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Transient cooling episodes during Cretaceous Oceanic Anoxic Events with special reference to OAE 1a (Early Aptian)

The two major oceanic anoxic events of the Cretaceous, those of the Early Aptian (OAE 1a) and the Cenomanian–Turonian boundary (OAE 2), registered some of the highest temperatures reconstructed for the Cretaceous Period, and are thought to be related to the input of volcanically derived carbon dioxi...

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Wedi'i Gadw mewn:
Manylion Llyfryddiaeth
Cyhoeddwyd yn:Philos Trans A Math Phys Eng Sci
Prif Awdur: Jenkyns, Hugh C.
Fformat: Artigo
Iaith:Inglês
Cyhoeddwyd: The Royal Society Publishing 2018
Pynciau:
Mynediad Ar-lein:https://ncbi.nlm.nih.gov/pmc/articles/PMC6127388/
https://ncbi.nlm.nih.gov/pubmed/30177559
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rsta.2017.0073
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