End-Triassic mass extinction started by intrusive CAMP activity

The end-Triassic extinction is one of the Phanerozoic's largest mass extinctions. This extinction is typically attributed to climate change associated with degassing of basalt flows from the central Atlantic magmatic province (CAMP). However, recent work suggests that the earliest known CAMP ba...

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Detalles Bibliográficos
Autores principales: Davies, J.H.F.L., Marzoli, A., Bertrand, H., Youbi, N., Ernesto, M., Schaltegger, U.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5460029/
https://www.ncbi.nlm.nih.gov/pubmed/28561025
http://dx.doi.org/10.1038/ncomms15596

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5460029/
https://www.ncbi.nlm.nih.gov/pubmed/28561025
http://dx.doi.org/10.1038/ncomms15596

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