<?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>S. Marca</dc:contributor>
  <dc:contributor>Richard D. Norris</dc:contributor>
  <dc:contributor>D. Kroon</dc:contributor>
  <dc:contributor>A. Klaus</dc:contributor>
  <dc:contributor>I. T. Alexander</dc:contributor>
  <dc:contributor>L. P. Bardot</dc:contributor>
  <dc:contributor>Charles E. Barker</dc:contributor>
  <dc:contributor>Charles D. Blome</dc:contributor>
  <dc:contributor>L. J. Clarke</dc:contributor>
  <dc:contributor>J. Erbacher</dc:contributor>
  <dc:contributor>K. L. Faul</dc:contributor>
  <dc:contributor>M. A. Holmes</dc:contributor>
  <dc:contributor>Brian T. Huber</dc:contributor>
  <dc:contributor>Miriam E. Katz</dc:contributor>
  <dc:contributor>Kenneth G. MacLeod</dc:contributor>
  <dc:contributor>F. C. Martinez-Ruiz</dc:contributor>
  <dc:contributor>I. Mita</dc:contributor>
  <dc:contributor>M. Nakai</dc:contributor>
  <dc:contributor>James G. Ogg</dc:contributor>
  <dc:contributor>Dorothy K. Pak</dc:contributor>
  <dc:contributor>T. K. Pletsch</dc:contributor>
  <dc:contributor>Jean Self-Trail</dc:contributor>
  <dc:contributor>N. J. Shackleton</dc:contributor>
  <dc:contributor>J. Smit</dc:contributor>
  <dc:contributor>William Ussler III</dc:contributor>
  <dc:contributor>David K. Watkins</dc:contributor>
  <dc:contributor>J. Widmark</dc:contributor>
  <dc:contributor>Paul A. Wilson</dc:contributor>
  <dc:creator>J. #NAME? Bellier</dc:creator>
  <dc:date>1997</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;During ODP Leg 171B, devoted to the analysis of the Blake Plateau margin in front of Florida, 16 holes have been drilled in 5 distinct sites. The sites have documented a sedimentary succession ranging in age from Aptian to Eocene. Emphasis has been put on critical periods, comprising the Paleocene-Eocene transition, the Cretaceous-Tertiary boundary which has been cored in excellent conditions, the middle Maastrichtian extinctions and the Albian anoxic episodes.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/S1251-8050(97)89868-0</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>The Blake Nose Cretaceous-Paleogene (Florida Atlantic margin, ODP Leg 171 B): An exemplar record of the Maastrichtian-Danian transition</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>