HR: 11:20h
AN: P42B-05    [Abstracts]
TI: Arsenophilic Bacterial Processes in Searles Lake: A Salt-saturated, Arsenic-rich, Alkaline Soda Lake.
AU: * Oremland, R S
EM: roremlan@usgs.gov
AF: US Geological Survey, 345 Middlefield Road, Menlo Park, CA 94025
AU: Kulp, T R
EM: trkulp@usgs.gov
AF: US Geological Survey, 345 Middlefield Road, Menlo Park, CA 94025
AU: Hoeft, S E
EM: sehoeft@usgs.gov
AF: US Geological Survey, 345 Middlefield Road, Menlo Park, CA 94025
AU: Miller, L G
EM: lgmiller@usgs.gov
AF: US Geological Survey, 345 Middlefield Road, Menlo Park, CA 94025
AU: Swizer Blum, J
EM: jsblum@usgs.gov
AF: US Geological Survey, 345 Middlefield Road, Menlo Park, CA 94025
AU: Stolz, J F
EM: stolz@duq.edu
AF: Department of Biological Sciences, Duquesne University, Pittsburgh, PA 15282
AB: Searles Lake, located in the Mojave Desert of California, is essentially a chemically-similar, concentrated version of Mono Lake, but having a much higher salinity (e.g., 340 vs. 90 g/L) and a greater dissolved inorganic arsenic content in its brine (e.g., 3.9 vs. 0.2 mM). The source of all this arsenic ultimately comes from hydrothermal spring inputs, thereby underscoring the importance of volcanic and fluvial processes in transporting this toxic element into these closed basin lakes. Nonetheless, the presence of microbial activities with regard to respiration of arsenate oxyanions under anaerobic conditions and the oxidation of arsenite oxyanions under aerobic conditions can be inferred from porewater profiles taken from handcores retrieved beneath Searles Lake's salt crust. Sediment slurry incubations confirmed biological arsenate respiration and arsenite oxidation, with the former processes notably enhanced by provision of the inorganic electron donor sulfide or H2. Hence, arsenic-linked chemo-autotrophy appears to be an important means of carbon fixation in this system. Subsequent efforts using 73As-arsenate as radiotracer detected dissimilatory arsenate reduction activity down the length of the core, but we were unable to detect any evidence for sulfate-reduction using 35S-sulfate. An extremely halophilic anaerobic bacterium of the order Haloanaerobiales [strain SLAS-1] was isolated from the sediments that grew via arsenate respiration using lactate or sulfide as its electron donors. These results show that, unlike sulfate-reduction, arsenic metabolism (i.e., both oxidation of arsenite and dissimilatory reduction of arsenate) is operative and even vigorous under the extreme conditions of salt-saturation and high pH. The occurrence of arsenophilic microbial processes in Searles Lake is relevant to the search for extant or extinct microbial life on Mars. It is evident from surface imagery that Mars had past episodes of volcanism, fluvial transport, and most likely brine concentration reactions (e.g., evapo- and cryo-concentration) occurring in its early Noachian/Hesperian epochs. We speculate that these processes may have created arsenic-rich, dense brines on the Martian surface or even within its underlying regolith. Whether such brines persisted long enough for prokaryotic life to evolve in them, and if so, was such life capable of adapting to and exploiting arsenic redox reactions for the purpose of generating metabolic energy remain tantalizing, but still hypothetical questions.
DE: 0406 Astrobiology and extraterrestrial materials
DE: 0448 Geomicrobiology
DE: 0456 Life in extreme environments
DE: 0461 Metals
DE: 0471 Oxidation/reduction reactions (4851)
SC: Planetary Sciences [P]
MN: Fall Meeting 2005