<?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>T. M. Cronin</dc:contributor>
  <dc:contributor>R.Z. Poore</dc:contributor>
  <dc:contributor>R.S. Thompson</dc:contributor>
  <dc:contributor>R.C. Whatley</dc:contributor>
  <dc:contributor>A.M. Wood</dc:contributor>
  <dc:creator>H.J. Dowsett</dc:creator>
  <dc:date>1992</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;The Middle Pliocene (∼3 million years ago) has been identified as the last time the Earth was significantly warmer than it was during the Last Interglacial and Holocene. A quantitative micropaleontological paleotemperature transect from equator to high latitudes in the North Atlantic indicates that Middle Pliocene warmth involved increased meridional oceanic heat transport.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.258.5085.1133</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Association for the Advancement of Science</dc:publisher>
  <dc:title>Micropaleontological evidence for increased meridional heat transport in the North Atlantic Ocean during the pliocene</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>