Black shale deposition, atmospheric CO2 drawdown, and cooling during the Cenomanian-Turonian Oceanic Anoxic Event
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...
| Main Authors: | , , , , |
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| Format: | Journal article |
| Published: |
2011
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