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Cited by 198

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Mineralogical and morphological constraints on the reduction of Fe(III) minerals by Geobacter sulfurreducens

Cutting, R.S., Coker, V.S., Fellowes, J.W., Lloyd, J.R., Vaughan, D.J.·2009·Geochimica et Cosmochimica Acta
DOI 10.1016/j.gca.2009.04.009
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  • Many factors contribute to formation of specific Fe(II)-bearing secondary minerals as products of dissimilatory iron reduction, including Fe(III) oxide mineralogy, particle aggregation, rate and extent of Fe(II) production, electron shuttles, DIRB species and population size, oxyanions, dissolved NOM, and electron donor concentration and type.

    “Many factors have been identified as contributing to the formation of specific Fe(II)-bearing secondary minerals as products of DIR, including Fe(III) oxide mineralogy, [20,35]; Fe(III) oxide particle aggregation, [41]; the rate and extent of Fe(II) production, [33,35,42,43]; the presence of electron shuttles, [33]; the species and population size of the DIRB, [44][45][46]; the presence of oxyanio”

    From Electron Donor Utilization and Secondary Mineral Formation during the Bioreduction of Lepidocrocite by Shewanella putrefaciens CN32 (2019) · cites this paper as [20]

  • Dissimilatory iron-reducing bacteria can use soluble Fe(III) complexes, Fe(III) oxides, and Fe(III)-bearing clay minerals as terminal electron acceptors for anaerobic respiration.

    “As a group, dissimilatory iron-reducing bacteria (DIRB) are able to use soluble Fe(III) complexes (e.g., ferric citrate), Fe(III) oxides, and Fe(III)-bearing clay minerals as terminal electron acceptors for anaerobic respiration [20][21][22][23][24][25][26][27][28].”

    From Electron Donor Utilization and Secondary Mineral Formation during the Bioreduction of Lepidocrocite by Shewanella putrefaciens CN32 (2019) · cites this paper as [20]

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Research works printed but not linked: 42

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  23. Lovley, 1986, Availability of ferric iron for microbial reduction in bottom sediments of the freshwater tidal Potomac River, Appl. Environ. Microbiol., 52, 751, 10.1128/AEM.52.4.751-757.1986 · DOI
  24. Lovley, 1987, Competitive mechanisms for inhibition of sulfate reduction and methane production in the zone of ferric iron reduction in sediments, Appl. Environ. Microbiol., 53, 2636, 10.1128/AEM.53.11.2636-2641.1987 · DOI
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Metadata

Authors
Cutting, R. S., Coker, V. S., Fellowes, J. W., Lloyd, J. R., & Vaughan, D. J.
Venue
Geochimica et Cosmochimica Acta
Publisher
Elsevier BV
Published
2009-07
Volume
73
Issue
14
Pages
4004-4022
ISSN
0016-7037
DOI
10.1016/j.gca.2009.04.009
Cited by
198
References
6
Language
en
Licence
www.elsevier.com/tdm/userlicense/1.0/ (tdm)

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