<?xml version='1.0' encoding='utf-8'?>
<?xml-stylesheet type="text/xsl" href="/v2/static/oai2.xsl"?>
<OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd">
  <responseDate>2026-10-11T18:23:04Z</responseDate>
  <request identifier="oai:figshare.com:article/33833121" metadataPrefix="oai_dc" verb="GetRecord">https://api.figshare.com/v2/oai</request>
  <GetRecord>
    <record>
      <header>
        <identifier>oai:figshare.com:article/33833121</identifier>
        <datestamp>2026-09-16T08:14:54Z</datestamp>
        <setSpec>category_15</setSpec>
        <setSpec>category_19</setSpec>
        <setSpec>category_21</setSpec>
        <setSpec>category_24</setSpec>
        <setSpec>category_272</setSpec>
        <setSpec>category_873</setSpec>
        <setSpec>category_39</setSpec>
        <setSpec>category_69</setSpec>
        <setSpec>portal_87</setSpec>
        <setSpec>item_type_3</setSpec>
        <setSpec>month_year_09_2026</setSpec>
      </header>
      <metadata>
        <oai_dc:dc xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance"  xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
          <dc:title>Salinity of Senegalese phreatic aquifers: the role of the geomorphology?</dc:title>
          <dc:creator>Luc Descroix (24965655)</dc:creator>
          <dc:creator>Souleymane Niang (24965658)</dc:creator>
          <dc:creator>Waly Faye (24965661)</dc:creator>
          <dc:creator>Lorenzo Spadini (2443288)</dc:creator>
          <dc:creator>Oumar Marega (24965664)</dc:creator>
          <dc:creator>Jean-Pierre Vandervaere (24965667)</dc:creator>
          <dc:creator>Olivier Grunberger (24965670)</dc:creator>
          <dc:creator>Céline Duwig (24965673)</dc:creator>
          <dc:creator>Sylvie Paméla Manga (24965676)</dc:creator>
          <dc:creator>Marie-Jeanne Senghor (24965679)</dc:creator>
          <dc:creator>Yancouba Sané (24965682)</dc:creator>
          <dc:creator>Ange Bouramanding Diedhiou (24965685)</dc:creator>
          <dc:creator>Yasmin Bouaïta (24965688)</dc:creator>
          <dc:creator>Ababacar Fall (24965691)</dc:creator>
          <dc:creator>Laurence Fleury (404025)</dc:creator>
          <dc:creator>Jean-Louis Rajot (24965694)</dc:creator>
          <dc:creator>Didier Orange (14054386)</dc:creator>
          <dc:creator>Olivier Ruë (24965697)</dc:creator>
          <dc:subject>Neuroscience</dc:subject>
          <dc:subject>Pharmacology</dc:subject>
          <dc:subject>Biotechnology</dc:subject>
          <dc:subject>Evolutionary Biology</dc:subject>
          <dc:subject>Environmental Sciences not elsewhere classified</dc:subject>
          <dc:subject>Chemical Sciences not elsewhere classified</dc:subject>
          <dc:subject>Ecology</dc:subject>
          <dc:subject>Inorganic Chemistry</dc:subject>
          <dc:subject>groundwater</dc:subject>
          <dc:subject>salinity</dc:subject>
          <dc:subject>Senegal</dc:subject>
          <dc:subject>dunes/interdunes</dc:subject>
          <dc:description>&lt;p&gt;Salinity is a common feature in amphibious environments. However, in Senegal (West Africa), elevated salinity levels are observed in groundwater hundreds of kilometres inland from the coastline – far beyond the marine influence. This raises questions about the origin of the salinity, decoupled from seawater intrusion. A spatial alignment of high (and, conversely, low) salinity values – parallel to a dune system – suggests a potential link to these aeolian formations. Field observations in four distinct regions of northwestern Senegal reveal sharp salinity contrasts between dunes and adjacent interdune depressions, even at scales of just a few hundred metres. Electrical conductivity (EC) values can shift abruptly from low (EC &lt; 0.5 mS/cm) to high (EC &gt; 5 mS/cm). The findings, reinforced by a principal component analysis based on data from over 500 wells, support a geomorphological hypothesis to explain the spatial distribution of salinity, highlighting the influence of palaeoenvironmental features on present-day hydrogeochemistry.&lt;/p&gt;</dc:description>
          <dc:date>2026-09-16T08:14:54Z</dc:date>
          <dc:type>Dataset</dc:type>
          <dc:type>Dataset</dc:type>
          <dc:identifier>10.6084/m9.figshare.33833121.v1</dc:identifier>
          <dc:relation>https://figshare.com/articles/dataset/Salinity_of_Senegalese_phreatic_aquifers_the_role_of_the_geomorphology_/33833121</dc:relation>
          <dc:rights>CC BY 4.0</dc:rights>
        </oai_dc:dc>
      </metadata>
    </record>
  </GetRecord>
</OAI-PMH>
