<?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>2026-06-06T05:00:12Z</responseDate><request verb="GetRecord" identifier="oai:riuma.uma.es:10630/9655" metadataPrefix="oai_dc">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><oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:doc="http://www.lyncode.com/xoai" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.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>
   <dc:subject>Marine biology</dc:subject>
   <dc:subject>Mesocosm</dc:subject>
   <dc:subject>Iron</dc:subject>
   <dc:subject>Co2</dc:subject>
   <dc:subject>Phytoplankton</dc:subject>
   <dc:description>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.</dc:description>
   <dc:description>Universidad de Málaga. Campus de Excelencia Internacional Andalucía Tech.</dc:description>
   <dc:date>2015-04-14T11:38:22Z</dc:date>
   <dc:date>2015-04-14T11:38:22Z</dc:date>
   <dc:date>2015</dc:date>
   <dc:date>2015-04-14</dc:date>
   <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>
   <dc:format>application/pdf</dc:format>
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