A CO2 decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous Oceanic Anoxic Event 2 (Q59139342)
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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)
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April 2010
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293
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1-2
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97-103
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