- Prehistoric Archeology, Lithic Technology, Middle Palaeolithic, Experimental Archaeology, Mousterian, Neanderthals (Palaeolithic Archaeology), and 20 morePetrology, Ethnoarchaeology, Archaeological Method & Theory, Human Behavioral Ecology, Archaeology, Petrology and Geochemistry, Geochronology, Paleoecology, Spatio Temporal Analysis, des Traces et des Hommes, Flake Cleavers, Acheulian (Archaeology), Paleoclimate, Experimental Knapping, Anthropology, Technology, Prehistoric Archaeology, Prehistory, Palaeolithic Archaeology, and Paleolithic Europeedit
Fondée sur des approches taphonomique et techno-économique des industries lithiques, cette étude vise à mener une réflexion sur le morcellement territorial perceptible au Paléolithique moyen. Cette géographie culturelle, particulièrement... more
Fondée sur des approches taphonomique et techno-économique des industries lithiques, cette étude vise à mener une réflexion sur le morcellement territorial perceptible au Paléolithique moyen. Cette géographie culturelle, particulièrement identifiable au Stade Isotopique Marin (MIS) 3 pourrait résulter de processus évolutifs déjà en place dès le MIS 5, ou être en discontinuité avec les périodes antérieures. Mon objectif est alors de tenter de retracer les origines de ce phénomène de morcellement territorial. Dans ce but, l'analyse techno-économique des industries de la Gruta da Oliveira (Portugal), rattachées aux MIS 5 à 3 permettra de construire une réflexion sur les liens potentiels entre ces industries, en termes de filiation et de rupture dans un secteur où le peuplement fut continu durant la période analysée. Abstract The aim of my research project is to investigate the process of territorialization during the Middle Palaeolithic based on taphonomic and techno-economic approaches to lithic industries. The cultural geography of the Middle Paleolithic is well apparent by Marine Isotopic Stage (MIS) 3, but it is not clear whether this might be the result of evolutionary processes already in place during MIS 5 or if there is a rupture with the preceding periods. The goal is thus to retrace the origin of this phenomenon and ultimately distinguish between cultural continuity or discontinuity. The analysis of the lithic industries from the Gruta da Oliveira (Portugal), dating between MIS 5 and 3, allow for the consideration of in situ cultural change in a region continuously occupied during the period under study.
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We use stone tool refitting to assess palimpsest formation and stratigraphic integrity in the basal units of the Gruta da Oliveira archeo-stratigraphic sequence, layers 15–27, which TL and U-series dating places in late Marine Isotope... more
We use stone tool refitting to assess palimpsest formation and stratigraphic integrity in the basal units of the Gruta da Oliveira archeo-stratigraphic sequence, layers 15–27, which TL and U-series dating places in late Marine Isotope Stage (MIS) 5 or early MIS 4. As in most karst contexts, the formation of this succession involved multiple and complex phenomena, including subsidence, bioturbation, carnivore activity and runoff as agents of potential post-depositional disturbance. During phases of stabilization, such as represented by layers 15, 21 and 22, the excavated area was inhabited and refits corroborate that post-depositional displacement is negligible. Layers 23–25 and 16–19 correspond to subdivisions that slice thick geological units primarily formed of material derived from the cave’s entrance via slope dynamics. Refit links are consistent with rapid fill-up of the interstitial spaces found in the Karren-like bedrock (for layers 23–25), or left between large boulders after major roof-collapse events (for layers 16–19). Layers 26 (the “Mousterian Cone”) and 27 are a “bottom-of-hourglass” deposit underlying the main sedimentary body; the refits show that this deposit consists of material derived from layers 15–25 that gravitated through fissures open in the sedimentary column above. Layer 20, at the interface between two major stratigraphic ensembles, requires additional analysis. Throughout, we found significant vertical dispersion along the contact between sedimentary fill and cave wall. Given these findings, a preliminary analysis of technological change across the studied sequence organized the lithic assemblages into five ensembles: layer 15; layers 16–19; layer 20; layers 21–22; layers 23–25. The lower ensembles show higher percentages of flint and of the Levallois method. Uniquely at the site, the two upper ensembles feature bifaces and cleavers.
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The analysis of several lithic assemblages with flake cleavers and bifaces from sites attributed to MIS 5 and 3 in the western Pyrenees provides the basis for a new chronological and typo-technological characterisation of the region's... more
The analysis of several lithic assemblages with flake cleavers and bifaces from sites attributed to MIS 5 and 3 in the western Pyrenees provides the basis for a new chronological and typo-technological characterisation of the region's late Middle Palaeolithic record. Previously assigned to the Vasconian based strictly on typological criteria, a certain degree of variability evident between the analysed assemblages likely indicates different occupation types. However, broad typo-technological traits reflecting a common regional tradition can be identified and are discussed against the backdrop of the regional diversity and cultural geography of late Middle Palaeolithic industries dated to around 50 ka BP. This 'regionalisation' of lithic techno-complexes may also have important ramifications for the socioeconomic organisation and demographic dynamics of late Middle Palaeolithic human groups.
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Le Vasconien a été défini par François Bordes en 1953 à partir des industries lithiques de la région franco-cantabrique. Il s’agit à ses yeux de l’un des faciès culturels qui coexistent au sein du Moustérien, et dont la principale... more
Le Vasconien a été défini par François Bordes en 1953 à partir des industries lithiques de la région franco-cantabrique. Il s’agit à ses yeux de l’un des faciès culturels qui coexistent au sein du Moustérien, et dont la principale caractéristique est la présence de hachereaux traduisant une influence africaine.
Depuis, la validité et la signification de ce faciès, défini sur des bases essentiellement typologiques, ont fait l’objet de discussions et de contestations récurrentes. Certains auteurs ont notamment souligné qu’il était difficile de trouver une unité typologique aux différents ensembles attribués au Vasconien, hormis la présence de hachereaux.
Une réévaluation en cours de séries classiques du Vasconien dans le cadre d’une approche technologique a d’ores et déjà fourni des arguments allant dans le sens d’une certaine unité de ce faciès. Si des interrogations subsistent, notamment concernant la position chrono-stratigraphique de ces industries ou l’importance respective des facteurs culturels, fonctionnels ou environnementaux dans leur production, la notion de Vasconien conserve une pertinence certaine plus d’un demi-siècle après sa définition.
The Vasconian, half a century after its definition by François Bordes
François Bordes defined the Vasconian in 1953 from lithic industries of the Franco-Cantabrian area. He considers it as one of the cultural facies coexisting within the Mousterian, and whose main characteristic is the presence of flake cleavers reflecting an African influence.
Since then, the validity and significance of this facies typologically defined have been discussed and recurrently challenged. Some authors have stressed that it was difficult to find a typological unity to the different series attributed to the Vasconian apart from the presence of flake cleavers.
An ongoing technological reassessment of classic Vasconian series has already provided arguments in favor of a certain unity of this facies. Questions remain particularly regarding the chrono-stratigraphic position of those industries or the importance of cultural, environmental or functional factors in their production, but the notion of Vasconian keeps certain relevance more than half a century after its definition.
Depuis, la validité et la signification de ce faciès, défini sur des bases essentiellement typologiques, ont fait l’objet de discussions et de contestations récurrentes. Certains auteurs ont notamment souligné qu’il était difficile de trouver une unité typologique aux différents ensembles attribués au Vasconien, hormis la présence de hachereaux.
Une réévaluation en cours de séries classiques du Vasconien dans le cadre d’une approche technologique a d’ores et déjà fourni des arguments allant dans le sens d’une certaine unité de ce faciès. Si des interrogations subsistent, notamment concernant la position chrono-stratigraphique de ces industries ou l’importance respective des facteurs culturels, fonctionnels ou environnementaux dans leur production, la notion de Vasconien conserve une pertinence certaine plus d’un demi-siècle après sa définition.
The Vasconian, half a century after its definition by François Bordes
François Bordes defined the Vasconian in 1953 from lithic industries of the Franco-Cantabrian area. He considers it as one of the cultural facies coexisting within the Mousterian, and whose main characteristic is the presence of flake cleavers reflecting an African influence.
Since then, the validity and significance of this facies typologically defined have been discussed and recurrently challenged. Some authors have stressed that it was difficult to find a typological unity to the different series attributed to the Vasconian apart from the presence of flake cleavers.
An ongoing technological reassessment of classic Vasconian series has already provided arguments in favor of a certain unity of this facies. Questions remain particularly regarding the chrono-stratigraphic position of those industries or the importance of cultural, environmental or functional factors in their production, but the notion of Vasconian keeps certain relevance more than half a century after its definition.
