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Chronostratigraphic sequence during the Late Quaternary in Sierra Morena Mountains: La Sima Cave (Constantina, Seville, SW Spain)

dc.contributor.authorRodríguez Vidal, Joaquín 
dc.contributor.authorCáceres Puro, Luis Miguel 
dc.contributor.authorÁlvarez, G.
dc.contributor.authorMartínez Aguirre, Arancha
dc.contributor.authorAlcaraz, J. M.
dc.contributor.authorRiquelme Cantal, José Antonio
dc.contributor.authorRecio Espejo, José Manuel
dc.date.accessioned2014-11-06T10:30:10Z
dc.date.available2014-11-06T10:30:10Z
dc.date.issued2002
dc.identifier.urihttp://hdl.handle.net/10272/9125
dc.description.abstractLa 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 AMSen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherUpper Pleistoceneen_US
dc.subject.otherBone brecciaen_US
dc.subject.otherSpeleothemen_US
dc.subject.otherIsotopic datingen_US
dc.subject.otherSierra Morenaen_US
dc.titleSecuencia cronoestratigráfica del Pleistoceno Superior en Sierra Morena: la cueva de La Sima (Constantina, Sevilla)en_US
dc.titleChronostratigraphic sequence during the Late Quaternary in Sierra Morena Mountains: La Sima Cave (Constantina, Seville, SW Spain)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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