<?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>2026-05-30T09:52:08Z</responseDate><request verb="GetRecord" identifier="oai:riuma.uma.es:10630/9655" metadataPrefix="qdc">https://riuma.uma.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:riuma.uma.es:10630/9655</identifier><datestamp>2026-02-03T11:50:24Z</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>Effect of increased CO&lt;sub>2&lt;/sub> and iron levels on the marine plankton food web during a mesocosm experiment</dc:title>
   <dc:creator>Segovia, MR</dc:creator>
   <dc:subject>Fitoplancton marino</dc:subject>
   <dcterms:abstract>A mesocosm experiment was carried out in the Raunefjord (Norway) during 25 days, to investigate the interactive effects of increased CO&lt;sub>2&lt;/sub>  and iron availability on the plankton community. The seawater carbonate system in the mesocosms was manipulated to achieve two different CO&lt;sub>2&lt;/sub>  levels, corresponding to the present (390 ppmv, LC) and to levels predicted for year 2100 (900 ppmv, HC), in combination with ambient and increased dissolved Fe (dFe) concentrations in a full factorial design. We observed a shift in the plankton community structure, initially dominated by picoeukaryotes and small nanoeukaryotes, changing to an &lt;em>Emiliania huxleyi&lt;/em> dominated bloom. &lt;em>E. huxleyi&lt;/em> and &lt;em>Synechococcus&lt;/em>  were the most sensitive organisms to changes in CO2 and Fe levels, being negatively affected by increased CO&lt;sub>2&lt;/sub>  and favoured by high dFe levels. Picoeukaryotes, large nanoplankton, viruses and ciliates abundances were not affected by changes in CO&lt;sub>2&lt;/sub>  or dFe levels. Bacterial abundance showed a significant positive response to high CO&lt;sub>2&lt;/sub>  but it was unaffected by dFe. Total mesozooplankton abundances did not change significantly. The relevance of these results within the global change scenario will be discussed.</dcterms:abstract>
   <dcterms:dateAccepted>2015-04-14T11:38:22Z</dcterms:dateAccepted>
   <dcterms:available>2015-04-14T11:38:22Z</dcterms:available>
   <dcterms:created>2015-04-14T11:38:22Z</dcterms:created>
   <dcterms:issued>2015-04-14</dcterms:issued>
   <dc:type>conference output</dc:type>
   <dc:identifier>http://hdl.handle.net/10630/9655</dc:identifier>
   <dc:language>eng</dc:language>
   <dc:relation>ASLO2015</dc:relation>
   <dc:relation>Granada, España</dc:relation>
   <dc:relation>Febrero 2015</dc:relation>
   <dc:rights>open access</dc:rights>
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