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A sluggish mid‐Proterozoic biosphere and its effect on Earth's redox balance
The possibility of low but nontrivial atmospheric oxygen (O(2)) levels during the mid‐Proterozoic (between 1.8 and 0.8 billion years ago, Ga) has important ramifications for understanding Earth's O(2) cycle, the evolution of complex life and evolving climate stability. However, the regulatory m...
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| Udgivet i: | Geobiology |
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| Main Authors: | , , |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
John Wiley and Sons Inc.
2018
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| Fag: | |
| Online adgang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6585969/ https://ncbi.nlm.nih.gov/pubmed/30281196 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1111/gbi.12317 |
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