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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="bold" font="default" size="100%">Desjardins, Thierry</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Turcq, Bruno</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Nguetnkam, J. P.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Achoundong, G.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Mandeng yogo, Magloire</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Cetin, Fethiye</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Lézine, Anne-Marie</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Delta C-13 variation of soil organic matter as an indicator of vegetation change during the Holocene in central Cameroon</title>
        <secondary-title>Comptes Rendus Geoscience</secondary-title>
      </titles>
      <pages>266-271</pages>
      <keywords>
        <keyword>Central Africa</keyword>
        <keyword>Semi-deciduous tropical forest</keyword>
        <keyword>Savanna</keyword>
        <keyword>C-14</keyword>
        <keyword>Paleoenvironments</keyword>
        <keyword>CAMEROUN</keyword>
      </keywords>
      <dates>
        <year>2013</year>
      </dates>
      <call-num>fdi:010061307</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Comptes Rendus Geoscience</full-title>
      </periodical>
      <isbn>1631-0713</isbn>
      <accession-num>ISI:000327002800002</accession-num>
      <number>7-8</number>
      <electronic-resource-num>10.1016/j.crte.2013.06.001</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:010061307</url>
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        <pdf-urls>
          <url>https://www.documentation.ird.fr/intranet/publi/2013/12/010061307.pdf</url>
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      <volume>345</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>In order to better understand the dynamics of the forest-savanna mosaic from central Cameroon, we analyzed C-13 and C-14 profiles of six oxisols: two under forests and four under savannas. The delta C-13 soil profiles collected in the forests indicate that these environments are stable at least since the mid-Holocene, whereas the areas currently covered by savannas were formerly occupied by more forested vegetations. The C-14 dating of organic matter indicate that the late extension of the savannas in central Cameroon date from the Late Holocene, starting from 4000-3500 C-14 yr BP.</abstract>
      <custom6>064 ; 082</custom6>
      <custom1>UR211 / UR182</custom1>
      <custom7>Cameroun</custom7>
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