Elevated CO2 degassing rates prevented the return of Snowball Earth during the Phanerozoic

Despite dramatic changes in carbon sinks, severe Snowball Earth glaciations have not occurred since the Cryogenian. Here, via the measurement of global subduction zone lengths and carbon cycle modelling, the authors show that a two fold increase in volcanic CO2 input likely thwarted global glaciatio...

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Autores principales:	Benjamin J. W. Mills, Christopher R. Scotese, Nicholas G. Walding, Graham A. Shields, Timothy M. Lenton
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2017
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/dedbbb78a8da4ba2a715a399d1335d4b
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spelling	oai:doaj.org-article:dedbbb78a8da4ba2a715a399d1335d4b2021-12-02T14:42:17ZElevated CO2 degassing rates prevented the return of Snowball Earth during the Phanerozoic10.1038/s41467-017-01456-w2041-1723https://doaj.org/article/dedbbb78a8da4ba2a715a399d1335d4b2017-10-01T00:00:00Zhttps://doi.org/10.1038/s41467-017-01456-whttps://doaj.org/toc/2041-1723Despite dramatic changes in carbon sinks, severe Snowball Earth glaciations have not occurred since the Cryogenian. Here, via the measurement of global subduction zone lengths and carbon cycle modelling, the authors show that a two fold increase in volcanic CO2 input likely thwarted global glaciation.Benjamin J. W. MillsChristopher R. ScoteseNicholas G. WaldingGraham A. ShieldsTimothy M. LentonNature PortfolioarticleScienceQENNature Communications, Vol 8, Iss 1, Pp 1-7 (2017)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Benjamin J. W. Mills Christopher R. Scotese Nicholas G. Walding Graham A. Shields Timothy M. Lenton Elevated CO2 degassing rates prevented the return of Snowball Earth during the Phanerozoic
description	Despite dramatic changes in carbon sinks, severe Snowball Earth glaciations have not occurred since the Cryogenian. Here, via the measurement of global subduction zone lengths and carbon cycle modelling, the authors show that a two fold increase in volcanic CO2 input likely thwarted global glaciation.
format	article
author	Benjamin J. W. Mills Christopher R. Scotese Nicholas G. Walding Graham A. Shields Timothy M. Lenton
author_facet	Benjamin J. W. Mills Christopher R. Scotese Nicholas G. Walding Graham A. Shields Timothy M. Lenton
author_sort	Benjamin J. W. Mills
title	Elevated CO2 degassing rates prevented the return of Snowball Earth during the Phanerozoic
title_short	Elevated CO2 degassing rates prevented the return of Snowball Earth during the Phanerozoic
title_full	Elevated CO2 degassing rates prevented the return of Snowball Earth during the Phanerozoic
title_fullStr	Elevated CO2 degassing rates prevented the return of Snowball Earth during the Phanerozoic
title_full_unstemmed	Elevated CO2 degassing rates prevented the return of Snowball Earth during the Phanerozoic
title_sort	elevated co2 degassing rates prevented the return of snowball earth during the phanerozoic
publisher	Nature Portfolio
publishDate	2017
url	https://doaj.org/article/dedbbb78a8da4ba2a715a399d1335d4b
work_keys_str_mv	AT benjaminjwmills elevatedco2degassingratespreventedthereturnofsnowballearthduringthephanerozoic AT christopherrscotese elevatedco2degassingratespreventedthereturnofsnowballearthduringthephanerozoic AT nicholasgwalding elevatedco2degassingratespreventedthereturnofsnowballearthduringthephanerozoic AT grahamashields elevatedco2degassingratespreventedthereturnofsnowballearthduringthephanerozoic AT timothymlenton elevatedco2degassingratespreventedthereturnofsnowballearthduringthephanerozoic
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Elevated CO2 degassing rates prevented the return of Snowball Earth during the Phanerozoic

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