Le Paléolithique Supérieur dans la moyenne vallée de l’Ebre

After 30 years of research, we begin to perceive an incipient outline of the Upper Palaeolithic in the central Ebro Valley. The assembled data permit us to speak of human occupation on the Southern face of the Pyrenees, but also on the borders of the Iberian Mountains and of the Ebro basin. All these sites seem to mark the passageways from and to the neighbour territories, emphasizing the communication pathway role of the Iberian basin.     

Le site Paléolithique de Suyanggae, Corée

The Suyanggae site is an open-air site in central part of South Korea. This site was discovered in 1980 and seven excavations have been carried out from 1983 to 1996. As a result, many stone artefacts were unearthed and 49 stone tool workshops were known. This site contains 5 cultural layers and the most important one is the Upper Paleolithic layer. This layer is dated to be 16,400 ~ 18,630 BP by ¹⁴C dating. It shows a massive blade production and microblade technique. It is one of the crucial sites for understanding the Upper Paleolithic of Korea.     

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.     

La culture du Paléolithique dans la région de Jungwon en Corée

The Jungwon region is located in the central part of Korea and it is one of crucial regions for understanding of the Korean Paleolithic culture. Many Paleolithic sites have been discovered in this region, from the lower Paleolithic to the upper Paleolithic. It is of interest the remarkable variety of archeological remains such as human bones, stone tools, animal bones and paleoenvironmental artifacts. As a result, it permits us to reconstruct the subsistence of prehistoric men. This region has an important role for Korean prehistoric researches.     

L'Aurignacien et le Gravettien ancien de la grotte Paglicci au Mont Gargano

The author illustrates, in a very synthetical way, Aurignacian and early Gravettian lithic industry from Paglicci Cave (Mount Gargano, South Italy), found during excavations carried out by University of Siena in the Eighties-Nineties. Layer 24 contains Aurignacian industries and is constituted by a fine silty-sandy sediment. The faunal remains from layer 24, dominated by Equus asinus, indicate a dry-temperate phase which on the basis of ¹⁴C dates, would be identified with the Arcy. Lithic industry contains numerous marginally backed bladelets and microbladelets Dufour like that, in the higher level evolve into a special type (denominated “PA 24 A1”). The early Gravettian occupies the overlying layers 23 and 22 that are rich in rough stones and blocks and contain more or less cold faunal remains (at first dominated by Capra ibex, subsequently Bos primigenius becomes abundant): the ¹⁴C dating insert them in a phase between Arcy and Tursac. Lithic industry includes a great number of La Gravette backed points and especially microgravette backed points. Some probable fléchettes are also present but unfortunately they are fragmented.     

L'industrie lithique du Paléolithique dans la région de Jungwon en Corée

Prehistoric people have been often lived in the Jungwon region during the Paleolithic. It is a reference for development of the Paleolithic cultures in Korea. During the lower Paleolithic, pebble tool culture has been developed: tools were made with local raw materials and direct percussion and anvil technique were utilized. Debitage and raw material of the middle Paleolithic did not make a great difference to the lower Paleolithic. Otherwise, tool size became small and the number of flake tools increased. The crucial changes occurred during the upper Paleolithic. Technique, acquisition of raw material and tool kits were thoroughly innovated. All of these changes would reveal that the upper Paleolithic people have carried out more various activities, that earlier periods and their social structure would be more complex than other ones'.     

Sols et structures d’habitat du Paléolithique supérieur, nouvelles données depuis les Cantabres : la Galerie Inférieure de La Garma (Cantabrie, Espagne)

A brief review is done of the history of the research on Upper Paleolithic floors and structures, with a general outline of the main substantive and theoretical-methodological aspects. On the resulting “state of the art” we present the preliminary results of the study of the occupation evidences from the Lower Gallery of La Garma. In essence, it constitutes an astonishing ensemble of extensive Middle Magdalenian occupation floors, exceptionally rich and quite well preserved, including several structures and associated with rock art paintings and carvings of that period. The potential of the site is superlative, and the research’s project already begins to offer some interesting results of which this article is a fairly small advance.     

Les séries silicoclastiques miocènes du Nord-Est au Sud-Ouest de la Tunisie : une mise au point

During the Miocene time, the Atlas-pelagian block, which is limited northward by the atlasic-alpin chain of North Africa-Sicily, southward by the Gafsa-Jeffara-Azizia fault and eastward by the Malta escarpment, resulted from the extension-compression regime, mainly controlled by the subduction-collision processes. This regime induced the opening of many Miocene microbasins, which have been infilled by silicoclastic materials showing lateral and vertical facies variations and several hiatus associated to tectonic and stratigraphic unconformities. Excepting the very local transgressive regimes, such as those of Langhian and Messinian periods, most of the Miocene deposits took place on internal platforms, especially at the NE part of the country. The fluviodeltaic and alluvial sediments are, in fact, lateral equivalents which infilled the valley and depression enclosed systems towards the SW. In this context (rapid facies variations in time and space, superposition of tectonic and eustatic unconformities, climatic variations, rare or absent stratigraphic markers…), some controversies remain as regards the correlation and dating of these series. This work consists of a study of the lateral and vertical facies and thickness variations, coupled to the identification of the main unconformities. It is also a study of significance of the main sedimentological mechanisms and an inventory of the different palynological and paleontological content of the sediments. The aim of this work is to propose a new vision on the Miocene deposits in Tunisia along a NE-SW axis. Then, using these data, we have correlated the different lithological formations, discuss their age and, finally, proposed paleogeographical drafts for them.     

Kabazi II (Crimée, Ukraine) : un site d'abattage et de boucherie du Paléolithique moyen

The site of Kabazi II is located on the second row of the Crimea Mounts in the west side of peninsula. The study presented in this article is about the archaeological material of the II/8 level. This level was excavated in 1987 and 1994. It is date of the Hengelo Interstadial. The lithic tools discovered in this level are attributed to the Western Crimea Mousterian (WCM). The E. hydruntinus dominates with more than 90% of the determinated remains. The crossed analysis of the results given by the studies of lithic and bone materials allowed to clarify the chronology, the environment and also the technical and subsistence behaviours of the Neandertals of the II/8 level of Kabazi II. These new interpretations are presented here.     

Paléogéographie des chasseurs de l’Europe du Paléolithique supérieur : répartition et spécialisation des sites

During the Upper Paleolithic, Europe was occupied by human populations mainly living from hunting of big terrestrial mammals. A repartition of fauna and of archeological sites was done with a database: a repartition of Upper Paleolithic sites in central and western Europe. This study shows that the european space was structured following several factors; climate, environment, cynegetic behaviours… We observe a partition of Europe with a mediterranean area with mainly deer, and ibex and an atlantic area with reindeer. Equally, most of the occupations are localized in the “aquitano-cantabric horn” around the Gulf of Gascony. The occupation of Europe undergone a pulsation with a retreat of occupations toward the west and the south during the glacial maximum, then a colonization of North Europe during the Tardiglacial climatic amelioration.     

Reconstitution de la végétation et du paléoclimat à partir de charbons de bois prélevés sur les sites du Paléolithique dans la région de Jungwon en Corée

Hundreds samples of the charcoals and waterlogged woods excavated from three late Paleolithic sites (Suyanggae, Gunang-gul and Sorori) in the Jungwon Region in Korea were analyzed to reconstruct the vegetation and paleoclimate in the region. Analyzed charcoal samples from the Suyanggae site show that the climate was cold in the lower part and it became more warm and dry in the upper part. From the Gunang-gul site, only Picea spp. was identified, indicating cool climates. From the Sorori site, two species were found; Alnus spp. (95%) and Ulmus spp. (5%). No conifers were discovered. The species composition indicates that the climate condition of central Korean peninsula around 8,800 BP was little cooler and wetter condition.     

Paléolithique supérieur et Mésolithique en Méditerranée : cadre culturel

The origin of the Upper Palaeolithic around the Mediterranean was the result of the local evolution, particularly in the Near East and in the Lower Nile basin, and of the migration from this zone to South-Eastern and Central Europe. The Initial Upper Palaeolithic in the Near East belt was the effect of local evolution from the industries based on Levallois concept to the industries which developed leptolithic blade technologies. This evolution is well registered in multi-layer sites in the Syro-Palestinian belt (Emirian/Ahmarian), which was the starting point of the diffusion of these “transitional” industries in South-Eastern and Central Europe. This diffusion could be identified with the migration of first anatomically Modern Humans. The Early Upper Palaeolithic in Europe — dated to the second half of the Interpleniglacial — was, at least partially, based on these “transitional” industries and manifested by the appearance of the Aurignacian, contrasted with local cultures such as the Uluzzian in Mediterranean Europe. During whole the Interpleniglacial Europe was separated from Northern Africa dominated by local evolution of Middle Palaeolithic (Middle Stone Age) cultures (mostly expressed by the Aterian), and by specific “transitional” industries on the southern Mediterranean coast (Early Dabbian) and in the Lower Nile basin. The Last Glacial Maximum and the corresponding sea level recession opened new possibilities of contacts between the Maghreb and the Iberian Peninsula in both directions (Aterian-Solutrean and Gravettian-Early Iberomaurusian), which are still difficult to be proved before new chronostratigraphic correlations are made. At the same time we register links between south-eastern Europe and western Anatolia; the real border between Near Eastern and European Mediterranean cultural zones was marked, in the Late Glacial, by the Taurus chain. During the Late Glacial the cultural separation between Europe and Africa was particularly marked. Only in the Aegean basin the first sea navigation facilitated contacts which become widespread as late as in the Early Holocene with neolithization trough maritime contacts.     

L’industrie microlithique du Paléolithique inférieur de Bizat Ruhama, Israël

Bizat Ruhama is a lower Palaeolithic site in the southern coastal plain of Israel. The site was recently dated to ca. 1ma. In terms of lithic industry, Bizat Ruhama is a unique phenomenon amongst the Lower Palaeolithic sites in the Levant. The lithic assemblage of the site is characterized by the production of small (ca. 25mm) tools, flakes and cores. An in-depth technotypological study was made in attempt to reconstruct the production mode of these artifacts. The results presented here reveal a well-developed cognitive production process, which includes selection of special-sized raw material, production of desired blanks and their subsequent shaping into tools. The implications of this study contribute significantly to our understanding of the phenomenon of lower Palaeolithic microlithic industries in Eurasia.     

Stratégies techniques dans le Paléolithique Moyen du sud-est des Pyrénées

In this article, the lithic reduction systems from Middle Paleolithic levels at Roca dels Bous and Tragó are presented. These two sites are located in the South-eastern Pyrenees in Catalunya (Spain) and yield Mousterian levels which are attributed to MIS 3 and MIS 5. At the two studied sites, there is coexistence between expedient knapping systems and more complex techniques such as the Levallois method. Furthermore, cores are heavily exhausted, showing a pattern that cannot be explained by the absence or scarcity of raw material. This technical pattern can be traced across several Mousterian assemblages in the South-eastern Pyrenees, suggesting technocognitive continuity in the Middle Palaeolithic during the Upper Pleistocene, in which changes in lithic reduction patterns are not evident. In this paper, the implications of such observations are contextualized within the general discussion on the behaviour of the South-eastern Pyrenees Neanderthals.     

Le Paléolithique ancien de l’Europe orientale et du Caucase

Currently, only Tréhougol’naya Cave has reliably dated evidence for human settlement in Eastern Europe and Caucasus, from the beginning through the middle of the Middle Pleistocene. In Eastern Europe, assemblages from Khriatchi and Mikhailovskoé, and possibly Darvagchai I, appear to be the only stratified locations that tentatively can be compared (despite problems with these materials) with Tréhougol’naya. In the eastern limits of Central Europe, layer VI in Korolevo I is the only stratified assemblage that may be compared with Tréhougol’naya. All these Lower Paleolithic occupations yielded the Pre-Mousterian small tool industries with some pebble tools, but without Acheulean bifaces and Levallois technique. These data suggest that Eastern Europe lies outside the distribution range of the Acheulean techno-complex demarcated with the “Movius Line”. In the Southern Caucasus, the Dmanissi hominine and lithic records document the fact that the earliest small-brained humans – probably later H. habilis-rudolfensis or earlier H. ergaster-erectus hominids bearing Pre-Oldowan technology – initially left Africa and appeared in Western Asia as early as 1.8 Ma ago. However, in the Southern Caucasus, the available chronological data indicate that the Acheulean complex has a later temporal appearance here compared to the Upper Acheulean or Acheulo-Yabrudian in Western Asia. Two main Upper Acheulean industrial variants currently can be recognized in the Southern Caucasus. The first, called the Kudarian by the author (from the caves of Kudaro I, Kudaro III, and Azyk), is characterized by lithics made from mostly siliceous rocks, rare Acheulean bifaces, and non-Levallois flaking technique. The second variant is characterized by lithics made from volcanic rocks, numerous Acheulean bifaces, and often more laminar or Levallois debitage. It can be suggested that there are independent origins for these Southern Caucasus Upper Acheulean industrial variants. Possible roots of the Acheulean assemblages of Kudarian variant might be in the local earlier Lower Paleolithic small tool assemblages with some pebble tools but without Acheulean bifaces. The other Caucasus variant of the Upper Acheulean appears to be related to the Levantine Upper Acheulean.     

Madonna dell'Arma (San Remo, Italie) : expression locale de la végétation ligure au cours du Paléolithique moyen

Pollen analysis of Madonna dell’Arma cave inside part (Liguria, Italy) allowed us to reconstitute, at local scale, the Ligurian coastal vegetation between the end of the last interglacial period and the beginning of the pleniglacial. This transition period shows an important representation of arboreal cover and a persistence of thermophilous elements that allowed us to considerate the western Liguria as a periglacial refuge. During the end of the last interglacial, xerophytic, halophytic herbs and shrubs taken over from a Mediterranean pre-forest unit in the first slopes constituted the coastal zone. The nearness of Argentina torrent and the Armea influenced, in the coast, the existence of marshy zones colonized by hygrophilous trees. In the Ligurian lowlands spread out sclerophyllous and mesophilous forests according to altitude. The beginning of the pleniglacial is indicated in the sequence by increases of Pinus, Cupressaceae and Artemisia in the context of a decline in the thermophilous components. This picture of vegetation has become integrated into the multidisciplinary studies of the site and contributed to the elaboration of palaeoclimatic hypothesis similar as those revealed by the fauna.     

Environnement et archéologie durant le Paléolithique final dans la région du Rhin moyen (Rhénanie, Allemagne) : conclusions des 15 dernières années de recherches

The Laacher See volcano erupted at 10,966 cal BC covered the whole Central Rhineland with huge tephra layers which are exploited now for some 150 years. During the last 15 years of research several new find locations exhibiting tree trunks of the hemi-boreal woodland, leaf imprints and animal tracks preserved in pumice and ashes reveal detailed insights into the (younger) Allerød environment. Five final Paleolithic (Federmessergruppen) habitation sites without any evident settlement structures but providing exogenous raw materials from outcrops in distances up to 170 km demonstrate the highly mobile mode of life of these hunter-gatherers groups some 13,000 years ago.     

Le site Épigravettien de l'Abri Dalmeri : aspects artistiques à la fin du Paléolithique supérieur en Italie du nord

Over the past fifteen years of research in the alpine area, the Dalmeri Rockshelter, located on the northeastern edge of the Sette Comuni Plateau (Trento, Italy), has become a key site for reconstructing the exploitation of the mountain territories by the human groups of the end of the Upper Palaeolithic. Excavations, carried out between 1991 and 2005, brought to light a sequence of Recent Epigravettian anthropic levels, which were radiocarbon dated to the Allerød interstadial. The well-preserved paleosurfaces provided the opportunity to carry out a thorough analysis on the faunal and lithic remains, enabling us to reconstruct the palaeoeconomy, the function and the internal organisation of the site. In the past five years, the discovery of a notable quantity of red ochre painted stones, which are linked to the earliest settlement phase, revealed different representations, both naturalistic paintings as well as signs. Following this discovery, the interpretation of the site began to touch the artistic-religious sphere, providing new insights into Epigravettian art.