<?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>C.E. Rostad</dc:contributor>
  <dc:contributor>T.J. Leiker</dc:contributor>
  <dc:contributor>D.M. Updegraff</dc:contributor>
  <dc:contributor>J.L. Bennett</dc:contributor>
  <dc:creator>W. E. Pereira</dc:creator>
  <dc:date>1988</dc:date>
  <dc:description>&lt;p&gt;Studies conducted in an aquifer contaminated by creosote suggest that quinoline is converted to 2(1H)quinolinone by an indigenous consortium of microorganisms. Laboratory microbial experiments using H&lt;sub&gt;2&lt;/sub&gt;&lt;sup&gt;18&lt;/sup&gt;O indicate that water is the source of the oxygen atom for this hydroxylation reaction under aerobic and anaerobic conditions.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1128/aem.54.3.827-829.1988</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Society for Microbiology</dc:publisher>
  <dc:title>Microbial hydroxylation of quinoline in contaminated groundwater: evidence for incorporation of the oxygen atom of water.</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>