North Atlantic sea surface temperature evolution across the Eocene–Oligocene transition

Utrecht University, The Netherlands (1); Unviersity of Bergen, Norway (2) The Eocene–Oligocene Transition (EOT, ~34 Ma), is marked by the rapid development of semi-permanent Antarctic ice-sheet1. Foraminiferal stable oxygen isotopes (δ18O) as well as Mg/Ca and other indicators (e.g. ice-rafted debri...

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Bibliographic Details
Main Authors: Kocken, Ilja Japhir, van der Veen, Kasper, Müller, Inigo R., Meckler, Anna Nele, Ziegler, Martin
Format: Text
Language:English
Published: Deutsche Geologische Gesellschaft - Geologische Vereinigung e.V. (DGGV) 2020
Subjects:
Antarctic
Norway
Bergen
Rosenthal
Antarc*
Newfoundland
North Atlantic
Online Access:https://dx.doi.org/10.48380/dggv-50x0-6c15
https://www.dggv.de/publikationen/dggv-e-publikationen/publication/80.html

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