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New luminescence dating results based on polymineral fine grains from the Middle and Upper Palaeolithic site of La Ferrassie (Dordogne, SW France)

Authors :
Laurent Bruxelles
Stéphane Madelaine
Laurent Chiotti
Shannon P. McPherron
Paul Goldberg
Norbert Mercier
Marine Frouin
Christelle Lahaye
Harold L. Dibble
Dennis Sandgathe
Alain Turq
Guillaume Guérin
Vera Aldeias
Sebastien Huot
Teresa E. Steele
Research Laboratory for Archaeology and the History of Art [Oxford]
University of Oxford [Oxford]
IRAMAT-Centre de recherche en physique appliquée à l’archéologie (IRAMAT-CRP2A)
Institut de Recherches sur les Archéomatériaux (IRAMAT)
Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Université Bordeaux Montaigne-Université de Technologie de Belfort-Montbeliard (UTBM)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Université Bordeaux Montaigne-Université de Technologie de Belfort-Montbeliard (UTBM)
University of Illinois at Urbana-Champaign [Urbana]
University of Illinois System
Max Planck Institute for Evolutionary Anthropology [Leipzig]
Max-Planck-Gesellschaft
Institut national de recherches archéologiques préventives (Inrap)
Travaux et recherches archéologiques sur les cultures, les espaces et les sociétés (TRACES)
Ministère de la Culture et de la Communication (MCC)-École des hautes études en sciences sociales (EHESS)-Université Toulouse - Jean Jaurès (UT2J)-Centre National de la Recherche Scientifique (CNRS)
Institut Français en Afrique du Sud (IFAS)
Institut Français en Afrique du Sud
Histoire naturelle de l'Homme préhistorique (HNHP)
Muséum national d'Histoire naturelle (MNHN)-Université de Perpignan Via Domitia (UPVD)-Centre National de la Recherche Scientifique (CNRS)
University of Pennsylvania [Philadelphia]
Archaeology Department
Boston University [Boston] (BU)
De la Préhistoire à l'Actuel : Culture, Environnement et Anthropologie (PACEA)
Université de Bordeaux (UB)-Centre National de la Recherche Scientifique (CNRS)
Simon Fraser University (SFU.ca)
Department of Human Evolution [Leipzig]
Max-Planck-Gesellschaft-Max-Planck-Gesellschaft
Musée National de Préhistoire
Ministère de la Culture et de la Communication (MCC)
École des hautes études en sciences sociales (EHESS)-Université Toulouse - Jean Jaurès (UT2J)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS)
Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS)-Université de Perpignan Via Domitia (UPVD)
Université de Technologie de Belfort-Montbeliard (UTBM)-Université d'Orléans (UO)-Université Bordeaux Montaigne-Centre National de la Recherche Scientifique (CNRS)-Université de Technologie de Belfort-Montbeliard (UTBM)-Université d'Orléans (UO)-Université Bordeaux Montaigne-Centre National de la Recherche Scientifique (CNRS)
Max Planck Institute for Evolutionary Anthropology
Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Université de Perpignan Via Domitia (UPVD)
Source :
HAL, Quaternary Geochronology, Quaternary Geochronology, Elsevier, 2017, 39, pp.131-141. ⟨10.1016/j.quageo.2017.02.009⟩, Quaternary Geochronology, Elsevier, 2017, 39, pp.131-141

Abstract

In this study we compare different infrared stimulated luminescence (IRSL) signals for dating archaeological deposits. The IRSL and the more recently developed post-IR IRSL (pIR-IR) methods were investigated using polymineral fine grains extracted from the Middle and Upper Palaeolithic western excavation area in the site of La Ferrassie (Dordogne, SW France). The IRSL data measured at 50 °C (IR 50 ) are compared to those obtained with the elevated pIR-IR signals measured for two stimulation temperatures, 225 °C (pIR-IR 225 ) and 290 °C (pIR-IR 290 ). The signals are documented in terms of bleaching and fading rates. In addition, comparisons of the IR 50 ages corrected either with the H + L method (Huntley and Lamothe, 2001) or with the dose rate correction method (DRC, Lamothe et al. , 2003) are presented. Results show that the polymineral fine grains give a reasonable estimate of the burial age of the samples. The IR 50 and pIR-IR 225 provide the most reliable ages when they are corrected using the DRC method (because of saturation effects). The polymineral ages are then compared with the previously obtained ages on K-feldspar coarse grains, quartz OSL (Guerin et al. , 2015) and radiocarbon ages with the aim of accessing information on the depositional processes. It appears that further comparison of polymineral fine grains to coarse grains is beneficial to evaluate bleaching. Moreover, the polymineral results either confirm or refine the chronology of the La Ferrassie sequence proposed by Guerin et al. (2015), that is, the Mousterian layers range from marine isotope stage (MIS) 5 to the middle of MIS 3. In particular, i) the base of Layer 3 is pushed back to the end of MIS 4 or beginning MIS 3 and ii) the chronological attribution of Layers 4 and 5 is confirmed as MIS 3. Finally, the chronology of the Aurignacian layer (Layer 7) is strengthened by all the feldspars results.

Details

ISSN :
18711014
Database :
OpenAIRE
Journal :
HAL, Quaternary Geochronology, Quaternary Geochronology, Elsevier, 2017, 39, pp.131-141. ⟨10.1016/j.quageo.2017.02.009⟩, Quaternary Geochronology, Elsevier, 2017, 39, pp.131-141
Accession number :
edsair.doi.dedup.....4dc989d2b190aaa9d47cdcc8146c4e62