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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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Bibliografiska uppgifter
Huvudupphovsmän: Beerling, D. J., Berner, R. A.
Materialtyp: Artigo
Språk:Inglês
Publicerad: The National Academy of Sciences 2000
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Länkar:https://ncbi.nlm.nih.gov/pmc/articles/PMC18779/
https://ncbi.nlm.nih.gov/pubmed/11050154
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