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  • 1
    Online Resource
    Online Resource
    American Society for Microbiology ; 1986
    In:  Applied and Environmental Microbiology Vol. 51, No. 4 ( 1986-04), p. 683-689
    In: Applied and Environmental Microbiology, American Society for Microbiology, Vol. 51, No. 4 ( 1986-04), p. 683-689
    Abstract: The potential for ferric iron reduction with fermentable substrates, fermentation products, and complex organic matter as electron donors was investigated with sediments from freshwater and brackish water sites in the Potomac River Estuary. In enrichments with glucose and hematite, iron reduction was a minor pathway for electron flow, and fermentation products accumulated. The substitution of amorphous ferric oxyhydroxide for hematite in glucose enrichments increased iron reduction 50-fold because the fermentation products could also be metabolized with concomitant iron reduction. Acetate, hydrogen, propionate, butyrate, ethanol, methanol, and trimethylamine stimulated the reduction of amorphous ferric oxyhydroxide in enrichments inoculated with sediments but not in uninoculated or heat-killed controls. The addition of ferric iron inhibited methane production in sediments. The degree of inhibition of methane production by various forms of ferric iron was related to the effectiveness of these ferric compounds as electron acceptors for the metabolism of acetate. The addition of acetate or hydrogen relieved the inhibition of methane production by ferric iron. The decrease of electron equivalents proceeding to methane in sediments supplemented with amorphous ferric oxyhydroxides was compensated for by a corresponding increase of electron equivalents in ferrous iron. These results indicate that iron reduction can outcompete methanogenic food chains for sediment organic matter. Thus, when amorphous ferric oxyhydroxides are available in anaerobic sediments, the transfer of electrons from organic matter to ferric iron can be a major pathway for organic matter decomposition.
    Type of Medium: Online Resource
    ISSN: 0099-2240 , 1098-5336
    RVK:
    Language: English
    Publisher: American Society for Microbiology
    Publication Date: 1986
    detail.hit.zdb_id: 223011-2
    detail.hit.zdb_id: 1478346-0
    SSG: 12
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  • 2
    Online Resource
    Online Resource
    American Society for Microbiology ; 1986
    In:  Applied and Environmental Microbiology Vol. 52, No. 4 ( 1986-10), p. 751-757
    In: Applied and Environmental Microbiology, American Society for Microbiology, Vol. 52, No. 4 ( 1986-10), p. 751-757
    Abstract: The distribution of Fe(III), its availability for microbial reduction, and factors controlling Fe(III) availability were investigated in sediments from a freshwater site in the Potomac River Estuary. Fe(III) reduction in sediments incubated under anaerobic conditions and depth profiles of oxalate-extractable Fe(III) indicated that Fe(III) reduction was limited to depths of 4 cm or less, with the most intense Fe(III) reduction in the top 1 cm. In incubations of the upper 4 cm of the sediments, Fe(III) reduction was as important as methane production as a pathway for anaerobic electron flow because of the high rates of Fe(III) reduction in the 0- to 0.5-cm interval. Most of the oxalate-extractable Fe(III) in the sediments was not reduced and persisted to a depth of at least 20 cm. The incomplete reduction was not the result of a lack of suitable electron donors. The oxalate-extractable Fe(III) that was preserved in the sediments was considered to be in a form other than amorphous Fe(III) oxyhydroxide, since synthetic amorphous Fe(III) oxyhydroxide, amorphous Fe(III) oxyhydroxide adsorbed onto clay, and amorphous Fe(III) oxyhydroxide saturated with adsorbed phosphate or fulvic acids were all readily reduced. Fe 3 O 4 and the mixed Fe(III)-Fe(II) compound(s) that were produced during the reduction of amorphous Fe(III) oxyhydroxide in an enrichment culture were oxalate extractable but were not reduced, suggesting that mixed Fe(III)-Fe(II) compounds might account for the persistence of oxalate-extractable Fe(III) in the sediments. The availability of microbially reducible Fe(III) in surficial sediments demonstrates that microbial Fe(III) reduction can be important to organic matter decomposition and iron geochemistry. However, the overall extent of microbial Fe(III) reduction is governed by the inability of microorganisms to reduce most of the Fe(III) in the sediment.
    Type of Medium: Online Resource
    ISSN: 0099-2240 , 1098-5336
    RVK:
    Language: English
    Publisher: American Society for Microbiology
    Publication Date: 1986
    detail.hit.zdb_id: 223011-2
    detail.hit.zdb_id: 1478346-0
    SSG: 12
    Location Call Number Limitation Availability
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  • 3
    Online Resource
    Online Resource
    Portland Press Ltd. ; 1986
    In:  Biochemical Society Transactions Vol. 14, No. 4 ( 1986-08-01), p. 765-765
    In: Biochemical Society Transactions, Portland Press Ltd., Vol. 14, No. 4 ( 1986-08-01), p. 765-765
    Type of Medium: Online Resource
    ISSN: 0300-5127 , 1470-8752
    Language: English
    Publisher: Portland Press Ltd.
    Publication Date: 1986
    SSG: 12
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  • 4
    Online Resource
    Online Resource
    Portland Press Ltd. ; 1986
    In:  Biochemical Society Transactions Vol. 14, No. 6 ( 1986-12-01), p. 1252-1253
    In: Biochemical Society Transactions, Portland Press Ltd., Vol. 14, No. 6 ( 1986-12-01), p. 1252-1253
    Type of Medium: Online Resource
    ISSN: 0300-5127 , 1470-8752
    Language: English
    Publisher: Portland Press Ltd.
    Publication Date: 1986
    SSG: 12
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  • 5
    Online Resource
    Online Resource
    Elsevier BV ; 1986
    In:  Biochimica et Biophysica Acta (BBA) - Protein Structure and Molecular Enzymology Vol. 874, No. 3 ( 1986-12), p. 305-311
    In: Biochimica et Biophysica Acta (BBA) - Protein Structure and Molecular Enzymology, Elsevier BV, Vol. 874, No. 3 ( 1986-12), p. 305-311
    Type of Medium: Online Resource
    ISSN: 0167-4838
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1986
    detail.hit.zdb_id: 2209539-1
    SSG: 12
    Location Call Number Limitation Availability
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