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         Chalk is a variety of limestone composed mainly of calcium carbonate derived from the shells of tiny marine animals known as foraminifera and from the calcareous remains of marine algae known as coccoliths.  Chalk is usually white or light g
  Cretaceous: A Time of Chalk         Much chalk was deposited during the Cretaceous Period of geologic time.  It was a time of global high sea levels that began at the end of the Jurassic Period about 145 million years ago and the beginning of the P
       Coccoliths are the microscopic algae which form chalk.  They are made by one of the most important eukaryote phytoplankton.  These are single celled protists whose full name is coccolithophorids or coccolithophores.  The spherical skeleton of
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       During the Late Cretaceous, between 100 and 66 million years ago, Great Britain and much of Europe were submerged under a great sea.  The sea bottom was covered with white mud formed from fragments of coccoliths, the skeletons of tiny algae th
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