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Applied and Environmental Microbiology, August 2007, p. 5130-5137, Vol. 73, No. 16
0099-2240/07/$08.00+0     doi:10.1128/AEM.00771-07
Copyright © 2007, American Society for Microbiology. All Rights Reserved.

Effects of Imposed Salinity Gradients on Dissimilatory Arsenate Reduction, Sulfate Reduction, and Other Microbial Processes in Sediments from Two California Soda Lakes{triangledown} ,{dagger}

T. R. Kulp,1* S. Han,2 C. W. Saltikov,3 B. D. Lanoil,2 K. Zargar,3 and R. S. Oremland1

U.S. Geological Survey, Menlo Park, California 94025,1 Department of Environmental Sciences, University of California at Riverside, Riverside, California 92521,2 Department of Environmental Toxicology, University of California at Santa Cruz, Santa Cruz, California 950643

Received 5 April 2007/ Accepted 19 June 2007

Salinity effects on microbial community structure and on potential rates of arsenate reduction, arsenite oxidation, sulfate reduction, denitrification, and methanogenesis were examined in sediment slurries from two California soda lakes. We conducted experiments with Mono Lake and Searles Lake sediments over a wide range of salt concentrations (25 to 346 g liter–1). With the exception of sulfate reduction, rates of all processes demonstrated an inverse relationship to total salinity. However, each of these processes persisted at low but detectable rates at salt saturation. Denaturing gradient gel electrophoresis analysis of partial 16S rRNA genes amplified from As(V) reduction slurries revealed that distinct microbial populations grew at low (25 to 50 g liter–1), intermediate (100 to 200 g liter–1), and high (>300 g liter–1) salinity. At intermediate and high salinities, a close relative of a cultivated As-respiring halophile was present. These results suggest that organisms adapted to more dilute conditions can remain viable at high salinity and rapidly repopulate the lake during periods of rising lake level. In contrast to As reduction, sulfate reduction in Mono Lake slurries was undetectable at salt saturation. Furthermore, sulfate reduction was excluded from Searles Lake sediments at any salinity despite the presence of abundant sulfate. Sulfate reduction occurred in Searles Lake sediment slurries only following inoculation with Mono Lake sediment, indicating the absence of sulfate-reducing flora. Experiments with borate-amended Mono Lake slurries suggest that the notably high (0.46 molal) concentration of borate in the Searles Lake brine was responsible for the exclusion of sulfate reducers from that ecosystem.


* Corresponding author. Mailing address: U.S. Geological Survey, Water Resources Division, 345 Middlefield Rd., Mailstop 480, Menlo Park, CA 94025. Phone: (650) 329-4473. Fax: (650) 329-4463. E-mail: trkulp{at}usgs.gov

{triangledown} Published ahead of print on 29 June 2007.

{dagger} Supplemental material for this article may be found at http://aem.asm.org/.


Applied and Environmental Microbiology, August 2007, p. 5130-5137, Vol. 73, No. 16
0099-2240/07/$08.00+0     doi:10.1128/AEM.00771-07
Copyright © 2007, American Society for Microbiology. All Rights Reserved.







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