RT Journal Article
T1 Secuencia cronoestratigráfica del Pleistoceno Superior en Sierra Morena: la cueva de La Sima (Constantina, Sevilla)
T1 Chronostratigraphic sequence during the Late Quaternary in Sierra Morena Mountains: La Sima Cave (Constantina, Seville, SW Spain)
A1 Rodríguez Vidal, Joaquín
A1 Cáceres Puro, Luis Miguel
A1 Álvarez, G.
A1 Martínez Aguirre, Arancha
A1 Alcaraz, J. M.
A1 Riquelme Cantal, José Antonio
A1 Recio Espejo, José Manuel
AB 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
PB Sociedad Geológica de España
YR 2002
FD 2002
LK http://hdl.handle.net/10272/9125
UL http://hdl.handle.net/10272/9125
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026