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The effect of temperature on organic carbon degradation in marine sediments
The degradation of sedimentary particulate organic carbon (POC) is a key carbon cycle process that fuels the deep subseafloor biosphere. The reactivity of POC is expected to decrease with increasing sediment age, severely restricting the energy available to microorganisms. Conversely, increasing tem...
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| 出版年: | Sci Rep |
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| 主要な著者: | , |
| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
Nature Publishing Group
2015
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4671099/ https://ncbi.nlm.nih.gov/pubmed/26640172 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep17861 |
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