Mercury evidence for pulsed volcanism during the end-Triassic mass extinction
Mercury evidence for pulsed volcanism during the end-Triassic mass extinction
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United States: National Academy of Sciences
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Language
English
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United States: National Academy of Sciences
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Contents
The Central Atlantic Magmatic Province (CAMP) has long been proposed as having a causal relationship with the end-Triassic extinction event (∼201.5 Ma). In North America and northern Africa, CAMP is preserved as multiple basaltic units interbedded with uppermost Triassic to lowermost Jurassic sediments. However, it has been unclear whether this app...
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Full title
Mercury evidence for pulsed volcanism during the end-Triassic mass extinction
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TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_5544315
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_5544315
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ISSN
0027-8424
E-ISSN
1091-6490
DOI
10.1073/pnas.1705378114