Articles | Volume 17, issue 1
Review article
 | Highlight paper
28 Jan 2021
Review article | Highlight paper |  | 28 Jan 2021

The Eocene–Oligocene transition: a review of marine and terrestrial proxy data, models and model–data comparisons

David K. Hutchinson, Helen K. Coxall, Daniel J. Lunt, Margret Steinthorsdottir, Agatha M. de Boer, Michiel Baatsen, Anna von der Heydt, Matthew Huber, Alan T. Kennedy-Asser, Lutz Kunzmann, Jean-Baptiste Ladant, Caroline H. Lear, Karolin Moraweck, Paul N. Pearson, Emanuela Piga, Matthew J. Pound, Ulrich Salzmann, Howie D. Scher, Willem P. Sijp, Kasia K. Śliwińska, Paul A. Wilson, and Zhongshi Zhang


Total article views: 12,269 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
8,532 3,573 164 12,269 467 159 188
  • HTML: 8,532
  • PDF: 3,573
  • XML: 164
  • Total: 12,269
  • Supplement: 467
  • BibTeX: 159
  • EndNote: 188
Views and downloads (calculated since 18 May 2020)
Cumulative views and downloads (calculated since 18 May 2020)

Viewed (geographical distribution)

Total article views: 12,269 (including HTML, PDF, and XML) Thereof 11,147 with geography defined and 1,122 with unknown origin.
Country # Views %
  • 1


Discussed (final revised paper)

Latest update: 21 Jun 2024
Short summary
The Eocene–Oligocene transition was a major climate cooling event from a largely ice-free world to the first major glaciation of Antarctica, approximately 34 million years ago. This paper reviews observed changes in temperature, CO2 and ice sheets from marine and land-based records at this time. We present a new model–data comparison of this transition and find that CO2-forced cooling provides the best explanation of the observed global temperature changes.