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dc.contributor.authorPeña, Viviana
dc.contributor.authorHarvey, Ben P.
dc.contributor.authorAgostini, Sylvain
dc.contributor.authorPorzio, Lucia
dc.contributor.authorMilazzo, Marco
dc.contributor.authorHorta, Paulo
dc.contributor.authorLine, Le Gall
dc.contributor.authorHall-Spencer, Jason
dc.date.accessioned2021-10-04T10:52:02Z
dc.date.available2021-10-04T10:52:02Z
dc.date.issued2021-07-16
dc.identifier.citationPeña, V., Harvey, B. P., Agostini, S., Porzio, L., Milazzo, M., Horta, P., Le Gall, L., & Hall-Spencer, J. M. (2021). Major loss of coralline algal diversity in response to ocean acidification. Global Change Biology, 27, 4785– 4798. https://doi.org/10.1111/gcb.15757es_ES
dc.identifier.issn1365-2486
dc.identifier.urihttp://hdl.handle.net/2183/28561
dc.description.abstract[Abstract] Calcified coralline algae are ecologically important in rocky habitats in the marine photic zone worldwide and there is growing concern that ocean acidification will severely impact them. Laboratory studies of these algae in simulated ocean acidification conditions have revealed wide variability in growth, photosynthesis and calcification responses, making it difficult to assess their future biodiversity, abundance and contribution to ecosystem function. Here, we apply molecular systematic tools to assess the impact of natural gradients in seawater carbonate chemistry on the biodiversity of coralline algae in the Mediterranean and the NW Pacific, link this to their evolutionary history and evaluate their potential future biodiversity and abundance. We found a decrease in the taxonomic diversity of coralline algae with increasing acidification with more than half of the species lost in high pCO2 conditions. Sporolithales is the oldest order (Lower Cretaceous) and diversified when ocean chemistry favoured low Mg calcite deposition; it is less diverse today and was the most sensitive to ocean acidification. Corallinales were also reduced in cover and diversity but several species survived at high pCO2; it is the most recent order of coralline algae and originated when ocean chemistry favoured aragonite and high Mg calcite deposition. The sharp decline in cover and thickness of coralline algal carbonate deposits at high pCO2 highlighted their lower fitness in response to ocean acidification. Reductions in CO2 emissions are needed to limit the risk of losing coralline algal diversity.es_ES
dc.description.sponsorshipFieldwork in the Mediterranean was supported by the EU ‘Mediterranean Sea Acidification under a changing climate’ project (MedSeA; grant agreement 265103; MM, JH-S)
dc.language.isoenges_ES
dc.publisherWileyes_ES
dc.relationinfo:eu-repo/grantAgreement/EC/FP7/265103es_ES
dc.relation.urihttps://doi.org/10.1111/gcb.15757es_ES
dc.rightsAtribución 4.0 Internacional (CC BY 4.0)es_ES
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/*
dc.subjectAdaptationes_ES
dc.subjectBiodiversityes_ES
dc.subjectClimate changees_ES
dc.subjectEcosystem engineerses_ES
dc.subjectEvolutionary historyes_ES
dc.subjectMacroalgaees_ES
dc.subjectpsbAes_ES
dc.subjectSeaweedses_ES
dc.titleMajor Loss of Coralline Algal Diversity in Response to Ocean Acidificationes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessinfo:eu-repo/semantics/openAccesses_ES
UDC.journalTitleGlobal Change Biologyes_ES
UDC.volume27es_ES
UDC.issue19es_ES
UDC.startPage4785es_ES
UDC.endPage4798es_ES


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