Geobacter daltonii

Geobacter daltonii is a Gram-negative, Fe(III)-reducing, Uranium(IV)-reducing and non-spore-forming bacterium from the genus of Geobacter which has been isolated from sediments from the Oak Ridge Field Research Center in Oak Ridge, Tennessee in the United States.[1][3][4][5][6]

Geobacter daltonii
Scientific classification
Kingdom:
Bacteria
Phylum:
Proteobacteria
Class:
Deltaproteobacteria
Order:
Desulfuromonadales
Family:
Geobacteraceae
Genus:
Geobacter
Species:
G. daltonii
Binomial name
Geobacter daltonii
Prakash et al. 2010[1]
Type strain
DSM 22248, FRC-32, JCM 15807[2]

References
  1. Parte, A.C. "Geobacter". www.bacterio.net.
  2. "Geobacter daltonii Taxon Passport - StrainInfo". www.straininfo.net.
  3. "Geobacter daltonii". www.uniprot.org.
  4. Parker, Charles Thomas; Taylor, Dorothea; Garrity, George M. "Nomenclature Abstract for Geobacter daltonii Prakash et al. 2010". The NamesforLife Abstracts. doi:10.1601/nm.17822.
  5. "Details: DSM-22248". www.dsmz.de.
  6. Prakash, O; Gihring, TM; Dalton, DD; Chin, KJ; Green, SJ; Akob, DM; Wanger, G; Kostka, JE (March 2010). "Geobacter daltonii sp. nov., an Fe(III)- and uranium(VI)-reducing bacterium isolated from a shallow subsurface exposed to mixed heavy metal and hydrocarbon contamination". International Journal of Systematic and Evolutionary Microbiology. 60 (Pt 3): 546–53. doi:10.1099/ijs.0.010843-0. PMID 19654355.


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