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.     

Ungulate carcass transport strategies at the Middle Palaeolithic site of Abric Romaní (Capellades,Spain)

We evaluated the skeletal profiles from several levels of the Neanderthal site of Abric Romaní, focusing on the methodology proposed by Faith and Gordon (2007): differences in the skeletal distribution of animals in accordance with their size and weight; the statistical correlation between the skeletal profiles and standard food utility index; and the anatomical diversity of size-weight categories. Results indicate an unconstrained transport strategy in all levels and all size-weight categories. However, we also found differences in the skeletal distribution of medium-sized and large animals, which may be due to different transport strategies. These characteristics suggest that the superposition of transport and occupation events could be responsible for our results. In addition, we applied the same analysis to Hadza assemblages, which revealed similar results to those found at Abric Romaní. The most striking feature of the Hadza assemblages examined is the superposition of transport events as a result of successive occupation/deposition events. This suggests that the transport strategies used by Neanderthals at Abric Romaní are also characterized by a high degree of diversity in transport decisions.     

New data on Sicilian prehistoric and historic evolution in a mountain context,Vallone Inferno (Scillato,Italy)

Vallone Inferno rock-shelter is an archaeological site located in the Madonie mountain range in Sicily. Archaeological excavation and research have provided a long prehistoric and historic sequence from the Neolithic to the medieval period, this being the most complete work in this area at present. In this paper we present the preliminary data provided by a multidisciplinary study based on pottery, lithic, human, faunal and plant remains. Stratigraphic studies have identified four complexes, of which complex 3 has provided almost all the archaeological remains. ¹⁴C AMS dates, obtained from four samples, place the human activities between 2601 cal BC and 644 cal AD. These dates are coherent with the cultural attribution of the ceramic and lithic remains. Macrofaunal and plant remains show a persistent use of the shelter for pastoral activities. Environmental data, obtained from microvertebrate and archaeobotanical remains, show the aridification and opening of the landscape from the base to the top of the sequence as a consequence of the human impact.     

Research on late Pliocene Oldowan sites at Kanjera South, Kenya

The late Pliocene is notable for the appearance of two new hominid genera as well as the first archaeological sites, generally attributed to the Oldowan Industrial Complex. However, the behavioral ecology of Oldowan hominids has been little explored, particularly at sites older than 2.0 Ma. Moreover, debates on Oldowan hominid foraging ecology and behavior have centered on data from only two regions, and often from single site levels. Here we describe the preliminary results of our investigation of Oldowan occurrences at Kanjera South. These occurrences preserve the oldest known traces of hominid activity in southwestern Kenya, and unlike most of the Oldowan sites in the 2.0-2.5 Ma time interval, artefacts are found in spatial association with a well-preserved fauna. In 1996 and 1997, this project initiated the first excavation program for Kanjera South. Magneto- and biostratigraphy indicate that deposition began approximately 2.2 Ma, substantially earlier than previously thought. At Excavation 1, artefacts were found in spatial association with a taxonomically diverse faunal assemblage in Beds KS-1 and KS-2. Excavation 2 yielded a partial hippopotamus axial skeleton with artefacts in KS-3. Cores from both sites were incidentally flaked and represent a Mode I lithic technology indistinguishable from the Oldowan. Approximately 15% of the artefacts were manufactured from non-local raw materials, indicating a flow of resources into the area. Stable isotopic analysis of KS-1 and KS-2 pedogenic carbonates suggests that the Excavation 1 assemblages formed in a relatively open (>75% C4 grass) habitat. The Excavation 1 and 2 faunas contain a high proportion of equids relative to Oldowan accumulations from Bed I Olduvai Gorge, Tanzania. Beds KS-1 and KS-2 thus preserve traces of Oldowan hominid activities in a more open setting than has been previously documented.     

Les premières occupations humaines dans le Sud du Brésil : une vision géoarchéologique intégrée

Between ≈13,000 and 7000 BP, the territory of southern Brazil was occupied in a stable and diverse manner, with the main anthropic trace being in lithic material. Archaeological research has provided more consistent evidence of occupation in different environments and associated with different stratigraphic formation processes since the Late Pleistocene. Therefore, this paper proposes to analyse the history of the earliest evidence of pre-colonial occupation in southern Brazil from a geoarchaeological point of view, focusing on stratigraphic and chronological data and the process of formation of archaeological layers. Thirty-three stratigraphic sections were analysed from 31 archaeological sites distributed along the Paraná, Uruguay and Atlantic basins. Evidence of archaeological levels was found in different geomorphological contexts: plateau, slopes, valley bottom, alluvial plains and rockshelters. The results indicate that the oldest archaeological levels in the region were formed in the Late Pleistocene, associated with periods of fluvial incision that signal important changes in the southern river systems, characterized by the formation of alluvial and colluvial-alluvial terraces in the valley bottoms. This is followed in the Lower Holocene by widespread colluvial processes in the incised valleys, alluvium in the middle river courses and anthropogenic deposits in the rockshelters that formed the main ancient levels. In the early Middle Holocene, sedimentary deposits containing archaeological material decrease significantly, marking regional changes in lithic industries. The data indicate that there appears to be a threshold between deposition and archaeology in the Early Holocene, characterized by high stratigraphic resolution, where stratigraphic sequences show greater thickness and density of archaeological levels. Finally, the diversity of inter-regional lithic assemblages is clearly highlighted, marked by the predominance of industries on pebbles and blocks, the debitage of flakes and blades as a support for various tools in the interior basins and the shaping of small projectile points on the Atlantic slope.     

Un exemple de gestion des géo-ressources au Paléolithique supérieur en moyenne montagne : le Badegoulien de la grotte du Rond-du-Barry (Sinzelles,Polignac, Haute-Loire)

Rond-du-Barry cave is situated in the centre of the Cenozoïc sedimentary basin of Puy-en-Velay in a mountainous environment. It contains Middle Palaeolithic, Badegoulian, Magdalenian and more recent occupation levels. Lying between two major river corridors (the Loire to the west and the Allier to the east), this site provides a special opportunity for defining exploitation and management modalities linked to the territory occupied by the prehistoric humans who inhabited the cave and the role played by the landscape's structural elements in human behavior at the end of the Upper Pleistocene. Lithic raw material analysis of the archaeological assemblages allowed us to define the dispersal of raw materials used in the site. Such dispersal has for some time been considered to provide a reliable reflection of actual movements of human groups. Our study, based on a modified methodology incorporating the concept of a chaine évolutive for flint, focused on the lithic artifacts from Rond-du-Barry unit F2, which are attributed to the Badegoulian. The results of our study differ from those of previous studies in terms of the diversity of the raw material being used and the frequency of occurrence for each type. Our conclusion is that Badegoulian humans were not physically constrained by a familiar territory, but traveled and/or traded widely in their quest for suitable raw materials. The diversity in the lithic raw materials, gathered locally and semi-locally from different primary and secondary outcrops demonstrates this territorial range. Importation of siliceous raw material originating from the meridional edge of the Paris basin (Berry, Touraine) suggests a planned resource-use strategy for obtaining large pieces of flint, which are rare in the regional outcrops. However, unraveling the resource use strategies to this degree of intention lies beyond what can be revealed by the lithic material alone.     

Modeling the formation of Early Stone Age artifact concentrations

The nature of stone artifact concentrations at early Plio-Pleistocene sites in East Africa is evaluated with regard to hominid transport behaviors responsible for their formation. These archaeological occurrences indicate ranging behaviors involving deliberate and repeated transport of flaked stone artifacts. The stone transported to archaeological sites within the time range of Homo habilis indicates planned transport of tools or material for tool manufacture to an extent far beyond transport behaviors reported among living apes, even stone hammer-using chimpanzees. Analysis of technological evidence in a lithic assemblage at a Plio-Pleistocene site at Koobi Fora (c. 1·5 ya) indicates on-site manufacturing activities and transport of flaked stone both to and from the site locale. Possible explanations for transport of stone artifacts are discussed in view of hominid strategies of environmental exploitation and resource utilization. A model is proposed for planned, habitual transport of artifacts by hominids positively correlated with distance of planned foraging range. In this model, larger-scale sites tended to develop at locales favorably located near abundant resources, where stone imports were high but export was relaxed due to the proximity of resources to be processed.     

The fragmented character of Middle Palaeolithic stone tool technology

The importance of the transport of stone artefacts in structuring Neandertal lithic assemblages has often been addressed, but the degree to which this led to fragmentation of lithic reduction over Middle Palaeolithic landscapes has not been explicitly studied thus far. Large-scale excavations of Middle Palaeolithic open-air sites and refitting studies of the retrieved assemblages have yielded new, high-resolution data on the mobile aspects of Neandertal stone tool technology. In this paper, we integrate lithic technology and raw material data from recent studies of Middle Palaeolithic open-air and rock shelter sites in Western Europe. We demonstrate that the results of a variety of typological, technological (especially refitting), and lithological studies have important consequences for our knowledge of the acquisition of raw materials and subsequent production, usage and discard of stone artefacts in the Middle Palaeolithic. Neandertal production and use of stone tools was fragmented in three domains: the spatial, the temporal and the social domain. We show that this versatile segmentation of stone artefact handling strategies is a main determinant of the character of the Neandertal archaeological record. Our data testify to ubiquitous and continuous transport of stone artefacts of a wide variety of forms, picked by Neandertals using selection criteria that were sometimes far removed from what archaeologists have traditionally considered, and to some degree still consider, to be desired end products of knapping activities. The data presented here testify to the variability and versatility of Middle Palaeolithic stone tool technology, whose fragmented character created very heterogeneous archaeological assemblages, usually the product of a wide variety of independent import, use, discard and/or subsequent transport events.     

Palaeoloxodon and Human Interaction: Depositional Setting,Chronology and Archaeology at the Middle Pleistocene Ficoncella Site (Tarquinia,Italy)

The Ficoncella site in northern Latium (Italy) represents a unique opportunity to investigate the modalities of a short occupation in an alluvial setting during the Lower Palaeolithic. The small excavation area yielded a lithic assemblage, a carcass of Palaeoloxodon antiquus, and some other faunal remains. The main objectives of the study are to better characterize the depositional context where the Palaeoloxodon and the lithic assemblage occur, and to evaluate with greater precision the occupation dynamics. A 25 m-long well was drilled just above the top of the terrace of the Ficoncella site and faunal and lithic remains were analyzed with current and innovative techniques. The archaeological site contains floodplain deposits as it is located next to a small incised valley that feeds into a larger valley of the Mignone River. A tephra layer capping the site is ⁴⁰Ar/³⁹Ar dated to 441± 8 ka. Collectively, the geochronologic, tephrochronologic and geologic data, suggest the site was occupied during MIS 13. The new results should prompt further research at Ficoncella in order to improve our understanding of the dynamics of human settlement in Europe during the Early to Middle Pleistocene.     

Neanderthal mobility and technological change in the northeastern of the Iberian Peninsula: The patterns of chert exploitation at the Abric Romaní rock-shelter

Understanding the changes in the technological organization of prehistoric hunter–gatherers is important to research into hominin foraging activities. During the Middle Paleolithic, the coexistence or the replacement between Levallois and discoid technologies has frequently been recorded, but there is still no clear understanding of the reasons for their alternating and fragmented use in the archaeological record. This paper aims to contribute with new data to the current debate, by exploring the chert assemblages from levels O and M of the Abric Romaní rock-shelter. The results reveal that the change from Levallois in level O to discoid in level M is accompanied by the use of different axes of mobility, a reduction in the foraging radius and a more careful management of raw materials. A cross comparison with other archaeological evidences indicates the general pattern in the Northeast of the Iberian Peninsula during the late Middle Paleolithic, in which the use of Levallois technology is associated with chert and high mobility patterns whereas discoid technology is more closely linked to the use of local raw materials and a lower degree of mobility. The modifications to the mountainous environments and to the distribution of preferred prey animals may have influenced the Neanderthals’ mobility patterns and contributed to modifying their technical behaviours in order to obtain better foraging incomes.     

湖北郧县余嘴2号地点砍砸器的实验研究

2009年在湖北郧县余嘴2号旧石器地点的发掘过程中, 我们利用文化层中出土的砾石原料与从该地点附近地表采集的砾石原料进行复制与使用实验。各复制样本50件, 并根据原料类型、大小与刃角选取样本进行了使用实验, 最后与出土标本进行对比。实验结果表明, 燧石最适合用作砍砸器的原料, 砂岩最不适合; 遗址出土砍砸器原料却以相对丰富的角页岩、石英岩为主, 这表明古人选取原料的策略是以方便与适度为原则。实验还显示, 碰砧法制作砍砸器非常有效, 但是出土标本却表现为以锤击法为主, 导致这种差别的原因可能是古人的上肢有更强大的打击力和图方便的目的。另外,实验还表明, 砍砸器的使用有最佳的力轴与握姿以及最佳的边刃长度, 考古标本的观察也印证了这一点。在此基础上, 我们对砍砸器的性质、传统以及作为一种文化适应所代表的意义进行了探讨。     

Early Evidence of Acheulean Settlement in Northwestern Europe - La Noira Site,a 700 000 Year-Old Occupation in the Center of France

The human settlement of Europe during Pleistocene times was sporadic and several stages have been recognized, both from paleaoanthropological and archaeological records. If the first phase of hominin occupation (as early as 1.4 Ma) seems mainly restricted to the southern part of the continent, the second phase, characterized by specific lithic tools (handaxes), is linked to Acheulean settlements and to the emergence of Homo heidelbergensis, the ancestor of Neanderthals. This phase reached northwestern Europe and is documented in numerous sites in Germany, Great Britain and northern France, generally after 600 ka.At la Noira (Brinay, Central France), the Middle Pleistocene alluvial formation of the Cher River covers an archaeological level associated with a slope deposit (diamicton). The lithic assemblage from this level includes Large Cutting Tools (LCTs), flakes and cores, associated with numerous millstone slabs. The lithic series is classified as Acheulean on the basis of both technological and typological analyses. Cryoturbation features indicate that the slope deposits and associated archaeological level were strongly frozen and disturbed after hominin occupation and before fluvial deposition. Eight sediment samples were dated by the electron spin resonance (ESR) method and the weighted average age obtained for the fluvial sands overlying the slope deposits is 665±55 ka. This age is older than previous chronological data placing the first European Acheulean assemblages north of 45^th parallel north at around 500 ka and modifies our current vision of the initial peopling of northern Europe. Acheulean settlements are older than previously assumed and the oldest evidences are not only located in southern Europe. La Noira is the oldest evidence of Acheulean presence in north-western Europe and attests to the possibility of pioneering phases of Acheulean settlement which would have taken place on a Mode 1-type substratum as early as 700 ka. The lithic assemblage from la Noira thus provides behavioral and technological data on early Acheulean occupation in Europe and contributes to our understanding of the diffusion of this tradition.     

Une nouvelle faune de vertébrés continentaux,associée à des artefacts dans le Pléistocène inférieur de l’Hérault (Sud de la France), vers 1,57 Ma

A new vertebrate fauna associated with lithic artefacts from the Early Pleistocene of the Hérault Valley (southern France) dated around 1.57 Ma. Some lithic artefacts associated with an Early Pleistocene (Upper Villafranchian) vertebrate fossil assemblage have been found from a quarry exploited for basalt in the lower Hérault Valley (Languedoc, southern France) at the Lézignan-le-Cèbe locality. A preliminary patrimony expertise led us to identify about 20 vertebrate taxa, and the autumnal rainfalls revealed the presence of roughly 30 lithic artefacts of “pebble culture” type. A basalt layer dated at 1.57 My directly overlies the fossiliferous level, extends along the little hill (locus 2) yielding artefacts. These new promising data offer new perspectives to improve our understanding of Early Pleistocene ecosystems (and possibly ancient hominin occupation) of southern Europe.     

La gestion du quartz au Pléistocène moyen et supérieur. Trois exemples d’Europe Méridionale

Quartz is one of the main lithic resources employed along the Pleistocene for the manufacturing of tools. The abundance in all kind of environments leads to its frequent presence in archaeological sites. In spite of its suitability for knapping, the scarcity of specific researches on quartz industries has led to a view of this raw material as a second-rate resource, only used when flint was not available in the surroundings. Quite in opposition to this prejudice, the familiarity with the petrological and mechanical properties of the different varieties of quartz has led the Middle/Upper Pleistocene groups to a rational and differential exploitation of the available resources. There is a distinct selection of the varieties attending to the purposes of the exploitation and configuration. The patterns of exploitation of the cores are very standardized, based on longitudinal extractions and documenting the bipolar flaking technique. Moreover, when the raw material is of good quality, more sophisticated reduction methods such as the discoidal or the Levallois may be employed. On the other hand, for the purposes of configuration a clearly differential management of the raw material is attested: thus quartz is used for the small products (denticulates, side-scrapers, notches), while other stones (quartzite, porphyry and others) are devoted to the manufacturing of those tools demanding a more complex control of the elaboration (bifaces, cleavers, etc.). Either acting as the main lithic resource or as a complement to other raw materials, we can observe through the technological analysis of these lithic collections the great conceptual complexity depending on the needs to be fulfilled. Raw material quality allowing, the state-of-the-art technology of knapping can be applied to the quartz and, therefore, we should not understand its use as a consequence of environmental constrictions but rather as a result of the variability of the procurement strategies and management of lithic resources among the prehistoric communities.     

What's in a beach? Soil micromorphology of sediments from the Lower Paleolithic site of 'Ubeidiya, Israel

A micromorphological study of archaeological sediments from the early Pleistocene site of 'Ubeidiya (Jordan Valley, Israel) was conducted to provide microenvironmental detail for the hominin occupation contexts and investigate site formation issues. Previous research shows that the hominin groups occupied the marshes and pebbly beaches at the shores of a lake during a regressive period, but given that some portions of the lithic and faunal assemblages are abraded and others fresh, there remains a question of whether the archaeological assemblages are in situ or reworked, and if reworked, by what mechanisms and from where. The rates of sedimentation within the regressive cycle, by which we can learn about the frequency and duration of exposed surfaces amenable for hominin occupation is also unknown. Finally, the artificial nature of some of the pebbly layers has been questioned. The micromorphological analysis yielded the identification of twelve microfacies; the majority of these represent fluvially derived floodplain soils or distal mudflow deposits, and a minor number are sediments of lacustrine origin: mudflats and shallow subaqueous sediments. These represent the natural habitats of the 'Ubeidiya hominins and might serve as a reference to similar contexts of other early hominin sites. The sedimentary model proposed here entails the rapid deposition of fluvially derived low-energy sediments at and around the shoreline, followed by prolonged periods of exposure, during which surfaces stabilized within a relatively wet, marshy environment. This interpretation suggests that the abraded portions of the archaeological assemblages are a result of prolonged surface exposure rather than high-energy transport from a distant source or to wave reworking at the shoreline, and supports the consideration of these assemblages as archaeological palimpsests, with locally reworked fresh and abraded elements. No micromorphological evidence supporting anthropogenic agency in the formation of the pebbly layers was found. The entire regressive cycle entailed unvarying climatic conditions with seasonal fluctuations and episodic lacustrine incursions, and with a trend towards arid conditions in the end.     

河北阳原泥河湾盆地籍箕滩遗址发现的新材料

河北阳原泥河湾盆地的籍箕滩旧石器时代晚期旷野遗址群于上世纪80年代被发现并系统发掘,目前,曾出土了丰富的细石叶制品及动物碎骨的第2地点(T2)由于后期工程建设的原因已不复存在,原记录中的第1地点(T1)、第3地点(T3)也均受到了不同程度的人为破坏或自然力侵蚀。为探明遗址堆积保存状况,工作队对遗址第1、3地点进行了复查及剖面清理,分别发现了密度较大的石制品遗存。对第1地点和第3地点的光释光和¹⁴C测年结果表明,该地有人类活动遗迹的堆积物形成年代为距今16000余年至全新世初期,与河对岸虎头梁遗址群中的马鞍山、于家沟相当,表明了当时古人类的活动范围同时覆盖了桑干河南北两岸。     

Hominin occupations at the Dmanisi site, Georgia, Southern Caucasus: raw materials and technical behaviours of Europe's first hominins

Dmanisi is the oldest site outside of Africa that records unquestioned hominin occupations as well as the dispersal of hominins in Europe and Asia. The site has yielded large numbers of artefacts from several periods of hominin occupation. This analysis of Dmanisi stone tool technology includes a review of all the pieces recovered during the last 15 years of excavations. This lithic assemblage gives insights into the hominin behaviour at 1.7-1.8 Ma in Eurasia. Dmanisi hominins exploited local rocks derived from either nearby riverbeds or outcrops, and petrographic study provides data on patterns of stone procurement. Recent geological surveys and technological studies of the artefacts illustrate the roles of hominins in composing the assemblage. Dmanisi hominins selected two types of blanks, including cobbles and angular blocks, of basalt, andesite, and tuffs. Many complete cobbles, pebbles, and rolled blocks in basalt were unmodified, and geological analyses and surveys indicate that hominins brought manuports back to the site, suggesting a complex procurement strategy. Cores, flakes and debris show that all stages of flaking activity took place at the site. Numerous unifacial cores suggest that knapping was not very elaborate. Centripetal knapping is observed on some flake-cores. Knapping was influenced by the blank shape and natural angles. Most flaked objects were either cores or chopper-cores. Flakes predominate while flake tools are rare. The Dmanisi lithic assemblage is comparable to Oldowan sites in Africa in terms of reduction sequence, organisation of the removals, platform types, and the lack of retouched flakes. Dmanisi artefacts and may have been produced by the original hominins in Europe and Asia.     

New evidence of old stone tools from the Mekong terraces,Cambodia

The study of prehistoric sites with lithic remains indicates that the occupation of continental Asia, notably India and China, seems to have taken place earlier than previously thought. However, this Early Pleistocene human dispersal out of Africa remains debatable for the Southeast of Asia, in spite of the discovery of original lithic assemblages on the Mekong terraces dated to the very beginning of the Middle Pleistocene in the centre of Cambodia, by Saurin and Carbonnel in the 1960–1970s. Although this fundamental lithic material has become a reference, it has not been subjected to renewed study of these artefacts over the past decades, and it is thus not possible, for the moment, to attribute it with certainty to a particular culture. In this paper, we present an analysis of the raw materials and a techno-typological study of a similar series of prehistoric tools gathered by one of us in order to bring to light new elements concerning the first Palaeolithic occupation of this region of the world.     

从技术组织论视角阐释中国古人类石器技术的多样性

石器的演化历史与早期人类技术活动的投入成本密切相关,也在一定程度上受制于可获取的原料与利用的动植物资源。克拉克有关早期人类的石器技术演化的5种技术模式,在解释旧大陆古人类技术演化具有深远的影响。然而,生活在东亚特别是中国北方地区的古人类,石制品文化面貌在约40 ka BP一直以石核-石片技术体系占据主导地位。学术界一般以中国本土旧石器文化传统根深蒂固,与西方文化交流有限为原因,解释这种石器技术发展的不平衡现象。本文以石制品生产技术组织的研究理念为出发点,强调精致加工代表人群的高投入技术与行为,在中国境内以模式2、3为代表,其产品可在一定程度上作为文化标识反映了外来人群的扩散,体现了东、西方文化有限交流;而权宜技术则多为低投入的技术与行为活动,以石核-石片技术体系为代表,随时间推移不断继承发展。同时,石核-石片技术体系在中国盛行的现象,表明本地古人类对一种比较成功的适应策略的坚持和继承,分布区域局限、内在技术变异程度相对较低的模式2、3技术,更有可能是欧亚大陆西侧和非洲规模有限的人群扩散或技术传播的结果。     

Productions lithiques et comportements techno-économiques de groupes humains acheuléens et moustériens en région liguro-provençale

Acheulean and Mousterian human occupations left an abundant record of lithic productions in the Liguro-Provençal region. Certain sites show the transition between the Lower and Middle Palaeolithic, yielding industries in which the shaping of bifaces continued along with partial Levallois reduction and the development of light-duty, retouched Mousterian tools. In the more recent sites, Mousterian lithic productions show further development in Levallois reduction techniques and sometimes blade production, while shaping techniques disappeared. The transport of artefacts of exotic lithic raw materials from sometimes very distant sources had already occurred by the end of the Acheulean, and the example of the use of allochthonous jasper illustrates an aspect of techno-economical behaviours and the mobility of these human groups. Such transport of jasper blanks from distant sources became further developed at certain Mousterian sites in Liguria, but with the addition of knapping and retouching activities at the occupation sites.