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, V.E., Wilson, Paul, Bohaty, S.M., Meckler, A.N.
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access:https://eprints.soton.ac.uk/482503/
https://eprints.soton.ac.uk/482503/1/Paleoceanog_and_Paleoclimatol_2023_Taylor_Transient_Deep_Ocean_Cooling_in_the_Eastern_Equatorial_Pacific_Ocean_at_the.pdf