Obsidian from the Epipalaeolithic and Neolithic eastern Maghreb : a view from the Hergla context (Tunisia)
Simone Mulazzani
(1, 2)
,
François-Xavier Le Bourdonnec
(3)
,
Lotfi Belhouchet
(4)
,
Gérard Poupeau
(3, 5)
,
Jamel Zoughlami
(4)
,
Stéphan Stephan Dubernet
(3)
,
Emiliano Tufano
(6)
,
Yannick Y. Lefrais
(3)
,
Rym Khedhaier
(7)
1
ArScAn -
Archéologies et Sciences de l'Antiquité
2 UNIBO - Alma Mater Studiorum Università di Bologna = University of Bologna
3 IRAMAT-CRP2A - IRAMAT-Centre de recherche en physique appliquée à l’archéologie
4 INP - Institut National du Patrimoine - Tunisie
5 MNHN - Muséum national d'Histoire naturelle
6 UNISOB - Università degli studi Suor Orsola Benincasa
7 LAMPEA - Laboratoire méditerranéen de préhistoire Europe-Afrique
2 UNIBO - Alma Mater Studiorum Università di Bologna = University of Bologna
3 IRAMAT-CRP2A - IRAMAT-Centre de recherche en physique appliquée à l’archéologie
4 INP - Institut National du Patrimoine - Tunisie
5 MNHN - Muséum national d'Histoire naturelle
6 UNISOB - Università degli studi Suor Orsola Benincasa
7 LAMPEA - Laboratoire méditerranéen de préhistoire Europe-Afrique
François-Xavier Le Bourdonnec
- Fonction : Auteur
- PersonId : 21105
- IdHAL : francois-xavier-le-bourdonnec
- ORCID : 0000-0002-1051-5337
- IdRef : 121786811
Stéphan Stephan Dubernet
- Fonction : Auteur
- PersonId : 750951
- IdHAL : stephan-dubernet
- ORCID : 0000-0003-4278-3501
- IdRef : 188975683
Yannick Y. Lefrais
- Fonction : Auteur
- PersonId : 183293
- IdHAL : yannick-lefrais
- IdRef : 228238838
Résumé
In the present paper, it is shown that in the Hergla area (eastern Tunisia), obsidian was present from the early to at least the late sixth millennium cal BC. The presence of cores indicates that obsidian knapping was at least partly carried out in situ. The origin of these obsidians was determined from their elemental composition, by comparison with those originating from western Mediterranean potential sources, including analyses of new samples from the nearby Pantelleria Island. All obsidians were measured following the same protocol, by particle induced X-ray emission or by scanning electron microscopy/energy dispersion spectrometry. All the Hergla obsidians were found to originate from the Balata dei Turchi sources of Pantelleria. A review of the present body of knowledge on eastern Maghreb suggests, in spite of the still very preliminary data available, that Pantelleria was almost its unique provider of obsidians from the Epipalaeolithic to and during the Neolithic. However, the relative importance of the two main Pantellerian sources of Balata dei Turchi and Lago di Venere as providers of obsidian to eastern Maghreb remains to be investigated.
Format du dépôt | Notice |
---|---|
Type de dépôt | Article dans une revue |
Titre |
en
Obsidian from the Epipalaeolithic and Neolithic eastern Maghreb : a view from the Hergla context (Tunisia)
|
Résumé |
en
In the present paper, it is shown that in the Hergla area (eastern Tunisia), obsidian was present from the early to at least the late sixth millennium cal BC. The presence of cores indicates that obsidian knapping was at least partly carried out in situ. The origin of these obsidians was determined from their elemental composition, by comparison with those originating from western Mediterranean potential sources, including analyses of new samples from the nearby Pantelleria Island. All obsidians were measured following the same protocol, by particle induced X-ray emission or by scanning electron microscopy/energy dispersion spectrometry. All the Hergla obsidians were found to originate from the Balata dei Turchi sources of Pantelleria. A review of the present body of knowledge on eastern Maghreb suggests, in spite of the still very preliminary data available, that Pantelleria was almost its unique provider of obsidians from the Epipalaeolithic to and during the Neolithic. However, the relative importance of the two main Pantellerian sources of Balata dei Turchi and Lago di Venere as providers of obsidian to eastern Maghreb remains to be investigated.
|
Auteur(s) |
Simone Mulazzani
1, 2
, François-Xavier Le Bourdonnec
3
, Lotfi Belhouchet
4
, Gérard Poupeau
3, 5
, Jamel Zoughlami
4
, Stéphan Stephan Dubernet
3
, Emiliano Tufano
6
, Yannick Y. Lefrais
3
, Rym Khedhaier
7
1
ArScAn -
Archéologies et Sciences de l'Antiquité
( 1003 )
- MSH Mondes (bâtiment René-Ginouvès). 21, allée de l’Université 92023 NANTERRE Cedex
- France
2
UNIBO -
Alma Mater Studiorum Università di Bologna = University of Bologna
( 30978 )
- Via Zamboni, 33 - 40126 Bologna
- Italie
3
IRAMAT-CRP2A -
IRAMAT-Centre de recherche en physique appliquée à l’archéologie
( 399901 )
- Maison de l’archéologie
Esplanade des Antilles
33607 Pessac Cedex
- France
4
INP -
Institut National du Patrimoine - Tunisie
( 537244 )
- 04, place du château 1008 Tunis
- Tunisie
5
MNHN -
Muséum national d'Histoire naturelle
( 7512 )
- 57, rue Cuvier - 75231 Paris Cedex 05
- France
6
UNISOB -
Università degli studi Suor Orsola Benincasa
( 578056 )
- Naples
- Italie
7
LAMPEA -
Laboratoire méditerranéen de préhistoire Europe-Afrique
( 208163 )
- MMSH 5 Rue du château de l'Horloge BP 647 13094 AIX EN PROVENCE CEDEX 2
- France
|
Page/Identifiant |
2529-2537
|
Langue du document |
Anglais
|
Nom de la revue |
|
Vulgarisation |
Non
|
Comité de lecture |
Oui
|
Audience |
Internationale
|
Date de publication |
2010
|
Volume |
37
|
Numéro |
10
|
Domaine(s) |
|
Mots-clés |
en
Obsidian, Provenance, Hergla, Epipalaeolithic, Neolithic, Pantelleria, Tunisia
|
DOI | 10.1016/j.jas.2010.05.013 |
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