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dc.contributor.authorGarcía García, Nuria
dc.contributor.authorBárez del Cueto, Sergio
dc.contributor.authorGaspar, Ignacio de
dc.contributor.authorPrieto, Santiago
dc.contributor.authorLaplana, César
dc.contributor.authorGalindo Pellicena, Mª Ángeles
dc.contributor.authorHuguet, Rosa
dc.contributor.authorBlázquez Orta, Raquel
dc.contributor.authorJiménez Carmona, Israel Jesús
dc.contributor.authorValle, Héctor del
dc.contributor.authorPérez Díaz, Sebastián 
dc.contributor.authorFeranec, Robert S.
dc.contributor.authorAranburu, Arantza
dc.contributor.authorSevilla, Paloma
dc.contributor.authorPrieto, Irene
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2023-01-19T13:26:02Z
dc.date.available2023-09-01T02:20:28Z
dc.date.issued2022-08
dc.identifier.issn0891-2963
dc.identifier.issn1029-2381
dc.identifier.issn1026-7980
dc.identifier.otherPGC2018-093925-B-C33es_ES
dc.identifier.urihttps://hdl.handle.net/10902/27316
dc.description.abstractHere we report the preliminary results from the 2015-19 s prospecting explorations, excavations, and research from Juan Labranz Cave, a new Quaternary palaeontological deposit rich in mammals that offers information on the faunal context of the southern sub-plateau. This cave is located on the border of the Iberian range, at the Sierra de Valdecabras, Cuenca, at 1.279 metres above sea level. This study includes the first georeferenced digital map of the cave and a preliminary analysis of its chronology, palynology, macro- and microvertebrate palaeontology, and taphonomy. The cave is interpreted as a hyena den, and this would represent one of the highest elevation cavities where the activity of this taxon is recorded. Moreover, we consider this site important and unique because it constitutes one of the very few Pleistocene cave sites in the southern sub-plateau. It is strategically located on the border between the Iberian range and the Tajo Tertiary Basin, at the Júcar River valley, which represents the only great natural corridor that covers hundreds of kilometres and connects two very important palaeoecological areas, the interior of the Iberian Peninsula and the Mediterranean basin.es_ES
dc.description.sponsorshipThis work was supported by the Consejería de Educación, Cultura y Deportes Junta de Castilla-La Mancha [SBPLY/19/180801/000013- SBPLY/18/180801-SBPLY/17/180801/000002]; Spanish Ministry of Science and Innovation [PGC2018-093925-B-C33]; Quaternary Ecosystems UCM Research group; The Laboratory of Human Evolution at the University of Burgos (UBU)es_ES
dc.format.extent26 p.es_ES
dc.language.isoenges_ES
dc.publisherTaylor & Francises_ES
dc.rights© Taylor & Francises_ES
dc.sourceHistorical Biology, 2022, 34(8), 1632-1641es_ES
dc.subject.otherHyena denes_ES
dc.subject.otherMiddle-Late Pleistocenees_ES
dc.subject.otherPaleoenvironmentes_ES
dc.subject.otherIberian rangees_ES
dc.titleJuan Labranz cave: a Quaternary deposit in the central Iberian Peninsulaes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherVersionhttps://doi.org/10.1080/08912963.2022.2060097es_ES
dc.rights.accessRightsopenAccesses_ES
dc.identifier.DOI10.1080/08912963.2022.2060097
dc.type.versionacceptedVersiones_ES


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