Middle Eocene greenhouse warming facilitated by diminished weathering feedback

Silicate rock weathering represents a negative feedback mechanism that regulates atmospheric CO2 levels on geological timescales. Here, the authors show that a diminished silicate weathering feedback may have set the stage for greenhouse warming and ocean acidification during the Middle Eocene, ~40...

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Autores principales:	Robin van der Ploeg, David Selby, Margot J. Cramwinckel, Yang Li, Steven M. Bohaty, Jack J. Middelburg, Appy Sluijs
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2018
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/7766b14b17574352ae11759b896d0d86
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id	oai:doaj.org-article:7766b14b17574352ae11759b896d0d86
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spelling	oai:doaj.org-article:7766b14b17574352ae11759b896d0d862021-12-02T14:38:52ZMiddle Eocene greenhouse warming facilitated by diminished weathering feedback10.1038/s41467-018-05104-92041-1723https://doaj.org/article/7766b14b17574352ae11759b896d0d862018-07-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-05104-9https://doaj.org/toc/2041-1723Silicate rock weathering represents a negative feedback mechanism that regulates atmospheric CO2 levels on geological timescales. Here, the authors show that a diminished silicate weathering feedback may have set the stage for greenhouse warming and ocean acidification during the Middle Eocene, ~40 million years ago.Robin van der PloegDavid SelbyMargot J. CramwinckelYang LiSteven M. BohatyJack J. MiddelburgAppy SluijsNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-10 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Robin van der Ploeg David Selby Margot J. Cramwinckel Yang Li Steven M. Bohaty Jack J. Middelburg Appy Sluijs Middle Eocene greenhouse warming facilitated by diminished weathering feedback
description	Silicate rock weathering represents a negative feedback mechanism that regulates atmospheric CO2 levels on geological timescales. Here, the authors show that a diminished silicate weathering feedback may have set the stage for greenhouse warming and ocean acidification during the Middle Eocene, ~40 million years ago.
format	article
author	Robin van der Ploeg David Selby Margot J. Cramwinckel Yang Li Steven M. Bohaty Jack J. Middelburg Appy Sluijs
author_facet	Robin van der Ploeg David Selby Margot J. Cramwinckel Yang Li Steven M. Bohaty Jack J. Middelburg Appy Sluijs
author_sort	Robin van der Ploeg
title	Middle Eocene greenhouse warming facilitated by diminished weathering feedback
title_short	Middle Eocene greenhouse warming facilitated by diminished weathering feedback
title_full	Middle Eocene greenhouse warming facilitated by diminished weathering feedback
title_fullStr	Middle Eocene greenhouse warming facilitated by diminished weathering feedback
title_full_unstemmed	Middle Eocene greenhouse warming facilitated by diminished weathering feedback
title_sort	middle eocene greenhouse warming facilitated by diminished weathering feedback
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/7766b14b17574352ae11759b896d0d86
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_version_	1718390842794704896

Middle Eocene greenhouse warming facilitated by diminished weathering feedback

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