Caracterización mineralógica de restos óseos pertenecientes al depósito endokárstico del yacimiento arqueológico Pleistoceno de la Cueva del Ángel: Lucena (Córdoba)

• G. Monge ^[1] ; M. I. Carretero ^[1] ; Manuel Pozo ^[2] ; Cecilio Barroso ^[3] ; D. Botella ^[4]
  1. [1] Universidad de Sevilla

     Universidad de Sevilla

     Sevilla, España

     
  2. [2] Universidad Autónoma de Madrid

     Universidad Autónoma de Madrid

     Madrid, España

     
  3. [3] Rincón de la Victoria (Málaga)
  4. [4] Museo Arqueológico y Etnológico de Lucena. Ayuntamiento de Lucena (Córdoba

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• Localización: El Cuaternario Ibérico. Investigación en el s. XXI: VIII Reunión de Cuaternario Ibérico (Sevilla - La Rinconada 2013) / coord. por Rafael Baena Escudero, José Juan Fernández Caro, Inmaculada Guerrero Amador, 2013, ISBN 978-84-695-8601-3, págs. 128-131
• Idioma: español
• Títulos paralelos:
  • Mineralogical characterization of bone remains belonging to the endokarstic deposit of the Pleistocene archaeological site of Cueva del Angel: Lucena (Córdoba)
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• Resumen

  • The site is located at the South of the Iberian Peninsula, on the outskirts of the town of Lucena. From a geologic point of view, this cavity is hosted by limestones and dolostones (Lias), belonging to the External Southern Subbetic Domain of the Betic Ranges. Within the endokarstic deposit, highlight the profile J/K, in which 18 samples of bone remains have been taken. The samples were characterized using X-ray diffraction, Fourier transform infrared spectroscopy and scanning electron microscopy. Crystallinity Index and Splitting Factor were also calculated. The results are interpreted as evidences of diagenetic processes and thermal events suffered by the bones (650°C - 700°C).