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<front>
<journal-meta>
<journal-id journal-id-type="publisher">CP</journal-id>
<journal-title-group>
<journal-title>Climate of the Past</journal-title>
<abbrev-journal-title abbrev-type="publisher">CP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1814-9332</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/cp-8-135-2012</article-id>
<title-group>
<article-title>Change in dust variability in the Atlantic sector of Antarctica at the end of the last deglaciation</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wegner</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gabrielli</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wilhelms-Dick</surname>
<given-names>D.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff10">
<sup>10</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ruth</surname>
<given-names>U.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kriews</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>De Deckker</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Barbante</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Cozzi</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Delmonte</surname>
<given-names>B.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Fischer</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Alfred Wegener Institute for Polar and Marine Research, Am Alten Hafen 26, 27568 Bremerhaven, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute for the Dynamics of Environmental Processes, CNR, 30123 Venice, Italy</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>School of Earth Science and Byrd Polar Research Center, The Ohio State University, Columbus, OH 43210-1002, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Climate Analysis and Consulting, Pfullingen, Germany</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Department of Environmental Sciences, University Ca&apos; Foscari of Venice, Dorsoduro 2137, 30123 Venice, Italy</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>DISAT – Department Environmental Sciences, University Milano Bicocca, 20126, Milan, Italy</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>Oeschger Institute for Climate Change Research, University of Bern, Bern, Switzerland</addr-line>
</aff>
<aff id="aff10">
<label>10</label>
<addr-line>now at: University of Bremen, Klagenfurter Strasse, Bremen, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>19</day>
<month>01</month>
<year>2012</year>
</pub-date>
<volume>8</volume>
<issue>1</issue>
<fpage>135</fpage>
<lpage>147</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.clim-past.net/8/135/2012/cp-8-135-2012.html">This article is available from http://www.clim-past.net/8/135/2012/cp-8-135-2012.html</self-uri>
<self-uri xlink:href="http://www.clim-past.net/8/135/2012/cp-8-135-2012.pdf">The full text article is available as a PDF file from http://www.clim-past.net/8/135/2012/cp-8-135-2012.pdf</self-uri>
<abstract>
<p>We present a Rare Earth Elements (REE) record determined on the EPICA ice
core drilled at Dronning Maud Land (EDML) in the Atlantic sector of the East
Antarctic Plateau. The record covers the transition from the last glacial
stage (LGS) to the early Holocene (26 600–7500 yr BP) at decadal to
centennial resolution. Additionally, samples from potential source areas
(PSAs) for Antarctic dust were analyzed for their REE characteristics. The
dust provenance is discussed by comparing the REE fingerprints in the ice
core and the PSA samples. We find a shift in variability in REE composition
at ~15 000 yr BP in the ice core samples. Before 15 000 yr BP, the
dust composition is very uniform and its provenance was most certainly
dominated by a South American source. After 15 000 yr BP, multiple sources
such as Australia and New Zealand become relatively more important, although
South America remains the major dust source. A similar change in the dust
characteristics was observed in the EPICA Dome C ice core at around
~15 000 yr BP, accompanied by a shift in the REE composition, thus
suggesting a change of atmospheric circulation in the Southern Hemisphere.</p>
</abstract>
<counts><page-count count="13"/></counts>
</article-meta>
</front>
<body/>
<back>
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