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Use of Ferric and Ferrous Iron Containing Minerals for Respiration by Desulfitobacterium frappieri
Abstract
The potential of Desulfitobacterium frappieri strain G2, which was isolated from subsurface smectite bedding, to participate in iron redox reactions was investigated. Strain G2 can use poorly crystalline Fe(III) oxide, soluble forms of Fe(III) and Fe(III) in the structure of phyllosilicate minerals as electron acceptors. It can also oxidize Fe(II)-NTA or Fe(II) in the structure of phyllosilicate minerals with nitrate as the electron acceptor. These results suggest for the first time that strains of Desulfitobacterium frappieri may play an important role in iron cycling in sedimentary environments.
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“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 [21]
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Dissimilatory Fe(III) and Mn(IV) Reduction
Lovley, D. R., Holmes, D. E., & Nevin, K. P. (2004) · Advances in Microbial Physiology · doi:10.1016/s0065-2911(04)49005-5 · Cited by 1,471
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O’Loughlin, E. J., Gorski, C. A., Flynn, T. M., & Scherer, M. M. (2019) · Minerals · doi:10.3390/min9070434 · Cited by 28
Metadata
- Authors
- Shelobolina, E. S., VanPraagh, C. G., & Lovley, D. R.
- Venue
- Geomicrobiology Journal
- Publisher
- Informa UK Limited
- Published
- 2003-03
- Volume
- 20
- Issue
- 2
- Pages
- 143-156
- ISSN
- 0149-0451
- 1521-0529
- Cited by
- 106
- References
- 3
- Language
- en
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