<?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>J. S. Gilmore</dc:contributor>
  <dc:contributor>J.D. Knight</dc:contributor>
  <dc:contributor>C. L. Pillmore</dc:contributor>
  <dc:contributor>R.H. Tschudy</dc:contributor>
  <dc:contributor>J.E. Fassett</dc:contributor>
  <dc:creator>C. J. Orth</dc:creator>
  <dc:date>1981</dc:date>
  <dc:description>&lt;p&gt;An iridium abundance anomaly, with concentrations up to 5000 parts per trillion over a background level of 4 to 20 parts per trillion, has been located in sedimentary rocks laid down under freshwater swamp conditions in the Raton Basin of northeastern New Mexico. The anomaly occurs at the base of a coal bed, at the same stratigraphic position at which several well-known species of Cretaceous-age pollen became extinct.&amp;nbsp;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.214.4527.1341</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Association for the Advancement of Science</dc:publisher>
  <dc:title>An iridium abundance anomaly at the palynological Cretaceous-Tertiary boundary in northern New Mexico</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>