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Controls on Fe reduction and mineral formation by a subsurface bacterium

Glasauer, Susan, Weidler, Peter G, Langley, Sean, Beveridge, Terry J·2003·Geochimica et Cosmochimica Acta
DOI 10.1016/s0016-7037(02)01199-7
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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 [35]

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Metadata

Authors
Glasauer, S., Weidler, P. G., Langley, S., & Beveridge, T. J.
Venue
Geochimica et Cosmochimica Acta
Publisher
Elsevier BV
Published
2003-04
Volume
67
Issue
7
Pages
1277-1288
ISSN
0016-7037
DOI
10.1016/s0016-7037(02)01199-7
Cited by
183
References
3
Language
en
Licence
www.elsevier.com/tdm/userlicense/1.0/ (tdm)

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