Outer Cell Surface Components Essential for Fe(III) Oxide Reduction by Geobacter metallireducens
ABSTRACTGeobacterspecies are important Fe(III) reducers in a diversity of soils and sediments. Mechanisms for Fe(III) oxide reduction have been studied in detail inGeobacter sulfurreducens, but a number of the most thoroughly studied outer surface components ofG. sulfurreducens, particularlyc-type cytochromes, are not well conserved amongGeobacterspecies. In order to identify cellular components potentially important for Fe(III) oxide reduction inGeobacter metallireducens, gene transcript abundance was compared in cells grown on Fe(III) oxide or soluble Fe(III) citrate with whole-genome microarrays. Outer-surface cytochromes were also identified. Deletion of genes forc-type cytochromes that had higher transcript abundance during growth on Fe(III) oxides and/or were detected in the outer-surface protein fraction identified sixc-type cytochrome genes, that when deleted removed the capacity for Fe(III) oxide reduction. Several of thec-type cytochromes which were essential for Fe(III) oxide reduction inG. metallireducenshave homologs inG. sulfurreducensthat are not important for Fe(III) oxide reduction. Other genes essential for Fe(III) oxide reduction included a gene predicted to encode an NHL (Ncl-1–HT2A–Lin-41) repeat-containing protein and a gene potentially involved in pili glycosylation. Genes associated with flagellum-based motility, chemotaxis, and pili had higher transcript abundance during growth on Fe(III) oxide, consistent with the previously proposed importance of these components in Fe(III) oxide reduction. These results demonstrate that there are similarities in extracellular electron transfer betweenG. metallireducensandG. sulfurreducensbut the outer-surfacec-type cytochromes involved in Fe(III) oxide reduction are different.