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...
Published in: | Antarctic Science |
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Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
2023
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Online Access: | http://dx.doi.org/10.1017/s0954102023000159 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102023000159 |