<?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:creator>David P. Adam</dc:creator>
  <dc:date>1973</dc:date>
  <dc:description>&lt;p&gt;Fossil pollen was recovered at Tahoe City, Calif., from&amp;nbsp;beneath a 1.9-m.y.-old volcanic flow. Pollen counts of four fossil&amp;nbsp;samples are compared with soil-surface pollen samples from the Sierra&amp;nbsp;Nevada. The presence of &lt;i&gt;Picea&lt;/i&gt; (spruce) pollen in the fossil samples&amp;nbsp;suggests that summer drought conditions in the central Sierra Nevada&amp;nbsp;were less severe prior to 1.9 m.y. ago than they are now.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Early Pleistocene(?) pollen spectra from near Lake Tahoe, California</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>