Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/286
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dc.contributor.authorLaplana, César-
dc.contributor.authorSevilla, Paloma-
dc.contributor.authorArsuaga, Juan Luis-
dc.contributor.authorArriaza, María del Carmen-
dc.contributor.authorBaquedano, Enrique-
dc.contributor.authorPérez-González, Alfredo-
dc.contributor.authorLópez Martínez, Nieves-
dc.date.accessioned2018-05-08T14:30:43Z-
dc.date.issued2015-11-
dc.identifier.citationPLoS ONE, 2015, 10 (11): e0140513es_ES
dc.identifier.issn1932-6203-
dc.identifier.urihttp://cir.cenieh.es/handle/20.500.12136/286-
dc.description.abstractThis paper reports the first find of pika remains in the Iberian Peninsula, at a site in central Spain. A fragmented mandible of Ochotona cf. pusilla was unearthed from Layer 3 (deposited some 63.4±5.5 ka ago as determined by thermoluminescence) of the Buena Pinta Cave. This record establishes new limits for the genus geographic distribution during the Pleistocene, shifting the previous edge of its known range southwest by some 500 km. It also supports the idea that, even though Europe’s alpine mountain ranges represented a barrier that prevented the dispersal into the south to this and other taxa of small mammals from central and eastern Europe, they were crossed or circumvented at the coldest time intervals of the end of the Middle Pleistocene and of the Late Pleistocene. During those periods both the reduction of the forest cover and the emersion of large areas of the continental shelf due to the drop of the sea level probably provided these species a way to surpass this barrier. The pika mandible was found accompanying the remains of other small mammals adapted to cold climates, indicating the presence of steppe environments in central Iberia during the Late Pleistocene.es_ES
dc.description.sponsorshipThis research was performed as part of project S2010/BMD-2330 of the Madrid Regional Government’s Consejería de Educación I+D activities programme for research groups. The study and excavation of the Pinilla del Valle sites were authorised by the Dirección General de Patrimonio Histórico de la Comunidad de Madrid and supported by the Museo Arqueológico Regional (MAR) de la Comunidad de Madrid, Grupo Mahou and Canal de Isabel II Gestión. The authors thank the Parque Nacional de Guadarrama and the Ayuntamiento de Pinilla del Valle for their collaboration. The Fundación General de la Universidad de Alcalá managed the funds assigned to the project. This work is also a contribution to project GR58/08-910607 of the Madrid Regional Government, and CGL2009-7896/BTE of the Spanish Ministerio de Ciencia e Innovacion.es_ES
dc.language.isoenes_ES
dc.publisherPublic Library of Sciencees_ES
dc.rightsAtribución 3.0 Estados Unidos de América*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/us/*
dc.subjectPleistocene epoches_ES
dc.subjectPikases_ES
dc.subjectPintaes_ES
dc.subjectCaveses_ES
dc.subjectMandiblees_ES
dc.subjectMammalses_ES
dc.subjectDentitiones_ES
dc.subjectFossilses_ES
dc.titleHow far into Europe did Pikas (Lagomorpha: Ochotonidae) go during the Pleistocene? New evidence from Central Iberiaes_ES
dc.typeArticlees_ES
dc.identifier.doi10.1371/journal.pone.0140513-
dc.relation.publisherversionhttps://doi.org/10.1371/journal.pone.0140513es_ES
dc.date.available2018-05-08T14:30:43Z-
Appears in Collections:Geocronología y Geología



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