Abstract:
:In various sediments in which Fe(III) reduction was the terminal electron-accepting process, [C]glucose was fermented to 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.
journal_name
Appl Environ Microbioljournal_title
Applied and environmental microbiologyauthors
Lovley DR,Phillips EJdoi
10.1128/AEM.55.12.3234-3236.1989keywords:
subject
Has Abstractpub_date
1989-12-01 00:00:00pages
3234-6issue
12eissn
0099-2240issn
1098-5336journal_volume
55pub_type
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journal_title:Applied and environmental microbiology
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