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...

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Bibliographic Details
Main Authors: Bornemann, André, Norris, Richard D
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2007
Subjects:
BC
ODP
PC
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.688711
https://doi.org/10.1594/PANGAEA.688711