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Atmospheric oxygen over Phanerozoic time

It is quite possible that the level of atmospheric oxygen has varied (roughly between 15 and 30% O(2)) over the past 550 million years. This variation is suggested by modeling of the carbon and sulfur cycles, by the excessive sediment burial of organic matter that accompanied the advent of large vas...

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Bibliographic Details
Main Author: Berner, Robert A.
Format: Artigo
Language:Inglês
Published: The National Academy of Sciences 1999
Subjects:
Online Access:https://ncbi.nlm.nih.gov/pmc/articles/PMC34224/
https://ncbi.nlm.nih.gov/pubmed/10500106
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