Articles producció científica> Història i Història de l'Art

Extended-range luminescence chronologies for the Middle Pleistocene units at the Sima del Elefante archaeological site (Sierra de Atapuerca, Burgos, Spain)

  • Datos identificativos

    Identificador: imarina:9262502
    Autores:
    Demuro MArnold LJParés JMAranburu AHuguet RVallverdú JArsuaga JLBermúdez de Castro JMCarbonell E
    Resumen:
    The Sima del Elefante site is located within the Sierra de Atapuerca karst system (Burgos, northern Spain), and forms part of a series of important Early, Middle and Late Pleistocene archaeological complexes that have been dated previously with luminescence techniques (Gran Dolina, Galería Complex, Sima de los Huesos, Galería de las Estatuas). This study focuses on the upper Middle Pleistocene units (TE18 and TE19) at Sima del Elefante, which contain Acheulean and transitional lithic assemblages (Mode 2/3), as well as large and small mammal fossils. Importantly, these uppermost units are associated with a sediment plug located in the cave's interior at Galería Baja, which marks the closure of a significant palaeoentrance to the Atapuerca karst system. Establishing the accumulation history of these related deposits is important for understanding both Lower Palaeolithic technological dynamics via comparisons with similar levels at other Atapuerca sites (i.e., Gran Dolina and Galería Complex), as well as past human occupation patterns and carnivore use of (and accessibility to) the caves. We present single-grain TT-OSL and multi-grain pIR-IR chronologies for the Sima del Elefante upper sequence and the Galería Baja sediment cone, as well as U-series dating results for a stalagmitic crust capping the combined clastic infill sequence. The paired luminescence ages for the upper occupation levels are in agreement with each other and reveal that the host deposits accumulated 576–481 ka for the TE18 stratified scree layers, 266–237 ka for TE19 and 206–250 ka for the Galería Baja upper cone section (weighted mean 2σ age ranges). A concordant U-series age of 202 ± 65 ka is obtained for the overlying stalagmitic crust at Galería Baja. The Sima del Elefante ages are consistent with
  • Otros:

    Autor según el artículo: Demuro M; Arnold LJ; Parés JM; Aranburu A; Huguet R; Vallverdú J; Arsuaga JL; Bermúdez de Castro JM; Carbonell E
    Departamento: Història i Història de l'Art
    Autor/es de la URV: Huguet Pàmies, Rosa
    Palabras clave: Single-grain tt-osl Sima del elefante Post ir-ir Middle pleistocene Los-huesos Atapuerca suitability single-grain tt-osl single sima del elefante post ir-ir middle pleistocene insights hominin half-lives gran dolina galeria deposits age
    Resumen: The Sima del Elefante site is located within the Sierra de Atapuerca karst system (Burgos, northern Spain), and forms part of a series of important Early, Middle and Late Pleistocene archaeological complexes that have been dated previously with luminescence techniques (Gran Dolina, Galería Complex, Sima de los Huesos, Galería de las Estatuas). This study focuses on the upper Middle Pleistocene units (TE18 and TE19) at Sima del Elefante, which contain Acheulean and transitional lithic assemblages (Mode 2/3), as well as large and small mammal fossils. Importantly, these uppermost units are associated with a sediment plug located in the cave's interior at Galería Baja, which marks the closure of a significant palaeoentrance to the Atapuerca karst system. Establishing the accumulation history of these related deposits is important for understanding both Lower Palaeolithic technological dynamics via comparisons with similar levels at other Atapuerca sites (i.e., Gran Dolina and Galería Complex), as well as past human occupation patterns and carnivore use of (and accessibility to) the caves. We present single-grain TT-OSL and multi-grain pIR-IR chronologies for the Sima del Elefante upper sequence and the Galería Baja sediment cone, as well as U-series dating results for a stalagmitic crust capping the combined clastic infill sequence. The paired luminescence ages for the upper occupation levels are in agreement with each other and reveal that the host deposits accumulated 576–481 ka for the TE18 stratified scree layers, 266–237 ka for TE19 and 206–250 ka for the Galería Baja upper cone section (weighted mean 2σ age ranges). A concordant U-series age of 202 ± 65 ka is obtained for the overlying stalagmitic crust at Galería Baja. The Sima del Elefante ages are consistent with those previously obtained using U-series and biochronology, confirming that there is an erosional unconformity and complex carbonate deposition phase associated with the upper layers of unit TE18 and that the original cave entrance likely closed by ∼200 ka. Chronological correlation with other Atapuerca sites reveals potential equivalence between TE18 and unit TD8 (at Gran Dolina), and between TE19 and units GIIb–GIIIb (at Galería Complex) and, possibly, TD10.1 and TD10.2 (at Gran Dolina), though more refined dating is required to confirm the latter.
    Áreas temáticas: Stratigraphy Geosciences, multidisciplinary Geology Geography, physical Geociências Geochemistry & geophysics Earth and planetary sciences (miscellaneous) Ciências ambientais Ciências agrárias i Biodiversidade Astronomia / física Antropologia / arqueologia
    Acceso a la licencia de uso: https://creativecommons.org/licenses/by/3.0/es/
    Direcció de correo del autor: rosa.huguet@urv.cat
    Identificador del autor: 0000-0002-1750-6249
    Fecha de alta del registro: 2024-09-07
    Versión del articulo depositado: info:eu-repo/semantics/publishedVersion
    Enlace a la fuente original: https://www.sciencedirect.com/science/article/pii/S1871101422000668
    URL Documento de licencia: https://repositori.urv.cat/ca/proteccio-de-dades/
    Referencia al articulo segun fuente origial: Quaternary Geochronology. 71
    Referencia de l'ítem segons les normes APA: Demuro M; Arnold LJ; Parés JM; Aranburu A; Huguet R; Vallverdú J; Arsuaga JL; Bermúdez de Castro JM; Carbonell E (2022). Extended-range luminescence chronologies for the Middle Pleistocene units at the Sima del Elefante archaeological site (Sierra de Atapuerca, Burgos, Spain). Quaternary Geochronology, 71(), -. DOI: 10.1016/j.quageo.2022.101318
    DOI del artículo: 10.1016/j.quageo.2022.101318
    Entidad: Universitat Rovira i Virgili
    Año de publicación de la revista: 2022
    Tipo de publicación: Journal Publications
  • Palabras clave:

    Earth and Planetary Sciences (Miscellaneous),Geochemistry & Geophysics,Geography, Physical,Geology,Geosciences, Multidisciplinary,Stratigraphy
    Single-grain tt-osl
    Sima del elefante
    Post ir-ir
    Middle pleistocene
    Los-huesos
    Atapuerca
    suitability
    single-grain tt-osl
    single
    sima del elefante
    post ir-ir
    middle pleistocene
    insights
    hominin
    half-lives
    gran dolina
    galeria
    deposits
    age
    Stratigraphy
    Geosciences, multidisciplinary
    Geology
    Geography, physical
    Geociências
    Geochemistry & geophysics
    Earth and planetary sciences (miscellaneous)
    Ciências ambientais
    Ciências agrárias i
    Biodiversidade
    Astronomia / física
    Antropologia / arqueologia
  • Documentos:

  • Cerca a google

    Search to google scholar