Variabilité et homogénéité des modes de débitage en Chine entre 300 000 et 50 000 ans |
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Authors: | Yinghua Li,É rika Bodin |
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Affiliation: | 1. École d’Histoire, université de Wuhan, Luojiashan, Wuchang, Wuhan, Province de Hubei 430072, Chine;2. UMR 7041, Archéologie et Sciences de l’Antiquité, Anthropologie des Techniques des Espaces et des Territoires au Plio-Pléistocène, 21, allée de l’Université, 92023 Nanterre cedex, France |
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Abstract: | The position of lithic industries of Chinese Paleolithic in comparison with those of other regions in the world is always a controversial topic. The typological analysis has made Chinese prehistorians reveal some variability between lithic industries of different regions of China in terms of technical tradition and industrial structure. But this recognition, based upon some morphological characters of stone artifacts, failed to define systematically the modes of production that exist in each site. To answer these problematic some new methods need to be applied. So the lithic materials from 8 Chinese sites dated from 300 ka to 50 ka B.P. were selected and analyzed by means of lithic technological analysis and a new approach for analyzing the structures of cores. This paper presents principally the analytical results of modes of débitage and revealed that the modes of débitage during this period were characterized essentially by system C (“simple débitage”) and E (discoid) and that the concept Levallois was absent during this period in technical systems of lithic production in China. The Chinese lithic industries between 300 ka and 50 ka B.P. saw some homogeneity in the scale of the continent and remarkable difference from those of other regions in the world. So a stable, continuous but independent even isolated evolution in comparison with those of other regions was observed in this period. In addition, despite of apparent homogeneity, some variability exists also between these industries. |
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Keywords: | Chine Palé olithique moyen Technologie lithique Systè me technique de production lithique Variabilité Homogé né ité |
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