It appears you don't have support to open PDFs in this web browser. To view this file, Open with your PDF reader
Abstract
Charcoal and micro-layers of soot trapped in speleothems from the inner galleries of Nerja Cave were analysed through an interdisciplinary study. The absolute dating of the prehistoric subterranean activity of the cave and the identification of different phases of visits to the deep parts are presented and discussed. The charcoal analysis includes anthracological analysis and SEM–EDX. The soot analysis includes optical microscopy, Raman spectroscopy and TEM–EDX, and the microcounting of soot microlayers. The 14C dating of 53 charcoals identified 12 phases of prehistoric visits to the cave between 41,218 and 3299 cal. BP, putting back the origin of human occupation of this emblematic cave by 10,000 years. The interdisciplinary analysis of the soot microlayers allowed us to perform a high-precision zoom on the last three visitation phases identified by Bayesian analysis (8003–2998 cal. BP.), demonstrating that these phases contain at least 64 distinct incursions, with an average of one visit every 35 years for the Neolithic period. Spatial analysis showed that not all areas of the cave were used in the same periods, highlighting the repetition of visits to certain specific sectors of the Lower Galleries of the cave. Lastly, the anthracological data indicate a cross-cultural and unique use of Pinus tp. sylvestris-nigra wood for lighting activities over an extended period between the Gravettian and Upper Magdalenian.
You have requested "on-the-fly" machine translation of selected content from our databases. This functionality is provided solely for your convenience and is in no way intended to replace human translation. Show full disclaimer
Neither ProQuest nor its licensors make any representations or warranties with respect to the translations. The translations are automatically generated "AS IS" and "AS AVAILABLE" and are not retained in our systems. PROQUEST AND ITS LICENSORS SPECIFICALLY DISCLAIM ANY AND ALL EXPRESS OR IMPLIED WARRANTIES, INCLUDING WITHOUT LIMITATION, ANY WARRANTIES FOR AVAILABILITY, ACCURACY, TIMELINESS, COMPLETENESS, NON-INFRINGMENT, MERCHANTABILITY OR FITNESS FOR A PARTICULAR PURPOSE. Your use of the translations is subject to all use restrictions contained in your Electronic Products License Agreement and by using the translation functionality you agree to forgo any and all claims against ProQuest or its licensors for your use of the translation functionality and any output derived there from. Hide full disclaimer
Details
1 Université de Bordeaux, UMR CNRS 5199 PACEA, Pessac, France (GRID:grid.412041.2) (ISNI:0000 0001 2106 639X); Universidad de Córdoba, Córdoba, Spain (GRID:grid.411901.c) (ISNI:0000 0001 2183 9102)
2 Université Paris-Saclay, Laboratoire des Sciences du Climat et de L’Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Gif-sur-Yvette, France (GRID:grid.460789.4) (ISNI:0000 0004 4910 6535)
3 Institut Français d’Archéologie Orientale, Pôle Archéométrie, Cairo, Egypt (GRID:grid.459257.8)
4 Euskal Herriko Unibertsitatea/Universidad del País Vasco, Departamento de Geología, Leioa, Spain (GRID:grid.11480.3c) (ISNI:0000000121671098)
5 Universidad de Córdoba, Córdoba, Spain (GRID:grid.411901.c) (ISNI:0000 0001 2183 9102)
6 PSL University, Laboratoire de Géologie, Département de Géosciences, École Normale Supérieure, CNRS, UMR 8538, Paris, France (GRID:grid.440907.e) (ISNI:0000 0004 1784 3645)
7 Université de Bordeaux, UMR CNRS 5199 PACEA, Pessac, France (GRID:grid.412041.2) (ISNI:0000 0001 2106 639X)
8 Universidad de Cantabria, Instituto Internacional de Investigaciones Prehistóricas de Cantabria (IIIPC), Santander, Spain (GRID:grid.7821.c) (ISNI:0000 0004 1770 272X)