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      <header>
        <identifier>doi:10.1594/pangaea.712599</identifier>
        <datestamp>2024-08-16T06:39:39Z</datestamp>
        <setSpec>PANGAEA</setSpec>
        <setSpec>PANGAEA.REPOSITORY</setSpec>
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        <oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
          <dc:title>Strontium isotope ratios of pore waters and planktonic foraminifera from DSDP holes</dc:title>
          <dc:creator>Hess, Jennifer</dc:creator>
          <dc:creator>Bender, Michael L</dc:creator>
          <dc:creator>Schilling, Jean-Guy</dc:creator>
          <dc:publisher>PANGAEA</dc:publisher>
          <dc:date>1986</dc:date>
          <dc:date>Issued: 1986</dc:date>
          <dc:relation>doi:10.1126/science.231.4741.979</dc:relation>
          <dc:subject>Drilling/drill rig</dc:subject>
          <dc:subject>Leg29</dc:subject>
          <dc:subject>Leg32</dc:subject>
          <dc:subject>Leg39</dc:subject>
          <dc:subject>Leg41</dc:subject>
          <dc:subject>Leg68</dc:subject>
          <dc:subject>Leg72</dc:subject>
          <dc:subject>Leg86</dc:subject>
          <dc:subject>Leg90</dc:subject>
          <dc:subject>Glomar Challenger</dc:subject>
          <dc:subject>Deep Sea Drilling Project (DSDP)</dc:subject>
          <dc:description>A detailed record of the strontium-87 to strontium-86 ratio in seawater during the last 100 million years was determined by measuring this ratio in 137 well-preserved and well-dated fossil foraminifera samples. Sample preservation was evaluated from scanning electron microscopy studies, measured strontium-calcium ratios, and pore water strontium isotope ratios. The evolution of the strontium isotopic ratio in seawater offers a means to evaluate long-term changes in the global strontium isotope mass balance. Results show that the marine strontium isotope composition can be used for correlating and dating well-preserved authigenic marine sediments throughout much of the Cenozoic to a precision of +/- 1 million years. The strontium-87 to strontium-86 ratio in seawater increased sharply across the Cretaceous/Tertiary boundary, but this feature is not readily explained as strontium input from a bolide impact on land.</dc:description>
          <dc:description>Supplement to: Hess, Jennifer; Bender, Michael L; Schilling, Jean-Guy (1986): Evolution of the ratio of strontium-87 to strontium-86 in seawater from Cretaceous to present. Science, 231(4741), 979-984</dc:description>
          <dc:language>en</dc:language>
          <dc:type>Collection</dc:type>
          <dc:type>Supplementary Publication Series of Datasets</dc:type>
          <dc:format>application/zip</dc:format>
          <dc:rights>Creative Commons Attribution 3.0 Unported</dc:rights>
          <dc:rights>https://creativecommons.org/licenses/by/3.0/legalcode</dc:rights>
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