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Journal ArticleDOI

Field and laboratory studies of methane oxidation in an anoxic marine sediment: Evidence for a methanogen-sulfate reducer consortium

TLDR
A seasonal survey of anoxic sediments from Cape Lookout Bight, North Carolina, suggests that anaerobic methane oxidation is mediated by a consortium of methanogenic and sulfate-reducing bacteria as mentioned in this paper.
Abstract
Field and laboratory studies of anoxic sediments from Cape Lookout Bight, North Carolina, suggest that anaerobic methane oxidation is mediated by a consortium of methanogenic and sulfate-reducing bacteria. A seasonal survey of methane oxidation and CO2 reduction rates indicates that methane production was confined to sulfate-depleted sediments at all times of year, while methane oxidation occurred in two modes. In the summer, methane oxidation was confined to sulfate-depleted sediments and occurred at rates lower than those of CO2 reduction. In the winter, net methane oxidation occurred in an interval at the base of the sulfate-containing zone. Sediment incubation experiments suggest both methanogens and sulfate reducers were responsible for the observed methane oxidation. In one incubation experiment both modes of oxidation were partially inhibited by 2-bromoethanesulfonic acid (a specific inhibitor of methanogens). This evidence, along with the apparent confinement of methane oxidation to sulfate-depleted sediments in the summer, indicates that methanogenic bacteria are involved in methane oxidation. In a second incubation experiment, net methane oxidation was induced by adding sulfate to homogenized methanogenic sediments, suggesting that sulfate reducers also play a role in the process. We hypothesize that methanogens oxidize methane and produce hydrogen via a reversal of CO2 reduction. The hydrogen is efficiently removed and maintained at low concentrations by sulfate reducers. Pore water H2 concentrations in the sediment incubation experiments (while net methane oxidation was occurring) were low enough that methanogenic bacteria could derive sufficient energy for growth from the oxidation of methane. The methanogen-sulfate reducer consortium is consistent not only with the results of this study, but may also be a feasible mechanism for previously documented anaerobic methane oxidation in both freshwater and marine environments.

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Citations
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Journal ArticleDOI

A marine microbial consortium apparently mediating anaerobic oxidation of methane

TL;DR: In this article, the authors provide microscopic evidence for a structured consortium of archaea and sulphate-reducing bacteria, which are identified by fluorescence in situ hybridization using specific 16S rRNA-targeted oligonucleotide probes.
Journal ArticleDOI

The ecology and biotechnology of sulphate-reducing bacteria

TL;DR: Sulphate-reducing bacteria are anaerobic microorganisms that use sulphate as a terminal electron acceptor in, for example, the degradation of organic compounds, and are ubiquitous in anoxic habitats.
Journal ArticleDOI

Energetics of syntrophic cooperation in methanogenic degradation.

TL;DR: S syntrophically fermenting bacteria synthesize ATP by substrate-level phosphorylation and reinvest part of the ATP-bound energy into reversed electron transport processes, to release the electrons at a redox level accessible by the partner bacteria and to balance their energy budget.
Journal ArticleDOI

Soil microorganisms as controllers of atmospheric trace gases (H2, CO, CH4, OCS, N2O, and NO).

TL;DR: It is completely unclear how important microbial diversity is for the control of trace gas flux at the ecosystem level, and different microbial communities may be part of the reason for differences in trace gas metabolism, e.g., effects of nitrogen fertilizers on CH4 uptake by soil; decrease of CH4 production with decreasing temperature.
Journal ArticleDOI

Anaerobic Oxidation of Methane: Progress with an Unknown Process

TL;DR: This review summarizes what is known and unknown about AOM on earth and its key catalysts, the anaerobic methanotrophic archaea clades and their bacterial partners.
References
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Journal ArticleDOI

Coupling of Phosphorylation to Electron and Hydrogen Transfer by a Chemi-Osmotic type of Mechanism

TL;DR: Coupling of Phosphorylation to Electron and Hydrogen Transfer by a Chemi-Osmotic type of Mechanism is described.
Journal ArticleDOI

Biogeochemical aspects of atmospheric methane

TL;DR: In this paper, the authors identify and evaluate several constraints on the budget of atmospheric methane, its sources, sinks and residence time, and construct a list of sources and sinks, identities, and sizes.
Journal ArticleDOI

A comparison of methods for the quantification of bacterial sulfate reduction in coastal marine sediments

TL;DR: A radiotracer technique for measuring in situ rates of sulfate reduction in marine sediments is described in this paper, where microliter portions of labeled sulfate solution are injected into undisturbed sediment cores, and the amount of labeled sulfide produced is analyzed.
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Hydrogen concentrations as an indicator of the predominant terminal electron-accepting reactions in aquatic sediments

TL;DR: In this article, the authors investigated factors controlling the concentration of dissolved hydrogen gas in anaerobic sedimentary environments and found that only microorganisms catalyze the oxidation of H 2 coupled to the reduction of nitrate, Mn(IV), Fe(III), sulfate, or carbon dioxide.
Journal ArticleDOI

Methane consumption in cariaco trench waters and sediments

TL;DR: In this article, the water column and the sediments of the Cariaco Trench were measured and the results showed that CH4 is non-conservative in both environments, and the concentrations of CH4 were found to be non-consistency.
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