Isolation and Characterization of Novel Psychrophilic, Neutrophilic, Fe-Oxidizing, Chemolithoautotrophic α- and γ-Proteobacteria from the Deep Sea

By Katrina J. Edwards, Daniel R. Rogers, C. Wirsen, T. McCollom. Applied and Environmental Microbiology, 2003

306 citations recorded by the source corpus.

Subfields: Environmental Chemistry, Environmental Engineering, Geochemistry and Petrology

View Paper: https://www.semanticscholar.org/paper/df39d44aafc78f84df0e9ea3f5dcf485553cbe52

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Environmental Chemistry

1. Jeremy A. Rentz
2. K. Straub
3. Y. Bashan
4. A. Kappler

In Environmental Engineering

1. A. Kappler
2. Jeremy A. Rentz
3. J. Weiss
4. K. Edwards
5. D. Emerson
6. J. Coates
7. K. Straub
8. L. Achenbach

In Geochemistry and Petrology

1. Jeremy A. Rentz
2. A. Kappler
3. J. Weiss
4. K. Edwards
5. D. Emerson

Citations in the corpus

• Microorganisms pumping iron: anaerobic microbial iron oxidation and reduction (2006, background): “Microaerophilic FOM capable of competing with the abiotic oxidation kinetics between oxygen and Fe( II ) have been shown to contribute to iron cycling in oxic environments, coupling this metabolism to growt”
• 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): “This capacity for lithotrophic growth appears to be common across known circumneutral FeOB, including Gallionella ferruginea (Hallbeck and Pederson 1991), and organisms enriched from the wetland rhizosphere [this study, (Sobolev and Roden 2004)], groundwater springs (Emerson and Moyer 1997), and mar”
• 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).”
• Bacterial Iron Oxidation in Circumneutral Freshwater Habitats: Findings from the Field and the Laboratory (2004, background): “Recently, Edwards and coworkers have isolated several novel strains of marine FeOB associated with weathered basalts on the seafloor ( Edwards, Rogers, Wirsen, and McCollom 2003 ); these strains, in addition to using soluble Fe(II), can also grow on Fe(II)-bearing minerals.”
• New insigths on the metabolic diversity among the epibiotic microbial communitiy of the hydrothermal shrimp Rimicaris exoculata (2008, background): “301 All the sequences are related to the Proteobacteria cluster (figure 7), mainly within the 302 Epsilon and Gamma groups, the Alpha and Deltaproteobacteria being less abundant.”
• Neutrophilic Iron-Oxidizing Bacteria in the Ocean: Their Habitats, Diversity, and Roles in Mineral Deposition, Rock Alteration, and Biomass Production in the Deep-Sea (2004, methodology): “Interestingly, OTU1 falls within the Marinobacter/Halomonas grouping, and is very closely related to some of the deep-sea Fe-oxidizing strains from Edwards et al. (2003b) (Figure 4).”
• Fe(III) mineral formation and cell encrustation by the nitrate‐dependent Fe(II)‐oxidizer strain BoFeN1 (2005, background): “2005) and neutrophilic, O2-dependent Fe(II) oxidizers (Emerson & Moyer, 1997; Edwards et al., 2003).”
• Rock-degrading endophytic bacteria in cacti (2009, background): “Additionally, iron and sulfides in rocks can be oxidized by bacteria and be transformed into newminerals at great sea depths and in deserts (Bach and Edwards, 2003; Bawden et al., 2003; Edwards et al., 2003; Hossner and Doolittle, 2003).”