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Carbon sequestration in an expanded lake system during the Toarcian oceanic anoxic event

Abstract:

The Early Jurassic Toarcian oceanic anoxic event (∼183 Ma) was marked by marine anoxia–euxinia and globally significant organic-matter burial, accompanied by a major global carbon-cycle perturbation probably linked to Karoo–Ferrar volcanism. Although the Toarcian oceanic anoxic event is well studied in the marine realm, accompanying climatic and environmental change on the continents is poorly understood. Here, utilizing radioisotopic, palynological and geochemical data from lacustrine black ...

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Publication status:
Published
Peer review status:
Peer reviewed
Version:
Accepted Manuscript

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Publisher copy:
10.1038/NGEO2871

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Institution:
University of Oxford
Department:
St Peters College
Role:
Author
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Institution:
University of Oxford
Department:
Oxford, MPLS, Earth Sciences
Role:
Author
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Institution:
University of Oxford
Department:
Oxford, MPLS, Earth Sciences
Role:
Author
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Shell International Exploration & Production B.V More from this funder
Publisher:
Springer Nature Publisher's website
Journal:
Nature Geoscience Journal website
Volume:
10
Issue:
2
Pages:
129–134
Publication date:
2017-01-16
Acceptance date:
2016-12-08
DOI:
EISSN:
1752-0908
ISSN:
1752-0894
Pubs id:
pubs:672223
URN:
uri:e6f3d924-e62e-4726-96fe-9ccd2d0168cc
UUID:
uuid:e6f3d924-e62e-4726-96fe-9ccd2d0168cc
Local pid:
pubs:672223
Paper number:
2

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