Anomalous fractionation of mercury isotopes in the Late Archean atmosphere

Earth’s surface underwent a dramatic transition ~2.3 billion years ago when atmospheric oxygen first accumulated during the Great Oxidation Event, but the detailed composition of the reducing early atmosphere is not well known. Here we develop mercury (Hg) stable isotopes as a proxy for paleoatmosph...

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Detalles Bibliográficos
Autores principales: Zerkle, Aubrey L., Yin, Runsheng, Chen, Chaoyue, Li, Xiangdong, Izon, Gareth J., Grasby, Stephen E.
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/PMC7136252/
https://www.ncbi.nlm.nih.gov/pubmed/32249783
http://dx.doi.org/10.1038/s41467-020-15495-3

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7136252/
https://www.ncbi.nlm.nih.gov/pubmed/32249783
http://dx.doi.org/10.1038/s41467-020-15495-3

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