Microstructural and geochemical perspectives on planktic foraminiferal preservation: “Glassy” versus “Frosty”

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Microstructural and geochemical perspectives on planktic foraminiferal preservation: Glassy versus Frosty

[1] In recent years it has become apparent that the ‘‘cool tropic paradox’’ of Paleogene and Cretaceous ‘‘greenhouse’’ climates arises because of the diagenetic alteration of tropical planktic foraminiferal calcite near the seafloor, yielding artificially high dO values. Because the Mg/Ca compositions of foraminiferal and inorganic calcite are thought to be quite different, Mg/Ca measurements s...

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ژورنال

عنوان ژورنال: Geochemistry, Geophysics, Geosystems

سال: 2006

ISSN: 1525-2027

DOI: 10.1029/2006gc001291