A CO2 decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous Oceanic Anoxic Event 2 (Q59139342)
Jump to navigation
Jump to search
scientific article
Language | Label | Description | Also known as |
---|---|---|---|
English | A CO2 decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous Oceanic Anoxic Event 2 |
scientific article |
Statements
A CO2 decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous Oceanic Anoxic Event 2 (English)
0 references
April 2010
0 references
293
0 references
1-2
0 references
97-103
0 references