<?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>M. M. Schnepfe</dc:contributor>
  <dc:contributor>C.C. Silber</dc:contributor>
  <dc:contributor>F.O. Simon</dc:contributor>
  <dc:creator>Z. S. Altschuler</dc:creator>
  <dc:date>1983</dc:date>
  <dc:description>The pattern of sulfur transformation in peat across the Everglades basin indicates that pyrite formation in organic-rich swamps depends on the use of organic oxysulfur compounds in dissimilatory respiration by sulfur-reducing bacteria. This paragenesis explains the primary distribution of sulfur compounds in low-sulfur coals and possibly in most coals and many organic-rich soils and sediments. It also accounts for the occurrence of framboidal pyrite bound in fossil tissue in coal and sediments.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.221.4607.221</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Association for the Advancement of Science</dc:publisher>
  <dc:title>Sulfur diagenesis in Everglades peat and origin of pyrite in coal</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>