- 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 ...
Expand abstract - Publication status:
- Published
- Publisher copy:
- 10.1029/2010PA002081
-
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- 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
- Copyright date:
- 2011
Journal article
Black shale deposition, atmospheric CO2 drawdown, and cooling during the Cenomanian-Turonian Oceanic Anoxic Event
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