Journal article icon

Journal article

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

Abstract:

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 apparent pulsing was a local feature, or if pulses in the intensity of CAMP volcanism characterized the emplacement of the province as a whole. Here, ...

Expand abstract
Publication status:
Published
Peer review status:
Peer reviewed

Actions


Access Document


Files:
Publisher copy:
10.1073/pnas.1705378114

Authors


More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
Expand authors...
More from this funder
Funding agency for:
Ruhl, M
Grant:
Research Grant
Shell International Exploration and Production Inc More from this funder
Leverhulme Trust More from this funder
Publisher:
National Academy of Sciences Publisher's website
Journal:
Proceedings of the National Academy of Sciences Journal website
Volume:
119
Issue:
4
Pages:
7929–7934
Publication date:
2017-07-01
Acceptance date:
2017-05-19
DOI:
EISSN:
1091-6490
ISSN:
0027-8424
Source identifiers:
696652
Keywords:
Pubs id:
pubs:696652
UUID:
uuid:8bc84111-bb67-48dd-ac61-f9d369af3518
Local pid:
pubs:696652
Deposit date:
2017-05-22

Terms of use


Views and Downloads






If you are the owner of this record, you can report an update to it here: Report update to this record

TO TOP