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Arsenic (As) is an ubiquitous constituent in geothermal water. Arsenite (As III ) is oxidized via microbial processes as the waters equilibrate with oxygen in the geothermal effluent. The distribution of arsenite oxdizing bacteria and its correlation with environment factors were studied in Tengchong geothermal areas of Yunnan, China. A total of 230  aio A clone sequences were obtained and these sequences were affiliated with four phyla:  Betaproteobacteria ,  Alphaproteobacteria ,  Deinococcus-Thermus  and  Aquificae . Temperature was negatively correlated with  aio A diversity and was the only environment factor that had correlation with diversity index.  Betaproteobacteria  was mainly distributed in low temperature (T = 28 to 43 °C) and circumneutral or light alkaline (pH = 7 to 9) springs;  Alphaproteobacteria  was mainly predominant in low pH (pH = 3.3 to 3.6) springs;  Deinococcus-Thermus  and  Aquificae  mainly inhabited in high temperature (T=55 to 78 °C) springs with a wide range of pH. Usually,  Deinococcus-Thermus  was dominant when springs had a pH within 4.0 to 8.0.  Aquificae  was dominated in springs with pH &gt; 8.0 or pH &lt; 4.0.

Distribution of arsenite-oxidizing bacteria and its correlation with environmental factors in geothermal areas of Tengchong, Yunnan, China