Articles producció científica> Història i Història de l'Art

New interpretation of the Gran Dolina-TD6 bearing Homo antecessor deposits through sedimentological analysis

  • Dades identificatives

    Identificador: PC:1871
    Autors:
    J. RosellI. CampañaA. Pérez-GonzálezA. Benito-CalvoR. BlascoJ. M. Bermúdez de CastroE. CarbonellJ. L. Arsuaga
    Resum:
    DOI: 10.1038/srep34799 URL: http://www.nature.com/articles/srep34799 Filiació URV: SI Inclòs a la memòria: SI
  • Altres:

    Autor segons l'article: J. Rosell; I. Campaña; A. Pérez-González; A. Benito-Calvo; R. Blasco; J. M. Bermúdez de Castro; E. Carbonell; J. L. Arsuaga
    Departament: Història i Història de l'Art
    Autor/s de la URV: ROSELL ARDÉVOL, JORDI; I. Campaña; A. Pérez-González; A. Benito-Calvo; R. Blasco; J. M. Bermúdez de Castro; CARBONELL ROURA, EUDALD; J. L. Arsuaga
    Paraules clau: cave floodplain fossil
    Resum: Gran Dolina is a cavity infilled by at least 25 m of Pleistocene sediments. This sequence contains the TD6 stratigraphic unit, whose records include around 170 hominin bones that have allowed the definition of a new species, Homo antecessor. This fossil accumulation was studied as a single assemblage and interpreted as a succession of several human home bases. We propose a complete stratigraphic context and sedimentological interpretation for TD6, analyzing the relationships between the sedimentary facies, the clasts and archaeo-palaeontological remains. The TD6 unit has been divided into three sub-units and 13 layers. Nine sedimentary facies have been defined. Hominin remains appear related to three different sedimentary facies: debris flow facies, channel facies and floodplain facies. They show three kinds of distribution: first a group of scattered fossils, then a group with layers of fossils in fluvial facies, and third a group with a layer of fossils in mixed fluvial and gravity flow facies. The results of this work suggest that some of these hominin remains accumulated in the cave by geological processes, coming from the adjacent slope above the cave or the cave entry, as the palaeogeography and sedimentary characteristics of these allochthonous facies suggest.
    Grup de recerca: Autoecologia Humana del Quaternari
    Àrees temàtiques: Història Historia History
    Accès a la llicència d'ús: https://creativecommons.org/licenses/by/3.0/es/
    ISSN: 2045-2322
    Identificador de l'autor: s/n; s/n; s/n; s/n; s/n; s/n; s/n; s/n
    Data d'alta del registre: 2016-10-28
    Volum de revista: 6
    Versió de l'article dipositat: info:eu-repo/semantics/publishedVersion
    Enllaç font original: https://www.nature.com/articles/srep34799?utm_medium=affiliate&utm_source=commission_junction&utm_campaign=3_nsn6445_deeplink_PID2190813&utm_content=deeplink
    URL Document de llicència: https://repositori.urv.cat/ca/proteccio-de-dades/
    DOI de l'article: 10.1038/srep34799
    Entitat: Universitat Rovira i Virgili
    Any de publicació de la revista: 2016
    Pàgina inicial: Art. num. 34799
    Tipus de publicació: Article Artículo Article
  • Paraules clau:

    Gran Dolina (Burgos : Jaciment arqueològic)
    Homínids
    cave
    floodplain
    fossil
    Història
    Historia
    History
    2045-2322
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