Secuencia cronoestratigráfica del Pleistoceno Superior en Sierra Morena: la cueva de La Sima (Constantina, Sevilla)
La Sima of Constantina, located at the northermost part of Seville province, is a karstic cave with a thick terrigenous and chemical (f/owstone) record. These sedimentary formations are representative of the Late Quaternary palaeoenvironmental history about these mountains (Sierra Morena) of the Sou...
| Autores: | , , , , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2002 |
| País: | España |
| Institución: | Universidad de Sevilla (US) |
| Repositorio: | idUS. Depósito de Investigación de la Universidad de Sevilla |
| OAI Identifier: | oai:idus.us.es:11441/137135 |
| Acceso en línea: | https://hdl.handle.net/11441/137135 |
| Access Level: | acceso abierto |
| Palabra clave: | Upper Pleistocene Bone breccia Speleothem Isotopic dating Sierra Morena |
| Sumario: | La Sima of Constantina, located at the northermost part of Seville province, is a karstic cave with a thick terrigenous and chemical (f/owstone) record. These sedimentary formations are representative of the Late Quaternary palaeoenvironmental history about these mountains (Sierra Morena) of the Southwestern lberian 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 e.a. 72.5 ky BP. Upper detritic sediments show Calcolithic remains, with human bones, pottery and charcoal layers aged 4 600 ± 200 cal yr AMS. |
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