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...
| Autores: | , |
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| 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 |
| 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. |
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