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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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Bibliographic Details
Published in:Nat Commun
Main Authors: Davies, J.H.F.L., Marzoli, A., Bertrand, H., Youbi, N., Ernesto, M., Schaltegger, U.
Format: Artigo
Language:Inglês
Published: Nature Publishing Group 2017
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Online Access:https://ncbi.nlm.nih.gov/pmc/articles/PMC5460029/
https://ncbi.nlm.nih.gov/pubmed/28561025
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms15596
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