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Three archaeomagnetic applications of archaeological interest to the study of burnt anthropogenic cave sediments

  • Datos identificativos

    Identificador: PC:1477
    Handle: http://hdl.handle.net/20.500.11797/PC1477
  • Autores:

    J.M. Vergès
    Á. Carrancho
    Á. Herrejón Lagunilla
  • Otros:

    Autor según el artículo: J.M. Vergès; Á. Carrancho; Á. Herrejón Lagunilla
    Departamento: Història i Història de l'Art
    Autor/es de la URV: VERGÈS BOSCH, JOSEP MARIA; Á. Carrancho; Á. Herrejón Lagunilla
    Palabras clave: Ashes Bronze Ages Fumiers
    Resumen: Recent archaeomagnetic studies carried out on Mid-to Late Holocene burnt anthropogenic cave sediments have shown that under certain conditions, these materials are suitable geomagnetic field recorders. Archaeomagnetic analyses carried out on these contexts constitute a rich source of information not only for geophysical purposes -in terms of reconstructing the variation of Earth's magnetic field in the past- but also from the archaeological point of view, for example by archaeomagnetic dating. Here, we report three different archaeomagnetic applications to the study of burnt cave sediments: (i) archaeomagnetic dating; (ii) determining palaeotemperatures and (iii) assessing post-depositional processes. The first case study is a dating attempt carried out on a Late Holocene (Bronze Age) burnt level from El Mirador Cave (Burgos, Spain). Using the directional European secular variation curve, several dating intervals were obtained for the last burning of this combustion feature. Considering the archaeological evidence and the independent radiometric (14C) dating available the possible ages obtained are discussed. This is the first archaeomagnetic dating obtained in these contexts so far. The second case study is an application of the method to determine the last heating temperatures reached by the carbonaceous facies of these fires. Stepwise thermal demagnetization of oriented samples can be used to quantitatively estimate heating temperatures. An intermediate normal polarity component interpreted as a partial thermo-remanence (pTRM) with maximum unblocking temperatures of 400-450 °C was systematically identified, revealing the last heating temperatures experienced by this facies. These temperatures were confirmed with partial thermomagnetic curve experiments. Finally, archaeomagnetic analyses on a partially bioturbated burning event were performed in order to evaluate until what spatial extent the burnt sediments were affected by post-depositional mechanical alteration processes. For each case study, the archaeological implications are discussed highlighting the potential of archaeomagnetic methods to retrieve archaeological information.
    Grupo de investigación: Autoecologia Humana del Quaternari
    Áreas temáticas: Història Historia History
    Acceso a la licencia de uso: https://creativecommons.org/licenses/by/3.0/es/
    ISSN: 1040-6182
    Identificador del autor: n/a; n/a; n/a
    Fecha de alta del registro: 2016-04-19
    Versión del articulo depositado: info:eu-repo/semantics/acceptedVersion
    Enlace a la fuente original: https://www.sciencedirect.com/science/article/abs/pii/S1040618215009696
    DOI del artículo: 10.1016/j.quaint.2015.10.010
    Entidad: Universitat Rovira i Virgili
    Año de publicación de la revista: 2016
    Tipo de publicación: Article Artículo Article
  • Palabras clave:

    Arqueologia
    Ashes
    Bronze Ages
    Fumiers
    Història
    Historia
    History
    1040-6182
  • Documentos:

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