Sea level fall during glaciation stabilized atmospheric CO2 by enhanced volcanic degassing

Ice core data show a breakdown in the long-term temperature-atmospheric CO2 correlation during interglacial-glacial transitions. Here, via a novel modelling approach, the authors reveal marine volcanism, triggered by a fall in sea level, as a likely mechanism for the observed delayed decline in atmo...

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Autores principales:	Jörg Hasenclever, Gregor Knorr, Lars H. Rüpke, Peter Köhler, Jason Morgan, Kristin Garofalo, Stephen Barker, Gerrit Lohmann, Ian R. Hall
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2017
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/bf7003cebdce408087e07283c7e43be9
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id	oai:doaj.org-article:bf7003cebdce408087e07283c7e43be9
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spelling	oai:doaj.org-article:bf7003cebdce408087e07283c7e43be92021-12-02T17:06:00ZSea level fall during glaciation stabilized atmospheric CO2 by enhanced volcanic degassing10.1038/ncomms158672041-1723https://doaj.org/article/bf7003cebdce408087e07283c7e43be92017-07-01T00:00:00Zhttps://doi.org/10.1038/ncomms15867https://doaj.org/toc/2041-1723Ice core data show a breakdown in the long-term temperature-atmospheric CO2 correlation during interglacial-glacial transitions. Here, via a novel modelling approach, the authors reveal marine volcanism, triggered by a fall in sea level, as a likely mechanism for the observed delayed decline in atmospheric CO2.Jörg HasencleverGregor KnorrLars H. RüpkePeter KöhlerJason MorganKristin GarofaloStephen BarkerGerrit LohmannIan R. HallNature PortfolioarticleScienceQENNature Communications, Vol 8, Iss 1, Pp 1-11 (2017)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Jörg Hasenclever Gregor Knorr Lars H. Rüpke Peter Köhler Jason Morgan Kristin Garofalo Stephen Barker Gerrit Lohmann Ian R. Hall Sea level fall during glaciation stabilized atmospheric CO2 by enhanced volcanic degassing
description	Ice core data show a breakdown in the long-term temperature-atmospheric CO2 correlation during interglacial-glacial transitions. Here, via a novel modelling approach, the authors reveal marine volcanism, triggered by a fall in sea level, as a likely mechanism for the observed delayed decline in atmospheric CO2.
format	article
author	Jörg Hasenclever Gregor Knorr Lars H. Rüpke Peter Köhler Jason Morgan Kristin Garofalo Stephen Barker Gerrit Lohmann Ian R. Hall
author_facet	Jörg Hasenclever Gregor Knorr Lars H. Rüpke Peter Köhler Jason Morgan Kristin Garofalo Stephen Barker Gerrit Lohmann Ian R. Hall
author_sort	Jörg Hasenclever
title	Sea level fall during glaciation stabilized atmospheric CO2 by enhanced volcanic degassing
title_short	Sea level fall during glaciation stabilized atmospheric CO2 by enhanced volcanic degassing
title_full	Sea level fall during glaciation stabilized atmospheric CO2 by enhanced volcanic degassing
title_fullStr	Sea level fall during glaciation stabilized atmospheric CO2 by enhanced volcanic degassing
title_full_unstemmed	Sea level fall during glaciation stabilized atmospheric CO2 by enhanced volcanic degassing
title_sort	sea level fall during glaciation stabilized atmospheric co2 by enhanced volcanic degassing
publisher	Nature Portfolio
publishDate	2017
url	https://doaj.org/article/bf7003cebdce408087e07283c7e43be9
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Sea level fall during glaciation stabilized atmospheric CO2 by enhanced volcanic degassing

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