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      <dc:title>Saltpan as carbon sink.</dc:title>
      <dc:creator>Warren-Jiménez, Paula</dc:creator>
      <dc:creator>Ledesma-Hernández, Guillermo</dc:creator>
      <dc:creator>Sánchez de Pedro Crespo, Raquel</dc:creator>
      <dc:creator>Ruiz Nieto, Miriam</dc:creator>
      <dc:creator>Rodríguez-Gómez, Sofía</dc:creator>
      <dc:creator>Montes-Pérez, Jorge Juan</dc:creator>
      <dc:creator>Conejo-Orosa, Teresa</dc:creator>
      <dc:creator>Gil Gil, Teresa</dc:creator>
      <dc:creator>Mancebo-Romero, Lidia</dc:creator>
      <dc:creator>Moreno-Ostos, Enrique</dc:creator>
      <dc:subject>Carbono - Fijación</dc:subject>
      <dc:subject>Salinas</dc:subject>
      <dc:subject>Biogeoquímica</dc:subject>
      <dc:description>Part of the Marchamalo saltpans (Murcia, Spain) has been abandoned for 28 years. The&#xd;
project “RESALAR” aims to restore 8 ha of this saltpan to extract salt in a traditional way&#xd;
while preserving biodiversity and historical heritage. The principal primary producers in&#xd;
hypersaline wetlands are microorganisms such as cyanobacteria and chlorophytes. Once the&#xd;
microorganism’s biomass becomes part of the decomposing sediment organic matter, the high&#xd;
sediment salinity and moisture levels leads to an anoxic environment, allowing it to be buried&#xd;
in the sediments. In this context, our study, previous to the restoration, aims to assess the&#xd;
carbon stock accumulated during the period of disuse as well as measure the carbon dioxide&#xd;
(CO2) efflux from the saltpan to the atmosphere and the effect of various physicochemical&#xd;
variables on soil CO2 emissions. To determine the carbon stock in the first 0.5 m we extracted&#xd;
a core from every tank, analyzed the bulk density, organic carbon, inorganic carbon and&#xd;
salinity in 5 cm sections. CO2 fluxes were measured using a soil respiration chamber&#xd;
connected to an infrared gas analyzer, and samples were taken from the first 10 cm of soil to&#xd;
analyze physicochemical variables. Our preliminary results shows that mean carbon stock&#xd;
value was 1349.71±251.39 Mg ha-1 and mean CO2 flux was 0.55±0.84 g m-2 h-1. Temperature&#xd;
was the main CO2 flux driver, while sediment moisture was the main carbon burial driver.&#xd;
Our results will be used to suggest management strategies to make the salt extraction&#xd;
compatible with carbon burial</dc:description>
      <dc:date>2024-07-12T11:18:30Z</dc:date>
      <dc:date>2024-07-12T11:18:30Z</dc:date>
      <dc:date>2024</dc:date>
      <dc:type>conference output</dc:type>
      <dc:identifier>https://hdl.handle.net/10630/32092</dc:identifier>
      <dc:language>eng</dc:language>
      <dc:relation>XXII AIL meeting</dc:relation>
      <dc:relation>Vigo</dc:relation>
      <dc:relation>Junio 2024</dc:relation>
      <dc:rights>open access</dc:rights>
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