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dc.contributor.authorGarcía-Merchán, V. H.es_ES
dc.contributor.authorRobainas-Barcia, A.es_ES
dc.contributor.authorAbelló, Perees_ES
dc.contributor.authorMacpherson, Enriquees_ES
dc.contributor.authorPalero, Ferranes_ES
dc.contributor.authorGarcía-Rodríguez, Marianoes_ES
dc.contributor.authorGil de Sola, Luises_ES
dc.contributor.authorPascual, Martaes_ES
dc.date.accessioned2012-01-11T12:20:18Z-
dc.date.available2012-01-11T12:20:18Z-
dc.date.issued2012-
dc.identifier.citationMolecular Phylogenetics and Evolution 62 : 664-672 (2012)es_ES
dc.identifier.issn1055-7903-
dc.identifier.urihttp://hdl.handle.net/10261/44146-
dc.description9 páginas, 4 figuras, 3 tablas.es_ES
dc.description.abstractComparative multispecies studies allow contrasting the effect of past and present oceanographic pro- 30 cesses on phylogeographic patterns. In the present study, a fragment of the COI gene was analyzed in 31 seven decapod crustacean species from five families and with different bathymetric distributions. A total 32 of 769 individuals were sampled along the Atlantic–Mediterranean transition area in order to test the 33 effect of three putative barriers to gene flow: Strait of Gibraltar, Almeria–Oran Front and Ibiza Channel. 34 A significant effect of the Strait of Gibraltar was found in the crabs Liocarcinus depurator and Macropipus 35 tuberculatus. The Ibiza Channel had a significant effect for L. depurator. However, the Almeria–Oran front 36 was not found to have a significant effect on any of the studied species. Higher levels of population struc- 37 ture were found in shallow-water species, although the number of species sampled should be increased 38 to obtain a conclusive pattern. The haplotypes within the different species coalesced at times that could 39 be related with past climatic events occurring before, during and after the last glacial maximum. Given 40 the large diversity of phylogeographic patterns obtained within decapods, it is concluded that both his- 41 torical and contemporary processes (marine current patterns, bathymetry and life-history traits) shape 42 the phylogeographic patterns of these crustaceans.es_ES
dc.description.sponsorshipThis work was funded by Projects 597 BIOCON08-187 from Fundación BBVA and CTM2010-22218 from 598 the Ministerio de Educación y Ciencia. The authors are part of the 599 Research Group 2009SGR-636, 2009SGR-655 and 2009SGR-1364 600 of the Generalitat de Catalunya. VHGM acknowledges a predoctoral 601 fellowship from Universidad del Quindío (Armenia, Colombia). ARB 602 acknowledges a postdoctoral fellowship from MAE-AECID 2009.es_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.rightsopenAccesses_ES
dc.subjectOceanographic discontinuitieses_ES
dc.subjectDepth distributiones_ES
dc.subjectmtDNAes_ES
dc.subjectGlaciationses_ES
dc.subjectPopulation structurees_ES
dc.titlePhylogeographic patterns of decapod crustaceans at the Atlantic–Mediterranean transitiones_ES
dc.typeartículoes_ES
dc.identifier.doi10.1016/j.ympev.2011.11.009-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1016/j.ympev.2011.11.009es_ES
dc.relation.csices_ES
dc.type.coarhttp://purl.org/coar/resource_type/c_6501es_ES
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
item.cerifentitytypePublications-
item.openairetypeartículo-
item.languageiso639-1en-
item.grantfulltextopen-
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