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      <header>
        <identifier>doi:10.1594/pangaea.690363</identifier>
        <datestamp>2024-07-20T21:51:50Z</datestamp>
        <setSpec>PANGAEA</setSpec>
        <setSpec>PANGAEA.REPOSITORY</setSpec>
      </header>
      <metadata>
        <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>Stable oxygen and carbon isotope ratios of Globigerinoides sacculifer of ODP Hole 134-828A from the Southwest Pacific (Table 2)</dc:title>
          <dc:creator>Martínez, José Ignacio</dc:creator>
          <dc:creator>De Deckker, Patrick</dc:creator>
          <dc:creator>Chivas, Allan R</dc:creator>
          <dc:publisher>PANGAEA</dc:publisher>
          <dc:date>1997</dc:date>
          <dc:date>Issued: 1997</dc:date>
          <dc:relation>doi:10.1016/s0377-8398(97)00029-7</dc:relation>
          <dc:subject>DEPTH, sediment/rock</dc:subject>
          <dc:subject>Sample code/label</dc:subject>
          <dc:subject>Globigerinoides sacculifer, δ18O</dc:subject>
          <dc:subject>Globigerinoides sacculifer, δ13C</dc:subject>
          <dc:subject>Drilling/drill rig</dc:subject>
          <dc:subject>DSDP/ODP/IODP sample designation</dc:subject>
          <dc:subject>Mass spectrometer Finnigan MAT 251</dc:subject>
          <dc:subject>Leg134</dc:subject>
          <dc:subject>Joides Resolution</dc:subject>
          <dc:subject>Ocean Drilling Program (ODP)</dc:subject>
          <dc:description>Oxygen-isotope analyses of planktonic foraminifera from 57 western Pacific deep-sea cores are compared for the Holocene and the Last Glacial Maximum (LGM). Carbonate dissolution, sedimentation rates/bioturbation, sample density, and vital effects are assessed before the sea-surface salinity signal of these records is reconstructed. Average glacial-interglacial Delta delta18O values in the western Pacific are found to be close to those in the Atlantic Ocean (1.76 ‰ in the Pacific compared to 1.80 ‰ in the Atlantic), questioning previous suggestions of a larger salinity difference between the Atlantic and the Pacific oceans during the LGM. During the LGM, sea-surface salinity was higher in the western Pacific than today (by &amp;gt;~1 ‰), implying that evaporation minus precipitation was higher all over the region. The minimum change in sea-surface salinity occurred around the equator at the core of the Western Pacific Warm Pool. Holocene high-amplitude, high-frequency fluctuations in planktonic delta18O records north and south of the present limits of the Western Pacific Warm Pool are indicative of sea-surface temperature and/or sea-surface salinity variations related to its expansion and contraction at the scale of thousands of years. Such high-amplitude, high-frequency fluctuations at the edge of the WPWP are best documented in the delta18O signal of ODP Hole 828A offshore Vanuatu, so far the best high-resolution record for the western Pacific.</dc:description>
          <dc:description>Supplement to: Martínez, José Ignacio; De Deckker, Patrick; Chivas, Allan R (1997): New estimates for salinity changes in the Western Pacific Warm Pool during the Last Glacial Maximum: oxygen-isotope evidence. Marine Micropaleontology, 32(3-4), 311-340</dc:description>
          <dc:language>en</dc:language>
          <dc:type>Dataset</dc:type>
          <dc:type>Supplementary Dataset</dc:type>
          <dc:format>text/tab-separated-values</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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