Identification of acetate-assimilating microorganisms under methanogenic conditions in anoxic rice field soil by comparative stable isotope probing of RNA.
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ABSTRACT: Acetate is the most abundant intermediate of organic matter degradation in anoxic rice field soil and is converted to CH(4) and/or CO(2). Aceticlastic methanogens are the primary microorganisms dissimilating acetate in the absence of sulfate and reducible ferric iron. In contrast, very little is known about bacteria capable of assimilating acetate under methanogenic conditions. Here, we identified active acetate-assimilating microorganisms by using a combined approach of frequent label application at a low concentration and comparative RNA-stable isotope probing with (13)C-labeled and unlabeled acetate. Rice field soil was incubated anaerobically at 25 degrees C for 12 days, during which (13)C-labeled acetate was added at a concentration of 500 muM every 3 days. (13)C-labeled CH(4) and CO(
SUBMITTER: Hori T
PROVIDER: S-EPMC1797110 | biostudies-literature | 2007 Jan
REPOSITORIES: biostudies-literature
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