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.     

La Lloseta : une grotte importante et presque méconnue dans l'ensemble de Ardines, Ribadesella

This summary on The Lloseta shows us a much richer reality that it had been presented through the precedent publications. To begin it is presented as an shelter environment decorated in all their extension whose decoration and parallel they find real sense if we put them in connection with the neigh boring Tito Bustillo. It possesses a prevalence of signs and old representations, a bad general conservation and an own and original internal organization. None of the caves of Ardines, including their main protagonist, she makes isolated significant sense, but rather they are and were supplemented in the past, for activities, occupation and use. We try to know the meaning of all and each one of the caves in connection with the other ones, because we think that their function should be collective and complementary.     

Témoins du froid. La faune dans l’art rupestre paléolithique de l’intérieur péninsulaire

It is our intention to analyse the environmental significance of the Palaeolithic artistic representations existing in the inner areas of the Iberian Peninsula. The fauna is used to create chronological and climatical criteria to affirm the condition of the castillan plateau during the last glaciation. In our opinion, it is dangerous to use the isolated animals in order to talk about coldness or heat situation because they reflect the cultural selection of their authors more than the ambiental reality. Neither the animals called thermometer nor the euritherm ones are solely represented in the tempered moments. Moreover, we have almost a no animal representation than artistic during the last finiglacial period in the peninsular interior. It means probably that the artistic representations are mainly cultural signs, which change for cultural reasons and not properly climatic ones within a general reality of glacial environment.     

Zaozer'e, un nouveau site du Paléolithique supérieur ancien dans le nord-est de l'Europe. Rapport préliminaire

This paper presents preliminary archaeological and chronostratigraphical data obtained during pilot excavations of one of the northernmost European Early Upper Palaeolithic sites, Zaozer'e, situated on the western slope of the Middle Urals.     

The death pathways in mussel larval cells after a freeze-thaw cycle

We analyzed cell viability, caspase activity, plasma membrane alterations and cell ultrastructure morphology to estimate the morphological and biochemical alterations that occur in bivalve molluscan cell cultures during cryopreservation. The use of 5% dymethyl sulfoxide as a cryoprotectant resulted in greater cell survival and a scarcity of destroyed cells lacking cytosol among dead cells. In this case, almost all cells died through necrosis or apoptosis, which appeared to increase in mussel cell cultures after a freeze-thaw cycle. Apoptosis was not a main death pathway in mussel cells, but it was induced in a significant part of these cells (up to 24%) immediately after thawing and depended mostly on the cryoprotectant used. Regardless of the type of the used cryoprotectant, we observed some nuclear aberrations in cells after freezing-thawing, such as few multipolar mitoses or the absence of a division spindle in mitotic cells. After analyzing different methods for assessing cell damage, the best results were obtained from optimal approaches that could provide information regarding the cell disruption level after freezing-thawing and could be considered for future studies.     

Neanderthals and volcanic rocks. Opportunistic behaviour or optimized management?

The use of volcanic rocks by Neanderthals is frequently considered to be opportunistic, especially when good-quality stones were rare in the site neighbourhood. An analysis of the lithic series made of volcanic rocks discovered in the Middle Palaeolithic sites of Payre and Sainte-Anne I, located in the south part and at the southeastern margin of the Massif Central of France and dated back to MIS 7 up until the end of MIS 5, illustrates the capacity of Neanderthals to manage these raw materials and enables us to compare the strategies used in two different mineral environments. Shaping and flaking reduction sequences coexist in both sites in varying proportions, depending on the available rocks in the surroundings. At Payre, artefacts made of volcanic rocks are rarer in surroundings rich in flint while at Sainte-Anne I, the different series comprise a large quantity of artefacts made of different basalts and trachy-phonolites in an environment relatively poor in flint. Most of the reduction processes took place in situ. Activities outside the sites only appear to have concerned the shaping of some heavy-duty tools and some large flakes. It is likely that volcanic rocks were considered by Neanderthals as a geo-resource, either major or lesser in importance, to provide large flakes and both heavy-duty and light-duty tools, besides flint quartz and other rocks.     

Identification des impacts de projectiles sur le squelette des grands ongulés

In the context of the collective research program “functional technology of solutrean points”, conducted from 1987 to 2000, more than 300 impacts were experimentally produced on ungulate carcasses (goat, cow, horse). Based on the classification of these types of impacts proposed by P. Morel in 1991, we can estimate that only the inclusions of point fragments in the bones remain diagnostic in most archaeological contexts. The other types, such as scrapings or splittings, can be confused with tool traces, carnivore tooth marks or postdepositional alterations. P. Morel has published the results for small herbivores, and we present our results here for large herbivores. More than 200 stigmata were observed on the carcasses of an adult cow and horse following experimental shots with solutrean projectiles (shouldered points, laurel leaf points and willow leaf points) and a few reindeer antler points. These traces are concentrated around the vital parts of the animals. The most common types are marginal scrapings and splittings, but implantations are more numerous than on small ungulate skeletons. This numerically significant body of data is derived from carefully controlled experiments. Indispensable for the interpretation of the stigmata observed on bones found in Paleolithic sites, such experiments contribute to our knowledge of the conditions prey exploitation and allow us to address questions concerning the fossilization of these traces and their apparent frequency.     

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.     

The evolution of the evolvability properties of the yeast prion [PSI+

Abstract.— Saccharomyces cerevisiae's ability to form the prion [PSI⁺] may increase the rate of evolvability, defined as the rate of appearance of heritable and potentially adaptive phenotypic variants. The increase in evolvability occurs when the appearance of the prion causes read-through translation and reveals hidden variation in untranslated regions. Eventually the portion of the phenotypic variation that is adaptive loses its dependence on the revealing mechanism. The mechanism is reversible, so the restoration of normal translation termination conceals the revealed deleterious variation, leaving the yeast without a permanent handicap. Given that the ability to form [PSI⁺] is known to be fixed and conserved in yeast, we construct a mathematical model to calculate whether this ability is more likely to have become fixed due to chance alone or due to its evolvability characteristics. We find that evolvability is a more likely explanation, as long as environmental change makes partial read-through of stop codons adaptive at a frequency of at least once every million years.     

Figurines du Paléolithique supérieur en matière minérale plastique cuite d’Afalou Bou Rhummel (Babors, Algérie). Premières analyses par spectroscopie d’absorption Infrarouge

From 1983 to 1993, S. Hachi’s last excavations at the Afalou Bou Rhummel (Algeria) Babors coastal shelter have contextually produced numerous anthropological and zoological, clay figurines, all hand made and cooked, among Iberomaurusian Late Upper Palaeolithic remains. Regarding Maghrebian territories (Morocco, Algeria, Tunisia and Libya), these so peculiar documents are strictly related to 15?000-11?000 BP levels, although deeper archaeological levels are 18?000 BP. Twenty eight small samples (less 1mg) were analysed through infrared absorption spectroscopy (IR) so as to precise, through typical transformation of the major mineral involved: kaolinite, smectites, and amorphous silicates, the final degree of temperature reached after cooking. These documents were all intentionally cooked between 500 and 800 °C. Local clay was obviously picked up for figurine elaboration.