Retourner à Moulin Quignon

In March 1863, Jacques Boucher de Perthes found in the alluvia of Moulin Quignon (Abbeville, France) a human jaw in association with lithic artifacts and fossil bones of mammals. Quickly challenged, this discovery will appear as a fraud whose prehistorian was the victim. Since that time, the collection and the Moulin Quignon site are synonymous with an archaeological forgery. Forgotten for almost 150 years, these collections became in 2012 a research topic in the context of a program devoted to oldest settlements and Acheulean. The objective was to identify and study the whole 1863–1864 documentation set (human remains, artifacts, sediments, fauna bones, malacological remains, archives, papers, site) to allow further analysis of the whole subject.     

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.     

La séquence de Moulin Quignon est-elle une séquence archéologique ?

The sequence of the Moulin Quignon quarry yielded archaeological findings (faunal remains, artefacts) and some of them are well located in the stratigraphy thanks to Jacques Boucher de Perthes and colleagues. These remains are often used to attest the early age of the site and the human remains. Some bifaces have been found in close relationship to the human remains and, in particular, the mandible found in 1863. Thanks to the handwritten label put on the pieces and their deposit at the National Museum of Natural History (Paris), it is possible to study them again in relation with the sequence. The study concerns the rare faunal remains and the bifaces given, among others, by Boucher de Perthes to the Museum. The paleontological and technological analyses allow us replacing the lithic material among the north-western European data. The material is presented according to the historical context of his discovery.     

Moulin Quignon 1863–1864 : détours inédits et bilan historiographique

The historical file of Moulin Quignon (Abbeville, France), around the human jaw unearthed in this site, is a form of black hole that swallowed a prehistoric archaeological site and Lower Palaeolithic collection. This article, based on a corpus of unpublished archives, illuminates the matter in a different light. It focuses on archaeological and epistemological issues, the roles of the different actors, interaction games and solidarity in a global scientific community previously welded by the recognition in 1859 of the paradigm of high antiquity of Man.     

La redécouverte du site de Moulin Quignon (Somme) et les premiers Acheuléens du Nord-Ouest de l’Europe (650 ka)

New surveys were undertaken in Abbeville in 2016 and 2017 on the site of the Moulin Quignon discovered before 1850 by Boucher de Perthes, relocated thanks to the archival work carried out by MNHN researchers. This research led 150 years later to the rediscovery of this emblematic Paleolithic site. Test pits and extensive excavation have led to the discovery of alluvial levels in situ and a lithic series composed of 254 fragments, 15 cores and 5 bifaces. The cores and flakes attest to in situ debitage on flint nodules according mainly to unipolar and centripetal unifacial technology, except for one core, which indicates a management on several debitage surfaces. The bifaces are diversified morphologically and technically (shaping modes). They attest to a general management of the bifacial volume and geometry of the tool, to the care taken at the tip of the tool and to the regularisation of the often peripheral edges. They resemble those discovered by Boucher de Perthes in 1837–1868 and described in the past as “Abbevillian”. Stratigraphic and ESR age studies on quartz date human occupation between 670 and 650 ka. These artifacts belong to the earliest Acheulean occupation ever dated in the Somme basin and more generally north of the 50th parallel north. The lithic series discovered at Moulin Quignon is indisputable proof of the presence of human occupations dated at more than 650 ka in the Somme valley, a natural pathway to northern sectors, present-day Great Britain. This discovery thus ages (1) the age of the oldest occupation in the North of France (previously 550 ka) and (2) the age of the oldest bifaces for Northwest Europe (100 ka older than the bifaces in Great Britain).     

Les terrasses fluviatiles quaternaires de la Somme à Abbeville : 150 ans de recherches mêlant géologie et archéologie,de Boucher de Perthes à aujourd’hui

Paleolithic localities associated with fossil fluvial formations of the Somme River at Abbeville have played a significant role in the recognition of human antiquity. From the end of the 18th century, the work carried out in particular by the “Société d’émulation d’Abbeville” led to the emergence of studies in the Somme valley on both Quaternary Geology and Prehistory. It was within this scholarly society that Jacques Boucher de Perthes initiated his research on the famous localities of Menchecourt, Hospital and Moulin Quignon in 1837. These observations were quickly confirmed by geologists such as Albert Gaudry, Charles-Joseph Buteux or Joseph Prestwich. It was the latter who introduced the Abbeville deposits into the United-Kingdom scientist community and his observations were used as early as 1859 by Charles Lyell to demonstrate the antiquity of the archaeological remains collected from these localities. However, the controversy surrounding by the discovery of the human jaw of Moulin Quignon (1863–1864), which undermined the credibility of this locality for a long time, led to the decrease of the archaeological researches in the Somme valley, and in particular in Abbeville, but it then resumed quite quickly. However, if the work carried out by Geoffroy d’Ault du Mesnil from 1875 to 1898 had the merit to reaffirm the archaeological importance of the Abbeville deposits and to reveal the complexity of their Quaternary records, the geographical and stratigraphic imprecision resulting from these rare publications, coupled with the gradual abandonment of the various gravel pits whose exploitation he followed, cast a significant discredit on these discoveries and on the stratigraphical observations he made there. The researches carried out then by Victor Commont at Carpentier Quarry between 1904 and 1918 were characterized by the excellence of the stratigraphic and iconographic data he produced for each of the studied sites. However the absence of archaeological discoveries in the fluvial deposits he studied lead the prehistorians who succeeded him increasingly doubted of the veracity of Ault's observations, despite the efforts made by Abbé Henri Breuil to reconcile these with Commont's observations. Between the two world wars, Breuil and Léon Aufrère resumed the study of the Abbeville deposits then still accessible, tried to ensure their preservation, through the purchase and protection of the Carpentier and Léon quarries, a decisive intervention in the archaeological rehabilitation of these deposits. These works were at the origin of the chronostratigraphic studies carried out on these major localities of the ancient European prehistory until today. Over the past ten years, some of these localities have been studied again, thus largely confirming the observations made by the elders (Boucher de Perthes, d’Ault du Mesnil, Commont) and validating the major place of Abbeville in the understanding of ancient prehistory settlement of northwestern Europe.     

L’industrie en calcaire du site Paléolithique d’Isernia la Pineta : un modèle interprétatif de stratégie comportementale

The studies and the researches carried out in the last years on the Palaeolithic site of Isernia La Pineta have brought to consider in new way the activities realized by the human group that lived the basin of Isernia during the Middle Pleistocene offering an important key of interpretation of the behavioural strategies of the prehistoric man. The analysis of the exploitation of the raw material has confirmed the presence on the site of two different lithotypes: flint and limestone; the lithological dichotomy is related to the functional dichotomy of the raw material that seems to have conditioned the activities of the human group in different areas of the site. The necessity to deepen the study on the limestone has derived from the evidence brought to light in the last excavation campaigns of a remarkable concentration of the flaked limestone pebbles and the flake scars in some areas of the explored archeosurfaces, particularly on the 3a and on the overlooking layers. The present study has the purpose to explain the characteristics of the limestone finds both in reference to the raw material and to its state of preservation both to the technotypological evidences and its spatial distribution with the purpose to better understand the modalities of the exploitation of the raw material. The information collected until today have permitted to obtain a precise knowledge of the environmental context and the territorial resources exploited by the human group showing an opportunistic capability to find the most advantageous behavioural solution for the necessities of subsistence.     

Sur un occipital néandertalien des Pradelles (Marillac-le-Franc, Charente) : étude morphométrique préliminaire

In 2001 and 2003, several occipital fragments of a single mature skull were unearthed on the site of les Pradelles (Marillac-le-Franc, Charente). The archaeological context of the deposit allowed us to provisionally assign the remains to the Neandertal taxon. A morphometric study of this piece was conducted in order to confirm its placement in this lineage. Some features observed on this specimen and commonly described among Neandertals (e.g. the presence of a suprainiac fossa) as well as dimensional data locate the les Pradelles occipital within the morphological variability of Neandertals.     

Ndindan : synthèse archéologique d’un site datant de trois millénaires à Yaoundé (Cameroun)

This text is a synthesis of the results from the archaeological study of Ndindan site (Ndedama in Ewondo language) (3°54’N; 11°30’E), located north-west of Yaoundé urban area, on the Mont-Febe eastern side. An overview of the historical of prehistoric research in Yaoundé is given. It then tackles the study of the archaeological materials and supplies the radiocarbon datings of the site. A reconstitution of ancient population and of the paleoeconomy on the regional scale is at last made.     

Le Paléolithique moyen de l'Abric Romaní. Comportements écosociaux des groupes néandertaliens

The Abric Romaní is one of the most important Upper Pleistocene sequence of the Iberian Peninsula, with archaeological levels belonging to the Middle Paleolithic and with one of the earliest Aurignacian samples from Western Europe. Research has been focused on the interpretation of patterns of manage and consume of natural resources and the spatial organization of the activities inside the site, and for that reason, the fieldwork strategy is lead to excavate the whole surface of the site. The results of more than 25 years of research on the Abric Romaní conclude that Neanderthal communities settled in the site forming domestic groups around hearths. Depending on the intensity of occupation, related to the length of occupation and with the number of people of these groups, this spatial domestic structure evolves forming the variability spectrum of settlement impacts in the site. In the same way, the manage of lithic and faunal resources increases its variability following the intensity of occupation, using clears technical patterns of lithic production and for catching and processing faunal preys. This variability from behaviors well established is interpreted like the way for adapting new historical and environmental situations.     

Les assemblages lithiques des niveaux du Paléolithique moyen de l’Abri des Pêcheurs (Ardèche, Sud-Est de la France): Des occupations néandertaliennes récurrentes dans un « fossé »

The Abri des Pêcheurs has yielded an extraordinary sequence with Middle and Upper Palaeolithic levels. Humans came and stayed in a ditch-cave that has been filled in along time. During Middle Palaeolithic occupations, they used first quartz, and this site is the only case in this area. Assemblages show similar technological behaviour along time. Flint is few employed and arrived as flakes from different areas if we consider its geological variety. Functions of the site are not well established. The base of the sequence has yielded sediments with a mixing of ibex, carnivore bones and artefacts. The study of the lithic assemblages brings information on the processing systems used on quartz and flint during occupations which left few evidence and used local stones while flint is available not far from the site. Hypothesis on short and specialized occupations is discussed.     

Contribution à la reconnaissance d’une microproduction au Paléolithique moyen : les industries de la grotte des Ramandils (Port-La Nouvelle, Aude, France)

The Ramandils Cave is a key archeological site situated on the Mediterranean coast. The importance of this site derives not only from its geographical and chronological position, but also from the density of the artefacts left by Neandertal populations who settled there on several occasions as early as isotopic stage 5. This study concerns 29,997 lithic objects from five stratigraphical units. The industries, mainly in flint, are all small sized (< 30 mm). The Ramandils Cave lithic assemblage fits within the variability of Middle Paleolithic sites, however differing by a characteristic size reduction in knapping economy, in matrix and resulting products production. How might we interpret this small size characteristic: as a purely cultural factor or as a result of circumstances? Results show that this micro-production does appear to be predetermined. The characteristics of the lithic assemblage from Ramandils Cave give them a special status in the debate regarding the definition of micro-Mousterian and in the identification of technocomplexes geared towards micro-production.     

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.     

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.     

Un premier jalon gravettien dans les Pyrénées-Orientales : le Jas-d’en-Biel-1

The open air site of Jas-d’en-Biel-1 (Tautavel, Pyrénées-Orientales) is the first trace of Gravettian presence in the extreme east zone of the Northern-Pyrenees Piedmont. The lithic series made up of surface finds indicates that this occupation could belong to a rather recent phase of southern-French Gravettian.     

Un nouveau Bovini dans la faune du Pléistocène supérieur d’Algérie

During the study of the Quaternary Maghrebian bovines in 1985, the review of the Bovini (aurochs and buffalos) found in Upper Pleistocene sites of Algeria showed that in comparison with most of the African bovine assemblage the attribution of genus Pelorovis to the species antiquus was inappropriate. The biometric and cladistic data revealed a close kinship with genus Syncerus. Later, other authors’conclusions confirmed its relevance. The antique buffalo of the Aterian site of the Phacochoeri has all the characteristics of genus Syncerus, but is different in that it shows a certain number of specific characteristics described in this article.     

Le Magdalénien de la grotte « Grappin » à Arlay (Jura, France) : nouveaux regards

The “Grappin” or “Saint-Vincent's” cave, on the western slope of Jura, East of France, has been explored since 1889. From then to 1960, it has yielded substantial material dated to middle “à navettes” Magdalenian developing during the late Pleniglacial. The study of this settlement, although often mentioned, was never dealt with comprehensively until now. Due to its scientific importance for the middle Magdalenian of western Europe, the site is to be reinvestigated through a global interdisciplinary project entitled “The Tardiglacial and the start of Holocene in the Jura and its margins”. This paper will review our present knowledge of the site, radiocarbon dates and archaeological data. It also focuses on ornaments and engraved mobile art.     

La gélifraction des restes fauniques. Expérimentation et transfert au fossile

The fragmentation observed in an archaeological site, which cannot be explained only in terms of anthropological action, we subjected faunal remains (bones and teeth) in alternations of frost/thaw at the center of geomorphology of the CNRS of Caen. At the same time, we arranged osseous and dental fragments in five cells of an artificial site in natural environment in the South Alps (program of multidisciplinary research transfert de référentiels actuels de l’étage nival aux sites paléolithiques [TRANSIT]). At the end of the experiments, we were able to bring to light the characteristics of some gelifracts but their direct comparison with the archaeological osseous fragments, although very promising, is there only for its debuts and requires others similar experiments.