Eocene to Oligocene cooling and ice growth based on the geochemistry of interglacial mudstones from the East Antarctic continental shelf

Abstract The Eocene-Oligocene Transition at c. 34 million years ago (Ma) marked the global change from greenhouse to icehouse and the establishment of the East Antarctic Ice Sheet (EAIS). How the ice-sheet behaviour changed during interglacials across this climate transition is poorly understood. We...

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Bibliographic Details
Published in:Antarctic Science
Main Authors: Light, Jennifer J., Passchier, Sandra
Other Authors: National Science Foundation
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2023
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102023000159
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102023000159