Journal
GEOMICROBIOLOGY JOURNAL
Volume 26, Issue 2, Pages 93-103Publisher
TAYLOR & FRANCIS INC
DOI: 10.1080/01490450802660573
Keywords
Fe(II) oxidation; iron-cycling; geomicrobiology
Funding
- Emmy-Noether fellowship
- German Research Foundation (DFG)
- BMBF research grant [13N8652]
- Region Ile-de-France [SESAME 2000 E1435]
- [JEOL 2100F TEM]
- [IMPMC UMR 7590]
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Microbial anaerobic Fe(II) oxidation at neutral pH produces poorly soluble Fe(III) which is expected to bind to cell surfaces causing cell encrustation and potentially impeding cell metabolism. The challenge for Fe(II)-oxidizing prokaryotes therefore is to avoid encrustation with Fe(III). Using different microscopic techniques we tracked Fe(III) minerals at the cell surface and within cells of phylogenetically distinct phototrophic and nitrate-reducing Fe(II)-oxidizing bacteria. While some strains successfully prevented encrustation others precipitated Fe(III) minerals at the cell surface and in the periplasm. Our results indicate differences in the cellular mechanisms of Fe(II) oxidation, transport of Fe(II)/Fe(III) ions, and Fe(III) mineral precipitation.
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