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Natural processes involved in the formation of Pleistocene bone assemblages in continental South-East Asian caves : the case of the cave of the monk (Chiang Dao Wildlife Sanctuary, Thailand).

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  • معلومة اضافية
    • Contributors:
      Histoire naturelle de l'Homme préhistorique (HNHP); Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS); Centre de recherches archéologiques indus - baluchistan - asie centrale et orientale (CRAIBACO); MUSEES DE FRANCE-Centre National de la Recherche Scientifique (CNRS); Travaux et recherches archéologiques sur les cultures, les espaces et les sociétés (TRACES); École des hautes études en sciences sociales (EHESS)-Université Toulouse - Jean Jaurès (UT2J); Université de Toulouse (UT)-Université de Toulouse (UT)-Ministère de la Culture et de la Communication (MCC)-Institut national de recherches archéologiques préventives (Inrap)-Centre National de la Recherche Scientifique (CNRS); Dynamique de l'évolution humaine : individus, populations, espèces Paris (DEHIPE); Centre National de la Recherche Scientifique (CNRS); 8th Regional Office of Fine Arts Department; Fine Arts Department; Pautreau J.-P.; Coupey A.-S.; Zeitoun V. et Rambault E.
    • بيانات النشر:
      HAL CCSD
      Siam Ratana Ltd, Chiang Mai
    • الموضوع:
      2006
    • Collection:
      Université Toulouse 2 - Jean Jaurès: HAL
    • الموضوع:
      Bougon; France
    • نبذة مختصرة :
      A large paleontological assemblage typical of Ailuropoda-Stegodon fauna was discovered in the Cave of the Monk, in northern Thailand. Geological and taphonomic approaches were conducted in order to determine site formation processes. A sedimentological study indicated that the fossiliferous layer resulted from mediumsize burrowing animals occupying the cave. Bone surface analysis confirmed that Porcupine was the main, if not exclusive, bone accumulator. A bone accumulation rate was calculated. The assemblage appears to have formed over an average period of one to several tens of thousand of years. This time frame means that the assemblage can not be considered as a homogeneous reference for palaeoenvironmental reconstruction as may have been assumed without the present analysis.
    • Relation:
      halshs-00423519; https://shs.hal.science/halshs-00423519; https://shs.hal.science/halshs-00423519/document; https://shs.hal.science/halshs-00423519/file/Lenoble-etal_Eurasea-2008.pdf
    • الدخول الالكتروني :
      https://shs.hal.science/halshs-00423519
      https://shs.hal.science/halshs-00423519/document
      https://shs.hal.science/halshs-00423519/file/Lenoble-etal_Eurasea-2008.pdf
    • Rights:
      info:eu-repo/semantics/OpenAccess
    • الرقم المعرف:
      edsbas.AFEADDD9