Carbon isotope evidence for large methane emissions to the Proterozoic atmosphere

The Proterozoic Era records two periods of abundant positive carbon isotope excursions (CIEs), conventionally interpreted as resulting from increased organic carbon burial and leading to Earth’s surface oxygenation. As strong spatial variations in the amplitude and duration of these excursions are u...

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Detalles Bibliográficos
Autores principales: Cadeau, Pierre, Jézéquel, Didier, Leboulanger, Christophe, Fouilland, Eric, Le Floc’h, Emilie, Chaduteau, Carine, Milesi, Vincent, Guélard, Julia, Sarazin, Gérard, Katz, Amandine, d’Amore, Sophie, Bernard, Cécile, Ader, Magali
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7585424/
https://www.ncbi.nlm.nih.gov/pubmed/33097795
http://dx.doi.org/10.1038/s41598-020-75100-x

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7585424/
https://www.ncbi.nlm.nih.gov/pubmed/33097795
http://dx.doi.org/10.1038/s41598-020-75100-x

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