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A mechanism for brief glacial episodes in the Mesozoic greenhouse
Donnadieu Y., Dromart G., Godderis Y., Pucéat E., Brigaud B., Dera G., Dumas C., Olivier N.
Paleoceanography 26 (2011) PA3212 - http://hal.archives-ouvertes.fr/hal-00674790
Article in peer-reviewed journal
Sciences of the Universe/Earth Sciences
A mechanism for brief glacial episodes in the Mesozoic greenhouse
Yannick Donnadieu ( ) 1, 2, Gilles Dromart () 3, Yves Godderis () 4, Emmanuelle Pucéat () 5, Benjamin Brigaud () 6, Guillaume Dera () 1, 2, Christophe Dumas 1, 2, Nicolas Olivier () 3
1:  Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE)
http://www.lsce.ipsl.fr/
CNRS : UMR8212 – CEA : DSM/LSCE – Université de Versailles Saint-Quentin-en-Yvelines
LSCE-CEA-Orme des Merisiers (point courrier 129) F-91191 GIF-SUR-YVETTE CEDEX LSCE-Vallée Bât. 12, avenue de la Terrasse, F-91198 GIF-SUR-YVETTE CEDEX
France
2:  Institut Pierre-Simon-Laplace (IPSL)
http://www.ipsl.jussieu.fr/
CNRS : FR636 – Institut de recherche pour le développement [IRD] – CEA – CNES – INSU – Université Pierre et Marie Curie (UPMC) - Paris VI – Université de Versailles Saint-Quentin-en-Yvelines – Ecole normale supérieure de Paris - ENS Paris
4 Place Jussieu 75252 PARIS CEDEX 05
France
3:  Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE)
CNRS : UMR5276 – INSU – Université Claude Bernard - Lyon I – École Normale Supérieure - Lyon
France
4:  Laboratoire des Mécanismes et Transfert en Géologie (LMTG)
http://www.lmtg.obs-mip.fr/
CNRS : UMR5563 – Observatoire Midi-Pyrénées – Université Paul Sabatier [UPS] - Toulouse III – Institut de recherche pour le développement [IRD] : UMR154
14 avenue Edouard Belin 31400 Toulouse
France
5:  Biogéosciences
http://biogeosciences.u-bourgogne.fr/
CNRS : UMR6282 – Université de Bourgogne
6 Bvd Gabriel 21000 DIJON
France
6:  IDES (Université Paris-Sud XI)
CNRS : UMR8148
bâts. 504 & 509, 91405 Orsay cedex
France
The Mesozoic, perhaps the longest period of warmth during the Phanerozoic Earth history, has been repeatedly affected by short-lived cold interludes lasting about one million years. While the origin of these cold snaps has been classically attributed to a temporary atmospheric CO(2) drawdown, quantified mechanisms explaining these instabilities of the carbon cycle are still lacking. Based on a climate carbon cycle model, we show that the general demise of carbonate platforms accompanying these short-lived cold interludes is a powerful mechanism capable of generating a fast atmospheric CO2 decrease and a moderate sea level drop associated with ice sheet buildup. The temporary nature of the carbonate production decline explains the relative short time of these cold events but makes it possible to account for ice sheet waxing and waning.
English

Paleoceanography
Publisher American Geophysical Union (AGU)
ISSN 0883-8305 
international
2011-08-17
26
PA3212

CARBON-ISOTOPE STRATIGRAPHY – EARLY CRETACEOUS CARBON – ATMOSPHERIC CO2 – PARIS BASIN – ANTARCTIC GLACIATION – GEOCHEMICAL EVIDENCE – JURASSIC TRANSITION – SNOWBALL EARTH – ANOXIC EVENT – PLATFORM

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