<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.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>2026-06-01T22:05:27Z</responseDate><request verb="GetRecord" identifier="oai:riuma.uma.es:10630/32090" metadataPrefix="qdc">https://riuma.uma.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:riuma.uma.es:10630/32090</identifier><datestamp>2026-02-03T11:50:31Z</datestamp><setSpec>com_10630_2254</setSpec><setSpec>col_10630_37959</setSpec></header><metadata><qdc:qualifieddc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dcterms="http://purl.org/dc/terms/" xmlns:doc="http://www.lyncode.com/xoai" xmlns:qdc="http://dspace.org/qualifieddc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://purl.org/dc/elements/1.1/ http://dublincore.org/schemas/xmls/qdc/2006/01/06/dc.xsd http://purl.org/dc/terms/ http://dublincore.org/schemas/xmls/qdc/2006/01/06/dcterms.xsd http://dspace.org/qualifieddc/ http://www.ukoln.ac.uk/metadata/dcmi/xmlschema/qualifieddc.xsd">
   <dc:title>Dark Carbon Uptake in Emerged Sediments: Seasonal and Daily CO2 Flux Patterns in a saline wetland.</dc:title>
   <dc:creator>Ledesma-Hernández, Guillermo</dc:creator>
   <dc:creator>Rodríguez-Gómez, Sofía</dc:creator>
   <dc:creator>Warren-Jiménez, Paula</dc:creator>
   <dc:creator>Ruiz Nieto, Miriam</dc:creator>
   <dc:creator>Montes-Pérez, Jorge Juan</dc:creator>
   <dc:creator>Conejo-Orosa, Teresa</dc:creator>
   <dc:creator>Moreno-Ostos, Enrique</dc:creator>
   <dc:subject>Carbono - Fijación</dc:subject>
   <dc:subject>Sedimentos (Geología)</dc:subject>
   <dc:subject>Zonas húmedas</dc:subject>
   <dcterms:abstract>Inland water bodies are currently shrinking due to alterations of the water cycle, exposing&#xd;
extensive areas of previously submerged sediments to the atmosphere. Consequently, the&#xd;
carbon cycle is altered, leading to an increased emission of CO2. To study this, we performed&#xd;
monthly surveys throughout one year to measure CO2 fluxes from dawn to dusk in the calcite-&#xd;
rich emerged sediments of the endorheic saline wetland of La Laguna de Fuente de Piedra,&#xd;
Málaga (Spain). Consistent with existing literature, CO2 emission fluxes predominated in&#xd;
these sediments. However, at dawn and dusk fluxes were considerably lower, and even CO2&#xd;
uptake into the sediment occurred.&#xd;
Consequently, we conducted three campaigns over a full 24-hour cycle to measure CO2 fluxes&#xd;
in the emerged sediments and their most influential environmental drivers. This approach&#xd;
revealed a net CO2 emission from the sediment during daylight hours, while a net CO2 uptake&#xd;
by the sediment was measured during darkness.&#xd;
The magnitude of CO2 fluxes exhibited seasonality with both highest uptake and emission&#xd;
fluxes in summer, reaching a maximum emission and uptake value of 0.29 g(CO2)m-2h-1 and&#xd;
-0.14 g(CO2)m-2h-1 respectively. In contrast, winter showed the lowest fluxes, with a&#xd;
maximum emission value of 0.04 g(CO2)m-2h-1 and a maximum uptake value of –0.01&#xd;
g(CO2)m-2h-1.&#xd;
Our results reveal that, in addition to seasonal variability of CO2 fluxes magnitude in Fuente&#xd;
de Piedra, a daily trend in CO2 fluxes exists. This trend shows that CO2 emissions from&#xd;
sediments increase towards midday but decrease towards midnight resulting in CO2 uptake by&#xd;
the sediment</dcterms:abstract>
   <dcterms:dateAccepted>2024-07-12T10:57:18Z</dcterms:dateAccepted>
   <dcterms:available>2024-07-12T10:57:18Z</dcterms:available>
   <dcterms:created>2024-07-12T10:57:18Z</dcterms:created>
   <dcterms:issued>2024</dcterms:issued>
   <dc:type>conference output</dc:type>
   <dc:identifier>https://hdl.handle.net/10630/32090</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>
</qdc:qualifieddc>
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