Le travail des matières d’origine dure animale dans le Magdalénien Morave : l’exemple des aiguilles à chas

Needles made from hard animal tissues are a stereotyped artefact; they have been found in six caves of the Moravian Karst / Czech Republic (Pekárna, ?itného, K?lna, Bý?í skála, Verun?ina, K?í?ova) containing Magdalenian layers. The paper deals with the technology of the production of these objects on the example of the Pekárna cave that has provided a lot of these artefacts in various degrees of wear, fragments, exploitation matrices and uncompleted needles. By the mean of spatial analysis we try to reconstitute the original context in the cave and insert the concerned artefact into the frame of the exploitation, treatment and utilisation of hard animal tissues by Magdalenian hunters in Moravia.     

La variabilité graphique du Molí del Salt (Vimbodí, Catalogne, Espagne) et l'art mobilier de la fin du Paléolithique supérieur à l'est de la Péninsule Ibérique

The Upper Paleolithic of Catalonia has been so far characterized by a very weak presence of artistic representations. This scarcity was especially surprising if we take into account the huge number of discoveries from other zones of the Iberian Peninsula (Valencia, the Cantabrian region). In this paper we present four objects of portable art found at the Molí del Salt site (Vimbodí, Conca de Barberà, Tarragona). Below a mesolithic layer, dated to 8 ka BP, there is an Upper Magdalenian sequence with several dates between 10.8 and 12.5 ka BP. These magdalenian levels have yielded four plaques of schist with engravings, including several animal figurines and one human representations. Once the objects are described, we will place them in the context of the portable art from the Late Upper Paleolithic of Mediterranean Spain. From these data, the chronocultural successions based on the Upper Magdalenian-Microlaminar Epipaleolithic distinction will be discussed.     

Le Magdalénien de la grotte « Grappin » à Arlay (Jura, France) : nouveaux regards

The “Grappin” or “Saint-Vincent's” cave, on the western slope of Jura, East of France, has been explored since 1889. From then to 1960, it has yielded substantial material dated to middle “à navettes” Magdalenian developing during the late Pleniglacial. The study of this settlement, although often mentioned, was never dealt with comprehensively until now. Due to its scientific importance for the middle Magdalenian of western Europe, the site is to be reinvestigated through a global interdisciplinary project entitled “The Tardiglacial and the start of Holocene in the Jura and its margins”. This paper will review our present knowledge of the site, radiocarbon dates and archaeological data. It also focuses on ornaments and engraved mobile art.     

Proposition méthodologique pour une étude des esthétiques du Mésolithique : une analyse sociologique-anthropologique de la fin du Tardiglaciaire et durant le Postglaciaire en Europe occidentale

Do the decorated productions cover esthetics, i.e. the whole of the symbolic systems of a culture of hunters-gatherers? How to leave this glance with the aesthetic requirements that we other Westerners, pose on all things… and to exceed the debate of the artistic expressions thought from the aesthetic point of view, like “works of art” objects and “stylistics” objects? It is out of question “to make a fetish” of the productions decorated “works of art” while placing them at the starting point with our reflexion, (Studying them from a functional, technological, typological, art for art, meaningful point of view…) but to associate another of dimensions of the aesthetic experiment, i.e., the context of the decorated productions.     

Les industries magdaléniennes de l’Ardèche (France) dans le contexte du bassin méditerranéen

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.     

Les gisements de Galería,Gran Dolina TD10 et Ambrona (le Complexe Inférieur) : trois modèles technologiques dans le deuxième tiers du Pléistocène moyen

In Europe, the second third of the middle Pleistocene is a key period in which the human settlement is increased, the occupied habitat multiplies, the use of fire begins, the Mode 2 generalizes, Mode 3 begins and the method of exploitation levallois develops. At this moment the occupations of Galería, Gran Dolina and Ambrona are developing. These three deposits of the north Plateau have a very complete archaeological record and a very long development in time, thus they represent three technological different models. These sites represent three technological different models that are determined by the quality of the raw materials that were used, the control and the safety of the sites, how many time it was spend in the knapping, the characteristics of the edges, they functionality and the cultural traditions.     

Les statuettes féminines en ivoire des faciès gravettiens et post-gravettiens en Europe centrale et orientale : modes de fabrication et de représentation

During the Upper Palaeolithic, especially in Gravettian times, the hunter-gatherer societies had an economy closely linked with the exploitation of two local species in Eastern Europe: reindeer and woolly mammoth. The ivory objects are rich archives about their ways of life and their collective imagination, as in particular the ivory female statuettes show. These figurines, also called “Venus”, are one of the cultural characteristics of the Gravettian sites. To date, although they are more numerous in Eastern Europe, they were discovered, in a variable number, also in site of Central and Western Europe; today, we have no clue that this cultural tradition crossed the Pyrenees. The corpus of pieces from the Gravettian sites of the Russian Plain (dated between 25,000 and 21,000 B.P.) is the more informative about technological know-how of the Gravettian craftsmen. He consists in the leading material of this paper, completed with some data about Epigravettian and Magdalenian statuettes. Whereas the Gravettian figurines show figurative female representations, those of the later cultural facies are more stylized. In a technological point of view, there is a close link between the choice of blanks within the mammoth tusk and the morphology of the statuettes, whatever the period of time considered.     

Le Gravettien ancien d’Europe centrale revisité : mise au point et perspectives

Focusing on central Europe, the present article aims at appraising the unity of the lithic technical systems related to the early Gravettian of the Swabian Jura and Lower Austria, generally treated as distinct cultural entities. Until recently, our knowledge of the Swabian Gravettian was known only through partial studies. Furthermore, according to the ¹⁴C dates available until the mid-nineties, the Swabian Gravettian tended to be attributed to a recent phase of this techno-complex, in contrast to the first manifestations of the Gravettian in the Middle Danube region. However, in the light of the new ¹⁴C dates, it appears today that the Swabian Gravettian doubtlessly belongs to the early stage of this techno-complex, in that comparable with the Gravettian of Weinberghöhlen in Bavaria or the early Gravettian of Willendorf II in Lower Austria. Our comparative study, integrating both typology and technology, deals with two reference sites with regard to the appearance and evolution of the Gravettian in Central Europe, Geißenklösterle and Willendorf II. The present study is a contribution to integrate the early stage of the Gravettian of this part of Europe in a broader discussion concerning the emergence of the generic cultural features of the Gravettian in its socioeconomical and cultural dimension, if we wish to progress in our understanding of what matters in the transition from the Aurignacian to the Gravettian.     

Les structures d’occupation gravettiennes en Europe centrale : le cas de Grub/Kranawetberg,Autriche

Grub/Kranawetberg, a multilayered Gravettian site in Lower Austria, is one of many Gravettian open-air sites of Central Europe. These sites are well-known since a long time for their settlement structures, but also rich lithic inventories as well as organic tools, personal adornments, and art objects (e.g., Pavlov, Dolní Vestonice). While old excavation and recording techniques do not allow a detailed intrasite spatial analysis of these sites, the ongoing fieldwork at Grub/Kranawetberg provides us with abundant and detailed information about spatial organization of a Gravettian open-air site in Central Europe. The site is excavated since 1993 and yielded four archaeological horizons with abundant finds (including numerous personal adornments) and some evident structures. The main focus of this paper is on the GIS-based methodology of intrasite spatial analysis, especially emphasizing the possibilities of recognizing formation processes, size-sorting and locating a possible dwelling. Application of various methods, among them piece-plotting, mapping of find quantities, application of kernel density estimates and ring and sector analysis, in the 1995 and 1996 excavation area showed latent structures which are interpreted as evidence for a dwelling in this area of the site. In the last part of the paper the evidence of Grub/Kranawetberg is discussed and compared with other European Gravettian sites.     

Les kystes de dinoflagellés du Crétacé moyen de la marge atlantique brésilienne, le bassin de Santos

Organic dinoflagellate cysts are studied from the sedimentary sequence of hole 1-SPS-14A, drilled during oil exploration in the Santos Basin, Brazilian continental margin. The Ariri and Florianópolis Formations (Transitional sequence) do not contain any dinocysts. The oldest found dinocysts occur at the base of the Drift sequence in sediments, within platform carbonates of the Guarujá Formation. Continuous sea-level rise throughout the late Albian and Cenomanian submerged the carbonate platform with the terrigenous input of the Itanhaém Formation. The transgressive phase reached its peak during the Cenomanian/Turonian transition. Pelites were deposited during oceanic anoxic event (OAE-2), consisting the lower part of the Itajaí-Açu Formation. Normal oceanic conditions re-established in the late Turonian. The Brazilian dinocyst assemblage has tethyan affinities. Some species (i.e., Dinopterygium cladoides, Litosphaeridium arundum, Odontochitina rhakodes and Systematophora cretacea) suggest a middle Albian age for the carbonate platform of the Guarujá Formation. The lower part of the Guarujá Formation was not dated by other microfossils. An uppermost Albian or lower Cenomanian age is suggested for the base of the Itanhaém Formation on the basis of species Palaeohystrichophora infusorioides and Ovoidinium verrucosum. The Cenomanian-Turonian boundary cannot be characterized by dinocysts. Species Atopodinium iuvene, which is known from Turonian sediments in Europe, was found at the top of the Itajaí-Açu Formation. The observed dinocyst bioevents (i.e., last occurrence) are correlated with known foraminiferal, nannofossil and other palynological bioevents. The diversity of the assemblages remains constant throughout the various palaeoenvironments as these are reflected by the Guarujá and Itajaí-Açu Formations, but relative abundances of taxa are variable. Genera Coronifera, Florentinia, Ovoidinium, Spiniferites and Trichodinium are abundant in the carbonate platform assemblages (Guarujá Formation). Genera Cribroperidinium and Cyclonephelium are abundant in detrital sediments (Itajaí-Açu Formation). Only one species (Subtilisphaera guarujaensis n. sp.) is restricted to the carbonate platform environment.     

L’exploitation non alimentaire des ressources animales pendant le Magdalénien au Nord-Est de la Peninsule Ibérique. L’exemple de la grotte du Parco (Alòs de Balaguer, Lleida, Espagne)

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.     

Nouvelles recherches sur l’identité culturelle et stylistique de la grotte Chauvet et sur sa datation par la méthode du C

The discovery of Chauvet cave, at Vallon-Pont-d’Arc (Ardèche), in 1994, was an important event for our knowledge of palaeolithic parietal art as a whole. Its painted and engraved figures, thanks to their number (425 graphic units), and their excellent state of preservation, provide a documentary thesaurus comparable to that of the greatest sites known, and far beyond what had already been found in the group of Rhône valley caves (Ardèche and Gard). But its study – when one places it in its natural regional, cultural and thematic framework – makes it impossible to see it as an isolated entity of astonishing precocity. This needs to be reconsidered, and the affinities that our research has brought to light are clearly incompatible with the very early age which has been attributed to it. And if one extends this examination to the whole of the Franco-Cantabrian domain, the conclusion is inescapable: although Chauvet cave displays some unique characteristics (like every decorated cave), it belongs to an evolved phase of parietal art that is far removed from the motifs of its origins (known from art on blocks and on shelter walls dated by stratigraphy to the Aurignacian, in France and Cantabrian Spain). The majority of its works are therefore to be placed, quite normally, within the framework of the well-defined artistic creations of the Gravettian and Solutrean. Moreover, this phase of the Middle Upper Palaeolithic (26,000–18,000) coincides with a particularly intensive and diversified local human occupation, unknown in earlier periods and far less dense afterwards in the Magdalenian. A detailed critique of the treatment of the samples subjected to AMS radiocarbon dating makes it impossible to retain the very early age (36,000 cal BP) attributed by some authors to the painted and engraved figures of Chauvet cave.     

Entre le Nord et le Sud—un site à pointes à dos de la fin de l’Allerød : Bad Breisig, district de Ahrweiler (vallée moyenne du Rhin, RFA)

Due to unparalleled conditions of preservation below volcanic ashes of the late glacial Laacher-See volcano, the Central Rhineland region, located at the geographic hinge between the North German Lowlands and the Highland zone, permits detailed insights into the environmental and vegetational history of the Allerød-Interstadial and has produced fundamental data for the reconstruction of the way of life of hunter-gatherer groups of that time. The recently investigated site of Bad Breisig, dating to the final part of the Allerød, is the first record of a Late Glacial human settlement of the Central Rhineland after the disastrous environmental destruction caused by the eruption of the Laacher-See volcano. The site is an important chronostratigraphic and typological key in the understanding of the development of the Final Palaeolithic technocomplex with backed points in Central Europe.     

Early Evidence of Acheulean Settlement in Northwestern Europe - La Noira Site,a 700 000 Year-Old Occupation in the Center of France

The human settlement of Europe during Pleistocene times was sporadic and several stages have been recognized, both from paleaoanthropological and archaeological records. If the first phase of hominin occupation (as early as 1.4 Ma) seems mainly restricted to the southern part of the continent, the second phase, characterized by specific lithic tools (handaxes), is linked to Acheulean settlements and to the emergence of Homo heidelbergensis, the ancestor of Neanderthals. This phase reached northwestern Europe and is documented in numerous sites in Germany, Great Britain and northern France, generally after 600 ka.At la Noira (Brinay, Central France), the Middle Pleistocene alluvial formation of the Cher River covers an archaeological level associated with a slope deposit (diamicton). The lithic assemblage from this level includes Large Cutting Tools (LCTs), flakes and cores, associated with numerous millstone slabs. The lithic series is classified as Acheulean on the basis of both technological and typological analyses. Cryoturbation features indicate that the slope deposits and associated archaeological level were strongly frozen and disturbed after hominin occupation and before fluvial deposition. Eight sediment samples were dated by the electron spin resonance (ESR) method and the weighted average age obtained for the fluvial sands overlying the slope deposits is 665±55 ka. This age is older than previous chronological data placing the first European Acheulean assemblages north of 45^th parallel north at around 500 ka and modifies our current vision of the initial peopling of northern Europe. Acheulean settlements are older than previously assumed and the oldest evidences are not only located in southern Europe. La Noira is the oldest evidence of Acheulean presence in north-western Europe and attests to the possibility of pioneering phases of Acheulean settlement which would have taken place on a Mode 1-type substratum as early as 700 ka. The lithic assemblage from la Noira thus provides behavioral and technological data on early Acheulean occupation in Europe and contributes to our understanding of the diffusion of this tradition.     

Nouvelles découvertes d'art rupestre au Mato Grosso (Cidade de Pedra, Rondonópolis, Brésil)

Since 1983, Professor Agueda Vilhena-Vialou is conducting in Mato Grosso (Brazil) the French-brasilian archeological mission Fossil men and their paleo-environments in the Paraná basin. Its goal is the study of the first prehistoric settlements of Latin America's heart, in their economic, social, cultural and symbolic dimensions. Thanks to the complementary and comparative analysis of the habitats, the regional settlements and the rock art, our research targets a more precise definition of territories and cultures proper of the prehistoric human groups from the South of the actual Mato Grosso state. The study of rock art, the most revealing aspect of symbolic behaviours, is one of the strongest programs inside our multidisciplinary team. Today, thanks to systematic prospections led along the Rio Vermelho (between Pantanal swamp at West and Rondonópolis city at East), a hundred rock art sites (walls, shelters and caves), decorated with signs, animals and humans, have been discovered, and, for the most of them, studied. These figures are painted, engraved and more rarely sculpted. Along those pages, the author is presenting the preliminary analysis of ten new rock art sites, recently identified in a cliff on the right bank of the Vermelho River. He starts a comparative study with the sites of the Cidade de Pedra and of close micro basin, from the left bank of the River. This research is showing the symbolic identities, both common and specific, proper to different territories of this major rock art region of Brazil, which is divided in several areas and micro territories, shared but autonomous.     

L’attribution culturelle des sculptures du Jura souabe selon les documents des découvreurs

The portable art discovered in the caves of the Swabian Jura has been dated to the Aurignacian for almost half a century, following work by J. Hahn, but that was not the opinion of the discoverers at the sites of Vogelherd and Hohlenstein Stadel. The dating of these figurines poses questions about the first development of figurative art. This paper examines the validity of the arguments presented about radiometric ages of the finds comparing to their stratigraphic locations. A varied chronology for these artworks becomes clear: in our view, some pieces from Vogelherd and Hohle Fels date to the Gravettian, while others from Vogelherd and Hohlenstein Stadel date to the Magdalenian. The arguments in favour of the Aurignacian do not hold up to critical examination.     

Les industries moustériennes de la Rouquette (Puycelci, Tarn, France)

The open-air site la Rouquette, located at the foot of a cliff, was excavated by André Tavoso (1979-1988). The seven Mousterian archaeological levels are all in place, but of different richness. The sedimentological and faunal studies define a series of dates between isotopic stages 4 and 3, maybe even at the end of stage 5 for the lowest levels. The industrial complexes represent three broad types of “Bordian” facies, with technological, typological and lithological evolution. The industries from levels E to B display interesting evolutionary traits in so far as technological and typological behaviour are concerned, in a general Charentian Quina type Mousterian from the south of France continuum. After a “classical” facies in the “western” sense of the term (levels E to C), an atypical form of this facies (levels Bb and B) displays characteristics generally marked in the Quina Mousterian of the Grands Causses in more eastern or Mediterranean Quina Mousterians. Level Bb presents a Mousterian facies with a Ferrassie tendency, characterizing a short-term occupation. Level A contains a Mousterian defined as “non classical denticulates”, in which typical Mousterian and Charentian Mousterian influences are clearly marked.     

Circulation of whale-bone artifacts in the northern Pyrenees during the late Upper Paleolithic

The importance of coastal resources in the late Upper Paleolithic of western Europe has been reevaluated in recent years thanks to a growing body of new archeological evidence, including the identification of more than 50 implements made of whale bone in the Magdalenian level of the Isturitz cave (western Pyrenees). In the present study, the assemblages of osseous industry from 23 Magdalenian sites and site clusters in the northern Pyrenees were investigated, systematically searching for whale-bone implements. The objective of this research was to determine if, and how, tools and weapons of coastal origin were circulated beyond Isturitz into the inland, and if similar implements existed on the eastern, Mediterranean side of the Pyrenees. A total of 109 whale-bone artifacts, mostly projectile heads of large dimensions, were identified in 11 sites. Their geographic distribution shows that whale bone in the Pyrenean Magdalenian is exclusively of Atlantic origin, and that objects made of this material were transported along the Pyrenees up to the central part of the range at travel distances of at least 350 km from the seashore. This phenomenon seems to have taken place during the second half of the Middle Magdalenian and the first half of the Late Magdalenian, ca. 17,500–15,000 cal BP (calibrated years before present). The existence of a durable, extended coastal-inland interaction network including the circulation of regular tools is thus demonstrated. Additionally, differences between the whale-bone projectile heads of the Middle Magdalenian and those of the Late Magdalenian document an evolutionary process in the design of hunting weapons.     

Gravettian ivory ornaments in Central Europe,Moravia (Czech Republic)

In the sense of the gravettian technocomplex of Central Europe in Moravia it is mammoth ivory which was mainly used to manufacture and create personal ornaments. The hunters and gatherers selected and stored mammoth tusks as the raw material for the manufacture of tools, weapons, furniture and ornaments. In Moravia, personal ornaments were found in a great variability of forms and sizes – mostly beads like breast-shaped beads, bilobated beads, bilobated flat beads, tear drop shaped beads and round ornaments – rings, bracelets, discs as well as flat elements – diadems and other pendants (zoomorphs, antropomorphs, geometric forms). Some types of personal ornaments show equivalent forms at other gravettian sites and some are unique in Moravia. This article illustrates the variability of these personal ornaments in the context of the Gravettian in Moravia.     

Style v dans le bassin du Douro: Tradition et changement dans les graphies des chasseurs du Paléolithique Supérieur européen

The documentation of some figures of hoofed in Siega Verde on panels of palaeolithic style and its stylistic references in the whole south of Europe, constitutes the starting point of the reflection on the presence of style v in the outdoors sites of the peninsular occident. In the Douro's region exists a richer documentation than the habitual in Europe: the outdoors panels of Côa and Siega Verde, the engravings on palaeolithic figures of La Griega, the paintings with direct chronologies of Ojo Guareña, the decorated plaquettes of the level 4 of Fariseu and the pebbles and plaquettes of Estebanvela. Painting in the caverns, outdoors and cave engravings and mobile art, with good references of absolute chronology between 11,500 BP and 9000 BP that confirm the continuity of the Palaeolithic art. If we compare the data of the peninsular occident with those of the north, those of Levant and those that begin to be known in Andalusia, the coincidence of dates is astonishing. In the same way if we compare these ones with the dates of the South of France and Italy. The external art of the western facade of the Iberian Peninsula possesses not only a unite palaeolithic contrasted sequence but rather it also puts in evidence the reality of the recurrent and continued locations in the whole sector during 30,000 years.Above the 11,000 BP, the transformations of the hunter groups begin to be evident in the whole south of Europe and the graphics demonstrate these changes, with a progressive transformation of contents and style that leads to a bigger schematization. The interesting cohabitation among naturalism and schematism that demonstrate the direct dates of C¹⁴, apparent a progressive transformation that discards radical ruptures between the social and graphic world of the palaeolithic hunters and their heirs.