Massive methane fluxing from magma–sediment interaction in the end-Triassic Central Atlantic Magmatic Province

Global climate changes triggered by massive output of greenhouse gases led to mass extinctions in Earth’s past. Here, the authors show that widespread release of methane at the time of the end-Triassic mass extinction was caused by interaction of a Large Igneous Province with sedimentary host-rocks....

Descripción completa

Guardado en:

Detalles Bibliográficos
Autores principales:	Manfredo Capriolo, Andrea Marzoli, László E. Aradi, Michael R. Ackerson, Omar Bartoli, Sara Callegaro, Jacopo Dal Corso, Marcia Ernesto, Eleonora M. Gouvêa Vasconcellos, Angelo De Min, Robert J. Newton, Csaba Szabó
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2021
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/594d1171932a423b92f83c1dde86ce34
Etiquetas:	Agregar Etiqueta Sin Etiquetas, Sea el primero en etiquetar este registro!

id	oai:doaj.org-article:594d1171932a423b92f83c1dde86ce34
record_format	dspace
spelling	oai:doaj.org-article:594d1171932a423b92f83c1dde86ce342021-12-02T17:26:56ZMassive methane fluxing from magma–sediment interaction in the end-Triassic Central Atlantic Magmatic Province10.1038/s41467-021-25510-w2041-1723https://doaj.org/article/594d1171932a423b92f83c1dde86ce342021-09-01T00:00:00Zhttps://doi.org/10.1038/s41467-021-25510-whttps://doaj.org/toc/2041-1723Global climate changes triggered by massive output of greenhouse gases led to mass extinctions in Earth’s past. Here, the authors show that widespread release of methane at the time of the end-Triassic mass extinction was caused by interaction of a Large Igneous Province with sedimentary host-rocks.Manfredo CaprioloAndrea MarzoliLászló E. AradiMichael R. AckersonOmar BartoliSara CallegaroJacopo Dal CorsoMarcia ErnestoEleonora M. Gouvêa VasconcellosAngelo De MinRobert J. NewtonCsaba SzabóNature PortfolioarticleScienceQENNature Communications, Vol 12, Iss 1, Pp 1-9 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Manfredo Capriolo Andrea Marzoli László E. Aradi Michael R. Ackerson Omar Bartoli Sara Callegaro Jacopo Dal Corso Marcia Ernesto Eleonora M. Gouvêa Vasconcellos Angelo De Min Robert J. Newton Csaba Szabó Massive methane fluxing from magma–sediment interaction in the end-Triassic Central Atlantic Magmatic Province
description	Global climate changes triggered by massive output of greenhouse gases led to mass extinctions in Earth’s past. Here, the authors show that widespread release of methane at the time of the end-Triassic mass extinction was caused by interaction of a Large Igneous Province with sedimentary host-rocks.
format	article
author	Manfredo Capriolo Andrea Marzoli László E. Aradi Michael R. Ackerson Omar Bartoli Sara Callegaro Jacopo Dal Corso Marcia Ernesto Eleonora M. Gouvêa Vasconcellos Angelo De Min Robert J. Newton Csaba Szabó
author_facet	Manfredo Capriolo Andrea Marzoli László E. Aradi Michael R. Ackerson Omar Bartoli Sara Callegaro Jacopo Dal Corso Marcia Ernesto Eleonora M. Gouvêa Vasconcellos Angelo De Min Robert J. Newton Csaba Szabó
author_sort	Manfredo Capriolo
title	Massive methane fluxing from magma–sediment interaction in the end-Triassic Central Atlantic Magmatic Province
title_short	Massive methane fluxing from magma–sediment interaction in the end-Triassic Central Atlantic Magmatic Province
title_full	Massive methane fluxing from magma–sediment interaction in the end-Triassic Central Atlantic Magmatic Province
title_fullStr	Massive methane fluxing from magma–sediment interaction in the end-Triassic Central Atlantic Magmatic Province
title_full_unstemmed	Massive methane fluxing from magma–sediment interaction in the end-Triassic Central Atlantic Magmatic Province
title_sort	massive methane fluxing from magma–sediment interaction in the end-triassic central atlantic magmatic province
publisher	Nature Portfolio
publishDate	2021
url	https://doaj.org/article/594d1171932a423b92f83c1dde86ce34
work_keys_str_mv	AT manfredocapriolo massivemethanefluxingfrommagmasedimentinteractionintheendtriassiccentralatlanticmagmaticprovince AT andreamarzoli massivemethanefluxingfrommagmasedimentinteractionintheendtriassiccentralatlanticmagmaticprovince AT laszloearadi massivemethanefluxingfrommagmasedimentinteractionintheendtriassiccentralatlanticmagmaticprovince AT michaelrackerson massivemethanefluxingfrommagmasedimentinteractionintheendtriassiccentralatlanticmagmaticprovince AT omarbartoli massivemethanefluxingfrommagmasedimentinteractionintheendtriassiccentralatlanticmagmaticprovince AT saracallegaro massivemethanefluxingfrommagmasedimentinteractionintheendtriassiccentralatlanticmagmaticprovince AT jacopodalcorso massivemethanefluxingfrommagmasedimentinteractionintheendtriassiccentralatlanticmagmaticprovince AT marciaernesto massivemethanefluxingfrommagmasedimentinteractionintheendtriassiccentralatlanticmagmaticprovince AT eleonoramgouveavasconcellos massivemethanefluxingfrommagmasedimentinteractionintheendtriassiccentralatlanticmagmaticprovince AT angelodemin massivemethanefluxingfrommagmasedimentinteractionintheendtriassiccentralatlanticmagmaticprovince AT robertjnewton massivemethanefluxingfrommagmasedimentinteractionintheendtriassiccentralatlanticmagmaticprovince AT csabaszabo massivemethanefluxingfrommagmasedimentinteractionintheendtriassiccentralatlanticmagmaticprovince
_version_	1718380789531410432

Massive methane fluxing from magma–sediment interaction in the end-Triassic Central Atlantic Magmatic Province

Ejemplares similares