<?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>J.D. Hudson</dc:contributor>
  <dc:contributor>M.L. Keith</dc:contributor>
  <dc:creator>F.C. Tan</dc:creator>
  <dc:date>1970</dc:date>
  <dc:description>&lt;div id="abstracts" class="Abstracts u-font-serif"&gt;&lt;div id="ab1" class="abstract author" lang="en"&gt;&lt;div id="aep-abstract-sec-id7"&gt;&lt;p&gt;Isotopic paleotemperature analyses of belemnites and ammonites from the Belemnite Sands and Oxford Clay of Staffin Bay, Isle of Skye, are presented. Ammonites are depleted in&lt;sup&gt;18&lt;/sup&gt;O compared with co-existing belemnites, which give mean temperatures of around 22°C, consistent with the Skye belemnite analysed by Urey et al. [1]. Possible reasons for the ammonite-belemnite difference are discussed.&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/0012-821X(70)90008-7</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Jurassic (callovian) paleotemperatures from Scotland</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>