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        <identifier>doi:10.1594/pangaea.733253</identifier>
        <datestamp>2024-06-27T02:33:58Z</datestamp>
        <setSpec>PANGAEA</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>A multi-proxy investigation of sediment core GeoB7165-1 and AMS 14C dating points from sediment cores off Conceptión (~ 36°S)</dc:title>
          <dc:creator>Mohtadi, Mahyar</dc:creator>
          <dc:creator>Rossel, Pamela E</dc:creator>
          <dc:creator>Lange, Carina Beatriz</dc:creator>
          <dc:creator>Pantoja, Silvio</dc:creator>
          <dc:creator>Böning, Philipp</dc:creator>
          <dc:creator>Repeta, Daniel J</dc:creator>
          <dc:creator>Grunwald, Maik</dc:creator>
          <dc:creator>Lamy, Frank</dc:creator>
          <dc:creator>Hebbeln, Dierk</dc:creator>
          <dc:creator>Brumsack, Hans-Jürgen</dc:creator>
          <dc:publisher>PANGAEA</dc:publisher>
          <dc:date>2010</dc:date>
          <dc:date>Issued: 2010</dc:date>
          <dc:relation>doi:10.1016/j.epsl.2008.04.043</dc:relation>
          <dc:subject>Gravity corer (Kiel type)</dc:subject>
          <dc:subject>SO101</dc:subject>
          <dc:subject>SO102/1</dc:subject>
          <dc:subject>SO156/2</dc:subject>
          <dc:subject>SO156/3</dc:subject>
          <dc:subject>SO80a</dc:subject>
          <dc:subject>Sonne</dc:subject>
          <dc:subject>Center for Marine Environmental Sciences (MARUM)</dc:subject>
          <dc:description>A high-resolution sea surface temperature and paleoproductivity reconstruction on a sedimentary record collected at 36°S off central-south Chile (GeoB 7165-1, 36°33'S, 73°40'W, 797 m water depth, core length 750 cm) indicates that paleoceanographic conditions changed abruptly between 18 and 17 ka. Comparative analysis of several cores along the Chilean continental margin (30°-41°S) suggests that the onset and the pattern of deglacial warming was not uniform off central-south Chile due to the progressive southward migration of the Southern Westerlies and local variations in upwelling. Marine productivity augmented rather abruptly at 13-14 ka, well after the oceanographic changes.We suggest that the late deglacial increase in paleoproductivity off central-south Chile reflects the onset of an active upwelling system bringing nutrient-rich, oxygen-poor Equatorial SubsurfaceWater to the euphotic zone, and a relatively higher nutrient load of the Antarctic Circumpolar Current. During the Last Glacial Maximum, when the Southern Westerlies were located further north, productivity off central-south Chile, in contrast to off northern Chile, was reduced due to direct onshore-blowing winds that prevented coastal upwelling and export production.</dc:description>
          <dc:description>Supplement to: Mohtadi, Mahyar; Rossel, Pamela E; Lange, Carina Beatriz; Pantoja, Silvio; Böning, Philipp; Repeta, Daniel J; Grunwald, Maik; Lamy, Frank; Hebbeln, Dierk; Brumsack, Hans-Jürgen (2008): Deglacial pattern of circulation and marine productivity in the upwelling region off central-south Chile. Earth and Planetary Science Letters, 272, 221-230</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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