טוען...
Proterozoic ocean redox and biogeochemical stasis
The partial pressure of oxygen in Earth’s atmosphere has increased dramatically through time, and this increase is thought to have occurred in two rapid steps at both ends of the Proterozoic Eon (∼2.5–0.543 Ga). However, the trajectory and mechanisms of Earth’s oxygenation are still poorly constrain...
שמור ב:
| Main Authors: | , , , , , , , , |
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| פורמט: | Artigo |
| שפה: | Inglês |
| יצא לאור: |
National Academy of Sciences
2013
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| נושאים: | |
| גישה מקוונת: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3619314/ https://ncbi.nlm.nih.gov/pubmed/23515332 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1208622110 |
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