A climatic control on reorganization of ocean circulation during the mid-Cenomanian event and Cenomanian-Turonian oceanic anoxic event (OAE 2): Nd isotope evidence
Although ocean circulation plays a vital role in the climate system, its response to major carbon-cycle perturbations during the mid-Cretaceous, including Mid-Cenomanian Event I (MCE I) and Cenomanian–Turonian oceanic anoxic event (OAE 2), is poorly constrained. Here we present Nd-isotope evidence f...
| Main Authors: | , , , , |
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| Formato: | Journal article |
| Publicado em: |
Geological Society of America
2017
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