Deep CO2 in the end-Triassic Central Atlantic Magmatic Province

Many major mass extinction events have been associated with large volcanic eruption events, with the argument that large volumes of volcanic degassing could trigger past global climate changes. Here, the authors find that during the end-Triassic extinction event volcanic pulses emitted large amounts...

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Autores principales:	Manfredo Capriolo, Andrea Marzoli, László E. Aradi, Sara Callegaro, Jacopo Dal Corso, Robert J. Newton, Benjamin J. W. Mills, Paul B. Wignall, Omar Bartoli, Don R. Baker, Nasrrddine Youbi, Laurent Remusat, Richard Spiess, Csaba Szabó
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2020
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/c5c978c3b9f2479b8407bcfd7d2a9024
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spelling	oai:doaj.org-article:c5c978c3b9f2479b8407bcfd7d2a90242021-12-02T14:41:26ZDeep CO2 in the end-Triassic Central Atlantic Magmatic Province10.1038/s41467-020-15325-62041-1723https://doaj.org/article/c5c978c3b9f2479b8407bcfd7d2a90242020-04-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-15325-6https://doaj.org/toc/2041-1723Many major mass extinction events have been associated with large volcanic eruption events, with the argument that large volumes of volcanic degassing could trigger past global climate changes. Here, the authors find that during the end-Triassic extinction event volcanic pulses emitted large amounts of CO2 comparable to projected anthropogenic emissions for the 21st century in the future 2 °C warming scenario.Manfredo CaprioloAndrea MarzoliLászló E. AradiSara CallegaroJacopo Dal CorsoRobert J. NewtonBenjamin J. W. MillsPaul B. WignallOmar BartoliDon R. BakerNasrrddine YoubiLaurent RemusatRichard SpiessCsaba SzabóNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-11 (2020)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Manfredo Capriolo Andrea Marzoli László E. Aradi Sara Callegaro Jacopo Dal Corso Robert J. Newton Benjamin J. W. Mills Paul B. Wignall Omar Bartoli Don R. Baker Nasrrddine Youbi Laurent Remusat Richard Spiess Csaba Szabó Deep CO2 in the end-Triassic Central Atlantic Magmatic Province
description	Many major mass extinction events have been associated with large volcanic eruption events, with the argument that large volumes of volcanic degassing could trigger past global climate changes. Here, the authors find that during the end-Triassic extinction event volcanic pulses emitted large amounts of CO2 comparable to projected anthropogenic emissions for the 21st century in the future 2 °C warming scenario.
format	article
author	Manfredo Capriolo Andrea Marzoli László E. Aradi Sara Callegaro Jacopo Dal Corso Robert J. Newton Benjamin J. W. Mills Paul B. Wignall Omar Bartoli Don R. Baker Nasrrddine Youbi Laurent Remusat Richard Spiess Csaba Szabó
author_facet	Manfredo Capriolo Andrea Marzoli László E. Aradi Sara Callegaro Jacopo Dal Corso Robert J. Newton Benjamin J. W. Mills Paul B. Wignall Omar Bartoli Don R. Baker Nasrrddine Youbi Laurent Remusat Richard Spiess Csaba Szabó
author_sort	Manfredo Capriolo
title	Deep CO2 in the end-Triassic Central Atlantic Magmatic Province
title_short	Deep CO2 in the end-Triassic Central Atlantic Magmatic Province
title_full	Deep CO2 in the end-Triassic Central Atlantic Magmatic Province
title_fullStr	Deep CO2 in the end-Triassic Central Atlantic Magmatic Province
title_full_unstemmed	Deep CO2 in the end-Triassic Central Atlantic Magmatic Province
title_sort	deep co2 in the end-triassic central atlantic magmatic province
publisher	Nature Portfolio
publishDate	2020
url	https://doaj.org/article/c5c978c3b9f2479b8407bcfd7d2a9024
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Deep CO2 in the end-Triassic Central Atlantic Magmatic Province

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