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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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| Gepubliceerd in: | Nat Commun |
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| Hoofdauteurs: | , , , , , |
| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
Nature Publishing Group
2017
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| Onderwerpen: | |
| Online toegang: | 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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