Articles producció científica> Història i Història de l'Art

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

  • Identification data

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

    Author, as appears in the article.: J. Rosell; I. Campaña; A. Pérez-González; A. Benito-Calvo; R. Blasco; J. M. Bermúdez de Castro; E. Carbonell; J. L. Arsuaga
    Department: Història i Història de l'Art
    URV's Author/s: ROSELL ARDÉVOL, JORDI; I. Campaña; A. Pérez-González; A. Benito-Calvo; R. Blasco; J. M. Bermúdez de Castro; CARBONELL ROURA, EUDALD; J. L. Arsuaga
    Keywords: cave floodplain fossil
    Abstract: 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.
    Research group: Autoecologia Humana del Quaternari
    Thematic Areas: Història Historia History
    licence for use: https://creativecommons.org/licenses/by/3.0/es/
    ISSN: 2045-2322
    Author identifier: s/n; s/n; s/n; s/n; s/n; s/n; s/n; s/n
    Record's date: 2016-10-28
    Journal volume: 6
    Papper version: info:eu-repo/semantics/publishedVersion
    Link to the original source: https://www.nature.com/articles/srep34799?utm_medium=affiliate&utm_source=commission_junction&utm_campaign=3_nsn6445_deeplink_PID2190813&utm_content=deeplink
    Licence document URL: https://repositori.urv.cat/ca/proteccio-de-dades/
    Article's DOI: 10.1038/srep34799
    Entity: Universitat Rovira i Virgili
    Journal publication year: 2016
    First page: Art. num. 34799
    Publication Type: Article Artículo Article
  • Keywords:

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