Les néandertaliens de la Caverna delle Fate (Finale Ligure,Italie). II – Les dents

The neandertalian remains discovered in the Caverna delle Fate, Finale Ligure (Italy) gave up a majority of dental material: 10 isolated teeth and six teeth upon arcade or included in the adult mandible Fate 3 and in the child mandible 8–10 years old, Fate 2. Until now, this assemblage is the most numerous of neandertalian teeth excavated in Italy, with archeostratigraphic and paleoenvironmental accurate context. No decidual tooth, lost naturally, has been recognized. The dental material is well preserved, not much altered by wear. The morphometric data confirm the possibility of presence of a gracile neandertalian population living along the mediterranean septentrional European shore. These populations were present since the MIS 5.1, between 80,000 and 70,000 years. This gracility can be explained by the geographic impact and not by the evolutive stage.     

Le site des Vachons : étude de la partie gravettienne de la collection de l’IPH

This article firstly summarizes the process of study of an old collection, which had not been considered since the excavations at the site Les Vachons, started before 1914 and completed around 1939. The studied collection of J. Coiffard, both excavator and inventor of this site, includes four-fifths of the artefacts because, in 1940, he donated approximately one fifth to the Eyzies Museum. For his part, J. Bouyssonie who participated in the excavations for 3 years gave the major part of his own collection to the Archaeological Society of Charentes Angouleme where its condition makes it difficult to analyze. Despite these restrictions, based on statistical comparisons with counts many other sites, I came to the conclusion that the top three layers of Les Vachons are a confirmation of the Gravettian model, developed by B. Bosselin and F. Djindjian through their factor analysis. This model seems much better suited to the stratigraphy of Les Vachons, than all assumptions made by previous analysts in their attempt to bring the industries from the three layers in what remains from the Peyrony model.     

Les cultures moustériennes en Ligurie italienne : analyse du matériel lithique de trois sites en grotte

Multidisciplinary studies realized these last years about cave sites of Madonna dell’Arma, Arma delle Manie and Santa Lucia superiore, in italian Liguria, have stated precisely the conditions of neandertalian frequentations of those sites, placing at intervals, according to the cases, from isotopic stage five to the beginning of stage three. The mousterian industries recovered in those sites, associated with a lot of faunal remains, are here analyzed about the different stratigraphic levels in each site. In Madonna dell’Arma and Arma delle Manie, those industries show a certain constancy in the different levels, about technological and typological point of view or about raw material management. In Santa Lucia superiore, on the contrary, two different types of occupation have let lithical vestiges with different facies in lower levels and above levels. For the three sites, the analysis of the raw material management shows an essentially local supplying, but also some origins much more far like in the case of the jasper. This carrying of distant stones reveals us one aspect of the mobility or at least the territories extension that were able to apprehend those neandertalian human groups in Liguria region and beyond also. Otherwise, some preferential choices for certain raw materials were done by knappers for the débitage or for the small retouched tool supports. The flaking technics are identified in each site and certain regularities have been stated, like the high frequency of Levallois flaking in the different levels (also external levels) of Madonna dell’Arma site that is not the case in the two other sites.     

L’industrie lithique du site Pléistocène inférieur de Pirro Nord (Apricena, Italie du sud) : une occupation humaine entre 1,3 et 1,7 Ma

The site of Pirro Nord (also known as Cava Pirro or Cava Dell’Erba) is known in literature since the 1970's of the last century as a palaeontological site, of which the mammalian fossil association constitutes a reference (local) fauna for the European latest Villafranchian. This fossil association is also known for the occurrence of some African elements. During the 2005, a lithic industry has been found in three karst fissures, together with the typical elements of the Pirro Nord vertebrate assemblage. The biochronological assessment based on the vertebrate assemblage attributes it to a time interval bracketed between 1.3 Ma and 1.7 Ma. Thus the site of Pirro Nord represents the oldest human occupation of Europe so far known. The lithic assemblage, attributable to the Mode 1, is constituted by three cores and seven flakes, and is made only on flint. Lithic artefacts have been found in stratigraphic context during the preliminary surveys of the three fissures, that they will be the object of systematic excavations in the years to come.     

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.     

First Partial Skeleton of a 1.34-Million-Year-Old Paranthropus boisei from Bed II,Olduvai Gorge,Tanzania

Recent excavations in Level 4 at BK (Bed II, Olduvai Gorge, Tanzania) have yielded nine hominin teeth, a distal humerus fragment, a proximal radius with much of its shaft, a femur shaft, and a tibia shaft fragment (cataloged collectively as OH 80). Those elements identified more specifically than to simply Hominidae gen. et sp. indet are attributed to Paranthropus boisei. Before this study, incontrovertible P. boisei partial skeletons, for which postcranial remains occurred in association with taxonomically diagnostic craniodental remains, were unknown. Thus, OH 80 stands as the first unambiguous, dentally associated Paranthropus partial skeleton from East Africa. The morphology and size of its constituent parts suggest that the fossils derived from an extremely robust individual who, at 1.338±0.024 Ma (1 sigma), represents one of the most recent occurrences of Paranthropus before its extinction in East Africa.     

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.     

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.     

Dimension anthropique de l'éruption du Mont Pinatubo, Philippines, entre 800 et 500 ans BP

Before its worldwide famous awakening in 1991, Mt Pinatubo volcano erupted between 800 and 500 year BP. The impacts of this little known eruption are progressively coming to light with the discovery of archaeological sites and the study of oral and geographical records. Recent archaeological excavations have shown that pyroclastic flows and lahar onslaughts have probably led to the abandonment of major settlements on both sides of Mt. Pinatubo. The location of these archaeological sites and the toponyms on the east flanks of the volcano suggest a general redistribution of the population downstream toward lands reclaimed on the sea due to heavy lahar material deposition. These population movements did not occur on the west side of the mountain despite similar land reclamation. Such topographic and socio-demographic changes have deeply disturbed the economic environment since it is hypothesized that extensive trade with China and other foreign “countries” profited from the easy penetration of commercial vessels into the bays that would have been filled up by lahar deposits. Finally oral memory records, such as legends and epics, help define the ethnic groups that have suffered from the eruption (e.g. Aetas, Kapampangans and Sambals). Understanding what happened 500 years ago turns very useful to anticipate the consequences of future events.     

Le « nucléus Donggutuo » et sa signification dans l’industrie du paléolithique inférieur de Donggutuo, bassin de Nihewan, Chine du Nord

As one of the most important Lower Pleistocene sites of the Nihewan basin in North China, Donggutuo (DGT) site is well known for its fine retouched small tools and characters of flake industry. However, new excavations still reveal some new discoveries and educe some new issues to us. For example, the “DGT core” introduced in this article is a new discovered typotechnology and indicates new economic strategy of the local people, which was never known before in this area at the time of 1.1 Ma B.P. The paper provides general background and statistic analysis of DGT industry including special method applied to the “DGT core” and discusses possible influence of environmental change for the emerging of the “DGT core”. The “DGT core” shows a germinated microlithic tradition and reflects a cultural diversity of early humans in the Lower Paleolithic in North China.     

Les derniers Homo heidelbergensis et leurs descendants les néandertaliens : datation des sites d’Orgnac 3, du Lazaret et de Zafarraya

This article presents the dating results recently obtained on three archaeological sites in Europe. At Orgnac 3 (Ardèche, France) from where the last Homo heidelbergensis fossils are associated with the first evidence of levallois technique, two speleothem formations from the 5b–6–7^th layers were U-Th dated with MC-ICPMS, giving an age range of 319–255 ka (2σ) (MIS 8–9), while the volcanic ash-bearing second layer was dated by ⁴⁰Ar/³⁹Ar, obtaining a preliminary date of 308.2 ± 6.8 ka (2σ). The combined ESR/U-Th dating of red deer enamel teeth from Lazaret cave (Alpes-Maritimes, France) attributed ages of 120–190 ka to the Acheulean and pre-Mousterian layers (MIS 6), which is in agreement with previous TIMS U-Th dates between 108 and 44 ka on calcite samples from the overlying TRA trench (MIS 5, 4, 3). At Zafarraya (Andalousie, Espagne), a number of ¹⁴C measurements on charcoal samples as well as combined ESR/U-Th dates on Capra and Equus dental enamels assigned the Mousterian artefacts and neandertalian fossils-bearing deposits an age interval between 42 and 34 ka (MIS 3).     

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.     

Les industries acheuléennes de la France septentrionale

The excavations of several open air sites in Northern France and, especially in the Somme basin, have given numerous data concerning the age and the environment of the human occupations for the period from MIS 12 to MIS 8. The quality of the raw material and the function of the different sites have a great effect on the composition of the lithic assemblages as it has been seen for the different sites located near the confluence of the Somme and Avre (Cagny-la Garenne, Cagny-l’Épinette, Ferme de l’Épinette, Gentelles). The characteristics of the lithic industries of Gouzeaucourt show the complexity of the transition from Lower to Middle Palaeolithic.     

La Grotte des Félins, site paléolithique du Pléistocène supérieur à Dar Bouazza (Maroc)

In the continental sediments filling a cave that developed in Middle Pleistocene deposits near Casablanca, Morocco, a very rich mammal fauna from the last climatic cycle was discovered. It was associated with a Middle Palaeolithic poor and atypical lithic assemblage manufactured on blocks and pebbles. The lower fossiliferous layer contained abundant carbonized remains of felids. Unfortunately, the site was destroyed by quarrying before adequate excavations could be carried out.     

Données stratigraphiques, archéologiques et insertion chronologique de la séquence de Longgupo

The site of Longgupo is located north of the subtropical zone and is part of the domain of eastern fauna. The large number of mammal species identified at this site enables clarification of the broad pattern of paleoenvironmental change for the three assemblages from the first stratigraphic sequence (Huang W.-B. excavations). The different species have been classified in four biogeographic groups: subtropical (moderate monsoon), tropical forest (hot and humid climate), montane (cold climate) and prairie (cold and dry climate). Variation in the representation rate of each of these groups enables general reconstruction of the paleoenvironments for the three assemblages identified at Longgupo: a lower assemblage in a hot and humid climate with cold and dry episodes, an intermediate assemblage in a rather cold and dry climate in the lower part, becoming progressively warmer and humid toward the top of the sequence with a monsoon influence more marked than the present day, and an upper assemblage in a rather cold and dry climate. This biochronology and general paleoenvironmental reconstruction are clearly important, but as mentioned above, the stratum by stratum correspondence between the old and new stratigraphic sequences has been quite difficult because the position of material recovered during the early excavations was not recorded.     

La grotte de Santa Ana (Cáceres, Espagne) et l'évolution technologique au Pléistocène dans la Péninsule ibérique

The excavations carried out in the cave of Santa Ana (Cáceres, Spain), cave of the karstic network of the “Calerizo” of Cáceres, enabled us to know the existence, in stratigraphy, of the three lito-techniques modes which characterize the industrial development of lower and middle Pleistocene in the Iberian Peninsula. On standby of new research, the results obtained until now permit us two work out a diachronic assumption of technical evolution. In the Iberian Peninsula, there are only two karstic systems where we can fallow this technological development; one is the “Sierra de Atapuerca” (Burgos) and the other is the “Calerizo de Cáceres” (Cáceres).     

Le plus vieil arc du monde ? Une pièce intéressante en provenance de Mannheim, Allemagne

A Pine-wood (Pinus sylvestris) fragment from Mannheim-Vogelstang (Germany) of early Magdalenian age shows traces of modification that could be related to a bow. Those are for example a smoothing of a face opposite to an unmodified face, the correction of a deviation on one of the lateral sides and a notch that could have served to fix a rope. Nevertheless, some characteristics make this interpretation uncertain. For example, the piece can only represent a fragment of a bow, but the lower end is too damaged to have conserved any traces of breaking or working. A reconstruction of the piece shows that the bow wouldn't have been longer than around 110 cm, which is quite small but documented for several ethnic groups as well as for children's bows. His power reaches 25-30 lbs (British pounds). As for the chronological position of the piece, the oldest direct traces of archery are the 12.680-11.590 calBP old arrows from Stellmoor and the 8000 calBP old bows of Holmegård. The invention of the bow as early as the Upper Palaeolithic has however been postulated for a long time.     

The Iron Gates Mesolithic – a brief review of recent developments

The Iron Gates section of the Lower Danube valley along the border between Romania and Serbia has an unparalleled record of Mesolithic and Early Neolithic settlement spanning the period from ca. 12,700 to 5600 cal BC. Over 50 cave and open-air sites were identified during archaeological surveys in advance of dam construction in the 1960s and 1980s, and follow-up rescue excavations revealed numerous burials and architectural remains and produced rich inventories of faunal material and portable artifacts including artworks and ornaments of bone, shell and stone. Most sites are no longer accessible, submerged beneath the reservoirs created by the Iron Gates I and II dams. Since 1990, new excavations have been conducted at Aria Babi and Vlasac in Serbia, and Schela Cladovei in Romania, while detailed studies of the finds from both new and old excavations have been undertaken by researchers based in Romania, Serbia and the UK fueled by developments in archaeological science. In this paper, we review the main advances in knowledge of the Mesolithic and the transition to farming in the Iron Gates over the past 25 years, and especially the period since 2005. The paper is divided into sections dealing with chronology, mortuary practices, isotopic studies of subsistence and mobility patterns, and the nature and timing of the transition from Mesolithic to Neolithic in the Iron Gates region. The review concludes with a forward look at research in progress.     

Barogali et l’Oued Doure. Deux gisements représentatifs du Paléolithique ancien en République de Djibouti

In the Republic of Djibouti, surveys and excavations, carried out from 1985 to 1992, confirmed the presence of the pre-Acheulean (Oldowan) and Acheulean sites in the country. Three seasons of excavations (1985-1987 in the Gobaad Basin, have unearthed in a hardened compact clay strata of an ancient marshland dating to the Lower Pleistocene, the fossilized skeletal remains of an Elephas recki ileretensis. Numerous stone tools have been gathered with the bones. The E.S.R. dating the elephant’s lower third molar gave a date between 1,.6 and 1,.3 MY that would confirm its paleontological grouping and the membership of this butchery site to the Oldowan period. The animal appeared to have been lying on its left side. The cranial roof had been separated from the calvarium, perhaps to get at the brain; but the skull remains in anatomic connection with the tusks. The jaw (mandible) seems to have been broken to extract the tongue. Hominids, perhaps Homo ergaster, knapped tools from a nearly outcrop of poor quality lava. The tools were specifically adapted to their needs, such as scraping, chopping and scattering the bones. The site has yielded 569 artifacts: utilized material and hammerstones (121); pebble tools (32); cores (14); “debitage” products (366); retouched flakes (36). Artifacts are rarely retouched and often broken. Five different types of choppers have been classified. The polyedrons and one bola make up 22% of the pebble tools. The cores are divided into unipolar, centripetal and polyhedrical types. In another site, Haïdalo, an almost complete skeleton of an Elephas recki recki in anatomical connection and without any sign of predation, has been found at eight kilometers from Barogali. During surveys in the Ali Sabîh region (1990-1992) seven sectors have been discovered and prospected in the Oued Doure Basin. On the surface area and also in situ into some little pits, 345 rhiolitic Acheulean artifacts have been found, near rhyolitic outcrop. These artifacts are generally large. The choppers (18) can be dividended into 2 sets : side choppers (55%) and end choppers (27%), often with a bifacial cutting edge. There is only one polyedron, but we have found eight heavy scrapers. The Acheulean group is important (43 tools). The bifaces are varied and there are also a few cleavers and picks. Cores are numerous (92) and Levallois cores are preponderant (45%). We find also centripetal cores (27%) and so unipolar, bipolar and polyhedral cores. Tools made of flakes (118) are numerous: scrapers are typologically diversified. Some of them have a double utilization. Notch tools, denticulate tools are presents but also end scrapers, burin, borer, back knifes and scantily retouched flakes. The characters of this lithic material, large cores and big flakes, large bifaces of various types, cleavers and retouched flakes, indicates that they are Acheulean products. So, the Doure Site can be placed in the Middle / Upper Acheulean transition.     

Iberomaurusian funerary behaviour: evidence from Grotte des Pigeons, Taforalt, Morocco

Grotte des Pigeons at Taforalt, north-east Morocco, is well known for a large assemblage of Iberomaurusian (Epipalaeolithic) skeletons, possibly representing the earliest and most extensively used prehistoric cemetery in North Africa. New archaeological excavations carried out in 2005 and 2006 revealed further human remains in a largely undisturbed burial area in an alcove at the back of the cave. This discovery provides the first opportunity to report on Iberomaurusian human mortuary activity at this site. Reported here are a closely spaced and inter-cutting series of four burials. These contained the remains of four adults, of which three were buried in a seated or slightly reclining position facing towards the cave entrance and one was buried in a highly flexed position on its left side. The distribution of articulated and disarticulated bones suggested intensive use of the area, with earlier burials disturbed or truncated by subsequent burials, and displaced skeletal elements deliberately or unwittingly incorporated into later depositions. Through this process, parts of a single skeleton were redistributed among several discrete graves and within the surrounding deposit. Some aspects of the Iberomaurusian funerary tradition that are evident from the human remains excavated in the 1950s are absent in the newly excavated adult burials, suggesting a possible elaboration of funerary activity over time.