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Science 27 May 2005: Vol. 308. no. 5726, pp. 1305 - 1308 DOI: 10.1126/science.1110832
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Reports
A Microbial Arsenic Cycle in a Salt-Saturated, Extreme Environment
Ronald S. Oremland,1*
Thomas R. Kulp,1
Jodi Switzer Blum,1
Shelley E. Hoeft,1
Shaun Baesman,1
Laurence G. Miller,1
John F. Stolz2
Searles Lake is a salt-saturated, alkaline brine unusually rich in the toxic element arsenic. Arsenic speciation changed from arsenate [As(V)] to arsenite [As(III)] with sediment depth. Incubated anoxic sediment slurries displayed dissimilatory As(V)-reductase activity that was markedly stimulated by H 2 or sulfide, whereas aerobic slurries had rapid As(III)-oxidase activity. An anaerobic, extremely haloalkaliphilic bacterium was isolated from the sediment that grew via As(V) respiration, using either lactate or sulfide as its electron donor. Hence, a full biogeochemical cycle of arsenic occurs in Searles Lake, driven in part by inorganic electron donors.
1 U.S. Geological Survey, ms 480, 345 Middlefield Road, Menlo Park, CA 94025, USA.
2 Department of Biological Science, Duquesne University, Pittsburgh, PA 15282, USA.
* To whom correspondence should be addressed. E-mail: roremlan{at}usgs.gov
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