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. 2016 Jul 15;31(3):293–298. doi: 10.1264/jsme2.ME16001

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Copyright © 2016 by Japanese Society of Microbial Ecology / Japanese Society of Soil Microbiology / Taiwan Society of Microbial Ecology / Japanese Society of Plant Microbe Interactions.

This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

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Fig. 1 — Occurrence of anaerobic, nitrate-dependent Fe(II) oxidation by Pseudogulbenkiania sp. strain NH8B. Washed cells (5 × 10⁷ cells) were inoculated into anoxic basal medium supplemented with 10 mM FeCl₂ and 5 mM NaNO₃, and incubated under anoxic conditions at 30°C for 10 d. Legends: Concentrations of Fe(II) ( ), Fe(III) (○), NO₃ ⁻ ( ), and NO₂ ⁻ (△). The mean ± SD is shown.

Inline graphic — Occurrence of anaerobic, nitrate-dependent Fe(II) oxidation by Pseudogulbenkiania sp. strain NH8B. Washed cells (5 × 10⁷ cells) were inoculated into anoxic basal medium supplemented with 10 mM FeCl₂ and 5 mM NaNO₃, and incubated under anoxic conditions at 30°C for 10 d. Legends: Concentrations of Fe(II) ( ), Fe(III) (○), NO₃ ⁻ ( ), and NO₂ ⁻ (△). The mean ± SD is shown.