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Biotransformation of lepidocrocite in the presence of quinones and flavins
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“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 [43]
In the citing paper
“Vivianite formation requires the presence of substantial phosphate (e.g., vivianite was not observed at P:Fe rations lower than 0.08 [33,43,48,63]), and vivianite was not observed in any of our experimental systems (P:Fe = 0.005 [63]).”
From Electron Donor Utilization and Secondary Mineral Formation during the Bioreduction of Lepidocrocite by Shewanella putrefaciens CN32 (2019) · cites this paper as [43]
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Humic substances as electron acceptors for microbial respiration
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Fredrickson, J. K., Zachara, J. M., Kennedy, D. W., Dong, H., Onstott, T. C., Hinman, N. W., & Li, S.-M. (1998) · Geochimica et Cosmochimica Acta · doi:10.1016/s0016-7037(98)00243-9 · Cited by 807
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Sorted by citations
O’Loughlin, E. J., Gorski, C. A., Flynn, T. M., & Scherer, M. M. (2019) · Minerals · doi:10.3390/min9070434 · Cited by 28
Metadata
- Authors
- Bae, S., & Lee, W.
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 2013-08
- Volume
- 114
- Pages
- 144-155
- ISSN
- 0016-7037
- Cited by
- 39
- References
- 2
- Language
- en
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