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Open AccessJournal ArticleDOI

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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Carbon and hydrogen isotope fractionation during anaerobic toluene oxidation by Geobacter metallireducens with different Fe(III) phases as terminal electron acceptors.

TL;DR: It is hypothesize that smaller 2H and 13C fractionation in suspensions is due to toluene transport limitations to cells of G. metallireducens at surfaces of solid Fe(III) phases, and enrichment factors determined in Fe( III) mineral suspensions should be more representative for anaerobic toLUene degradation owing to the abundance ofSolid Fe(II) in soils and aquifers.
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Biotransformation of monoaromatic and chlorinated hydrocarbons at an aviation gasoline spill site.

TL;DR: A shallow water table aquifer under the U.S. Coast Guard Air Station at Traverse City, MI, has acclimated to the aerobic and anaerobic transformation of monoaromatic hydrocarbons (BTX) released from an aviation gasoline spill.
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Dominance of Geobacteraceae in BTX-degrading enrichments from an iron-reducing aquifer.

TL;DR: This research suggests that Geobacteraceae play a key role in the natural attenuation of each BTX compound in situ.
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Electron transfer in the dissimilatory iron-reducing bacterium Geobacter metallireducens

TL;DR: The growth yield, redox reactions, and electron transfer components are discussed with regards to possible sites of energy conservation during growth on iron(III).
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Geochemical changes during biodegradation of petroleum hydrocarbons: Field investigations and biogeochemical modelling.

TL;DR: In this paper, the role of ferric iron during biodegradation of dissolved petroleum hydrocarbon compounds at a field site in Perth, Western Australia was investigated using wet extraction techniques and model simulations.
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