Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
7439936 | L'Anthropologie | 2017 | 34 Pages |
Abstract
The palaeolithic site of Gentelles (Somme, France) is situated on a chalky plateau unlike most Lower and Middle Palaeolithic sites of the Somme basin, which are related to fluvial environments (alluvial and slope deposits). The archaeological material of the site excavated at Gentelles on several thousand square meters is recovered from the infilling of a dolina. The archaeological sequence is attributed to Late Middle and Upper Pleistocene (MIS 10 to MIS 5). The assignment of the loess infilling the dolina to MIS 6 is supported by ESR/U-Th dates obtained on teeth and the IRSL age of the sediment. All lithic assemblages include bifacial production and debitage with cores showing one or several surfaces of debitage. There is no evidence of Levallois flaking methods, which are very common in many Middle Palaeolithic industries of Northern France. The first steps of the reducing sequences are not present in most lithic assemblages. Some faunal remains (equids, bovids) have been discovered in the loess deposits. In most cases, the function of the site corresponds to short occupations of hunters moving on the plateau. In contrast, the CLG assemblage (MIS 8) which shows many phases of the reducing sequence suggests longer occupations.
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History
Authors
Alain Tuffreau, Patrick Auguste, Sanda Balescu, Jean-Jacques Bahain,