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...
প্রধান লেখক: | Zheng, X, Jenkyns, H, Gale, A, Ward, D, Henderson, G |
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বিন্যাস: | Journal article |
প্রকাশিত: |
Geological Society of America
2017
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অনুরূপ উপাদানগুলি
অনুরূপ উপাদানগুলি
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First evidence for the Cenomanian-Turonian oceanic anoxic event (OAE2, 'Bonarelli' event) from the Ionian Zone, western continental Greece
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Nitrate reduction, sulfate reduction, and sedimentary iron isotope evolution during the Cenomanian-Turonian oceanic anoxic event
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