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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

Anaerobic degradation of toluene by a denitrifying bacterium.

TL;DR: O-xylene was transformed to a metabolite in the presence of toluene but did not serve as the sole source of carbon for growth of strain T1, which was distinct from other bacteria that oxidize toLUene anaerobically, but it may utilize a similar biochemical pathway of oxidation.
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Complete mineralization of benzene by aquifer microorganisms under strictly anaerobic conditions.

TL;DR: Benzene was mineralized to CO2 by aquifer-derived microorganisms under strictly anaerobic conditions in microcosms containing gasoline-contaminated subsurface sediment from Seal Beach, California and an aerobic, sulfide-reduced defined mineral medium supplemented with 20 mM sulfate.
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The geochemical evolution of low-molecular-weight organic acids derived from the degradation of petroleum contaminants in groundwater

TL;DR: The geochemical evolution of low-molecular-weight organic acids in groundwater downgradient from a crude-oil spill near Bemidji, Minnesota, was studied over a five-year period (1986-1990).
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Anaerobic Degradation of Benzene in Diverse Anoxic Environments

TL;DR: In this article, the authors extended the previous reports of anaerobic benzene degradation to sediments that varied with respect to contamination input, predominant redox condition, and salinity.
Journal ArticleDOI

Isolation and characterization of a novel toluene-degrading, sulfate-reducing bacterium.

TL;DR: A novel sulfate-reducing bacterium isolated from fuel-contaminated subsurface soil, strain PRTOL1, mineralizes toluene as the sole electron donor and carbon source under strictly anaerobic conditions and transforms o- and p-xylene to metabolic products when grown with toLUene, but xylene transformation by PRTol1 is slow relative to toluenes degradation and cannot be sustained over time.
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