Kick-starting ancient warming

Nisbet, EG, Jones, SM, Maclennan, J, Eagles, G, Moed, J, Warwick, N, Bekki, S, Braesicke, P, Pyle, JA and Fowler, CMR ;

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graeme.eagles [ at ] awi.de

Abstract

Rapid global warming marked the boundary between the Palaeocene and Eocene periods 55.6 million years ago, but how the temperature rise was initiated remains elusive. A catastrophic release of greenhouse gases from the Kilda basin could have served as a trigger.

Item Type

Article

Authors

Nisbet, EG, Jones, SM, Maclennan, J, Eagles, G, Moed, J, Warwick, N, Bekki, S, Braesicke, P, Pyle, JA and Fowler, CMR ;

Divisions

AWI Organizations > Geosciences > Geophysics

Primary Division

Organizations > AWI Organizations > Geosciences > Geophysics

Programs

Basic Research > Helmholtz Independent Research

Primary Topic

Helmholtz Programs > Basic Research > Helmholtz Independent Research

Publication Status

Published

Eprint ID

33240

DOI https://www.doi.org/10.1038/ngeo454

Cite as

Nisbet, E. , Jones, S. , Maclennan, J. , Eagles, G. , Moed, J. , Warwick, N. , Bekki, S. , Braesicke, P. , Pyle, J. and Fowler, C. (2009): Kick-starting ancient warming , Nature Geoscience, 2 (3), pp. 156-159 . doi: https://www.doi.org/10.1038/ngeo454

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Cite this document as:

hdl:10013/epic.41728.d001

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