Sulfate-induced isotopic variation in biogenic methane from a tropical swamp without anaerobic methane oxidation |
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Authors: | Miyajima Toshihiro Wada Eitaro |
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Institution: | (1) Center for Ecological Research, Kyoto University, Shimosakamoto, Otsu 520-0105, Japan;(2) Present address: Laboratory of Marine Biochemistry, The University of Tokyo, Minamidai, Nakano, Tokyo 164-8639, Japan |
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Abstract: | The oxidative consumption of methane (CH4) generally proceeds with a significant isotope fractionation, and isotopic variations
in CH4 observed in sulfate-containing anaerobic sediments have often been interpreted as an indicator of anaerobic methane
oxidation at the expense of sulfate. However, we found variations in δ13C value of CH4 depending on sulfate availability in
tropical swamp sediments, in which no anaerobic CH4 oxidation was detected. In one sediment, the range of δ13C variation due
to sulfate was as large as 20‰. The variations in δ13C of decomposed organic matter and CO2 failed to explain the variation
in CH4 δ13C. We postulate a syntrophic linkage between sulfate-reducing and methanogenic bacteria via acetate as a mechanism of the
observed δ'13C variation.
This revised version was published online in July 2006 with corrections to the Cover Date. |
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Keywords: | methanogenesis sediment stable carbon isotopes sulfate tropical forest |
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