Did high Neo-Tethys subduction rates contribute to early Cenozoic warming?

Did high Neo-Tethys subduction rates contribute to early Cenozoic warming?

The 58–51 Ma interval was characterized by a long-term increase of global temperatures (+4 to +6 °C) up to the Early Eocene Climate Optimum (EECO, 52.9–50.7 Ma), the warmest interval of the Cenozoic. It was recently suggested that sustained high atmospheric <i>p</i>CO<sub>2</sub...

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Bibliographic Details
Main Authors:	G. Hoareau, B. Bomou, D. J. J. van Hinsbergen, N. Carry, D. Marquer, Y. Donnadieu, G. Le Hir, B. Vrielynck, A.-V. Walter-Simonnet
Format:	Article
Language:	English
Published:	Copernicus Publications 2015-12-01
Series:	Climate of the Past
Online Access:	http://www.clim-past.net/11/1751/2015/cp-11-1751-2015.pdf

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