Transient Deep Ocean Cooling in the Eastern Equatorial Pacific Ocean at the Eocene-Oligocene Transition

At the Eocene-Oligocene Transition (EOT), approximately 34 million years ago, Earth abruptly transitioned to a climate state sufficiently cool for Antarctica to sustain large ice sheets for the first time in tens to hundreds of millions of years. Oxygen isotope records from deep-sea benthic foramini...

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Bibliographic Details
Published in:Paleoceanography and Paleoclimatology
Main Authors: Taylor, Victoria Emma, Wilson, P.A., Bohaty, S.M., Meckler, Anna Nele
Format: Article in Journal/Newspaper
Language:English
Published: AGU 2023
Subjects:
Online Access:https://hdl.handle.net/11250/3108964
https://doi.org/10.1029/2023PA004650