El límite Pleistoceno–Holoceno en el yacimiento arqueológico de la Cueva de Nerja (Málaga, España): nuevas aportaciones cronoestratigráficas y paleoclimáticas.

During the Late Upper Pleistocene and the Lower and Middle Holocene an important sedimentary record was deposited in the ancien entry of Nerja Cave (Málaga, Spain). The 41 calibrated valid 14C dates obtained from this record show a chronological spread between 30 and 3,6 ky. cal. BP for the archaeol...

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Detalles Bibliográficos
Autores: Aura Tortosa, J. Emili, Jordá Pardo, Jesús Francisco
Tipo de recurso: artículo
Fecha de publicación:1970
País:España
Institución:Universidad Nacional de Educación a Distancia
Repositorio:e-spacio. Repositorio Institucional de la UNED
Idioma:español
OAI Identifier:oai:e-spacio.uned.es:20.500.14468/19557
Acceso en línea:https://hdl.handle.net/20.500.14468/19557
Access Level:acceso abierto
Palabra clave:Nerja Cave
archaeological record
radiocarbony
radiocarbon
Palaeoclimatology
Chronostratigraph
Descripción
Sumario:During the Late Upper Pleistocene and the Lower and Middle Holocene an important sedimentary record was deposited in the ancien entry of Nerja Cave (Málaga, Spain). The 41 calibrated valid 14C dates obtained from this record show a chronological spread between 30 and 3,6 ky. cal. BP for the archaeological record of Nerja Cave. This large stratigraphic record constitutes one of the most important archaeological. and palaeobiological sequences of the western Mediterranean, which contains remains of the Gravettian, Solutrian, Magdalenian, Epipaleolithic, Neolithic and Cooper Age. In this paper we establish a narrower correlation between the main palaeoclimatological events detected in Alborán Sea and the sedimentary and occupational episodes of the cave.