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Sulfur isotopes in coal constrain the evolution of the Phanerozoic sulfur cycle
Sulfate is the second most abundant anion (behind chloride) in modern seawater, and its cycling is intimately coupled to the cycling of organic matter and oxygen at the Earth’s surface. For example, the reduction of sulfide by microbes oxidizes vast amounts of organic carbon and the subsequent react...
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| 第一著者: | |
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| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
National Academy of Sciences
2013
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3666666/ https://ncbi.nlm.nih.gov/pubmed/23650346 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1306450110 |
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