Secuencia cronoestratigráfica del Pleistoceno Superior en Sierra Morenala cueva de La Sima (Constantina, Sevilla).

  1. Rodríguez Vidal, J. 1
  2. Cáceres, L.M. 1
  3. Álvarez, G.
  4. Martínez Aguirre, A. 2
  5. Alcaraz, J.M. 3
  6. Riquelme, J.A. 4
  7. Recio, J.M. 3
  1. 1 Universidad de Huelva
    info

    Universidad de Huelva

    Huelva, España

    ROR https://ror.org/03a1kt624

  2. 2 Universidad de Sevilla
    info

    Universidad de Sevilla

    Sevilla, España

    ROR https://ror.org/03yxnpp24

  3. 3 Universidad de Córdoba
    info

    Universidad de Córdoba

    Córdoba, España

    ROR https://ror.org/05yc77b46

  4. 4 Universidad Autónoma de Madrid
    info

    Universidad Autónoma de Madrid

    Madrid, España

    ROR https://ror.org/01cby8j38

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Journal:
Geogaceta

ISSN: 0213-683X

Year of publication: 2002

Issue: 33

Pages: 47-50

Type: Article

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Abstract

La Sima of Constantina, located at the northermost part of Seville province, is a karstic cave with a thick terrigenous and chemical (flowstone) record. These sedimentary formations are representative of the Late Quaternary palaeoenvironmental history about these mountains (Sierra Morena) of the Southwestern Iberian Peninsula. There are many evidences of vertebrate bone remains of alleged prays, coprolites and bones of spotted hyaena (Crocuta cf. crocuta), mainly at the lower sedimentary layers, dated c.a. 72.5 ky BP. Upper detritic sediments show Calcolithic remains, with human bones, pottery and charcoallayers aged 4 600 ± 200 cal yr AMS.

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