<?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>E. Barrera</dc:contributor>
  <dc:contributor>R.K. Olsson</dc:contributor>
  <dc:contributor>P. J. Sugarman</dc:contributor>
  <dc:contributor>S.M. Savin</dc:contributor>
  <dc:creator>K.G. Miller</dc:creator>
  <dc:date>1999</dc:date>
  <dc:description>&lt;div id="15578990" class="article-section-wrapper js-article-section js-content-section  " data-section-parent-id="0"&gt;&lt;p&gt;A large (30–40 m), rapid (≪1 m.y.), earliest Maastrichtian sea-level drop inferred from New Jersey sequence stratigraphic records correlates with synchronous δ&lt;sup&gt;18&lt;/sup&gt;O increases in deep-water benthic and low-latitude surface-dwelling planktonic foraminifera. The coincidence of these events argues for the development of a moderate-sized ice sheet during the early Maastrichtian.&lt;/p&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1130/0091-7613(1999)027&lt;0783:DIDEME&gt;2.3.CO;2</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Geological Society of America</dc:publisher>
  <dc:title>Does ice drive early Maastrichtian eustasy?</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>