Human remains from Valdegoba Cave (Huérmeces, Burgos, Spain)

dc.contributor.authorQuam, R.
dc.contributor.authorArsuaga Ferreras, Juan Luis
dc.contributor.authorBermúdez de Castro, José María
dc.contributor.authorDíez Fernández-Lomana, Juan Carlos
dc.contributor.authorLorenzo Merino, Carlos
dc.contributor.authorCarretero, José Miguel
dc.contributor.authorGarcía García, Nuria
dc.contributor.authorOrtega Martínez, Ana Isabel
dc.date.accessioned2023-06-20T19:06:46Z
dc.date.available2023-06-20T19:06:46Z
dc.date.issued2001
dc.description.abstractSystematic excavations, begun in 1987, at the Valdegoba cave site in northern Spain have yielded the remains of five individuals associated with a Middle Paleolithic stone tool technology and Pleistocene fauna. A fragmentary mandible of an adolescent (VB1), preserving nearly a full set of teeth, exhibits a symphyseal tubercle and slight incurvatio mandibulae anterior on the external symphysis. Both the superior and inferior transverse tori are present on the internal aspect. A second individual (VB2) is represented by a set of ten deciduous teeth consistent with an age at death of 6–9 months. A proximal manual phalanx (VB3) displays a relatively broad head, a characteristic which is found in both Neandertals, as well as European Middle Pleistocene hominids. VB4 is a fourth metatarsal that lacks the distal epiphysis, indicating it comes from an adolescent individual, and has a relatively high robusticity index. Finally, VB5 is a fifth metatarsal of an adult. The VB1 mandible shows a combination of archaic characteristics as well as more specific Neandertal morphological traits. The VB2 deciduous teeth are very small, and both the metrics and morphology seem more consistent with a modern human classification. The postcranial elements are undiagnostic, U-Th dating has provided an age of >350 ka for the base of the sequence and a date of <73·2 ± �5 ka for level 7, near the top. Faunal analysis and radiometric dates from other nearby Mousterian sites suggests that the Valdegoba site is correlative with oxygen isotope stages 3–6 on the Iberian peninsula, and an Upper Pleistocene age for the Valdegoba hominids seems most reasonable.
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/26854
dc.identifier.doi10.1006/jhev.2001.0486
dc.identifier.issn0047-2484
dc.identifier.officialurlhttp://www.journals.elsevier.com/journal-of-human-evolution/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/59256
dc.journal.titleJournal of Human Evolution
dc.language.isoeng
dc.page.final435
dc.page.initial385
dc.publisherElsevier Science B.V., Amsterdam
dc.rights.accessRightsopen access
dc.subject.cdu569.89
dc.subject.keywordValdegoba
dc.subject.keywordNeandertal
dc.subject.keywordEarly modern Human
dc.subject.keywordWestern Europe
dc.subject.keywordSpain
dc.subject.keywordMandible
dc.subject.keywordDeciduous Teeth
dc.subject.keywordHand phalanx
dc.subject.keywordMetatarsal
dc.subject.ucmPaleontología
dc.subject.unesco2416 Paleontología
dc.titleHuman remains from Valdegoba Cave (Huérmeces, Burgos, Spain)
dc.typejournal article
dc.volume.number41
dspace.entity.typePublication
relation.isAuthorOfPublicationd8e770fc-0ebe-43f3-9966-3a7d5cbd2353
relation.isAuthorOfPublicationaa039b32-8168-4c9c-8deb-181668a786be
relation.isAuthorOfPublication.latestForDiscoveryaa039b32-8168-4c9c-8deb-181668a786be

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