<?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>N. J. Shackleton</dc:contributor>
  <dc:contributor>A. A. Abdel-Monem</dc:contributor>
  <dc:contributor>J. D. Obradovich</dc:contributor>
  <dc:contributor>G. Izett</dc:contributor>
  <dc:creator>D. Ninkovich</dc:creator>
  <dc:date>1978</dc:date>
  <dc:description>The late Pleistocene eruption of Toba is the largest magnitude explosive eruption documented from the Quaternary. K-Ar dating of the uppermost unit of the Toba Tuff gives an age of [~amp]sim; 75,000 yr. A chemically and petrographically equivalent ash layer in deep-sea cores helps calibrate the Stage 4-5 boundary of the standard oxygen isotope stratigraphy. A similar ash in Malaya that overlies finds of Tampan Palaeolithic tools indicates that they are older than 75,000 yr. ?? 1978 Nature Publishing Group.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1038/276574a0</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>K-Ar age of the late Pleistocene eruption of Toba, north Sumatra</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>