Les occupations gravettiennes de Buran-Kaya III (Crimée) : contexte archéologique

Buran-Kaya III (Crimea, Ukraine) is a unique site, with a stratigraphy from Middle to Final Palaeolithic. The Gravettian layers 5-2, 6-1 and 6-2 of this site yielded numerous lithic and bone industries, ornaments from marine and freshwater shells, mammal teeth and mammoth ivory, human fossils and abundant faunal remains. Аccording to the stylistic indications of the lithic and bone inventories, the settlements of layers 5-2, 6-1 and 6-2 of Buran-Kaya III represent local variants of the Gravettian in Crimea and in mainland Ukraine and, therefore, the existence of separately social communities. Conversely, ornament objects and human remains (with specific mortuary practices) of Buran-Kaya III may suggest extensive social contacts of its Gravettian inhabitants with other human populations from mainland Ukraine. These hypotheses make necessary future investigations about the social organisation of the Epigravettian societies in Eastern Europe.     

Analyse préliminaire des ensembles lithiques de Hakemi Use, site du Néolithique final dans le sud-est de la Turquie

Hakemi Use is a mound in southeastern Anatolia where rescue excavations have recently brought to light cultural remains dated to the late Neolithic from the Hassuna and Samarra periods. The lithic assemblages from this site were produced from flint and obsidian. Although flint is available locally, obsidian was imported but its sources are as yet unknown. Retouched elements are generally rare among the lithic assemblage. Most of the blades and bladelets are represented by the mesial parts of the blanks, and were obtained by unidirectional flaking. Debitage products such as core tablets and crested blades are rare. The study of the groundstone objects is still ongoing. Thus, this paper reports the results of the analysis of the knapped stone products recovered during the first and the second excavation campaigns at Hakemi Use.     

Réexamen du contexte géologique,chrono- et biostratigraphique du site de Moulin Quignon à Abbeville (Vallée de la Somme,France)

The geological context of the discoveries made by Boucher de Perthes at Moulin Quignon in 1863–1864 was examined through the testimonies left by himself, by his detractors, then by geologists and archaeologists who later worked on the alluvial deposits of the Somme at Abbeville. This critical approach has been completed by specific studies, through a restricted excavation performed at Carpentier Quarrya locality known since the end of the 19th century as a sequence analogous to Moulin Quignon, and by a series of new analyses (microvertebrate, malacofauna, dating). The main results of these studies confirm the fluvial nature of the ‘archaeological’ layers at Moulin Quignon that correspond to a high terrace of the Somme River, about 40 m above the current valley incision at Abbeville. Dating results provide an age of 584 ± 48 ka for the fluvial levels at Carpentier Quarry, in good agreement with the available biostratigraphic data, inferred from malacofaunas collected at both Moulin Quignon (Boucher de Perthes collection) and Carpentier Quarry, and from mammals fauna recovered since the end of the 19th century from the white marl at Carpentier Quarry which allow the allocation of these alluvial deposits to an interglacial stage of the second half of the Cromerian, the marine isotopic stage (MIS) 15. From these data and taking into account the identification of the human remains of Moulin Quignon as an anatomically modern man, the contemporaneity of these remains with the alluvial deposits of a high terrace of the Somme River is virtually impossible and supports the hypothesis of a hoax. Besides, it is possible that at least some of the lithic material collected at the time of the discovery by Boucher de Perthes could derive from fluvial levels dated of approximately 600,000 years. They would be then the oldest evidence of a human presence in the Somme Valley.     

Considérations sur l’extension géographique du Néolithique final à « livre de beurre » en Touraine et Poitou (France)

The “livre de beurre” blades debitage is classically attached to Grand-Pressigny country (Indre-et-Loire). This question is reconsidered by the autors to ligth on their knowledge of the sites and raw materials in a broadest geographic expanse: the South of Touraine and Poitou. Cultural attribution of this practice is also reconsidered and replaced in largest context.     

Une lame de faucille sous la stèle gravée Chalcolithique dite du « Chef de tribu », Vallée des Merveilles, région du Mont Bego, Tende, Alpes-Maritimes

The carved stele known as the “head of the tribe”, attributed to the Chalcolithic, erected at an altitude of 2290 m in the chaos of blocks in the Merveilles torrent in the Mont Bego region at Tende, was removed from its original standing place. Earth extracted from under the stele and sieved yielded a sickle blade in very fine and homogeneous Bedoulian pale biege translucid flint, pressure flaked on a heated core. The blade bears a light polish caused by cereal harvesting. This sickle blade is similar to those widely used in the southern Chassey culture (4300 to 3000 years before our era) but also sometimes in the Campaniform culture, during the ancient and middle Bronze age, like in Murée cave, in the Verdon gorges. The location of the sickle blade at the foot of the carved stele, known as the “head of the tribe”, is not just coincidental. It is highly probable that the blade was intentionally placed beside this rock. It is seemingly during a ritual ceremony that this sickle blade, probably still inserted in a wooden handle, was intentionally placed, in a propitious gesture or as an offering, beside the stele known as the “head of the tribe”.     

La chronologie du Néolithique ancien cardial du nord-est de la péninsule Ibérique. Datations, problématique et méthodologie

In this work, we make a compilation of all radiocarbonical data existing for the cardial Neolithic culture in the northwest of the Iberian Peninsula with the aim to delimit as much as possible the chronological range attributed for this period. For this reason calibration of all data is presented on the same curve, taking into account the critical process for all of them based on stratigraphical, taphonomical and radiometrical concepts. Finally, is shown that chronological range of cardial Neolithic culture could be focused on the 2nd half of the VI millennium cal. BC.     

J. Deprat,l’Eubée,la Corse et la Sardaigne. À propos de l’article de C. Guernet « J. Deprat,l’Eubée (Grèce) et les fossiles introuvables »

In a recent publication, C. Guernet picks up again the accusations of fraud against J. Deprat, who, in the early 20th century, had suffered such attacks to the point to be removed from the Geological Society of France. At the end of the same century, one among us (M D.D.) reexamined this affair, and drew the conclusion that J. Deprat was innocent, after which the Geological Society of France reinstated him posthumously. The new accusations issued by Guernet are about Deprat's work in Euboea, as well as Corsica and Sardinia. Our own work rather disagrees and shows that, here again, Deprat is innocent. At this occasion, we present or remind new elements about those regions’ geology.     

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.     

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.