A CO2 decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous Oceanic Anoxic Event 2

Author:

Sinninghe Damsté Jaap S.,van Bentum Elisabeth C.,Reichart Gert-Jan,Pross Jörg,Schouten Stefan

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference48 articles.

1. Data report: multiproxy geochemical characterization of OAE-related black shales at Site 1276, Newfoundland Basin;Arnaboldi,2006

2. Variations in the global carbon cycle during the Cretaceous related to climate, volcanism, and changes in atmospheric CO2;Arthur,1985

3. Geochemical and climatic effects of increased marine organic carbon burial at the Cenomanian/Turonian boundary;Arthur;Nature,1988

4. A warm and equable Cretaceous: the nature of the problem;Barron;Earth-Sci. Rev.,1983

5. Palaeo-CO2 and climate;Berner;Nature,1992

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