<?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>Robert T. Anderson</dc:contributor>
  <dc:creator>Derek R. Lovely</dc:creator>
  <dc:date>2000</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Geobacter become dominant members of the microbial community when Fe(III)-reducing conditions develop as the result of organic contamination, or when Fe(III) reduction is artificially stimulated. These results suggest that further understanding of the ecophysiology of &lt;/span&gt;&lt;i class="EmphasisTypeItalic "&gt;Geobacter &lt;/i&gt;&lt;span&gt;species would aid in better prediction of the natural attenuation of organic contaminants under anaerobic conditions and in the design of strategies for the bioremediation of subsurface metal contamination.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/PL00010974</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Springer-Verlag</dc:publisher>
  <dc:title>Influence of dissimilatory metal reduction on fate of organic and metal contaminants in the subsurface</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>