<?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.G. Zreda</dc:contributor>
  <dc:contributor>L. V. Benson</dc:contributor>
  <dc:contributor>M.A. Plummer</dc:contributor>
  <dc:contributor>D. Elmore</dc:contributor>
  <dc:contributor>Prakash Sharma</dc:contributor>
  <dc:creator>F. M. Phillips</dc:creator>
  <dc:date>1996</dc:date>
  <dc:description>Mountain glaciers, because of their small size, are usually close to equilibrium with the local climate and thus should provide a test of whether temperature oscillations in Greenland late in the last glacial period are part of global-scale climate variability or are restricted to the North Atlantic region. Correlation of cosmogenic chlorine-36 dates on Sierra Nevada moraines with a continuous radiocarbon-dated sediment record from nearby Owens Lake shows that Sierra Nevada glacial advances were associated with Heinrich events 5, 3, 2, and 1.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.274.5288.749</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Chronology for fluctuations in late Pleistocene Sierra Nevada glaciers and lakes</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>