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”.     

« Terre des cités fortifiées ». Sites de la civilisation des steppes de l’époque du Bronze moyen en Oural du Sud

The “Earth of fortified settlement” is one of the last big discoveries of the end of the xx^th century. Situated on the oriental slopes of the mounts of Ural, fortified settlement, date the Middle Bronze Age. These strengthened structures are particular in the archaeology of steppes. They were built according to geometrical plans, Cities in oval being the most ancient, the rectangular cities being the most recent. The most remarkable are together of strengthened structures appropriate for the culture of Sintachta-Arkaïm. This city distinguishes itself from the others by the unique integrity of the works of fortification and by the graves which are connected to these last ones. Situated on a prominence, Arkaim consists of two defensive walls, maybe of a third, the rampart and the ditch. The space between the defensive walls was occupied by the houses of trapezoidal shape and directed as beams to the center of the city. The center of the city, the rectangular shape, was not built and formed a place where foyers were found. Complex entrances were at the four corner of the city. The excavations of fortified settlement and graves allowed to have an idea on the level of development of the everyday life at the time of the Middle Bronze Age in transuralian plains.     

The archaeological results of Prehistoric societies obtained in the Archaeological Map of North Morocco Project

This paper presents the results of the “Archaeological Map in Northern Morocco” project, which has been carried out by researchers from the University of Cadiz, University of Abdelmalek Essaadi and INSAP of Rabat. Four seasons of archaeological survey have taken place in the Tetouan region as well as excavations in the Cave El Hafa and the rock-shelter of Marsa. This study includes geomorphological data and a petrographic study to pinpoint of the origins of raw material used by the different human groups that duelled in the area. Lastly, this paper presents settlement patterns of the studied groups, most importantly, this is an updated study of the relevant occupations that correspond to Palaeolithic hunter-gatherer societies, Neolithic tribal societies and also, of human settlements associated to Recent Prehistory stages.     

Métastase rénale d’un carcinome vésiculaire de la thyroïde révélée par le balayage du corps entier à l’iode 131

Distant metastasis of differentiated thyroid carcinoma generally affect lung and/or bone tissue. Renal metastasis from thyroid carcinoma is extremely rare. We report a case of renal metastasis from a follicular thyroid carcinoma in a 55-year-old man, occuring 11 years after total thyroidectomy, fortuitously discovered on a whole body scan carried out after 131-iodine therapy for neck recurrence of disease. Salient features of our clinical case are the fortuitous mode of discovery the unilateral localization of metastases and especially the long time interval which separates its detection from that of the primitive tumour. This case report exemplifies the useful role of the whole body scan carried out after 131-iodine therapy better adapted to reveal often undetectable occult metastases with low dose, but also to ensure a regular and protracted follow-up of patients treated for differentiated thyroid carcinoma.     

Calcium as an extracellular signalling molecule: perspectives on the Calcium Sensing Receptor in the brain

Calcium acts as a universal signal that is responsible for controlling a spectrum of cellular processes ranging from fertilization to apoptosis. For a long time, calcium was regarded solely as an intracellular second messenger. However, the discovery that calcium can also act as an external ligand together with the molecular cloning of its cell surface receptor, the Calcium Sensing Receptor (CaSR), demonstrated that calcium also acts as an important extracellular or first messenger. Here, we give an overview of the main structural, pharmacological and physiological features of the CaSR and provide an assessment of its functions and cellular and molecular mechanisms of action. In addition, we propose possible avenues for future research into the trafficking of CaSR and the role(s) of this receptor in the central nervous system.     

Palynofacies Analysis of Inner Continental Shelf and Middle Slope Sediments offshore Egypt, South-eastern Mediterranean

Marine palynological studies of Quaternary sediments usually focus on dinoflagellate and pollen assemblages for paleoceanographic and paleohydrographic interpretations of past events. This paper focuses on the use of palynofacies analysis for paleohydrological reconstructions of deltaic and deep sea environments to evaluate transport of organic matter to the ocean. These palynodebris data are used to interpret palaeoenvironmental and paleohydrographic changes in two marine cores from the continental shelf (core-1, 27 m water depth) and middle slope (core-2, 1030 m) offshore Egypt, south-eastern Mediterranean Sea, during the latest Pleistocene and the Holocene. The relative abundances of various types of sedimentary organic matter such as phytoclasts, zooclasts, amorphous organic matter and palynomorphs are related to paleohydrographic changes of the overlying water column. Based on the total palynodebris and organic carbon content, sediments of the inner continental shelf core are characteristic of a prodelta environment proximal to a fluvio-deltaic source and moderately distal oxic environments with enhanced structured organic matter preservation potential. In contrast, the palynodebris of the middle slope core show that the basal sediments (105-140 cm depth) indicate suboxic to dysoxic bottom water conditions, followed by anoxic-suboxic bottom water conditions for the interval from 30-85 cm, which represents the S1 Sapropel. The top sediments of core-2 (0-25 cm) were deposited under oxic bottom water conditions, suggesting good ventilation in the water column. A quantitative approach was also used for interpreting the Holocene sea-level changes, based on the correlation between phytoclast and organic matter abundances. Sedimentation rate in the continental shelf is varied, being relatively very low (6.7 cm/kyr) in the basal part and increased upward to be 20 cm/kyr (depth 115-120 cm). In the upper Gray clayey silt layer the sedimentation rate was high (about 40-45 cm/kyr) due to the high discharge from El Manzala Lagoon and Damietta Nile branch. In the middle slope depth the sedimentation rate was relatively low and uniform, around 14 cm/kyr.     

Les anthropomorphes du mont Bego aux pieds tournés vers l'intérieur : une hypothèse

Three major figures from the Vallée des Merveilles have the feet turned inward. The extreme rarity of this posture in the plastic arts of all times and the fact it is attributed essentially to major figures indicate the particular significance of this stand for the authors of the engravings. de Lumley et al. (1995, 2003) interpret this feet position as a hieratic attitude, as the mark the figure belongs to the world of the gods. In this study another hypothesis, which doesn't necessarily exclude the first one, is proposed from an ethological point of view based on the reading of body language made by Wex (1993). She claims that the inward turning of the feet represents a protective reaction to a situation which put the person in a fragile or harmful position. This hypothesis, as well other characteristics, questions the divine or human nature of our three anthropomorphic figures. The shamanistic approach (Hedges, 1993; Whitley, 2001) is raised with respect to this issue and the inward feet position.     

Composition des faunes de mammifères quaternaires en Chine selon un gradient Nord-Sud

During Pleistocene Epoch, quite a number of meridionale mammals inhabited north China, such as Stegodon, Macaca, Hystrix, Dicerorhinus, Bubalus and several kinds of other probscideans. On the contrary, some boreal mammals once appeared in south China, such as Megaloceros and Ursus arctos etc. The frequent appearance of warm-adapted mammals in North China can be explained by two alternative assumptions: one is that those mammals were of palearctic origin; the other is the climate-driven northward dispersal. According to the fossil evidences, it seems that the northward dispersal events were much more frequent than the southward ones during Pleistocene in China. It maybe means that during Pleistocene, the temperature fluctuated very frequently and the boundary between the Paleartic and Oriental Regions were always keeping on shifting. But it's still not clear how many episodes or phases of such dispersal events had occurred. The Qinling Mountains weren't responsible for the faunal differentiation between the North and the South, neither was the Yangtze River; because the former is not big enough, and the latter cannot be regarded as an efficient barrier for those animals, which are capable of flying and swimming. Maybe the climate zonation is the root cause of zoogeographical changes.     

Paedomorphosis in <Emphasis Type="Italic">Ambystoma talpoideum</Emphasis>: effects of initial body size variation and density

Facultative paedomorphosis is the ability of a salamander to either metamorphose into a terrestrial, metamorphic adult or retain a larval morphology to become a sexually mature paedomorphic adult. It has been hypothesized that density and initial body size variation within populations are instrumental in cueing metamorphosis or paedomorphosis in salamanders, yet few studies have adequately tested these hypotheses in long-term experiments. Beginning in the spring of 2004, 36 experimental ponds were used to manipulate three body size variation levels (low, medium, high) and two density levels (low, high) of Ambystoma talpoideum larvae. Larvae were individually marked using visible implant elastomers and collected every 2 weeks in order to measure snout–vent length and mass. Bi-nightly sampling was used to collect new metamorphs as they appeared. Analysis revealed significant effects of density, size variation and morph on body size of individuals during the summer. Individuals that metamorphosed during the fall and following spring were significantly larger as larvae than those becoming paedomorphic across all treatments. These results support the Best-of-a-Bad-Lot hypothesis, which proposes that the largest larvae metamorphose in order to escape unfavorable aquatic habitats. Large larvae may metamorphose to leave aquatic habitats, regardless of treatment, due to the colder climate and lower productivity found in Kentucky, which is in the northern-most part of A. talpoideum’s range. By maintaining a long-term experiment, we have provided evidence for the transition of both larvae and paedomorphs into metamorphs during fall and spring metamorphosis events. Furthermore, the production of similar morphs under different environmental conditions observed in this research suggests that the ecological mechanisms maintaining polyphenisms may be more diverse that first suspected. Electronic supplementary material The online version of this article (doi:) contains supplementary material, which is available to authorized users.     

Le Middle Stone Age de la grotte du Porc-Épic (Dire Dawa, Éthiopie) : gestion des matières premières et comportements techniques

With the emergence of Modern Humans in Africa a new post-Acheulean culture seems to take form: the Middle Stone Age. Although the geo-chronological limits of this period remain unclear, it may however be characterised by behavioural modifications, in particular an important change in the relationship between humans and their environment. Theses changes may partially result from the diversification of stone-tool production techniques, as well as socio-economical conditions. Sites dating of this period show that flake types are more abundant and result from exploitation methods that become gradually more sophisticated from about 300ka.In this context, study of the lithic assemblage from Porc-Epic Cave in Ethiopia contributes to the knowledge about operative methods used during the Middle Stone Age. The combined production of flakes, blades, bladelets and points using various methods, a differential economy towards raw materials and the diversity of tool types produced, underline the large extent of technological variability that the Porc-Epic tool-makers were capable of. We may conclude that, in spite of certain differences concerning raw material acquisition, a chronological homogeneity exists in the production modes and their variability. This apparent homogeneity throughout the stratigraphical sequence underlines the difficulty of attributing a cultural characteristic to stone assemblages of this period.