In this study with the model organism Agrobacterium tumefaciens, we used a combination of lacZ gene fusions, reverse transcriptase PCR (RT-PCR), and deletion and insertional inactivation mutations to show unambiguously that the alternative sigma factor RpoN participates in the regulation of As III oxidation. A deletion mutation that removed the RpoN binding site from the aioBA promoter and an aacC3 (gentamicin resistance) cassette insertional inactivation of the rpoN coding region eliminated aioBA expression and As III oxidation, although rpoN expression was not related to cell exposure to As III . Putative RpoN binding sites were identified throughout the genome and, as examples, included promoters for aioB, phoB1, pstS1, dctA, glnA, glnB, and flgB that were examined by using qualitative RT-PCR and lacZ reporter fusions to assess the relative contribution of RpoN to their transcription. The expressions of aioB and dctA in the wild-type strain were considerably enhanced in cells exposed to As III , and both genes were silent in the rpoN::aacC3 mutant regardless of As III . The expression level of glnA was not influenced by As III but was reduced (but not silent) in the rpoN::aacC3 mutant and further reduced in the mutant under N starvation conditions. The rpoN::aacC3 mutation had no obvious effect on the expression of glnB, pstS1, phoB1, or flgB. These experiments provide definitive evidence to document the requirement of RpoN for As III oxidation but also illustrate that the presence of a consensus RpoN binding site does not necessarily link the associated gene with regulation by As III or by this sigma factor. E vidence of microbial arsenite (As III ) oxidation was first reported nearly a century ago (18). Subsequent progress has been sporadic, with work that identified some organisms capable of As III oxidation (46,48,60) and then a study of a Pseudomonas arsenitoxidans strain reported to grow chemolithoautotrophically with As III as a sole electron donor (23). Subsequent follow-up characterizations of this organism and this process failed to materialize; however, approximately 2 decades later, Santini et al. (52) described the isolation and initial characterization of a Rhizobiumlike bacterium (strain NT-26) that could grow chemolithoautotrophically with As III as a sole electron donor for energy generation and with CO 2 as a sole carbon source. Soon thereafter, and in part stimulated by the massive arsenic poisoning disaster in Bangladesh (2), a series of studies initiated the characterization of microbial As III oxidation in natural environments, including geothermal springs (9,11,12,17,19,24,25,35,51) and soils (41); in mining-contaminated environments (6, 13, 40); and, most recently, in anoxic photosynthesis (21, 33). Likewise, progress has been made in the understanding of the biochemistry of the As III oxidase enzyme (1,14,37 oxidase structural genes were later cloned from the above-mentioned Rhizobium NT-26 organism (53). The symbols for genes coding for functions associated with As III oxidation have...