Charcoal evidence that rising atmospheric oxygen terminated Early Jurassic ocean anoxia

The Toarcian Oceanic Anoxic Event (T-OAE) was characterized by a major disturbance to the global carbon(C)-cycle, and depleted oxygen in Earth's oceans resulting in marine mass extinction. Numerical models predict that increased organic carbon burial should drive a rise in atmospheric oxygen (p...

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Detalles Bibliográficos
Autores principales: Baker, Sarah J., Hesselbo, Stephen P., Lenton, Timothy M., Duarte, Luís V., Belcher, Claire M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5437290/
https://www.ncbi.nlm.nih.gov/pubmed/28497785
http://dx.doi.org/10.1038/ncomms15018

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5437290/
https://www.ncbi.nlm.nih.gov/pubmed/28497785
http://dx.doi.org/10.1038/ncomms15018

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