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...
Guardado en:
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: | |
Acceso en línea: | https://doaj.org/article/c5c978c3b9f2479b8407bcfd7d2a9024 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Massive methane fluxing from magma–sediment interaction in the end-Triassic Central Atlantic Magmatic Province
por: Manfredo Capriolo, et al.
Publicado: (2021) -
Permo–Triassic boundary carbon and mercury cycling linked to terrestrial ecosystem collapse
por: Jacopo Dal Corso, et al.
Publicado: (2020) -
Six-fold increase of atmospheric pCO2 during the Permian–Triassic mass extinction
por: Yuyang Wu, et al.
Publicado: (2021) -
End-Triassic mass extinction started by intrusive CAMP activity
por: J.H.F.L. Davies, et al.
Publicado: (2017) -
Limited and localized magmatism in the Central Atlantic Magmatic Province
por: R. E. Marzen, et al.
Publicado: (2020)