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

✍ Scribed by Jaap S. Sinninghe Damsté; Elisabeth C. van Bentum; Gert-Jan Reichart; Jörg Pross; Stefan Schouten


Book ID
116453350
Publisher
Elsevier Science
Year
2010
Tongue
English
Weight
915 KB
Volume
293
Category
Article
ISSN
0012-821X

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