Benthic foraminiferal and bulk sediment stable isotope records, and carbonate content records from the eastern equatorial Pacific, and a reconstruction of the calcite compensation depth, across the EO

The major Cenozoic shift from a shallow (~3‒4 km) to deep (~4.5 km) calcite compensation depth (CCD) occurred at the Eocene-Oligocene Transition (EOT; ~34 Ma), suggesting a strong relationship between calcium carbonate (CaCO3) cycling and Antarctic glaciation. To further investigate the linkages bet...

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Bibliographic Details
Main Authors: Taylor, Victoria E, Westerhold, Thomas, Bohaty, Steven M, Backman, Jan, Dunkley Jones, Tom, Egan, Katie, Edgar, Kirsty M, Lyle, Mitchell W, Pälike, Heiko, Röhl, Ursula, Zachos, James C, Wilson, Paul A
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2023
Subjects:
CCD
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.956848
https://doi.org/10.1594/PANGAEA.956848