Diurnal Fe(II)/Fe(III) cycling and enhanced O(2) production in a simulated Archean marine oxygen oasis

The oxygenation of early Earth’s atmosphere during the Great Oxidation Event, is generally accepted to have been caused by oceanic Cyanobacterial oxygenic photosynthesis. Recent studies suggest that Fe(II) toxicity delayed the Cyanobacterial expansion necessary for the GOE. This study investigates t...

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Detalles Bibliográficos
Autores principales: Herrmann, A. J., Sorwat, J., Byrne, J. M., Frankenberg-Dinkel, N., Gehringer, M. M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8024245/
https://www.ncbi.nlm.nih.gov/pubmed/33824308
http://dx.doi.org/10.1038/s41467-021-22258-1

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8024245/
https://www.ncbi.nlm.nih.gov/pubmed/33824308
http://dx.doi.org/10.1038/s41467-021-22258-1

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