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      <ref-type name="Journal Article">17</ref-type>
      <work-type>ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES</work-type>
      <contributors>
        <authors>
          <author>
            <style face="normal" font="default" size="100%">Lavergne, A.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Daux, V.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Villalba, R.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Pierre, M.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Stievenard, M.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Vimeux, Françoise</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Srur, A. M.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Are the oxygen isotopic compositions of Fitzroya cupressoides and Nothofagus pumilio cellulose promising proxies for climate reconstructions in northern Patagonia ?</title>
        <secondary-title>Journal of Geophysical Research : Biogeosciences</secondary-title>
      </titles>
      <pages>767-776</pages>
      <keywords>
        <keyword>north Patagonia</keyword>
        <keyword>cellulose</keyword>
        <keyword>O-18</keyword>
        <keyword>Fitzroya cupressoides</keyword>
        <keyword>Nothofagus pumilio</keyword>
        <keyword>climate change</keyword>
        <keyword>ARGENTINE</keyword>
        <keyword>CHILI</keyword>
        <keyword>ANDES</keyword>
        <keyword>PATAGONIE</keyword>
      </keywords>
      <dates>
        <year>2016</year>
      </dates>
      <call-num>fdi:010066809</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Journal of Geophysical Research : Biogeosciences</full-title>
      </periodical>
      <isbn>2169-8953</isbn>
      <accession-num>ISI:000374345000010</accession-num>
      <number>3</number>
      <electronic-resource-num>10.1002/2015jg003260</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:010066809</url>
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          <url>https://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers17-10/010066809.pdf</url>
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      <volume>121</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>Tree ring O-18 chronologies from two native species (Fitzroya cupressoides and Nothofagus pumilio) in northern Patagonia were developed to assess their potential for paleoclimate reconstructions. The five annually resolved cellulose O-18 chronologies (two for F. cupressoides and three for N. pumilio) are located on the Andes along the steep west-to-east precipitation gradient. Over the common 60years long interval, the five site-O-18(cell) chronologies exhibit a strong common signal as indicated by the significant mean intercorrelation (r=0.61, p&lt;0.05) and the high percentage (65%) of total variance explained by the first empirical orthogonal function. Although correlation analyses reveal that the two mean species-O-18(cell) chronologies are mainly modulated by December-May temperature, the N. pumilio chronology shows a greater sensitivity to record temperature variations (r=0.57, p&lt;0.05). The O-18(cell) of N. pumilio contains a regional temperature signal representative of a large area in southern South America under the influence of the Southern Annular Mode. This study indicates that O-18(cell) in N. pumilio is a promising proxy to reconstruct past variations in temperature in South America south of 38 degrees S.</abstract>
      <custom6>021 ; 082 ; 020 ; 076</custom6>
      <custom1>UR050</custom1>
      <custom7>Argentine</custom7>
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