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Anaerobic oxidation of methane at different temperature regimes in Guaymas Basin hydrothermal sediments
Anaerobic oxidation of methane (AOM) was investigated in hydrothermal sediments of Guaymas Basin based on δ(13)C signatures of CH(4), dissolved inorganic carbon and porewater concentration profiles of CH(4) and sulfate. Cool, warm and hot in-situ temperature regimes (15–20 °C, 30–35 °C and 70–95 °C)...
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| Главные авторы: | , , , , , , |
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| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
Nature Publishing Group
2012
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| Предметы: | |
| Online-ссылка: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3329104/ https://ncbi.nlm.nih.gov/pubmed/22094346 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ismej.2011.164 |
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