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....

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Auteurs principaux: 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
Format: article
Langue:EN
Publié: Nature Portfolio 2021
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Accès en ligne:https://doaj.org/article/594d1171932a423b92f83c1dde86ce34
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