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Anaerobic Oxidation of Toluene, Phenol, and p-Cresol by the Dissimilatory Iron-Reducing Organism, GS-15

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TLDR
The metabolism of toluene, phenol, and p-cresol by GS-15 provides a model for how aromatic hydrocarbons and phenols may be oxidized with the reduction of Fe(III) in contaminated aquifers and petroleum-containing sediments.
Abstract
The dissimilatory Fe(III) reducer, GS-15, is the first microorganism known to couple the oxidation of aromatic compounds to the reduction of Fe(III) and the first example of a pure culture of any kind known to anaerobically oxidize an aromatic hydrocarbon, toluene. In this study, the metabolism of toluene, phenol, and p-cresol by GS-15 was investigated in more detail. GS-15 grew in an anaerobic medium with toluene as the sole electron donor and Fe(III) oxide as the electron acceptor. Growth coincided with Fe(III) reduction. [ring-14C]toluene was oxidized to 14CO2, and the stoichiometry of 14CO2 production and Fe(III) reduction indicated that GS-15 completely oxidized toluene to carbon dioxide with Fe(III) as the electron acceptor. Magnetite was the primary iron end product during toluene oxidation. Phenol and p-cresol were also completely oxidized to carbon dioxide with Fe(III) as the sole electron acceptor, and GS-15 could obtain energy to support growth by oxidizing either of these compounds as the sole electron donor. p-Hydroxybenzoate was a transitory extracellular intermediate of phenol and p-cresol metabolism but not of toluene metabolism. GS-15 oxidized potential aromatic intermediates in the oxidation of toluene (benzylalcohol and benzaldehyde) and p-cresol (p-hydroxybenzylalcohol and p-hydroxybenzaldehyde). The metabolism described here provides a model for how aromatic hydrocarbons and phenols may be oxidized with the reduction of Fe(III) in contaminated aquifers and petroleum-containing sediments. Images

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Journal ArticleDOI

Dissimilatory Fe(III) and Mn(IV) reduction.

TL;DR: The physiological characteristics of Geobacter species appear to explain why they have consistently been found to be the predominant Fe(III)- and Mn(IV)-reducing microorganisms in a variety of sedimentary environments.
Journal ArticleDOI

Recent Advances in Petroleum Microbiology

TL;DR: The physiological responses of microorganisms to the presence of hydrocarbons, including cell surface alterations and adaptive mechanisms for uptake and efflux of these substrates, have been characterized and used to investigate the dynamics of microbial communities in petroleum-impacted ecosystems.
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Microbial reduction of uranium

TL;DR: In this article, dissimilatory Fe(III)-reducing microorganisms can obtain energy for growth by electron transport to U(VI), which can be much faster than commonly cited abiological mechanisms for reduction.
Book ChapterDOI

Dissimilatory Fe(III) and Mn(IV) reduction.

TL;DR: The ability to oxidize hydrogen with the reduction of Fe(III) is a highly conserved characteristic of hyperthermophilic microorganisms, most notably those in the Geobacteraceae family as mentioned in this paper.
Journal ArticleDOI

Dissimilatory Metal Reduction

TL;DR: Microorganisms can enzymatically reduce a variety of metals in metabolic processes that are not related to metal assimilation, including technetium, vanadium, molybdenum, gold, silver, and copper, but reduction of these metals has not been studied extensively.
References
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Journal ArticleDOI

Rapid microbial mineralization of toluene and 1,3-dimethylbenzene in the absence of molecular oxygen.

TL;DR: The results suggest that aromatic hydrocarbons present in anoxic environments such as lake sediments, sludge digestors, and groundwater infiltration zones from landfills and polluted rivers are not necessarily persistent but may be mineralized in the absence of molecular oxygen.
Journal ArticleDOI

Anaerobic degradation of phenol and phenol derivatives by Desulfobacterium phenolicum sp. nov.

TL;DR: A new sulfate-reducing bacterium was enriched and isolated from marine sediment with phenol as sole electron donor and carbon source and strain Ph01 was able to degrade all these aromatic compounds (except o-cresol) no further studies with the enrichment cultures were carried out.
Journal ArticleDOI

Long-term fate of organic micropollutants in sewage-contaminated groundwater.

TL;DR: Almost 50 volatile organic compounds were detected and identified in the plume, at concentrations ranging from 10 ng/L to 500 {mu}g/L, by closed-loop stripping and purge-and-trap in conjunction with gas chromatography-mass spectrometry.
Journal ArticleDOI

Evidence for a relationship between hydrocarbons and authigenic magnetite

TL;DR: In this article, the authors report palaeomagnetic, rock magnetic, petrographic and geochemical results of a study of samples from Permian spelebthems and gilsonite found in the Ordovician Arbuckle Group in southern Oklahoma.
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