Midlatitude Southern Hemisphere Temperature Change at the End of the Eocene Greenhouse Shortly Before Dawn of the Oligocene Icehouse

The Eocene‐Oligocene transition (EOT) marked the initiation of large‐scale Antarcticglaciation. This fundamental change in Cenozoic climate state is recorded in deep‐sea sediments by arapid benthic foraminiferalδ18O increase and appearance of ice‐rafted debris in the Southern Ocean.However, we know...

Full description

Bibliographic Details
Published in:Paleoceanography and Paleoclimatology
Main Authors: Haiblen, Anna, Opdyke, Bradley, Roberts, Andrew P., Heslop, David, Wilson, Paul A.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley-Blackwell Publishing, Inc.
Subjects:
Online Access:http://hdl.handle.net/1885/219038
https://doi.org/10.1029/2019PA003679
https://openresearch-repository.anu.edu.au/bitstream/1885/219038/3/01_Haiblen_Midlatitude_Southern_2019.pdf.jpg