Requirement for a microbial consortium to completely oxidize glucose in Fe(III)- reducing sediments

Derek R. Lovley; Elizabeth J.P. Phillips

doi:10.1128/aem.55.12.3234-3236.1989

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Requirement for a microbial consortium to completely oxidize glucose in Fe(III)- reducing sediments

Derek R. Lovley·Elizabeth J.P. Phillips

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Abstract

In various sediments in which Fe(III) reduction was the terminal electron-accepting process, [ 14 C]glucose was fermented to 14 C-fatty acids in a manner similar to that observed in methanogenic sediments. These results are consistent with the hypothesis that, in Fe(III)-reducing sediments, fermentable substrates are oxidized to carbon dioxide by the combined activity of fermentative bacteria and fatty acid-oxidizing, Fe(III)-reducing bacteria.

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Applied and Environmental Microbiology Article

Source-reported bounding extent: 38.31095815247622° to 47.55051472223806° latitude; -94.98111410896342° to -76.95194413988348° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Derek R. Lovley, Elizabeth J.P. Phillips. 1989. Requirement for a microbial consortium to completely oxidize glucose in Fe(III)- reducing sediments. https://doi.org/10.1128/aem.55.12.3234-3236.1989

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