Sedimentary sulfur isotopes and Neoarchean ocean oxygenation

Abrupt disappearance of mass-independent fractionation of sulfur isotopes (MIF-S) from the geologic record and an apparent ingrowth in seawater sulfate around 2.45 billion years ago (Ga) signal the first large-scale oxygenation of the atmosphere [the Great Oxygenation Event (GOE)]. Pre-GOE O(2) prod...

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Detalles Bibliográficos
Autores principales: Fakhraee, Mojtaba, Crowe, Sean A., Katsev, Sergei
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2018
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5783677/
https://www.ncbi.nlm.nih.gov/pubmed/29376118
http://dx.doi.org/10.1126/sciadv.1701835

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5783677/
https://www.ncbi.nlm.nih.gov/pubmed/29376118
http://dx.doi.org/10.1126/sciadv.1701835

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