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Globally asynchronous sulphur isotope signals require re-definition of the Great Oxidation Event

The Great Oxidation Event (GOE) has been defined as the time interval when sufficient atmospheric oxygen accumulated to prevent the generation and preservation of mass-independent fractionation of sulphur isotopes (MIF-S) in sedimentary rocks. Existing correlations suggest that the GOE was rapid and...

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Detalhes bibliográficos
Publicado no:Nat Commun
Main Authors: Philippot, Pascal, Ávila, Janaína N., Killingsworth, Bryan A., Tessalina, Svetlana, Baton, Franck, Caquineau, Tom, Muller, Elodie, Pecoits, Ernesto, Cartigny, Pierre, Lalonde, Stefan V., Ireland, Trevor R., Thomazo, Christophe, van Kranendonk, Martin J., Busigny, Vincent
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group UK 2018
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Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC5993798/
https://ncbi.nlm.nih.gov/pubmed/29884814
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-04621-x
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