ISLANDSCAPES AND 'ISLANDNESS': THE PREHISTORIC ISLE OF MAN IN THE IRISH SEASCAPE

Summary.   This paper will explore the role of the Isle of Man in the prehistory of the Irish Sea area through an examination of its changing islandscape from the Neolithic through the Iron Age. It was far from insular during prehistory, but the social and economic interactions of prehistoric Manx people around the Irish Sea and beyond were heavily affected by their water-bound environment. The way that the prehistoric Manx perceived their boundaries and their coastal situation is reflected in their ritual and social landscape, their preferential use of coastal areas for monumental architecture, and in the choices they made with regard to the island landscape they inhabited. This culturally constructed sense of islandness allowed the prehistoric Manx people to maintain distinctive local cultures while still playing an active role in the larger Irish Sea region.     

MINERALOGICAL ANALYSES OF CERAMIC MATERIALS FROM QUINUA,DEPARTMENT OF AYACUCHO,PERU

Mineralogical analyses of clays, tempers and paints from contemporary sources in the vicinity of Quinua, Peru, were carried out by means of X-ray diffraction, microscopic examination and physical separation. The data indicates that (1) there is a substantial amount of mineralogical variability in these materials, (2) the differences between the clays and tempers consist of the differences between the relative amounts of plastics and non-plastics present in each of these kinds of materials, (3) the paints contain a mineral known for its superior spreading qualities. The study concludes that (1) the region had the ceramic resources to support a tradition of several polychrome styles like those made during the Peruvian Middle Horizon (a.d. 600–800), (2) ancient pastes made in the region had a great deal of mineralogical variability, (3) archaeologists should redefine their notion of ‘temper’, and (4) modern mineralogical differences between pastes tempered by the potter and those not tempered by the potter can also apply to ancient pastes of the region.     

Selected with care? – the technology of crucibles in late prehistoric Scotland. A petrographic and chemical assessment

Prehistoric crucibles and other metalworking ceramics are often described as highly specialised tools made from refractory materials, but little is known about regional trajectories and individual material developments. Hence, further analyses of materials from less studied regions are needed. The current study investigates the technological development of crucibles from late prehistoric Scotland and its relation to technological choices and specialisation. The examination, using ceramic petrography and Energy Dispersive X-Ray Spectroscopy, focuses on the selection of clays and additives for the manufacture of crucibles in contrast to moulds and pottery. It is demonstrated that the production of crucibles in the late prehistoric period predominantly used local resources. Late Bronze Age crucibles have a close relationship with other types of technical and domestic ceramics, while materials in the Iron Age indicate an increased material specialisation for the preparation of particular fabrics. This development is seen across Scotland and echoes trends seen in other areas of Europe, emphasising the role and importance of metallurgical and technological networks.     

PLAIN POTTERY AND SOCIAL LANDSCAPES: REINTERPRETING THE SIGNIFICANCE OF CERAMIC PROVENANCE IN THE NEOLITHIC

This paper focuses on plain, stylistically unvaried pottery from three Late Neolithic sites from the Mondego Plateau, Portugal, and investigates ceramic production and exchange among small‐scale prehistoric societies by means of thin‐section petrography and chemical analysis (INAA). The results show that the majority of the pottery was made with widely available, granite‐derived sedimentary clays, but petrographic differences between fabrics indicate collection at multiple locations within these deposits. Variation in chemical composition is consistent with site‐specific sourcing areas, while comparison with data from earlier sites in the Mondego and surrounding mountains suggests that such sources were geographically restricted within the plateau. In contrast, the small percentage of vessels produced with residual clays of metamorphic and intermediate igneous origin, which outcrop over 10 km and 30 km from the archaeological sites, demonstrates that plain pottery did circulate during the Neolithic beyond the funerary sphere. This is the product of the routines of mobility and social networks of Neolithic groups across the wider landscape, which involved the exchange of ‘mundane’ vessels. Finally, the study demonstrates that micro‐regional provenance studies can provide significant insights into prehistoric social landscapes if the data are interrogated beyond simplistic classifications of local and non‐local.     

Selinunte (Sicily) and its productive context: the clayey raw materials applied in a long-lived ceramic production (seventh to third century BCE)

The westernmost of the Greek-Sicilian towns, Selinunte, founded in western Sicily during the second half of the seventh century BCE, gives amazing evidences of a historic activity of ceramic production (seventh to third century BCE). The present study aims to identify the raw materials available in the vicinity of the archaeological site of Selinunte, which were possibly used by the ancient potters, and to characterise them by means of petrographic and chemical techniques. A sampling campaign of clays and sands for tempering was undertaken in the archaeological site and the adjacent area. Moreover, locally produced archaeological bricks and tiles were considered helpful for comparison regarding the definition of local ceramic macro- and micro-fabrics and were analysed as well. The comparison between textural, mineralogical and chemical data allowed us to highlight a good similarity between the clayey materials available in the area and the local ancient bricks and tiles. Their compositional resemblance suggests the hypothesis of a systematic use of the studied clays for ceramic productions from the Archaic to the Hellenistic period. The preliminary archaeometric results obtained so far could enhance the distinction between local manufactures and imports and may well lead to the identification of ceramic artefacts produced by the Archaic-Hellenistic workshops of Selinunte at various consumption sites.     

CHARACTERIZATION AND THERMOLUMINESCENCE DATING OF PREHISTORIC POTTERY SHERDS FROM MILENA

This paper reports the results obtained applying absolute dating methodologies and mineralogical, petrographical and micropalaeontological characterization techniques to prehistoric pottery sherds varying in age from the Sicilian Middle Neolithic to Bronze Age. All samples came from the archaeological area of Milena (Caltanissetta, Sicily); those of the Bronze Age were found on a site with a precise stratigraphic succession. The investigation has contributed to the determination of an absolute chronology for the Milena prehistoric period. The data provide, for the first time in Sicily, absolute dates covering a wide spectrum of cultures following one another in the same area and, for the Bronze Age site, correlated to the precise stratigraphic succession. The petrographical and mineralogical analyses allowed not only the identification of the principal constituents of the pottery, but also the formulation of some hypotheses regarding the specific manufacturing techniques of different epochs. The microfacies, obtained from the presence of fossils in the groundmass of the pottery, were also analysed and compared with the microfauna present in the Miocene clays outcropping in the area. The data identified local Messinian clay as the raw material probably used in the manufacture of the pottery and also support the presence, already assumed by archaeologists, of imported Mycenaean pottery, thus supporting the dates obtained on pottery taken from the same stratum.     

ELECTRON PROBE MICROANALYSIS OF MIXED-ALKALI GLASSES

European mixed-alkali glasses are compared with Sayre and Smith's categorisation for ancient glass and with the chemical compositions of other prehistoric and later European glasses. The new categories reported here indicate that a wide range of alkali raw materials was used in the production of glasses found in prehistoric European contexts. At least five major chemical categories of glass are now known to have been used in prehistoric and early Roman Europe. A plant species of the genus Sulicorniu is suggested as a possible alkali source in ancient European glasses.     

Raw Material and Technological Changes in Ceramic Productions at Sai Island,Northern Sudan,from the Seventh to the Third Millennium BC

This study presents the results of integrated mineralogical, petrographic and chemical analyses of different ceramic assemblages and local sediments from Sai Island, northern Sudan, dating to between the seventh and the third millennium bc , and highlights a significant variability in the raw materials and technology of these productions. Although archaeometric analyses of ceramics are widely employed in many parts of the world, a lamentable scientific gap exists for African pottery, which this paper aims to bridge with new and compelling results.     

Minero-petrographic characterization of fine ware from Cales (South Italy)

79 samples of black glazed pottery, Terra sigillata, fine common ware, and production indicators were recovered in the archaeological site of Cales and investigated via a multi-analytical program (polarized light microscopy, thermal analyses, XRPD, XRF, FESEM, FESEM-EDS). Among the materials, finds of important production indicators, represented by welded pieces of black glazed pottery and spacers, attest a local production. Polarized light microscopy shows that the inclusions consist of feldspar, quartz, mica, calcite, and lithic fragments of both volcanic and sedimentary nature. Additional information about the mineralogical assemblage comes from the XRPD that revealed the presence of neoformed Ca-silicates, indicating equivalent firing temperatures ranging from 750 to 1050°C. All the samples show a Ca-rich character and an extreme compositional homogeneity, including the production indicators. The comparison with some Ca-rich Campanian clay raw materials shows a greater affinity with the Mio-Pliocene marine clay sediments of the Apennine sector, which include local clays. This allowed us to formulate the first hypotheses about clay sources used to produce fine pottery during the third century BCE to the early imperial period in Cales.     

A Palaeoenvironmental Investigation of Sediments from the Prehistoric Mine of Copa Hill,Cwmystwyth, mid-Wales

This paper investigates the use of mine sediments to reconstruct the vegetational changes and atmospheric pollution history associated with prehistoric and Mediaeval metal mining in the Ystwyth valley, Dyfed, mid-Wales. Pollen, charcoal, plant macrofossils, fossil insects and chemical analyses are presented from radiocarbon-dated sediments contained within a prehistoric mine situated on the upper slope of Copa Hill, close to the village of Cwmystwyth. The results provide additional support to the hypothesis that prehistoric mining had a negligible impact on woodland and that deforestation took place after Bronze Age mining ceased. Although high concentrations of Cu, Pb and Zn were determined from sediments of prehistoric and Roman Age, the patterns bear little resemblance to off site atmospheric pollution records and to the archaeological evidence for metal mining. Interpreting geochemical data from mine contexts is problematic as numerous factors influence the distribution and concentration of metals. However, an on-site and off-site approach to investigate human-environment interactions caused by metal mining is advocated.     

Integrating human dimensions of Arctic palaeoenvironmental science: SEAD – the strategic environmental archaeology database

Environmental change has a human dimension, and has had so for at least the last 10 000 years. The prehistoric impact of people on the Arctic landscape has occasionally left visible traces, such as house and field structures. More often than not, however, the only evidence available is at the microscopic or geochemical level, such as fossil insect and seed assemblages or changes in the physical and chemical properties of soils and sediments. These records are the subject of SEAD, a multidisciplinary database and software project currently underway at Umeå University, Sweden, which aims to create an online database and set of tools for investigating these traces, as part of an international research infrastructure for palaeoecology and environmental archaeology.     

A characterisation study of Ubaid period ceramics from As-Sabbiya,Kuwait, using a non-destructive portable X-Ray fluorescence (pXRF) spectrometer and petrographic analyses

The Ubaid cultural phenomena (6500–4200 BC) of southern Mesopotamia has been used to characterise other archaeological sites in the Arabian Gulf region. The aim of this inquiry is to explore the nature of the interaction between the homeland of the Ubaid and the wider Gulf region. Through the use of a non-destructive portable X-ray fluorescence (pXRF) spectrometer, this study seeks to characterise and identify the chemical and mineralogical compositions of the ceramic assemblage from the Bahra 1 site of the As-Sabbiya region, Kuwait. The chemical results demonstrated that a combination of six trace elements [rubidium (Rb), strontium (Sr), yttrium (Y), zirconium (Zr), niobium (Nb) and barium (Ba)] occur significantly enough to delineate clay-based artifact groups—local red coarse from Ubaid, while the mineralogical analysis confirms the pXRF result and identifies the source of the raw materials and temper as well. Also, the comparison between the Ubaid and Bronze Age assemblage results suggests that potters used different clay resources within their own regions and/or production techniques.     

ASSESSING NATURAL CLAY COMPOSITION IN THE VALLEY OF OAXACA AS A BASIS FOR CERAMIC PROVENANCE STUDIES

The Oaxaca Clay Survey was initiated to provide baseline data on clay composition within the Valley of Oaxaca, Mexico, to assist in provenance determination of prehistoric ceramics. Natural clays were sampled from 135 locations throughout the valley, and analysed using INAA in combination with ceramic petrography. Observed geographical trends in trace‐element and mineralogical composition confirm that while parent material (surficial geology) strongly affects clay composition, a continuum of variation exists within the valley. The study develops and tests a continuous spatial model of clay composition that provides greater resolution in ceramic sourcing than bedrock alone. By establishing a regional framework for Oaxaca Valley clays, the survey will support significant advances in our understanding of pottery production and exchange within the valley, and provide a more robust means for monitoring exchange between the valley and neighbouring regions.     

APPROACHING THE LANDSCAPE DIMENSION OF THE MEGALITHIC PHENOMENON IN SOUTHERN SPAIN

Although the megalithic phenomenon in southern Iberia has received attention since the mid‐nineteenth century, there has been very little attention paid to the role that megalithic structures played in the organization of prehistoric landscapes. Just as in other areas of Europe, however, southern Iberian megalithic structures must have played complex roles in the social organization of landscapes that go far beyond their use as funerary containers. Using examples from our work in southern Iberia, we employ GIS‐based spatial analysis to explore for the first time various aspects of the landscape dimension of these monuments. We discuss three case‐studies for which fresh field data have been recently made available. In the first (Almadén de la Plata) we find patterns of association between medieval transhumance routes and megaliths, and we use cost‐surface modelling to suggest that medieval routes may reflect earlier, prehistoric patterns of movement which in turn suggest that megalithic structures functioned in this area as waypoints within an emerging mobility system for people and livestock. In the second case (Aroche) we show correlations between the locations of megaliths and theoretical territories defined by isochrones and contrast this pattern with the distribution of non‐megalithic funerary sites of the Early Bronze Age, concluding that the spatial distribution of megaliths in this region may relate to their role as landmarks. Lastly we describe a far more specific relationship which we have encountered in the Antequera region, where we believe we have identified a relationship between the orientation of the megalithic structure of Menga, a prominent natural feature and several newly discovered prehistoric sites. Together, these three examples suggest that the current focus on typology, chronology and contents in the study of Iberian megaliths needs to be matched with efforts to identify and interpret the often highly complex structure of the prehistoric landscapes of which they form an integral part.     

Diatoms as indicators of provenance in Finnish sub-neolithic pottery

The clays of Finland originated from glacial deposits formed during the deglaciation of the Weichselian ice-sheet and during the different stages of the Baltic Sea. The analysis of the fossil diatom flora is of central importance in the study of its developmental history. The diatoms in the clay indicate its sedimentary environment, which can be linked to the stages of the Baltic Sea. The siliceous valves of diatoms tolerate heating up to 1400°C and can consequently be identified in ceramics fired at lower temperatures. Several diatom analyses have been made in Finnish Sub-Neolithic comb ware pottery in order to determinate the origin of their clay materials. According to the results of these studies, prehistoric potteries used clays deposited during the Yoldia and the Ancylus stages. The criteria used in selecting raw materials were identical to those of modern ceramic industries. Further details as to provenance of clay materials have been illustrated in connection with research on pottery from the Aland Islands. In the example from Kymi, South-eastern Finland, changes in the composition of the diatom flora have been found to correlate with changes in pottery decoration styles.     

马家浜文化晚期陶鼎的兴起及其影响

环太湖地区马家浜文化晚期,形态各异的陶鼎开始兴起。各个类型陶鼎在时空分布、创制机理和发展过程等方面都存在着明显的不同,与本地区固有的以釜为主的炊器传统有着亲疏程度上的显著差异。不同制鼎传统之间彼此影响,关系错综复杂,一度形成了多个本土和外来传统并立的局面。厘清这些陶鼎类型的源流谱系,对于明确其后续影响,乃至阐释整个环太湖地区史前陶鼎传统的形成问题,都具有重要意义。     

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.     

What is on the craftsmen’s menu? Plant consumption at Datrana,a 5000-year-old lithic blade workshop in North Gujarat,India

The exploitation of lithic resources was an important aspect of prehistoric resource exploitation strategies and adaptation. Research has mostly focused on technological and spatial aspects of lithic factory sites, often overlooking how these sites were integrated within local socioecological dynamics in terms of food acquisition and consumption. The aim of this paper is to study plant consumption at Datrana, a 5000-year-old lithic blade workshop in North Gujarat, India, in order to understand its occupants’ subsistence strategies. The results of archaeobotanical, mineralogical and soil pH analyses show that the occupants of this factory site were consuming local crops but not processing them, suggesting that either (a) food was being processed in other areas of the site or (b) it was acquired in a ‘ready-to-consume’ state from local food-producing communities. This study highlights the integration of a lithic factory site within its surrounding cultural and natural landscape, offering an example of how the inhabitants of a workshop interacted with local communities to acquire food resources.     

Geoarchaeology and Archaeological Site Patterning on the Middle Gila River,Arizona

Abstract

Archaeological surveys and prehistoric settlement patterns are best interpreted when placed on a geomorphic map that defines the distribution and age of physical landforms. Survey data can thus be used to address questions of archaeological site visibility and synchronic and diachronic site patterning on the Gila River Indian Reservation, Arizona. A chronological series of alluvial and eolian landforms are defined on the reservation. The age of the landforms and underlying sediments has affected the preservation and visibility of the archaeological record. Further, late prehistoric Hohokam settlements (A.D. 700–1500) and their associated agricultural lands show a clear landform zonation and that the intensity of use of these landforms has changed over time.     

Another (mud)brick in the wall: scientific analysis of Bronze Age earthen construction materials from East Crete

Mudbricks appear to have been one of the most common building materials used in domestic architecture in Bronze Age Crete. Well-preserved earthen construction materials from the sites of Vasiliki, Makrygialos and Mochlos in East Crete have been examined with regard to their macromorphological characteristics and their mineralogical and chemical composition in order to investigate the nature of the raw materials used, the technology of manufacture and the potential use of specific recipes. The methods applied include a combination of mineralogical and chemical analytical techniques, namely petrography, neutron activation (NAA), X-ray fluorescence (XRF), and X-ray diffraction (XRD) analysis. Finally, a range of raw materials from the immediate vicinity of each site were sampled and analyzed in order to compare with the archaeological data and identify potential sources. The analyses suggested that there is a degree of standardization in the recipes and the manufacturing process and that the selection of the raw materials depends on availability.