Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/519
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dc.contributor.authorBlasco, Ruth-
dc.contributor.authorRosell, Jordi-
dc.contributor.authorMade, Jan van der-
dc.contributor.authorRodríguez, Jesús-
dc.contributor.authorCampeny Vall-llosera, Gerard-
dc.contributor.authorArsuaga, Juan Luis-
dc.contributor.authorBermúdez de Castro, José María-
dc.contributor.authorCarbonell, Eudald-
dc.date.accessioned2018-06-25T14:40:10Z-
dc.date.issued2011-12-
dc.identifier.citationJournal of Archaeological Science, 2011, 38 (12), 3373-3386es_ES
dc.identifier.issn0305-4403-
dc.identifier.issn1095-9238-
dc.identifier.urihttp://cir.cenieh.es/handle/20.500.12136/519-
dc.description.abstractDamage generated by large and small carnivores is common in many Middle Pleistocene sites. However, identifying the predator that produces the faunal accumulations is often a difficult task. In order to recognize the main type of carnivore that acts on a faunal assemblage, a combination of several characteristics should be taken into account: taxonomic and skeletal element representation, age profiles, carnivore damage (location, frequencies and dimensions of tooth-marks, bone breakage and digested bones), degree of fragmentation and frequencies of coprolites. But, adding environmental characteristics and the ethology of non-human predators/scavengers is also important. All these aspects are applied to the faunal assemblage from the TD8 level of the Gran Dolina site (Sierra de Atapuerca, Burgos, Spain). Paleomagnetic data combined with ESR and U-series place the TD8 level at the beginning of the Middle Pleistocene, specifically circa 700 kyr ago. The TD8 level contains a large faunal accumulation primarily composed of ungulate skeletal elements, and to a lesser extent carnivore remains. This assemblage is characterized by an overrepresentation of fallow deer (Dama vallonetensis), a skeletal profile biased towards cranial remains and limb bones, diversity of ages at death, a high proportion of carnivore damage and tooth-marks of large size, and an absence of human activity. According to these data, the accumulation seems to have been produced primarily by large carnivores, possibly hyenas. This observation does not rule out the possible occasional activity by other carnivores. Nevertheless, the characteristics of the TD8 assemblage do not correlate entirely with those traditionally used to define carnivore dens. In TD8, there are (1) no immature carnivore remains (remains of just one young Mosbach wolf); (2) scarce traces related to the end stages of consumption and some anatomical connexions; (3) few coprolites; (4) high proportion of adult ungulates and; (5) high quantities of whole bones and epiphyses. From this perspective, the TD8 faunal assemblage seems to correspond to a succession of carnivore occupations that allows the development of a suite of features to identify the activities of several species of predators that may have used the cave in different ways and durations. This study aims to emphasize the importance of these analyzes in order to know the behaviour of different non-human predators/scavengers in the European Middle Pleistocene sites.es_ES
dc.description.sponsorshipThis research was supported by Ministerio de Educación y Ciencia Spanish Government Grants CGL2009- 12703-C03-01, CGL2009-12703-C03-02, CGL2009-12703-C03-03, and CGL2009-7896, and by Generalitat de Catalunya Grant 2009 SGR 188. Ruth Blasco is the beneficiary of a FI Grant from Generalitat de Catalunya and financed by European Social Found. The field excavation work was supported by Junta de Castilla y León and Fundación Atapuerca.es_ES
dc.language.isoenes_ES
dc.publisherElsevieres_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.subjectMiddle Pleistocenees_ES
dc.subjectTaphonomyes_ES
dc.subjectCarnivoreses_ES
dc.subjectGran Dolinaes_ES
dc.subjectTD8es_ES
dc.titleHiding to eat: the role of carnivores in the Early Middle Pleistocene from the TD8 level of Gran Dolina (Sierra de Atapuerca, Burgos, Spain)es_ES
dc.typeArticlees_ES
dc.identifier.doi10.1016/j.jas.2011.07.023-
dc.relation.publisherversionhttps://doi.org/10.1016/j.jas.2011.07.023es_ES
dc.date.available2018-06-25T14:40:10Z-
Appears in Collections:Paleobiología



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