Upper Paleolithic Rock Crystal Artifacts from the Southeastern Shore of Lake Bolshiye Allaki,the Southern Urals

Artifacts from the second cultural horizon of Bolshiye Allaki-2 are described, and data on the topography and stratigraphy of the site are examined. Results of technological, typological, petrographic, and faunal analyses along with radiocarbon dates suggest that this may be the earliest Upper Paleolithic ritual site in the Urals.     

Small shifts in handedness bias during the Early Mesolithic? A reconstruction inferred from Microburin technology in the eastern Italian Alps

This study discusses the existence of a variability recorded in lateralization indexes of proximal microburins, a by-product of the individual manufacture of microliths, in a sample of Sauveterrian sites from the Italian Eastern Alps. At first glance, such variability may appear to support the existence of customary handling, pertaining perhaps to an ensemble of normalized technical procedures accomplished by the members of the human group regardless of site type, context and economic activities. However, plotting the patterns in lateralization index against the regional Sauveterrian chrono-cultural sequence reveals a diverse correlation emerges and indicates how the early settlement phase involved greater functional differentiation among sites used by selected human groups compared with the successive phases, when this pattern vanishes. This trend may correspond to the decrease in lateralization observed on skeletal markers from the Upper Paleolithic to the Mesolithic, linked to the change in technological models and techniques employed in food gathering. The implications of this research at different levels are also discussed.     

Chert sources and distribution patterns in the stone age of West Finnmark,North Norway: A preliminary view

A preliminary analysis of chert sources and distribution patterns in west Finnmark is described. Three small quarries and a fourth possible source area are situated on the coast west of Alta. Petrographic and geochemical analyses lend tentative support to the proposition that chert from these coastal sources was distributed inland during the Late Stone Age and Early Metal Periods.     

History,Chronology and Techno-Typology of the Upper Paleolithic Sequence in the Shuidonggou Area,Northern China

The timing and behavioral markers of the Upper Paleolithic in different parts of the world are of great importance to research on modern human dispersals. The pattern of behavioral developments in the Upper Paleolithic in northern China differs in important ways from the patterns observed in West Eurasia, Africa, and South Asia. Shuidonggou (SDG), a cluster of Paleolithic sites in northern China, contains several of the most important Upper Paleolithic sites in the region. Various localities yield evidence of three major cultural components dated by ¹⁴C, uranium-series, and optically stimulated luminescence (OSL) methods to between roughly 46 ka and 10 ka. The oldest component, blade assemblages with western Eurasian early Upper Paleolithic characteristics, appears to be intrusive from Siberia and/or Mongolia, beginning at least 41 ka (e.g., SDG 1 and SDG 9). Advanced core and flake assemblages may mark the appearance of an indigenous Late Paleolithic of North China beginning at around 33 ka (e.g., SDG 2 and SDG 8). Finally, around 10.5 ka, microblade technology arrived in the area (SDG 12), although we are not sure of its origins at present. Other typical Upper Paleolithic cultural remains, such as bone tools and body decorations, have been found at various localities in the SDG area as well (e.g., ostrich eggshell beads from SDG 2, 7, and 8). Information from this cluster of occupations increases our understanding of cultural variability, adaptation, and demographic dynamics of modern humans in Late Pleistocene northern Asia.

     

First Geochemical ‘Fingerprinting’ of Balkan and Prut Flint from Palaeolithic Romania: Potentials,Limitations and Future Directions

Long‐distance raw material transfers across Romania prior to the Last Glacial Maximum have previously been inferred from either visual and/or petrographic observations of East Carpathian sites. We investigated the potential to ‘fingerprint’ flint from archaeological sites at Mitoc‐Malu Galben and Bistricioara–Lut?rie III in Eastern Romania, using in situ high‐precision analyses of 28 major, minor and trace elements determined by laser ablation – inductively coupled plasma – mass spectrometry (LA–ICP–MS) in combination with multivariate statistical analysis. Our results suggest that geochemical analyses have the ability to distinguish between different geographical sources but are unable to positively associate flint artefacts from archaeological contexts to these geochemical groups. The mismatches of signatures between artefacts and geological materials, however, raise new questions and open unforeseen perspectives.     

The Upper Paleolithic of Northern Asia: Achievements,problems, and perspectives. II. Central and Eastern Siberia

Earlier scholars believed that the Upper Paleolithic of Central and Eastern Siberia appeared very late. However, modern research has shown that not only was there a local Middle Paleolithic, but also there was a very early series of sites in Central Siberia which show both Middle and early Upper Paleolithic traits. These are called the Makarovo horizon and may be 70,000–50,000 years old; features derived from this horizon can be dated to about 30,000 B.P. and can be seen in the early D'uktai culture. The true early Upper Paleolithic is relatively homogeneous in Central and Eastern Siberia and includes artwork. The local Upper Paleolithic reached its florescence in the culture of Mal'ta and Bur'et', which developed out of local antecedents and which is here reinterpreted in light of recent research (including the artwork, structures, and burials). The final stages of the Upper Paleolithic show considerable variability, perhaps including some exotic traits.     

Typological Classification,Attribute Analysis,and Lithic Variability

Abstract

A typological research strategy can distort the analysis of Upper Paleolithic stone tools because it is ill-equipped to distinguish stylistic and functional similarity. This lack can make the significance of formal stone tool types in either culture-historical or behavioral analysis ambiguous. “Attribute analysis,” as it is being developed with French Upper Paleolithic materials, is introduced as an alternative strategy. The stylistic and functional analysis of burins in three Upper Paleolithic cultures, the Perigordian VI, the Proto-Magdalenian , and the Magdalenian II-III, is presented as an example indicating the advantages of one approach over the other.     

New Archaeological Books and Journals

Abstract

As part of a research program aimed at clarifying the date of the Middle Paleolithic in Greece and its relationship with contemporary industries in the Balkans, a survey of the Larisa area of Thessaly for Paleolithic remains was undertaken in 1987. The results of this survey are reported, along with a reinterpretation of the available evidence in Greece for the date of the Middle Paleolithic. The banks and terrace system of the Peneios River were systematically searched along with those parts of Thessaly with deposits old enough to contain prehistoric artifacts. In 1987, we discovered 32 find spots and collected211 lithic artifacts. The lithic artifacts are Middle and Upper Paleolithic types, and are dated by their association with the fluviatile deposits exposed by downcutting of the river. Radiometric dates for the fluviatile deposits indicate an age of 45–27 KYA (thousands of years ago) for the Paleolithic finds. Other dates for the Middle Paleolithic in Greece are on the same order. The Thessalian Paleolithic industry is a Levallois-Mousterian facies with bifacial leafpoints, side Scrapers, Mousterian points, denticulates, andAurignacian-type end scrapers, burins, retouched Blades, and bifacial leafpoints with rounded bases. The Thessalian industry with its mixture of Middle and Upper Paleolithic types, is similar to other assemblages in Greece. The Greek Levallois-Mousterian resembles the Szeletian of Hungary and is of approximately the same age. It was perhaps produced by late Neanderthals in contact with an anatomically-modern human population. Late Upper Paleolithic Epigravettian and Mesolithic industries were not identified in Thessaly and are rare in Greece. Some areas may have been uninhabited or little used until 9 KYA when the first Neolithic settlements appear in Thessaly.     

THE PROBLEMS WITH VISUAL IDENTIFICATION OF DOVER AND FORT PAYNE CHERT

Abstract

Similar characteristics including color, luster, texture, and mineral inclusions of both Dover and Fort Payne chert types coupled with the wide geologic and geographic distribution of these deposits compound interobserver errors associated with visual identification methods. Samples were obtained from outcrops of Dover from Kentucky and Tennessee and Fort Payne chert from Alabama, Georgia, Illinois, Kentucky, Mississippi, and Tennessee demonstrating their extensive geologic distribution as well as the great similarity in macroscopic traits. A logistic regression analysis upon the sample database demonstrates successful differentiation of the chert types. However, the Dover/Fort Payne case study provides a cautionary example of the potential pitfalls with sourcing studies solely reliant upon visual attributes to assign artifact provenance. In general, the use of visual chert identification should be a “first approximation” and it is argued here that large type databases systematically sampled from both primary and secondary sources highlight the possible wide range of macroscopic variation present.     

THE ORIGIN AND GEOCHEMICAL CHARACTERIZATION OF RED OCHRES FROM THE TITO BUSTILLO AND MONTE CASTILLO CAVES (NORTHERN SPAIN)*

Ochres were the most common source materials for pigments used in Palaeolithic rock art paintings. This work analyses the petrographic and geochemical signatures of different ochre samples from outcrops inside Tito Bustillo Cave and the Monte Castillo Caves using the most common techniques (petrography, XRD, SEM–EDS and ICP–MS) in archaeological pigment characterization studies. The results obtained permit the identification and characterization of the different source ochre types and, furthermore, allow the establishment of mineralogical and geochemical proxies for the study of questions related to ochre characterization, formation processes and provenance.     

The chert from the Castelltallat Formation (south-central Pyrenees): archaeometric characterisation and archaeological implications

Chert from the limestones and marly limestones of Castelltallat Formation (Ebro Basin) was widely used throughout prehistoric times in north-eastern Iberia to produce stone tools due to its properties and accessibility. A rough estimate indicates that this rock—either as raw material or as lithic products—was distributed mainly to the north of the outcrops, over an area of 6000–8000 km². However, other rocks in the area have similar characteristics which can lead to confusion in the interpretation of its prehistoric use and distribution. In order to establish useful archaeometric criteria for differentiating this chert from other similar, the Castelltallat chert is characterised in petrographic, mineralogical and geochemical terms. The chert nodules are found to be homogenous at the macroscopic and microscopic level, with a significant presence of bioclasts, thus indicating they might be formed in a freshwater lake environment by the early diagenetic replacement of carbonates in shallow waters. The mineralogical composition is homogeneously uniform and of a flint type, characterised by an almost exclusive predominance of quartz, without any opaline phases, and a variable proportion of moganite. The iron oxide content is very low, whereas its chemical composition is unusually high in uranium which correlates positively with carbonate content and negatively with silica. Archaeometrical parameters are provided to reach a proper identification of tools knapped with this chert. This way, chert from Castelltallat Formation turns out to be a valuable lithological marker to evaluate the range of mobility of the human groups who lived in the north-eastern Iberia and their contacts with neighbouring areas.     

The chert abundance ratio (CAR): a new parameter for interpreting Palaeolithic raw material procurement

Raw material provenance and procurement studies are an essential research line to infer landscape exploitation, mobility dynamics and territorial management among prehistoric hunter-gatherer groups. This paper proposes an original and intuitive method, the chert abundance ratio, aimed at quantifying lithic resource occurrence in the landscape while considering the geological natural factors of an area (chert-bearing formation extent, thickness, occurrence index, size and chert content). The resource availability can be statistically compared to any archaeological assemblage distribution to define the procurement strategies, whether generalist or selective, and the mobility patterns. The study area, the north-east of the Iberian Peninsula, focused in the Prades Mountains, represents a regional scenario with high chert disposal shared by several Late Upper Palaeolithic occupations. The discrimination of the procurement areas is used as a parameter for outlining the foraging radius and the territorial range, contributing to an understanding of several aspects of the settlement, such as site functions, occupation length or intensity and group size.     

Assessing XRF for the geochemical characterization of radiolarian chert artifacts from northeastern North America

The purpose of this paper is to emphasize the benefits of adopting non-destructive energy dispersive X-ray fluorescence (ED-XRF) as a first-order technique to determine chert whole-rock geochemistry for archaeological sourcing. Chemical signatures for the Touladi and La Martre prehistoric quarries from the lower St. Lawrence and Gaspé Peninsula region of Quebec, Canada, are determined and serve as references to test the provenance of regional chert artifacts. Chert experimental flakes, created from quarry geological hand samples, are analyzed and used to validate the method. Archaeological flakes and tools recovered from three archaeological sites are analyzed and tested against quarry samples. Geochemical diagrams and Principal Component Analysis are used to establish artifact-quarry relationships. The effects of surface weathering on the geochemical analysis of archaeological chert artifacts are presented. Sample restoration and research avenues are discussed and proposed to further enhance the robustness of future chert geochemical data sets.     

Petrographic and Geochemical Investigations on the Pottery Production from Arslantepe–Malatya (Eastern Anatolia) from the Fourth to the Second Millennium BCE: Technological Continuity,Innovation and Cultural Change

The petrographic and geochemical analyses of 130 Late Chalcolithic 3 (LC3, 3800 bce ) to Early Bronze Age IIIB (EBAIIIB, 2000 bce ) ceramics from Arslantepe and the Malatya Plain in the Eastern Anatolian Upper Euphrates have identified critical differences in raw material procurement and paste preparation, reflecting typological, chronological and cultural changes. Based on these differences, distinct modes of production that correspond to phases reflecting significant social, economic and political changes were recognized. In particular, the interruption of the centralization process and the establishment of mobile groups during EBAI (3000–2900 bce ) were accompanied by the exploitation of new sources.     

Three Scenarios Of The Middle To Upper Paleolithic Transition The Middle to Upper Paleolithic Transition in Africa and the Early Peopling of Eurasia by Anatomically Modern Humans

Previous papers of this cycle describe the Middle to Upper Paleolithic transition in Eurasia and in the Sino-Malayan zone. Archaeological evidence from Africa however, suggests a completely different model of the transition. Despite the variability of Paleolithic industries in Africa, the maintenance of the Middle Paleolithic strategy of core reduction constitutes a common trend. The transitional industries in North and East Africa are characterized by Aterian points and backed geometric implements.     

Early Upper Paleolithic industries of Eastern Europe

Early Upper Paleolithic sites are known in various parts of Eastern Europe, but the two main concentrations of them are the Prut-Dniester basin and the middle Don. The flint industries are divided into archaeological cultures (cultural traditions), of which some show clear archaic features (Kostenki-Streletsian, Gorodtsovian, Brynzenian, etc.), while others have no Mousteroid characteristics (Spitsynian, Telmanian, etc.). Both types of culture coexisted throughout the Early Upper Paleolithic. In some cases, it is possible to trace genetic links between archaeological cultures and to follow the transition between the Middle and the Upper Paleolithic. The radiocarbon age of the oldest Upper Paleolithic sites in the Russian Plain is about 40,000 B.P., but some sites may be older. The Early Upper Paleolithic ended about 24,000–23,000 B.P. In the Crimea, the Middle-Upper Paleolithic transition appears to have taken place at about 20,000–18,000 B.P.     

Temporal nature and recycling of Upper Paleolithic artifacts: the burned tools from the Molí del Salt site (Vimbodí i Poblet,northeastern Spain)

Recent research in Paleolithic archeology has stressed the importance of temporal issues in assemblage interpretation. Archeological assemblages are temporal constructs, formed by the addition of an unknown number of depositional events. This temporal dimension is also evident at the artifactual level, since single artifacts may undergo different events of modification and/or uses over time. The recycling of previously discarded blanks for tool production is one of the best examples of the temporal nature of artifacts. The aim of this paper is to evaluate the importance of recycling in a Late Upper Paleolithic site, examining a type of artifact – burned tools – that has up to now been little used to approach this issue. Our results suggest that recycling was probably a significant component of Upper Paleolithic provisioning behavior, with important implications in site formation processes and the typological variability of assemblages. The expedient or curated character of recycling is also discussed.     

The Middle-Upper Paleolithic transition in Southeastern Central Europe (Czechoslovakia and Hungary)

Southeastern Central Europe is quite rich in finds of progressive Neandertals from Middle Paleolithic contexts and early modern humans associated with evolved Upper Paleolithic (Aurignacian and Pavlovian). There are no human fossils that can be related to the transitional Middle-Upper Paleolithic units (the Bohunician and the Szeletian); thus, from anthropology we know only that the transitional period began with Neandertals and ended with modern humans. The archaeological record is more complex. The Jankovichian industries of Hungary differ from the mostly non-Levallois Middle Paleolithic of Central Europe in the presence of some Levallois; they seem to be technologically related to the Levallois-Leptolithic Bohunician industries of Moravia, dated to 43,000–38,000 B.P., which are the first transitional Upper Paleolithic unit. The appearance of the Szeletian before 42,000 B.P. in Hungary and at about 39,000 in Moravia represents a technological variation of the transition, although retaining marked local Middle Paleolithic elements. The date of the appearance of the typical Aurignacian, the first culture clearly related to modern humans, is unclear, but it certainly developed after 36,000 B.P. and has several dates between 35,000 and 30,000 B.P.     

Levantine Perspectives on the Middle to Upper Paleolithic “Transition”

This article presents a synthesis of the presently available data concerning the processes and meaning of the technical changes in lithic productions across the Middle Paleolithic/Upper Paleolithic boundary in the Levant. As a “corridor” between Africa and Eurasia, this area is of first importance in the discussion of Modern Human origins. The results of several new field projects (especially concerning the Initial Upper Paleolithic), the recent lithic technological studies (based on the chaîne opératoire concept) as well as radiometric dating were used here to discuss the rhythms and processes of technical changes at the onset of the Upper Paleolithic, examining carefully the lithic repertoire from the Late Middle Paleolithic through the Initial Upper Paleolithic from Lebanon, Syria, Turkey, and Israel. This paper puts forward the idea that the emergence of Upper Paleolithic technical characteristics did not occur following a single process, even in the same region (here the Levant), but most probably followed a “mosaic” pattern. However taking into account the data presently available, the main basic scenario for the onset of the Upper Paleolithic in this region would have been the generalization of new technical traits that would have emerged within certain local Late Middle Paleolithic and the following Initial Upper Paleolithic groups. If a diffusion phenomenon should be considered, as claimed by many scholars, the available information suggests that it has functioned more as a stimulus rather than the simplistic scenario of a catastrophic wave of population and the resulting acculturation.