The Eocene–Oligocene transition: a review of marine and terrestrial proxy data, models and model–data comparisons
<p>The Eocene–Oligocene transition (EOT) was a climate shift from a largely ice-free greenhouse world to an icehouse climate, involving the first major glaciation of Antarctica and global cooling occurring <span class="inline-formula">∼34</span> million years ago (Ma) and...
Main Authors: | D. K. Hutchinson, H. K. Coxall, D. J. Lunt, M. Steinthorsdottir, A. M. de Boer, M. Baatsen, A. von der Heydt, M. Huber, A. T. Kennedy-Asser, L. Kunzmann, J.-B. Ladant, C. H. Lear, K. Moraweck, P. N. Pearson, E. Piga, M. J. Pound, U. Salzmann, H. D. Scher, W. P. Sijp, K. K. Śliwińska, P. A. Wilson, Z. Zhang |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2021-01-01
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Series: | Climate of the Past |
Online Access: | https://cp.copernicus.org/articles/17/269/2021/cp-17-269-2021.pdf |
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