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      <header>
        <identifier>doi:10.1594/pangaea.767356</identifier>
        <datestamp>2025-02-09T03:55:08Z</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>Age model and palaeoclimate records over the past 22,000 years of sediment core GeoB10053-7</dc:title>
          <dc:creator>Mohtadi, Mahyar</dc:creator>
          <dc:creator>Oppo, Delia W</dc:creator>
          <dc:creator>Steinke, Stephan</dc:creator>
          <dc:creator>Stuut, Jan-Berend W</dc:creator>
          <dc:creator>De Pol-Holz, Ricardo</dc:creator>
          <dc:creator>Hebbeln, Dierk</dc:creator>
          <dc:creator>Lückge, Andreas</dc:creator>
          <dc:publisher>PANGAEA</dc:publisher>
          <dc:date>2011</dc:date>
          <dc:date>Collected: 2005-08-29T12:03:00</dc:date>
          <dc:date>Issued: 2011</dc:date>
          <dc:relation>doi:10.1038/ngeo1209</dc:relation>
          <dc:subject>Gravity corer (Kiel type)</dc:subject>
          <dc:subject>SO184/2</dc:subject>
          <dc:subject>Sonne</dc:subject>
          <dc:subject>Center for Marine Environmental Sciences (MARUM)</dc:subject>
          <dc:description>The Australian-Indonesian monsoon is an important component of the climate system in the tropical Indo-Pacific region. However, its past variability, relation with northern and southern high-latitude climate and connection to the other Asian monsoon systems are poorly understood. Here we present high-resolution records of monsoon-controlled austral winter upwelling during the past 22,000 years, based on planktic foraminiferal oxygen isotopes and faunal composition in a sedimentary archive collected offshore southern Java. We show that glacial-interglacial variations in the Australian-Indonesian winter monsoon were in phase with the Indian summer monsoon system, consistent with their modern linkage through cross-equatorial surface winds. Likewise, millennial-scale variability of upwelling shares similar sign and timing with upwelling variability in the Arabian Sea. On the basis of element composition and grain-size distribution as precipitation-sensitive proxies in the same archive, we infer that (austral) summer monsoon rainfall was highest during the Bølling-Allerød period and the past 2,500 years. Our results indicate drier conditions during Heinrich Stadial 1 due to a southward shift of summer rainfall and a relatively weak Hadley cell south of the Equator. We suggest that the Australian-Indonesian summer and winter monsoon variability were closely linked to summer insolation and abrupt climate changes in the northern hemisphere.</dc:description>
          <dc:description>Supplement to: Mohtadi, Mahyar; Oppo, Delia W; Steinke, Stephan; Stuut, Jan-Berend W; De Pol-Holz, Ricardo; Hebbeln, Dierk; Lückge, Andreas (2011): Glacial to Holocene swings of the Australian–Indonesian monsoon. Nature Geoscience, 4(8), 540-544</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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