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

Autor Manfredo Capriolo
Autores 12. Capriolo, M., Marzoli, A., Aradi, L.E., Ackerson, M.R., Bartoli, O., Callegaro, S., Dal Corso, J., Ernesto, M., Vasconcellos, E.M.G., De Min, A., Newton, R.J. & Szabó, C.
Resumo

Exceptional magmatic events coincided with the largest mass extinctions throughout Earth’s history. Extensive degassing from organic-rich sediments intruded by magmas is a possible driver of the catastrophic environmental changes, which triggered the biotic crises. One of Earth’s largest magmatic events is represented by the Central Atlantic Magmatic Province, which was synchronous with the end-Triassic mass extinction. Here, we show direct evidence for the presence in basaltic magmas of methane, generated or remobilized from the host sedimentary sequence during the emplacement of this Large Igneous Province. Abundant methane-rich fluid inclusions were entrapped within quartz at the end of magmatic crystallization in voluminous (about 1.0 × 106 km3) intrusions in Brazilian Amazonia, indicating a massive (about 7.2 × 103 Gt) fluxing of methane. These micrometre-sized imperfections in quartz crystals attest an extensive release of methane from magma–sediment interaction, which likely contributed to the global climate changes responsible for the end-Triassic mass extinction.

Programa Geofísica
Ano de publicação 2021
Tipo de publicação Artigo publicado em revista
Nome da revista/jornal Nature Communications
Localidade Publicação Internacional
Volume 12
Número 5534
DOI https://doi.org/10.1038/s41467-021-25510-w
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Página web https://www.nature.com/articles/s41467-021-25510-w.pdf