Epipaleolithic human appendicular remains from Ein Gev I,Israel

The Upper Paleolithic (Early Epipaleolithic/Kebaran; ∼ 19,000 cal BP) human skeleton, from Layer 3 of Ein Gev I on the western flanks of the Golan Heights adjacent to the Sea of Galilee, retains sufficient limb remains to permit assessment of its body size and proportions, as well as diaphyseal reflections of skeletal hypertrophy. The individual was of modest stature but average mass for a later Upper Paleolithic individual, providing it with the body mass-to-stature body proportions characteristic of later Upper Paleolithic and more recent circum-Mediterranean humans. The humeri exhibit unexceptional diaphyseal asymmetry and robustness for an Upper Paleolithic human, and the femur exhibits similar relative diaphyseal hypertrophy. The humeral midshafts are relatively round, but the femoral and tibial midshafts are pronounced anteroposteriorly. As such, Ein Gev 1 provides additional paleobiological data on the appendicular remains of these Southwest Asian humans prior to the increasing sedentism of the terminal Pleistocene.     

Some aspects of the Upper Palaeolithic period in Sindh,Pakistan

The study of the Upper Palaeolithic of Sindh is still in its infancy. Although it has slightly improved during the last twenty years, and a few more sites have been discovered in different parts of the province, we are still far from achieving a good knowledge of the sequence of the events that took place during the final stages of the Pleistocene in this region of the Indian Subcontinent. Despite the archaeological importance of the southern part of the country, the Arabian Sea coast in particular, which represents the suggested route followed by Modern Humans to move to India and farther east, most of this territory has not yielded any tangible trace of their passage. The scope of this paper is to update the evidence available for the Upper Palaeolithic of Sindh, and to discuss it within the general framework of the Upper Palaeolithic period of the Indian Subcontinent.     

Early human dispersal at the western edge of the Eastern European plain: Data from Ukraine

The current state of research on Lower Palaeolithic sites in Ukraine within its 1991 borders is the focus of this paper. Over the last 10–15 years, many new sites have been discovered in different parts of the eastern European area of the country, reassessed some old materials. In the central European region of the country, in the Ukrainian Transcarpathia, important new stratified Lower Palaeolithic sites have also been found. The current Ukrainian Lower Palaeolithic records demonstrate hominin presence in mountainous areas (Carpathians, Crimea) and the valleys of all major rivers, namely the Dniester, Southern Buh, Dnieper and Severskiy Donets. The article presents a brief review of the main currently known Lower Palaeolithic assemblages. Available geological, geomorphological, biostratigraphical data and ESR dates allow defining their age between 1.2 and 0.4 Myг; sites correlate with few warm phases between MIS 35 and MIS 11. Earlier sites, very tentatively dated at around 2 Myг, gravitate towards the seashore and mountainous areas. Later sites witness steady, though not continuous, colonisation of East European plain fringe areas. The main regularities of geographical setting, chronology, morphological and technological characteristics of assemblages of the Lower Palaeolithic sites of the Western segment of the East European plain are characterised. Typologically, industries are mainly characterised as belonging to Mode I. Core-and-flake industries survives to the Holsteinian. Essential difficulties in lithic raw materials supply could probably be a reason for the rise of a peculiar pattern of technological behaviour that involved mainly bipolar knapping and widely applied trimming technique of shaping the working edges of tools. Some signals of probable population movements penetrated the territory of Ukraine by the Asia Minor “western” trajectory and by Caucasian “eastern” way are revealed.     

Ivory Ornaments of the Aurignacian in Western Europe: Case studies from France and Germany

Here we present an overview of the personal ornaments of the Swabian Aurignacian and the Early Aurignacian sites of south-western France made from mammoth ivory. The production sequences for the serial manufacture of beads from these sites are quite similar. While the Swabian sites have yielded numerous different types of beads with a focus of the double-perforated bead, the nearly exclusive use of one bead-type, the perle en forme de panier, is striking at the sites of south-western France. Following the presentation of major inventories of ivory ornaments in the two regions concerned, we discuss potential factors underlying both the differences and the similarities we observe in these assemblages.     

The open-air Paleolithic site of Mirak,northern edge of the Iranian Central Desert (Semnan,Iran): Evidence of repeated human occupations during the late Pleistocene

The northern edge of the Iranian Central Desert has provided valuable evidence of terminal Pleistocene human settlements. Mirak constitutes one of the largest open-air lithic scatters in the region, consisting of eight natural mounds. Fieldwork was initiated in 2015 by the joint Iranian-French program at Mirak 8. Preliminary results have demonstrated at least three successive phases of human occupation during the MIS3: an upper layer with clear Upper Paleolithic affinities and a maximum age of 28 ky, a lower layer with clear Middle Paleolithic affinities that dates around 47 ky, and an intermediate layer with mixed characteristics that can be seen as an intermediate Paleolithic phase which dates between 28 ± 2 and 38 ± 2 ky. At the time when Upper Paleolithic cultures originated in the Zagros Mountains, cultures with clear Middle Paleolithic affinities persisted nearby along the northern edge of the Iranian Central Plateau.     

Utilitarian art and art-related objects in the Urals’ Palaeolithic

Stone and bone artefacts serving as expedient food-procurement and processing implements are the principal and most frequent findings at Palaeolithic sites. Utilitarian art items, often aesthetically fashioned artefacts, are much less common. Emergence of cognitive art within the broader Ural region was determined by progressive cultural developments and adaptations of anatomically modern human beings to mosaic mountain settings and parkland-steppes. At the Urals’ Late Pleistocene cave sites, objects, which were made frequently of unusual and rare materials and are presumed to be of a ritual nature, are represented by adornments and artworks bearing stylized pictorial images. Zoomorphic figurines produced from flint and mammoth ivory document the high skills of Stone Age artisans. The earliest, utilitarian, art-related works of the Urals include sculptures using natural pre-forms such as river pebbles and animal bones, occasionally ochre-painted or ornamented by incising or engraving. Personal decorations are represented by pendants and beads made of stone, shell, bone, and teeth of animals. Rare exemplars are made from material of non-local provenance, such as petrified wood or segments of fossil sea-lily (crinoids) and are indicators of a broad geographic activity-range and/or regional interactions among local groups of hunter-gatherers. Artisanal instruments associated with rock art, for example, lamps made from stone and clay as well as pieces of ochre, belong to a specific category. Aesthetic-looking minerals with appealing colours and textures, such as serpentine, rock crystal, chalcedony, and jasper, it may be assumed, were intended for religious or cultic purposes, but also may have been curated simply because of their natural rarity. These art-related items likely had symbolic value and spiritual meaning apart from purely decorative function. Understanding utilitarian art objects offers insights to every-day life of the Palaeolithic people of the Urals, and their behavioural and environmental adjustments, which culminated in multifarious, iconographic expressions at the end of the Last Glacial stage.     

The Lower Palaeolithic assemblages in Central Europe in stratigraphic and palaeogeographic background

The hominin presence during Lower Palaeolithic in Central Europe was sporadic and followed cold-warm climatic cycle connected with spreading of Scandinavian ice sheet. Up to now there had been discovered about 50 archaeological assemblages from 17 sites from 700 ka years, mostly from second part of it, during c. 300 ka between MIS 15 and 9. The Lower Paleolithic hominins visited Central Europe during warmer periods with deciduous or coniferous forests, even during open domination of open or partly open landscape. Incredible finds, like Bilzingsleben and Schöningen show how complex was life of early hunter-gatherers. In opposite to the previous concept, according to which Lower Palaeolithic hominins were mostly scavengers. The discovery of wooden tools, like spears in lakeshore in opencast mine Schöningen, denies this concept. Contrary to that, early hominins were smart hunters following animal herds and hunted distant way and experienced gatherers. Local lithic technology based on core-flake processing in opposite to Western and Southern Europe dominated by handaxes. Moreover, the preferred usage of “small tools”, which are difficult to use only by fingers may be explained by identification of wooden hafts on few lithic artifacts in Schöningen. However, very long duration of unchanged lithic technology is surprising. An intense accumulation of glacial, eolian and alluvial sediments covered large part of Central Europe and this way Lower Palaeolithic sites are very difficult to discover. All known sites were identified in deep travertine quarries or opencast mines. Future research must be focused on systematic prospection of such outcrops.     

New anthropological data from Cussac Cave (Gravettian,Dordogne, France): In situ and virtual analyses of Locus 3

Cussac Cave presents a unique combination of parietal art and several hundred parts of scattered human remains, dated to the Middle Gravettian (29–28,000 cal BP). The cave is protected as a National Heritage site. As a result, only noninvasive bioanthropological analyses are allowed, consisting of in situ observations and the study of 3D models obtained by photogrammetry. Here we present the first results of these analyses of the human remains from Locus 3. Only 65 of the 106 human skeletal fragments and bones could be firmly identified. Virtual analyses were carried out on 3D models of 16 skeletal elements so that osteometric data could be provided. Despite the limitations inherent in studying commingled remains and those specific to Cussac Cave, the search for virtual pair-matching, articular congruence, and osteometric sorting allowed the allocation of twelve bones to three individuals, one late adolescent and two adults.     

40 Years of Excavations at Mitoc–Malu Galben (Romania): Changing fieldwork methodologies and implications for the comparability of archaeological assemblages

Mitoc–Malu Galben (Romania) is one of the key-sites for the Upper Palaeolithic in Eastern Europe, with abundant Upper Palaeolithic archaeological layers embedded in a ∼14 meters long loess-palaeosol sequence. The excavations in 1978–1990 yielded rich remains of Aurignacian and Gravettian workshops. From 1992 to 1995, an international collaboration helped better define their stratigraphical position, age, and typological characteristics. Since 2013, our team has conducted new fieldwork focusing on interdisciplinary study of site formation processes and a detailed technological study of the lithic artefacts. These different excavation phases have employed quite substantially different fieldwork methodologies. Here, we explore the impact of the changing excavation methodologies on the comparability of the generated assemblages by analyzing the frequency of bladelets among the elongated blanks as well as the length distribution of elongated blanks. Our preliminary study allows us to suggest that some of the assemblages seem to be influenced by the fieldwork methodology employed by each excavation phase, but more studies are needed to start to understand how the assemblages are biased.     

Chronostratigraphy and the Palaeoenvironment of the Bistrița Valley. New Interpretations and a Critical Retrospective Evaluation

The Carpathian Arch was certainly a difficult obstacle for the Palaeolithic communities of Eastern and Central Europe, at least during certain stages of the Upper Pleistocene glaciation, such as the Last Glacial Maximum. The density and perennity of the Palaeolithic occupations in the Bistri?a Valley were favoured by the propitious conditions of living and developing long-term survival strategies. The importance of the Bistri?a Valley lies in the fact that it is strongly embedded in the mountainous landscape, with a route extended in the Sub-Carpathian area and a generous opening towards the east to the plateau region and further towards the Great Russian Plain. The Bistri?a Valley is a landmark of the Romanian Palaeolithic due to the number of investigated Palaeolithic settlements, the wealth and variety of archaeological materials and the extensive interdisciplinary studies. All this has entailed a better assessment of the evolution of the palaeoenvironment and of the chronostratigraphy of the Palaeolithic occupations. In a matter of speaking, the Bistri?a Valley is to Romania what the Vézère Valley is to the Dordogne region in France.     

Test excavations and initial results at the Middle and Upper Paleolithic sites of Gilvaran,Kaldar, Ghamari caves and Gar Arjene Rockshelter,Khorramabad Valley,western Iran

This paper introduces the excavations in several Paleolithic sites in the Khorramabad Valley, Western Iran. Apart from the two well-known sites of Ghamari Cave and Gar Arjene rock shelter, first excavated by Frank Hole and Kent Flannery in the 1960s, the Gilvaran and Kaldar caves were excavated for the first time. Here we present the stratigraphy of these sites, general data from the lithic assemblages, and the identifications of a small part of the faunal remains. Preliminary results are showing that all of the sites were occupied from the Middle and Upper Paleolithic onward, and therefore provide great potential for the study of the transition between these cultural periods. Our preliminary techno-typological observations show that the lower levels of the Gilvaran and Ghamari sequences may represent an early phase of the Middle Paleolithic.     

The paleobiology of two adult skeletons from Baousso da Torre (Bausu da Ture) (Liguria,Italy): Implications for Gravettian lifestyle

This article presents the main skeletal characteristics of the two largely unpublished Gravettian adult skeletons from Baousso da Torre (Liguria, Italy). BT1 and BT2 were two adult tall males, who died aged respectively between 20 and 50 years, and between 20 and 30 years. Their body proportions fall within the range of variation known for the middle Upper Paleolithic, and their skeletal remains are characterized by considerable osteometric values, which fall consistently in the upper part of the Upper Paleolithic male sample variation. They show a high degree of upper limb lateralization, implying that they were likely involved in strenuous and/or repetitive unimanual tasks. They also exhibit very robust lower limbs, likely related to repeated long-distance travels in mountainous terrains. These results are in total agreement with previous hypotheses on Late Pleistocene population behavioral patterns.     

Humanizing European Paleolithic art: A new visual evidence of human/bird interactions at L’Hort de la Boquera site (Margalef de Montsant,Tarragona, Spain)

This paper reports the discovery of a new example of portable art in North-eastern Iberia dating to the Late Upper Palaeolithic (12.250 ± 60 BP). The piece is analysed in relation to the European Palaeolithic art assemblage to determine its significance and how it contributes to our understandings of Palaeolithic artistic practices. Both the motifs depicted (birds and humans) and the patterns of composition (a narrative scene) are unusual in Palaeolithic assemblages. In addition, this new find contributes to filling a geographic gap in the artistic record as evidence of Palaeolithic art is rare in Catalonia. The anatomical features of one of the birds suggest that it is a crane, a species that has been depicted in a limited number of sites, as summarized in this paper. Moreover, there are only three known example of birds and humans interacting in a narrative scene in Palaeolithic art. Exhibiting innovations in media, subject matter and compositional norms, this new find has the potential to change the classic definition of European Upper Palaeolithic art and integrate the region in the artistic trends circulating along Mediterranean Iberia during the Upper Magdalenian.     

New advances on the Aurignacian in the central Iberian Mediterranean basin

This study aims to obtain a chronological and cultural framework of the Evolved Aurignacian in the central Iberian Mediterranean basin and find agreement between this framework and other sequences of the Iberian southeast. Over the last few years, there has been remarkable progress in the research of the Evolved Aurignacian sites in the Valencian area, making a review of the main characteristics of the technocomplex on a regional scale necessary. The recent fieldwork carried out in Cova de les Malladetes (Valencia) and in Cova de les Cendres (Alicante) have been key to understanding the lithic, osseous and ornament assemblages ascribed to the Evolved Aurignacian. Several Bayesian modelled ages have been constructed from the large dataset of chronological dates obtained at Malladetes and Cendres, as well as in other sites. The Bayesian models have allowed us to chronologically place the characteristics of the analysed assemblages. The present research supports the importance of the Aurignacian as the first technocomplex of the Upper Palaeolithic in this area of the Iberian Peninsula.     

The onset of Late Paleolithic in North China: An integrative review of the Shuidonggou site complex,China

Shuidonggou (SDG) attracts scholars who are interested in Late Paleolithic of China, even east Asia, from generation to generation since 1923 when rich lithic artifacts and animal fossils were discovered at locality 1. During the past almost one century, many excavations have been conducted by different institutes at different localities of SDG. Numerous data has been obtained and tens of thousands of artifacts were yielded. The understanding of nature and context of SDG is increasing gradually with the repeated excavation and in-depth research. The present paper reviewed the formal excavations and achievements in SDG. Especially, a series investigations and excavations since 2002 have been emphasized. After this long-term fieldwork, the geographic range of SDG has extended far beyond the range suggested by previous findings. The presence of discrete cultural horizons at various SDG localities indicate repeated use and occupation of the area by early human groups between 50–10 kya with a gap in LGM. During the repeated occupations, diverse and complex behaviors including gathering various plants, heat treatment preparation for knapping, making ornaments, engraving were identified using different kinds of methods and techniques by scholars. Paleoenvironmental reconstruction based on pollen analysis suggests that late Pleistocene/early Holocene human utilization of the SDG area occurred primarily around 32–24 kya and 13–11 kya when climatic conditions were more favorable. Years of excavations and researches make progress with nature of SDG. However, the issues about Initial Upper Paleolithic assemblages in SDG, origin/disappearance of Levallois-like technology in China are still open to debate. Further excavation and research at SDG1 will clarify these issues.     

Middle to Late Pleistocene herpetofauna from Scladina and Sous-Saint-Paul caves (Namur,Belgium)

For the first time, the fossil herpetofauna from the Middle and Late Pleistocene of Scladina and Sous-Saint-Paul caves (Sclayn, Belgium) is described. The amphibians and squamate reptiles are represented by one salamander (Salamandra salamandra), three anurans (Pelodytes punctatus, Bufo bufo and Rana temporaria), two lizards (Lacerta cf. agilis and Anguis fragilis) and two snakes (Zamenis longissimus and Vipera cf. berus). The occurrence of the Parsley Frog (Pelodytes punctatus) and the Aesculapian Snake (Zamenis longissimus), which are not currently represented in Belgium, is of particular interest. Scladina also represents one of the northernmost fossil mentions for the Fire Salamander (Salamandra salamandra) although it is within its current distribution in Europe. Finally, the presence of the Adder (Vipera cf. berus) is very probably attested in Scladina whereas today this snake is infrequent and classified as endangered in Belgium.     

Fauna,environment and human presence during MIS5 in the North of Spain: The new site of Valdavara 3

Valdavara 3 is a new early late Pleistocene paleontological and archeological cave site in northwestern Iberia. Over 1400 fossils have been collected, representing about 40 species. The fauna is of interglacial aspect and is in accordance with the OSL dates from the fossiliferous layer, which indicate an age of 103–113 ka. The great taxonomical diversity indicates a varied landscape. A small collection of lithic artifacts was found associated with the fossils, demostrating presence of humans and suggesting short non-residential visits to the cave. The fossiliferous site was predominantly formed by natural processes. Many fossil localities have short or biased faunal lists, but the fossil fauna recovered from Valdavara 3 is remarkably diverse and may reflect the fauna which once lived there.     

Palaeoenvironment and palaeoclimate in the western Liguria region (northwestern Italy) during the Last Glacial. The small mammal sequence of Riparo Mochi (Balzi Rossi,Ventimiglia)

Riparo Mochi is considered a key site for the Middle–Upper Palaeolithic chrono-cultural sequence in the Mediterranean area. Climatic and environmental conditions have been reconstructed after the study of the small mammal assemblage by means of linear regression method and the Habitat Weighting method. The climate proxies for the late Mousterian and Proto-Aurignacian (cultural units I to G) indicate an environment with a relative high percentage of forest component during two cold and one relative warm oscillations. Open environments with low temperatures are registered for the Gravettian (cultural Unit D) allowing a possible relation to the Heinrich 3 Event. The final Gravettian (cultural Unit C) shows a relative warm peak, tentatively related to Greenland Interstadial 2. The late Epigravettian (cultural Unit A) is characterized by a high percentage of forest-related environment suggesting that this horizon formed during the Bølling–Allerød Interstadial. Finally, the Riparo Mochi sequence contributes to reconstruct the processes of faunal changes along the northern Tyrrhenian coast in a period of climatic instability, especially during the end of Marine Isotope Stage 3 when foraging groups adopted different mobility strategies between southern France and the Italian peninsula.