Constraining the rate of oceanic deoxygenation leading up to a Cretaceous Oceanic Anoxic Event (OAE-2: ~94 Ma)

The rates of marine deoxygenation leading to Cretaceous Oceanic Anoxic Events are poorly recognized and constrained. If increases in primary productivity are the primary driver of these episodes, progressive oxygen loss from global waters should predate enhanced carbon burial in underlying sediments...

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Detalles Bibliográficos
Autores principales: Ostrander, Chadlin M., Owens, Jeremy D., Nielsen, Sune G.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2017
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5550229/
https://www.ncbi.nlm.nih.gov/pubmed/28808684
http://dx.doi.org/10.1126/sciadv.1701020

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5550229/
https://www.ncbi.nlm.nih.gov/pubmed/28808684
http://dx.doi.org/10.1126/sciadv.1701020

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