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Limited role for methane in the mid-Proterozoic greenhouse
Pervasive anoxia in the subsurface ocean during the Proterozoic may have allowed large fluxes of biogenic CH(4) to the atmosphere, enhancing the climatic significance of CH(4) early in Earth’s history. Indeed, the assumption of elevated pCH(4) during the Proterozoic underlies most models for both an...
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| Опубликовано в: : | Proc Natl Acad Sci U S A |
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| Главные авторы: | , , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
National Academy of Sciences
2016
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| Предметы: | |
| Online-ссылка: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5068276/ https://ncbi.nlm.nih.gov/pubmed/27671638 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1608549113 |
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