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Impact of a Permo-Carboniferous high O(2) event on the terrestrial carbon cycle
Independent models predicting the Phanerozoic (past 600 million years) history of atmospheric O(2) partial pressure (pO(2)) indicate a marked rise to approximately 35% in the Permo-Carboniferous, around 300 million years before present, with the strong potential for altering the biogeochemical cycli...
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| Main Authors: | , |
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| Format: | Artigo |
| Language: | Inglês |
| Published: |
The National Academy of Sciences
2000
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| Subjects: | |
| Online Access: | https://ncbi.nlm.nih.gov/pmc/articles/PMC18779/ https://ncbi.nlm.nih.gov/pubmed/11050154 |
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