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Black shale deposition, atmospheric CO2 drawdown, and cooling during the Cenomanian-Turonian Oceanic Anoxic Event

Abstract:

Oceanic Anoxic Event 2 (OAE2), spanning the Cenomanian-Turonian boundary (CTB), represents one of the largest perturbations in the global carbon cycle in the last 100 Myr. The δ 13C carb, δ 13C org, and δ 18O chemostratigraphy of a black shale-bearing CTB succession in the Vocontian Basin of France is described and correlated at high resolution to the European CTB reference section at Eastbourne, England, and to successions in Germany, the equatorial and midlatitude proto-North Atlantic, and ...

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Publication status:
Published

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Publisher copy:
10.1029/2010PA002081

Authors


Lignum, JS More by this author
Groecke, DR More by this author
More by this author
Institution:
University of Oxford
Department:
Oxford, MPLS, Earth Sciences
Pearce, MA More by this author
Journal:
PALEOCEANOGRAPHY
Volume:
26
Issue:
3
Pages:
n/a-n/a
Publication date:
2011-07-19
DOI:
ISSN:
0883-8305
URN:
uuid:c5abe6bb-4910-4615-b002-054891a0c4b6
Source identifiers:
170220
Local pid:
pubs:170220

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