Size-related stable isotope changes in Late Cretaceous and Recent planktic foraminifera from the western tropical Atlantic
The paleoecology of Cretaceous planktic foraminifera during the Late Cenomanian to Coniacian period (~95-86 Ma) remains controversial since much of the tropical marine record is preserved as chalk and limestone with uncertain geochemical overprints. Here we present delta13C and delta18O data from si...
Main Authors: | , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2007
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.688711 https://doi.org/10.1594/PANGAEA.688711 |