<?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>John Oro</dc:contributor>
  <dc:contributor>P. Toulmin III</dc:contributor>
  <dc:contributor>Leslie E. Orgel</dc:contributor>
  <dc:contributor>A.O. Nier</dc:contributor>
  <dc:contributor>D.M. Anderson</dc:contributor>
  <dc:contributor>P.G. Simmonds</dc:contributor>
  <dc:contributor>D. Flory</dc:contributor>
  <dc:contributor>A.V. Diaz</dc:contributor>
  <dc:contributor>D.R. Rushneck</dc:contributor>
  <dc:contributor>J.A. Biller</dc:contributor>
  <dc:creator>K. Biemann</dc:creator>
  <dc:date>1976</dc:date>
  <dc:description>Two surface samples collected from the Chryse Planitia region of Mars were heated to temperatures up to 500??C, and the volatiles that they evolved were analyzed with a gas chromatograph-mass spectrometer. Only water and carbon dioxide were detected. This implies that organic compounds have not accumulated to the extent that individual components could be detected at levels of a few parts in 109 by weight in our samples. Proposed mechanisms for the accumulation and destruction of organic compounds are discussed in the light of this limit.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.194.4260.72</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Association for the Advancement of Science</dc:publisher>
  <dc:title>Search for organic and volatile inorganic compounds in two surface samples from the chryse planitia region of Mars</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>