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

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

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 inline-formula∼34 million years ago (Ma) and lasting inline-formula∼790inline-formulakyr. The change is marked by a global shift in deep-sea inline-formulaδ18O representing a combination of deep-ocean cooling and growth in land ice volume. At the same time, multiple independent proxies for ocean temperature indicate sea surface cooling, and major changes in global fauna and flora record a shift toward more cold-climate-adapted species. The two principal suggested explanations of this transition are a decline in atmospheric inline-formulaCO2 and changes to ocean gateways, while orbital forcing likely influenced the precise timing of the glaciation. Here we review and synthesise proxy evidence of palaeogeography, temperature, ice sheets, ocean circulation and inline-formulaCO2 change from the marine and terrestrial realms. Furthermore, we quantitatively compare proxy records of change to an ensemble of climate model simulations of temperature change across the EOT. The simulations compare three forcing mechanisms across the EOT: inline-formulaCO2 decrease, palaeogeographic changes and ice sheet growth. Our model ensemble results demonstrate the need for a global cooling mechanism beyond the imposition of an ice sheet or palaeogeographic changes. We find that inline-formulaCO2 forcing involving a large decrease in inline-formulaCO2 of ca. 40 % (inline-formula∼325inline-formulappm drop) provides the best fit to the available proxy evidence, with ice sheet and palaeogeographic changes playing a secondary role. While this large decrease is consistent with some inline-formulaCO2 proxy records (the extreme endmember ofpage270 decrease), the positive feedback mechanisms on ice growth are so strong that a modest inline-formulaCO2 decrease beyond a critical threshold for ice sheet initiation is well capable of triggering rapid ice sheet growth. Thus, the amplitude of inline-formulaCO2 decrease signalled by our data–model comparison should be considered an upper estimate and perhaps artificially large, not least because the current generation of climate models do not include dynamic ice sheets and in some cases may be under-sensitive to inline-formulaCO2 forcing. The model ensemble also cannot exclude the possibility that palaeogeographic changes could have triggered a reduction in inline-formulaCO2.



Hutchinson, David K. / Coxall, Helen K. / Lunt, Daniel J. / et al: The Eocene–Oligocene transition: a review of marine and terrestrial proxy data, models and model–data comparisons. 2021. Copernicus Publications.


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