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coccolithophorid

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coccolithophorid

Microscopic, planktonic marine alga, which secretes a calcite shell. The shells (coccoliths) of coccolithophores are a major component of deep sea ooze. Coccolithophores were particularly abundant during the late Cretaceous period and their remains form the northern European chalk deposits, such as the white cliffs of Dover.



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An international research team led by Ulf Riebesell of Germany's Alfred Wegener Institite for Polar and Marine Research found that under the sort of acidic conditions expected in the upper levels of many oceans by century's end, coccolithophorid shell growth was as much as 83 percent slower and marked by malformations.
 
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