34 research outputs found

    The first Neanderthal remains from an open-air Middle Palaeolithic site in the Levant

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    The late Middle Palaeolithic (MP) settlement patterns in the Levant included the repeated use of caves and open landscape sites. The fossil record shows that two types of hominins occupied the region during this period - Neandertals and Homo sapiens. Until recently, diagnostic fossil remains were found only at cave sites. Because the two populations in this region left similar material cultural remains, it was impossible to attribute any open-air site to either species. In this study, we present newly discovered fossil remains from intact archaeological layers of the open-air site 'Ein Qashish, in northern Israel. The hominin remains represent three individuals: EQH1, a nondiagnostic skull fragment; EQH2, an upper right third molar (RM3); and EQH3, lower limb bones of a young Neandertal male. EQH2 and EQH3 constitute the first diagnostic anatomical remains of Neandertals at an open-air site in the Levant. The optically stimulated luminescence ages suggest that Neandertals repeatedly visited 'Ein Qashish between 70 and 60 ka. The discovery of Neandertals at open-air sites during the late MP reinforces the view that Neandertals were a resilient population in the Levant shortly before Upper Palaeolithic Homo sapiens populated the region

    Persistent Neanderthal occupation of the open-air site of ‘Ein Qashish, Israel

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    Over the last two decades, much of the recent efforts dedicated to the Levantine Middle Paleolithic has concentrated on the role of open-air sites in the settlement system in the region. Here focus on the site of ‘Ein Qashish as a cases study. Located in present-day northern Israel, the area of this site is estimated to have been >1300 m2, of which ca. 670 were excavated. The site is located at the confluence of the Qishon stream with a small tributary running off the eastern flanks of the Mt. Carmel. At the area of this confluence, water channels and alluvial deposits created a dynamic depositional environment. Four Archaeological Units were identified in a 4.5-m thick stratigraphic sequence were dated by Optically Stimulated Luminescence (OSL) to between—71 and 54 ka, and probably shorter time span–~70-~60 ka. Here we present the diverse material culture remains from the site (lithics, including refitted sequences; modified limestone pieces; molluscs; faunal remains) against their changing paleogeographic backdrop. Skeletal evidence suggests that these remains were associated with Neanderthals. The large-scale repeated accumulation of late Middle Paleolithic remains in the same place on the landscape provides a unique opportunity to address questions of occupation duration and intensity in open-air sites. We find that each occupation was of ephemeral nature, yet presents a range of activities, suggesting that the locale has been used as a generalized residential site rather than specialized task-specific ones. This role of ‘Ein Qashish did not change through time, suggesting that during the late Middle Paleolithic settlement system in this part of the southern Levant were stable

    New Data from Shovakh Cave and Its Implications for Reconstructing Middle Paleolithic Settlement Patterns in the Amud Drainage, Israel

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    Abstract: This study presents the geoarchaeological and geochronological aspects of Shovakh Cave and the first comparative context to the nearby Amud Cave (~ 500 m downstream), providing an exceptional opportunity to explore the range of human behaviours within a small geographic area. Sediment samples from two newly excavated areas at the rear and entrance of the cave were analysed using infrared spectroscopy, micromorphology and phytolith analysis and dated through uranium-thorium and luminescence techniques. The rear of the cave shows carnivore activity and low artefact concentrations. It also exhibits a shift in sedimentation from wind-blown deposits to colluviation of terra rossa. Direct dating of the deposits associated with the Middle Palaeolithic (MP) occupation at this area could not be obtained due to the breccia forming at the lower part of the excavation area. However, the later phases of the Middle Palaeolithic occupation at this area gave an age estimate of 45.5 ± 3.7 ka. At the entrance of the cave, there are relatively more residues associated with human use of fire. Post-depositional processes in this area include decalcification of the upper layer, cementation of the lower layer and phosphatisation due to guano decomposition, which indicates that this area was probably roofed. The ages obtained in this area range between 67.5 ± 5.5 to 56.2 ± 5.9 ka, overlapping with the occupation time of Amud cave. The evidence from Shovakh Cave presents lower intensity of occupation compared to Amud, indicating variable modes of site use by humans in the Amud drainage during the Late Middle Palaeolithic

    Middle Palaeolithic raw material procurement and early stage reduction at Jubbah, Saudi Arabia

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    Several hundred Middle Palaeolithic (MP) archaeological sites have now been identified in the Arabian Peninsula. However, the study of lithic raw material properties and related procurement behaviours is still in its infancy. Here we describe raw material procurement and early stage lithic reduction at MP sites in the Jubbah palaeolake basin, in the Nefud Desert, northern Saudi Arabia. We describe the sites identified during our surveys, and we use petrographic studies to demonstrate that MP assemblages were mostly produced from differing forms of ferruginous quartzite. These raw materials do not substantially vary in composition, although they are not identical in terms of factors such as grain size and the proportion of iron oxide. We then describe the lithic technology at these sites, with a particular focus on the largest assemblage identified, Jebel Katefeh-12 (JKF-12), which provides detailed information on lithic reduction at a quartzite source. Analyses from this site are then considered together with data from other MP sites in the Jubbah basin, where similar raw material was used. The results indicate that factors such as initial clast size/shape and reduction intensity play important roles in influencing aspects of morphological and technological variability. Our results suggest that incursions of MP populations into northern Arabia were probably temporally limited, as might be expected in a marginal and generally arid region. MP raw material procurement sites provide a highly visible signal of these ephemeral incursions, providing information on the ways that human populations adapted to the challenging conditions of the Saharo-Arabian arid belt. © 201

    Going the distance: Mapping mobility in the Kalahari Desert during the Middle Stone Age through multi-site geochemical provenancing of silcrete artefacts

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    Givat Rabi East. a New Middle Paleolithic Knapping Site in the Lower Galilee (Israel)

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    Givat Rabi East is a newly-discovered flint outcrops centrally located within the Galilee in relative proximity to several Middle Paleolithic sites. In this paper we present the site and discuss the function of a dense accumulation of Middle Paleolithic flint knapping wastes excavated on its eastern edge. Our results suggest that the knapping wastes are likely the remains of a Mousterian workshop site. In comparison to the workshop site at Sede Ilan, located 15 km to the east where flint was quarried, the Givat Rabi East flint knappers collected eroded flint blocks in situ. The Lithic evidence indicates that the knapping sequences were initiated at the site. Furthermore several Levallois knapping methods had been employed. Therefore we suggest that the lithic assemblage left at Givat Rabi East represent knapping activities of several groups who exploited this location during the Middle Paleolithic period. Subsequently some of the lithic material (e. g. unfinished cores, Levallois blanks) was taken to other locations (e. g., caves) in order to continue the knapping sequence. The site location combined with the characteristics of the debitage and cores found within it, suggests that Givat Rabi East could have been one of the flint source for Qafzeh Cave and perhaps to other Mousterian cave sites.Givat Rabi Est est un affleurement de silex rĂ©cemment dĂ©couvert dans le centre de la GalilĂ©e, Ă  proximitĂ© de plusieurs sites du PalĂ©olithique moyen. Cet article prĂ©sente le site et traite de l’utilisation d’un amas de dĂ©chets de taille du PalĂ©olithique moyen, fouillĂ©e sur son bord oriental. Les rĂ©sultats suggĂšrent que les dĂ©chets de taille sont probablement les vestiges d’un atelier moustĂ©rien. En comparaison avec le site d’atelier de Sde Ilan, situĂ© Ă  15 km Ă  l’est, oĂč le silex Ă  Ă©tĂ© extrait, Ă  Givat Rabi Est les tailleurs ont acquis le silex par ramassage de blocs de silex qui ont Ă©tĂ© Ă©rodĂ©s in situ. L’assemblage lithique indique que les sĂ©quences de taille Ă©taient initiĂ©es sur le site et que plusieurs mĂ©thodes de Levallois ont Ă©tĂ© utilisĂ©es. Par consĂ©quent, nous suggĂ©rons que les assemblages lithiques qui ont Ă©tĂ© laissĂ©s Ă  Givat Rabi Est reprĂ©sentent des activitĂ©s de taille de plusieurs groupes, qui ont utilisĂ© cet emplacement pendant le PalĂ©olithique moyen. Une partie du matĂ©riau lithique Ă©tait emportĂ©e en d’autres lieux (par exemple des grottes) pour continuer la sĂ©quence de taille. L’emplacement du site, tout comme les caractĂ©ristiques du dĂ©bitage, laissent supposer que le site de Givat Rabi Est a pu ĂȘtre utilisĂ© comme une source de silex pour la grotte de Qafzeh et peut-ĂȘtre pour d’autres grottes moustĂ©riennes.Ekshtain Ravid, Barzilai Omry, Inbar Moshe, Milevski Ianir, Ullman Micka. Givat Rabi East. a New Middle Paleolithic Knapping Site in the Lower Galilee (Israel) . In: PalĂ©orient, 2011, vol. 37, n°2. pp. 107-122
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