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Uranium isotope evidence for two episodes of deoxygenation during Oceanic Anoxic Event 2

Oceanic Anoxic Event 2 (OAE 2), occurring ∼94 million years ago, was one of the most extreme carbon cycle and climatic perturbations of the Phanerozoic Eon. It was typified by a rapid rise in atmospheric CO(2), global warming, and marine anoxia, leading to the widespread devastation of marine ecosys...

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Publicado en:Proc Natl Acad Sci U S A
Autores principales: Clarkson, Matthew O., Stirling, Claudine H., Jenkyns, Hugh C., Dickson, Alexander J., Porcelli, Don, Moy, Christopher M., Pogge von Strandmann, Philip A. E., Cooke, Ilsa R., Lenton, Timothy M.
Formato: Artigo
Lenguaje:Inglês
Publicado: National Academy of Sciences 2018
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Acceso en línea:https://ncbi.nlm.nih.gov/pmc/articles/PMC5866551/
https://ncbi.nlm.nih.gov/pubmed/29507196
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1715278115
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