Characterization of a Neutrophilic, Chemolithoautotrophic Fe(II)-Oxidizing β -Proteobacterium from Freshwater Wetland Sediments
By D. Sobolev, E. Roden. 2004
108 citations recorded by the source corpus.
Subfields: Environmental Engineering, Health, Toxicology and Mutagenesis, Pollution
View Paper: https://www.semanticscholar.org/paper/eb09f28cb8b59149d23b6aa14966381066f33115
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Citations in the corpus
- Fe(III) mineral formation and cell encrustation by the nitrate‐dependent Fe(II)‐oxidizer strain BoFeN1 (2005, background): “While it was demonstrated that phototrophic and microaerophilic Fe(II) oxidizers are truly lithoautotrophic microorganisms (Ehrenreich & Widdel, 1994; Emerson & Moyer, 1997; Sobolev & Roden, 2004 ), most nitrate-dependent Fe(II) oxidizers isolated so far need an organic cosubstrate for growth (Stra”
- Geomicrobiological cycling of iron (2005, background): “Representatives of the a-, ß- and y-subgroup of Proteobacteria were isolated flom groundwater, deep sea sediments and freshwater wetland sampIes (Emerson and Moyer 1997; Edwards et al. 2003; Sobolev and Roden 2004).”
- Characterization of Neutrophilic Fe(II)-Oxidizing Bacteria Isolated from the Rhizosphere of Wetland Plants and Description of Ferritrophicum radicicola gen. nov. sp. nov., and Sideroxydans paludicola sp. nov. (2007, background): “In addition, the isolation of new unicellular chemolithotrophic Fe(II)-oxidizing bacteria (FeOB) have been reported (Emerson and Moyer 2002; Edwards et al. 2003; Sobolev and Roden 2004 ).”
- Potential for Microscale Bacterial Fe Redox Cycling at the Aerobic-Anaerobic Interface (2004, methodology): “Emerson and Moyer (1997) found that FeOB do not alter the rate of Fe(III) oxide accumulation in circumneutral pH diffusion-controlled opposing-gradient culture systems, a result verified by our own studies with opposing-gradient FeOB cultures (Sobolev and Roden 2004).”
- Bacterial Iron Oxidation in Circumneutral Freshwater Habitats: Findings from the Field and the Laboratory (2004, unknown): “Recent work by Sobolev and Roden (2004) described a new Fe-oxidizing bacterium (TW-2) that was isolated using the gradient tube method from the sediments of a wetland in Alabama with very high Fe(II) concentrations in the underlying pore water.”
- Returning to Their Roots: Iron-Oxidizing Bacteria Enhance Short-Term Plaque Formation in the Wetland-Plant Rhizosphere (2007, background): “However, other studies have reported that Fe(III) accumulation rates in diffusion-limited gradient cultures did not differ between +FeOB cultures and abiotic controls (Emerson and Moyer 1997; Sobolev and Roden 2004 ).”