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Evolution of the Toarcian (Early Jurassic) carbon-cycle and global climatic controls on local sedimentary processes (Cardigan Bay Basin, UK)

Abstract:

The late Early Jurassic Toarcian Stage represents the warmest interval of the Jurassic Period, with an abrupt rise in global temperatures of up to ~7°C in mid-latitudes at the onset of the early Toarcian Oceanic Anoxic Event (T-OAE; ~183Ma). The T-OAE, which has been extensively studied in marine and continental successions from both hemispheres, was marked by the widespread expansion of anoxic and euxinic waters, geographically extensive deposition of organic-rich black shales, and clim...

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Publication status:
Published
Peer review status:
Peer reviewed

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Institution:
University of Oxford
Division:
MPLS Division
Department:
Earth Sciences
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS Division
Department:
Earth Sciences
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS Division
Department:
Earth Sciences
Role:
Author
More from this funder
Name:
Natural Environmental Research Council
Grant:
NE/N018508/1
More from this funder
Name:
International Continental Scientific Drilling Program
More from this funder
Name:
Shell International Exploration and Production B.V.
Publisher:
Elsevier
Journal:
Earth and Planetary Science Letters More from this journal
Volume:
484
Pages:
396–411
Publication date:
2018-01-08
Acceptance date:
2017-12-16
DOI:
ISSN:
0012-821X
Keywords:
Pubs id:
pubs:811670
UUID:
uuid:6bd6dfea-879f-48e5-bb2b-014fe74cde45
Local pid:
pubs:811670
Source identifiers:
811670
Deposit date:
2017-12-18

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