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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ADGEO</journal-id>
<journal-title-group>
<journal-title>Advances in Geosciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">ADGEO</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Adv. Geosci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7359</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/adgeo-6-23-2006</article-id>
<title-group>
<article-title>ENSO and interdecadal climate variability over the last century documented by geochemical records of two coral cores from the South West Pacific</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ourbak</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Corrège</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Malaizé</surname>
<given-names>B.</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>Le Cornec</surname>
<given-names>F.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Charlier</surname>
<given-names>K.</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>Peypouquet</surname>
<given-names>J. P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Département de Géologie et Océanographie (DGO), UMR CNRS 5805 EPOC, Université Bordeaux 1, Avenue des facultés, 33405 Talence cedex, France</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institut de Recherche pour le Développement (IRD) UR055 Paleotropique 32, avenue Henri Varagnat 93143 Bondy cedex, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>09</day>
<month>01</month>
<year>2006</year>
</pub-date>
<volume>6</volume>
<fpage>23</fpage>
<lpage>27</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2006 T. Ourbak et al.</copyright-statement>
<copyright-year>2006</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Generic License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by-nc-sa/2.5/">https://creativecommons.org/licenses/by-nc-sa/2.5/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://adgeo.copernicus.org/articles/6/23/2006/adgeo-6-23-2006.html">This article is available from https://adgeo.copernicus.org/articles/6/23/2006/adgeo-6-23-2006.html</self-uri>
<self-uri xlink:href="https://adgeo.copernicus.org/articles/6/23/2006/adgeo-6-23-2006.pdf">The full text article is available as a PDF file from https://adgeo.copernicus.org/articles/6/23/2006/adgeo-6-23-2006.pdf</self-uri>
<abstract>
<p>The south west Pacific is affected by climatic phenomena such as ENSO (El
Ni&amp;#241;o Southern Oscillation) or the PDO (Pacific Decadal Oscillation).
Near-monthly resolution calibrations of Sr/Ca, U/Ca and &lt;span style=&quot;font-family: &apos;Symbol, Times New Roman, Times&apos;; font-size: 16px;&quot;&gt;&amp;delta;&lt;/span&gt;&lt;sup&gt;18&lt;/sup&gt;Oc
were made on corals taken from New Caledonia and Wallis Island. These
geochemical variations could be linked to SST (sea surface temperature) and
SSS (sea surface salinity) variations over the last two decades, itselves
dependent on ENSO occurrences. On the other hand, near-half-yearly
resolution over the last century smoothes seasonal and interannual climate
signals, but emphasizes low frequency climate variability.</p>
</abstract>
<counts><page-count count="5"/></counts>
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</front>
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