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Mercury evidence for pulsed volcanism during the end-Triassic mass extinction

Mercury evidence for pulsed volcanism during the end-Triassic mass extinction

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_5544315

Mercury evidence for pulsed volcanism during the end-Triassic mass extinction

About this item

Full title

Mercury evidence for pulsed volcanism during the end-Triassic mass extinction

Publisher

United States: National Academy of Sciences

Journal title

Proceedings of the National Academy of Sciences - PNAS, 2017-07, Vol.114 (30), p.7929-7934

Language

English

Formats

Publication information

Publisher

United States: National Academy of Sciences

More information

Scope and Contents

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...

Alternative Titles

Full title

Mercury evidence for pulsed volcanism during the end-Triassic mass extinction

Identifiers

Primary Identifiers

Record Identifier

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

Other Identifiers

ISSN

0027-8424

E-ISSN

1091-6490

DOI

10.1073/pnas.1705378114

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