Novel strains of obligately chemolithoautotrophic, sulfur-oxidizing bacteria have been isolated from various depths of Lake Fryxell, Antarctica. Physiological, morphological, and phylogenetic analyses showed these strains to be related to mesophilic Thiobacillus species, such as T. thioparus. However, the psychrotolerant Antarctic isolates showed an adaptation to cold temperatures and thus should be active in the nearly freezing waters of the lake. Enumeration by most-probable-number analysis in an oxic, thiosulfate-containing medium revealed that the sulfur-oxidizing chemolithotroph population peaks precisely at the oxycline (9.5 m), although viable cells exist well into the anoxic, sulfidic waters of the lake. The sulfur-oxidizing bacteria described here likely play a key role in the biogeochemical cycling of carbon and sulfur in Lake Fryxell.The role of sulfur-oxidizing bacteria (SOB) in carbon and sulfur cycling has been well studied in both temperate and geothermal aquatic environments (1,17,29). Many metabolically and phylogenetically diverse organisms involved in sulfur cycling have been isolated in pure culture from these environments and characterized in detail (6,10,32,36). However, the same cannot be said for sulfur-oxidizing chemolithotrophs in permanently cold environments.Although SOB have been identified in cold environments (25, 37), well-characterized pure cultures of these organisms are rare. One exception is in the work of Knittel et al. (19), in which two psychrophilic Thiomicrospira species, T. arctica and T. psychrophila, from sediments off the coast of Svalbard were described. These organisms were the first psychrophilic, chemolithoautotrophic, sulfur-oxidizing bacteria isolated in pure culture. In contrast to those studies, which focused on new species of SOB from marine sediments, our work describes planktonic SOB from the water column of the permanently ice-covered Lake Fryxell, Antarctica.Lake Fryxell is one of the most productive of several lakes in the McMurdo Dry Valleys of southern Victoria Land, Antarctica (41). The lake is just over 18 m deep and has a length of about 5.5 km, a width of 2 km, and a surface area of approximately 7 km 2 (21). A salinity gradient ranging from freshwater to about 0.8% NaCl near the sediments is also present in the lake (21). In addition to the increasing density of the water with depth, a thick ice cover that is currently just over 6 m contributes to a highly stratified and amictic water column (27,41). Water directly beneath the ice cover is supersaturated with dissolved gases, including oxygen and carbon dioxide (31). However, dissolved oxygen levels decrease dramatically below 8 m, and the water column becomes anoxic below 10 m, soon after the appearance of sulfide at 9.5 m (15). The sulfide, a product of sulfate-reducing bacteria, diffuses up from the sediments and anoxic portions of the water column, with concentrations increasing with depth to more than 1 mM near the sediments (13).The gradients of oxygen and sulfide in Lake Fryxell should prov...