Microorganisms in the family Geobacteraceae are the predominant Fe(III)-reducing microorganisms in a variety of subsurface environments in which Fe(III) reduction is an important process, but little is known about the mechanisms for electron transport to Fe(III) in these organisms. The Geobacter sulfurreducens genome was found to contain a 10-kb chromosomal duplication consisting of two tandem three-gene clusters. The last genes of the two clusters, designated omcB and omcC, encode putative outer membrane polyheme c-type cytochromes which are 79% identical. The role of the omcB and omcC genes in Fe(III) reduction in G. sulfurreducens was investigated. OmcB and OmcC were both expressed during growth with acetate as the electron donor and either fumarate or Fe(III) as the electron acceptor. OmcB was ca. twofold more abundant under both conditions. Disrupting omcB or omcC by gene replacement had no impact on growth with fumarate. However, the OmcB-deficient mutant was greatly impaired in its ability to reduce Fe(III) both in cell suspensions and under growth conditions. In contrast, the ability of the OmcC-deficient mutant to reduce Fe(III) was similar to that of the wild type. When omcB was reintroduced into the OmcB-deficient mutant, the capacity for Fe(III) reduction was restored in proportion to the level of OmcB production. These results indicate that OmcB, but not OmcC, has a major role in electron transport to Fe(III) and suggest that electron transport to the outer membrane is an important feature in Fe(III) reduction in this organism.Microbial oxidation of organic matter coupled to the reduction of Fe(III) plays an important role in the degradation of natural and contaminant organic matter in aquatic sediments and the subsurface, and this process influences the mobility of a variety of trace metals in these environments (for reviews, see references 23 and 24). Insoluble Fe(III) oxides, which are the primary form of Fe(III) in most soils and sediments, are unlike commonly considered electron acceptors such as oxygen, nitrate, fumarate, sulfate, and carbon dioxide, which are soluble and can readily enter a cell to be reduced. If, as is generally considered to be the case (23, 43), Fe(III)-reducing microorganisms reduce extracellular Fe(III), then electron transport to Fe(III) is likely to proceed via mechanisms significantly different from those for the reduction of soluble electron acceptors.Furthermore, phylogenetically distinct Fe(III) reducers might reduce Fe(III) oxides via significantly different mechanisms. For example, Geothrix fermentans and Shewanella species produce soluble electron shuttles and/or Fe(III)-chelating compounds which alleviate the need for contact between cells and insoluble Fe(III) for Fe(III) reduction (38)(39)(40)54). Others, such as Geobacter metallireducens, do not produce electron shuttles or Fe(III) chelators (37) but utilize appendages such as flagella and pili to search for or to make direct contact with insoluble Fe(III) (6).The mechanisms for Fe(III) reduction in Geobacte...