Isolation and Taxonomic Characterization of a Halotolerant, Facultatively Iron-reducing Bacterium
References (27)
- et al.
Gene organization and primary structure of a ribosomal RNA operon from Escherichia coll
J. Molec. Biol.
(1981) - et al.
Phylogeny of the Vibrionaceae, and recommendation for two new genera, Listonella and Shewanella
System. Appl. Microbiol.
(1985) - et al.
Phylogenetic oligodeoxynucleotide probes for the major subclasses of Proteobacteria: problems and solutions
System. Appl. Microbiol.
(1992) - et al.
Polar lipids, fatty acids, and isoprenoid quinones of Alteromonas putrefaciens (Shewanella putrefaciens)
System. Appl. Microbiol.
(1987) - et al.
Nitrous oxide producing heterotrophic bacteria from the water column of the central Baltic: abundance and molecular identification
Mar. Ecol. Prog. Ser.
(1993) - et al.
A hydrogen-oxidizing, Fe(III)-reducing microorganism from the Great Bay Estuary, New Hampshire
Appl. Environ. Microbiol.
(1992) - et al.
Design and application of rRNA-tergeted oligonucleotide probes for the dissimilatory iron- and Manganese-reducing bacterium Shewanella putrefaciens
Appl. Environ. Microbiol.
(1993) Numerical methods for inferring phylogenetic trees
Quart. Rev. Biol.
(1982)- et al.
The ribosomal database project
Nucl. Acids Res.
(1993) - et al.
Potential risks of gene amplification by PCR as determined by 16S rDNA analysis of a mixed-culture of strict barophilic bacteria
Microb. Ecol.
(1991)
Clinical strains of Enterobacter agglomerans (synonyms: Erwinia herbicola, Erwinia milletiae) identified by DNA-DNA-hybridization
Acta Path. Microbiol. Immunol. Scand. Sect. B.
Dissimilatory Fe(III) and Mn(IV) reduction
Microbiol. Rev.
Geobacter metallireducans gen. nov. sp. nov., a microorganism capable of coupling the complete oxidation of organic compounds to the reduction of iron and other metals
Arch. Microbiol.
Cited by (75)
Exploring the links between bacterial communities and magnetic susceptibility in bulk soil and rhizosphere of beech (Fagus sylvatica L.)
2019, Applied Soil EcologyCitation Excerpt :Bacterial siderophores are low-molecular-weight (<10 kDa) molecules (Sah and Singh, 2015), whose function is to chelate Fe3+ and to reduce it to the more soluble Fe2+ form (Guerinot, 1994). Several Fe-reducing bacteria have been isolated from soil samples in the past (e.g., Fischer, 1988; Rossellomora et al., 1995), revealing a key role in the pedogenic formation of ultrafine grained magnetite and extracellular excretion of Fe2+ (Maher, 1991). This latter process is crucial to increase Fe availability in soil and, consequently, to enhance plant growth (e.g., Lankford, 1973; Hider and Kong, 2010), since concentrations of available Fe ranging from 10−9 to 10−4 M are needed for a normal plant growth (Romheld and Marschner, 1981; Lindsay and Schwab, 1982).
Isolation of Shewanella algae from rectal swabs of patients with bloody diarrhoea
2011, Indian Journal of Medical MicrobiologyMagnetic mineralogy of soils across the Russian Steppe: Climatic dependence of pedogenic magnetite formation
2003, Palaeogeography, Palaeoclimatology, PalaeoecologyCarbon isotope signatures of fatty acids in Geobacter metallireducens and Shewanella algae
2003, Chemical GeologyCitation Excerpt :The distribution of fatty acids in BrY and MR-4 was significantly different from the distribution of fatty acids in BrY (Rossello-Mora et al., 1994) and other S. putrefaciens species (Moule and Wilkinson, 1987; Venkateswaran et al., 1999) grown on multiple carbon sources such as the nutrient agar. In studies by Moule and Wilkinson (1987) and Rossello-Mora et al. (1994), the fatty acids were dominated by odd-number components (i15:0, 15:0, and 17:1ω9c), which were low in abundance in Teece et al. (1999) and this study (Table 1). This suggests that different substrates can affect the composition of fatty acids in the same bacterial species.