Enumeration of Fe(II)-oxidizing and Fe(III)-reducing bacteria in the root zone of wetland plants: Implications for a rhizosphere iron cycle
By Johanna V. Weiss, D. Emerson, S. Backer, J. Megonigal. 2003
217 citations recorded by the source corpus.
Subfields: Geochemistry and Petrology, Plant Science, Renewable Energy, Sustainability and the Environment
View Paper: https://www.semanticscholar.org/paper/ce6fd8eecc45ff8bb102bb4132060d8fb3cbb366
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In Geochemistry and Petrology
In Plant Science
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Citations in the corpus
- Phylogenetic diversity of dissimilatory ferric iron reducers in paddy soil of Hunan, South China (2009, background): “Furthermore, numerous dissimilatory iron-reducing bacteria belonging to different phylogenetic groups have been described by both culture-dependent and -independent methods in various environments, including freshwater (Lovley and Phillips 1988), marine sediments (Roden and Lovley 1993), natural wet”
- Linking soil process and microbial ecology in freshwater wetland ecosystems (2006, background): “Iron reducing and oxidizing bacteria (IRB) have also been characterized in freshwater wetlands (Lowe et al. 2000; Kusel et al. 2003; Weiss et al. 2003; Emerson et al. 1999).”
- SEASONAL PATTERNS AND PLANT‐MEDIATED CONTROLS OF SUBSURFACE WETLAND BIOGEOCHEMISTRY (2005, unknown): “Furthermore, Fe(III) oxides in the root zone are more amorphous than oxides in bulk soil (Weiss et al. 2004), and both Fe(II)-oxidizing and Fe(III)-reducing bacteria are proportionally more abundant on the root surface than in bulk soil (Weiss et al. 2003).”
- Bacterial Iron Oxidation in Circumneutral Freshwater Habitats: Findings from the Field and the Laboratory (2004, background): “Two strains, ES-1 and ES-2, were isolated from groundwater in Michigan that contained approximately 10µM Fe(II) and had a pH of 7.1 (Emerson and Moyer 1997).”
- 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): “The samples used to enrich FeOB from the rhizosphere were obtained as part of a larger survey on the presence of FeOB in association with wetland plants in the Middle Atlantic region of the United States (Weiss et al. 2003).”
- Acquisition and Homeostasis of Iron in Higher Plants and Their Probable Role in Abiotic Stress Tolerance (2018, background): “…1964, 1967; Bacha and Hossner, 1977; Chen et al., 1980; Mendelssohn and Postek, 1982; Davison and Seed, 1983; Taylor and Crowder, 1983; Taylor et al., 1984; Levan and Riha, 1986; Greipsson and Crowder, 1992; Emerson et al., 1999; Hansel et al., 2001; Weiss et al., 2003; Emamverdian et al., 2015).”
- Potential for Microscale Bacterial Fe Redox Cycling at the Aerobic-Anaerobic Interface (2004, background): “It is important to acknowledge that our findings with strain TW2 may not necessarily apply to other phylogenetically and physiologically different neutrophilic FeOB, in particular the unicellular FeOB from the γ -subclass of the Proteobacteria that have been isolated from a variety of environments b”
- Control by fiddler crabs (Uca vocans) and plant roots (Avicennia marina) on carbon, iron, and sulfur biogeochemistry in mangrove sediment (2006, background): “Most, if not all, of this rhizosphere O2 is utilized for microbial and chemical oxidation of reduced iron and sulfide rather than for aerobic degradation (Roden and Wetzel 1996; Weiss et al. 2003).”
- Returning to Their Roots: Iron-Oxidizing Bacteria Enhance Short-Term Plaque Formation in the Wetland-Plant Rhizosphere (2007, background): “A survey of mid-Atlantic (USA) wetlands and aquatic habitats revealed that these FeOB are widespread and may comprise up to 5% of the total microbial community in the wetland rhizosphere (Weiss et al. 2003).”