Sb(III) oxidation was documented in an Agrobacterium tumefaciens isolate that can also oxidize As(III). Equivalent Sb(III) oxidation rates were observed in the parental wild-type organism and in two well-characterized mutants that cannot oxidize As(III) for fundamentally different reasons. Therefore, despite the literature suggesting that Sb(III) and As(III) may be biochemical analogs, Sb(III) oxidation is catalyzed by a pathway different than that used for As(III). Sb(III) and As(III) oxidation was also observed for an eukaryotic acidothermophilic alga belonging to the order Cyanidiales, implying that the ability to oxidize metalloids may be phylogenetically widespread.Antimony (Sb) occurs globally in fresh and marine waters and in soils, with the most common mineral form being stibnite (Sb 2 S 3 ) (6). Sb is typically found with arsenic (As), another group V element having similar chemistry and toxicity, and is recognized by the U.S. Environmental Protection Agency as a priority pollutant (8,14). Unlike microbe-As interactions, for which significant progress has been made in defining the genetics and physiology of microbial arsenite [As(III)] oxidation and arsenate [As(V)] reduction (reviewed in references 19 and 20), microbe-Sb interactions are poorly understood, and as a consequence, the geomicrobiology of Sb is as yet essentially undefined. Sb(III) biomethylation has been reported (5), but otherwise, reports of microbe-Sb redox interactions are restricted to studies of an organism referred to as Stibiobacter senarmontii and described as being capable of oxidizing the mineral senarmontite to form Sb 2 O 5 (reviewed in reference 6). In the intervening 3 decades, no further characterization or confirmation of this organism has been reported, nor have there been reports of other microorganisms having the capacity to oxidize Sb(III).Given the structural similarities between As and Sb, the presence of one could influence the biological interactions of the other (4). Indeed, both As(III) and Sb(III) will induce the microbial ars-based arsenic defense response (11), both are taken up via the same aquaglyceroporin channel, GlyF (16), and in bacteria they are both extruded by the same porter, ArsB (16). These observations suggest the possibility that the same enzymatic pathways used for As(III) oxidation may also be used for Sb(III). In recent studies regarding the genetics underlying As(III) oxidation in Agrobacterium tumefaciens, we discovered regulatory (aoxR) and Na ϩ :H ϩ antiporter (mrpB) mutants which are defective in As(III) oxidation (12, 13). In subsequent investigations, we found the wild-type A. tumefaciens strain to also be capable of oxidizing Sb(III). This provided an exceptional opportunity to directly determine whether As(III) oxidation and Sb(III) oxidation share similar enzymes.As and Sb speciation and analysis. Borohydride reductionbased speciation was used for both As and Sb analysis. As(III) speciation protocols were as previously described (10). At near-neutral pH, Sb(III) and methyl-Sb species...