Typology and provenance of obsidians from the A Guaita Neolithic site (NW Cap Corse, Corse, France)

被引:5
作者
Le Bourdonnec, Francois-Xavier [1 ]
Poupeau, Gerard [1 ,2 ,3 ]
Lorenzi, Francoise [4 ,5 ]
Machut, Pierre [1 ]
Sicurani, Jean [4 ,6 ]
机构
[1] Univ Bordeaux 3, CNRS, IRAMAT CRP2A, UMR 5060, F-33607 Pessac, France
[2] Museum Natl Hist Nat, CNRS, Ctr Spectroscopie Infrarouge, Dept Prehist, F-75231 Paris 05, France
[3] Museum Natl Hist Nat, CNRS, Ctr Spectroscopie Infrarouge, UMR 7194, F-75231 Paris 05, France
[4] Univ Corse, CNRS, LISA, UMR 6240, F-20250 Corte, France
[5] Univ Corse, Apauc, Dept Archaeol, F-20250 Corte, France
[6] Univ Corse, Grp Rech Prehist & Protohist, F-20250 Corte, France
关键词
Obsidian; Provenance; SEM-EDS; PIXE; Typology; Neolithic; A Guaita; Corsica; PIXE; SARDINIA;
D O I
10.1016/j.crpv.2013.10.005
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
The provenance of a large fraction of the obsidians from the Neolithic site of A Guaita was determined for its three chronocultural layers, between the second half of the 6th millennium and the beginning of the 4th millennium. The elemental composition of 140 samples was obtained by scanning electron microscopy (SEM EDS) and/or ion beam analysis (PIXE). One hundred and thirty-eight obsidians were found to come from Sardinia and the remaining two from Palmarola Island. This result confirms the almost unique presence of Sardinian obsidians in Corsica and extends this observation to the northern end of the island. The three main Sardinian obsidian types, SA, SB2, and SC, are represented at A Guaita, with a predominance of SB2 and SC. The occurrence of two obsidians from Palmarola suggests that occasional contacts with the Italian Peninsula were in effect from the 6th millennium, in agreement with previous data from ceramics. (C) 2013 Academie des sciences. Published by Elsevier Masson SAS. All rights reserved.
引用
收藏
页码:317 / 331
页数:15
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