.
See also
External links
- - illustrated guide to Neogene coccolithophores and other nannofossils.
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