<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>T.R. Kulp</dc:contributor>
  <dc:contributor>J.S. Blum</dc:contributor>
  <dc:contributor>S.E. Hoeft</dc:contributor>
  <dc:contributor>S. Baesman</dc:contributor>
  <dc:contributor>L.G. Miller</dc:contributor>
  <dc:contributor>J.F. Stolz</dc:contributor>
  <dc:creator>R.S. Oremland</dc:creator>
  <dc:date>2005</dc:date>
  <dc:description>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 H2 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.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.1110832</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>AAAS</dc:publisher>
  <dc:title>Microbiology: A microbial arsenic cycle in a salt-saturated, extreme environment</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>