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Oscar Moro-Abadía 《L'Anthropologie》2003,107(4):455-470
On the occasion of the centenary of the Emile Cartailhac’s « Mea culpa d’un sceptique”, we want to reflect on one of the main questions of our discipline: Why has so-called « cave art” only been accepted as Paleolithic art in 1902, whereas the so-called « mobiliary art” had been accepted as Paleolithic art at the beginning of 1860s? In this paper, we want to suggest a definition of the conception of primitive art during the last third of the 19th century in order to understand: (A) Why Paleolithic paintings in the walls of some caves (Niaux, Chabot, Altamira) were not accepted as Paleolithic art between 1860 and 1902. (B) Given that what we now call mobiliary art is the same artistic phenomenon that prehistorians of the late 19th century thought of as primitive art, this article allows us to suggest a genealogy of mobiliary art. This genealogy will enable us to show that this concept not only defines a wide variety of forms, from engraving stones to carving in antler or ivory, but hides a multiplicity of meanings and connotations which originated in the period between 1860 and 1900. 相似文献
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Cinzia Joris 《L'Anthropologie》2002,106(1):99
Ardèche, a department of Rhone Alpes region, is rich in prehistoric sites belonging to a very large chronological period dated back to 350?000 years ago. But, the prehistory of the region has been unknown for a long time, mainly, because of its distance from traditional centres of research. Jean Combier, in his abstract dated 1967, defined for the first time Upper Palaelolithic stages: only towards the acquisition of new data, we are now able to suggest a new evolution for the Magdalenian from its origins to the Alleröd climatic episod. To define Ardèche originality within the Magdalenian context, we have compared its lithic industries with those of the Adaouste Cave oriental sites, the Cornille rock shelter and of the Gazel cave in the Aude western part. Ardèche Magdalenian dwelling is peculiar compared to the South West of France. Badegoulian has been substituted by a Mediterranean Facies culture rich in bladelets, the Salpestrian. This facies limited in its geographic extention to Gard and Ardèche, evolves gradually in situ gaining Magdalenian elements (such as backed bladelets and dihedral burins) giving birth to the transitory lithic complex of Huguenots and Baume d’Oullins Cave. An established Magdalenian is certified in the Blanchisserie camp, within a cold climatic context dated back to circa 16?000 years ago. Although the lithic industry is dominated by dihedral burins and backed bladeletse it is also characterised by some archaic features (such as keel endscrapers, transverse burins and scalene bladelets). The upper Magadalenian with bone harpoons appears soon in our region, in the Colombier rock shelter, in a fairly temperate climatic context dated according to 14C back to circa 14?000 BP. We could identify six stages within the evolution of this Upper Magdalenian.which are attested in the Colombier, Ebbou and Deux Avens Caves and in the Colombier rock shelter that has been occupied during several periods. The Magdalenian gradually changed loosing his most typical elements, the bladelets and burins supremacy has been substituted by Azilian elements (such as short endscrapers and curved backed points). But even if the Azilian process happens very early (before 12?500 BP) the Magdalenian, in its fundamental features, never disappears completely and it has never been substituted by classic Azilian. After Alleröd appears a culture characterised by the recovery of Magdalenian features similar to the Epimagdalenian defined by D. Sacchi in Gazel. The described evolution can be compared, as regard to its upper stages, to that of several sites of Rhone region as well as of the North West of France, which allow to define a culturally homogeneous province having the Rhone corridor with Ardèche as its Southern border. At the end of Palaeolithic this province broke up and Ardèche opened to the South and the Mediterranean from where seems to come the retouched large blade facies and endscrapers attested by the Colombier rock shelter dating back to 12?150 BP. 相似文献
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Parco cave, discovered in 1974, has yielded more than 50 objects fashioned of hard animal parts from levels dating to later phases of the Magdalenian. In the work described here, we have undertaken a technotypological analysis of this previously unstudied bone and antler assemblage. The osseous series from Parco are homogeneous and very similar to those from nearby sites of roughly the same time period; that is to say of the late Upper Magdalenian of the peninsular Mediterranean. The latter are composed primarily of hunting weapons dominated by antler projectile points, as well as eyed bone needles and a few shell ornaments. Technological analysis shows production in which there is a tight relationship between morphological type and raw material employed. The production schema saw the removal of blanks by means of groove and splinter technique, followed by shaping of pieces by scraping and finishing of them - in some cases by abrasion. 相似文献
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A 122 cm-long core was taken in the El-Guettiate Sebkha of Skhira (southeastern part of Tunisia) in order to investigate the recent palaeoenvironmental evolution of this region. The quantitative and qualitative analysis of ostracod and benthic foraminifera assemblages coupled with a correspondence analysis allows the reconstruction of palaeoenvironmental changes during the Holocene in this area. Four typical associations of ostracods (open marine, coastal marine, lagoonal and estuarine brackish) and two associations of benthic foraminifera (coastal and lagoonal) were distinguished. The onset of restricted lagoonal environments linked to the building-up of sand spit led to the onset of restricted lagoon and brackish environment at cal. 5408 years BP. The Shannon and equitability index of diversity were used to decipher the structural variations of the populations of ostracods and benthic foraminifera along the sampled core. We note a reduction in the Shannon index from the bottom to the top, which indicates a progressive isolation of the biotope. The open lagoonal episode is characterized by high values of diversity. During restricted lagoonal episodes the Shannon and equitability index are reduced. The correspondence analysis reveals an environmental gradient related to the marine influence. It shows an antagonism between the widely opened estuarian lagoonal species and those of restricted lagoon. The less opened estuarian lagoonal taxa occupy an intermediate position. Based on these evidences, microfauna carried out in the El-Guettiate Sebkha allows us to recognize four phases beginning with a widely opened estuarian lagoon (ca. cal. 7460 years PB), followed by a restricted lagoon (ca. cal. 5408 years BP) and finally a brackish lagoon evolving towards the present-day sebkha environment. The opened estuarine lagoon is characterized by high values of species richness and diversity indices. 相似文献