@article{10272/9125,
year = {2002},
url = {http://hdl.handle.net/10272/9125},
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 BR Upper detritic sediments show Calcolithic remains, with human bones, pottery and charcoal layers aged 4 600 ± 200 cal yr AMS},
publisher = {Sociedad Geológica de España},
keywords = {Upper Pleistocene},
keywords = {Bone breccia},
keywords = {Speleothem},
keywords = {Isotopic dating},
keywords = {Sierra Morena},
title = {Secuencia cronoestratigráfica del Pleistoceno Superior en Sierra Morena: la cueva de La Sima (Constantina, Sevilla)},
title = {Chronostratigraphic sequence during the Late Quaternary in Sierra Morena Mountains: La Sima Cave (Constantina, Seville, SW Spain)},
author = {Rodríguez Vidal, Joaquín and Cáceres Puro, Luis Miguel and Álvarez, G. and Martínez Aguirre, Arancha and Alcaraz, J. M. and Riquelme Cantal, José Antonio and Recio Espejo, José Manuel},
}