Strong evidence for a weakly oxygenated ocean–atmosphere system during the Proterozoic

Earth’s surface has undergone a protracted oxygenation, which is commonly assumed to have profoundly affected the biosphere. However, basic aspects of this history are still debated—foremost oxygen (O(2)) levels in the oceans and atmosphere during the billion years leading up to the rise of algae an...

Descripción completa

Detalles Bibliográficos
Autores principales: Wang, Changle, Lechte, Maxwell A., Reinhard, Christopher T., Asael, Dan, Cole, Devon B., Halverson, Galen P., Porter, Susannah M., Galili, Nir, Halevy, Itay, Rainbird, Robert H., Lyons, Timothy W., Planavsky, Noah J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2022
Materias:
Physical Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8833159/
https://www.ncbi.nlm.nih.gov/pubmed/35101984
http://dx.doi.org/10.1073/pnas.2116101119

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8833159/
https://www.ncbi.nlm.nih.gov/pubmed/35101984
http://dx.doi.org/10.1073/pnas.2116101119

Ejemplares similares