Journal articles on the topic 'Mesolithic flint analysis'

A small-scale excavation, undertaken in advance of building works at Faraday Road, Newbury, Berkshire, encountered an apparently intact Early Mesolithic layer containing abundant worked flint directly associated with animal bones. The site lay on the floodplain of the River Kennet in an area already well-known for Mesolithic remains and certainly represents an extension of the site found at nearby Greenham Dairy Farm in 1963. The flint assemblage was dominated by obliquely-blunted microlithic forms accompanied by a restricted range of other items. The animal bones were, unusually, dominated by wild pig with clear evidence of both primary butchery and food waste. Spatial analysis of the bone and flint assemblages indicated discrete activity areas, possibly associated with hearths. Both pollen and molluscan data were recovered which, together with the results of soil micromorphological examination, confirmed an Early Holocene date for the formation of the Mesolithic layer. Radiocarbon dates place the site in the late 10th–early 9th millennium BP. The paper re-examines the nature of known Early Mesolithic activity in this part of the Kennet valley, with particular reference to the specific environmental conditions that seem to have prevailed. It is concluded that the Faraday Road site represents one part of a continuum of Early Mesolithic occupation that stretches along a considerable length of the floodplain, with each focus of activity witnessing repeated, but intermittent, occupation spanning a period of more than a millennium.

Vessey Ponds are a pair of irregularly-shaped hollows high on the Chalk Wolds of East Yorkshire at about 220 m OD (Fig. 1). Recent fieldwalking recovered a large flint scatter in the vicinity of these hollows. Mesolithic activity was represented by worked flint displaying soft hammer technology whereas hard hammer technologies indicate Neolithic and Bronze Age tool production and usage. The presence of large numbers of cores and a vast quantity of industrial waste indicates on-site preparation of tools. Statistical analysis of the fieldwalking data implies that the flints are concentrated around the hollows. Auger sampling across the ponds revealed natural clay deposits that still hold water close to the pond surface. Consideration of exploitation of mineral resources on the Wold top and possible mechanisms of formation of Vessey Ponds highlights the complex effects of glacial activities on the local surface geology. Karstic origins for some features of surface geology are suggested. The nature of the ‘prehistoric’ economies represented by the flint scatter is considered along with ethnoarchaeological evidence to support the assumption that the ponds at Vessey were a potential water supply during the Mesolithic, Neolithic, and Bronze Ages. Evidence from Vessey Ponds and elsewhere in Yorkshire implies an association between areas of ‘prehistoric’ activity and the availability of surface water. Above all else, this work highlights the impact of water supply on settlement pattern and land use on the Chalk of the Yorkshire Wolds.

Excavations were undertaken in advance of construction work at Newbury Sewage Treatment Works on the outskirts of Thatcham in Berkshire, close to the sites of previous excavations undertaken by Wymer and by Peake and Crawford. Worked flint of Mesolithic date was recovered from a sandy layer overlying river gravel in two distinct concentrations suggesting two distinct episodes. Use wear analysis of the flint suggests that the sites were used as home bases at which a wide range of activities took place, with an emphasis on the processing of plant foods. A 14C date of 9100±80 BP was obtained from a sample of hazel-nut shells from within one of the concentrations. Analysis of the soil and sedimentary sequence as well as the pollen indicates constantly changing localised environments in the early Holocene in the Thatcham area, with sporadic occupation by Mesolithic communities on the drier areas at the edge of the floodplain.

In the summer of 1978 pottery and flintwork were noticed in the sections to the south of Cliffe Village during the laying of a pipeline by British Gas (TQ 734744) (fig. 1). This led to the excavation of a series of small trial trenches by Mr David Thomson with the help of local volunteers in the same year. The retrieval of a Beaker and Collared Urn suggested an early Bronze Age site, and excavations by Dr Ian Kinnes for the British Museum were done in September 1979. Although the excavated features contained mainly Iron Age pottery and metalwork, both seasons' work also produced a large quantity of flint artefacts ranging from Mesolithic to Bronze Age in date. The following report is an analysis of the Mesolithic tranchet axe manufacturing debitage which could be distinguished as a discrete group from the other flintwork. It is not intended to present a comprehensive flint report for Cliffe, but to provide a framework for analysis at other sites where tranchet axe production has been shown to take place (Wymer 1962; Parfitt and Halliwell 1982).

This article addresses the issue of the Mesolithic settlement in the Tenczyn Hummock region. Although Mesolithic artefacts have been encountered in this region systematically since the beginning of the 19th century, they have never become the subject of any elaboration discussing this issue individually. Jointly, from the area of the Tenczyn Hummock and its immediate surroundings 29 Mesolithic sites have been identified. Most of them are finds of single objects that based on their typological features can be associated with the Mesolithic period. The Mesolithic sites are mainly concentrated within the southern peripheries of the Tenczyn Hummock. Based on the analysis of the materials presented in this paper, the authors concluded that most of them should be linked with the late phase of the Komornica culture, although there were also a few elements revealing connections with the Janisławice culture. The Mesolithic occupation in the Tenczyn Hummock region was strictly associated with the Vistula valley, and constituted an integral part of the Mesolithic settlement in the Cracow region. Upon comparing it with the well-recognised Palaeolithic settlement, the completely different nature of the former becomes clearly evident. The Mesolithic sites, contrary to the Palaeolithic ones, were not directly associated with the exploitation of Jurassic flint outcrops. Most of them are remains of small camps, the distribution of which marks the zone of penetration of hunter-gatherer societies from the Vistula valley.

This study examines the archaeological significance of the material from a group of Neolithic chipping floors rescued during the rebuilding of the Antrim coast road, at Mad Mans Window, south of Glenarm, Co. Antrim. It shows that the lithic production strategies vary significantly between assemblages although it is presumed that they are all Neolithic in date and come from the same area of coast. It is apparent that flint axe production was of limited importance on these sites and that in spite of the abundance of flint available along the Antrim coast, relatively few polished flint axes were manufactured. Instead the numerous flint caches found in adjacent parts of the north-east of Ireland tend to produce scrapers and blades. Hoards containing arrowheads may be confined to the Bronze Age.Around 300 polished flint axes and roughouts are known from Ireland. These are frequently small and only partially polished. A limited number of highly polished axes with ground flat side facets have been designated sub-type A. The tendency to use porcellanite rather than flint for axe manufacture may be due to its ability to withstand robust shock.During the last 100 years, the role of flint as a key resource in the stone age of north-eastern Ireland has always been recognized but this has usually led to an uncritical assumption as to the paramount importance of flint. Work in recent years has shown that its significance in attracting and retaining Mesolithic settlement may have been over-emphasized.The role of the flint industries in the Irish Neolithic in this region has never been properly assessed, either in relation to older Mesolithic manufacturing traditions or in the broader context of supply to the Neolithic communities of this part of Ireland.In particular, good or even reasonable quality flint is usually only exposed in Cretaceous outcrops along a narrow strip on the edge of the basalt plateau and, therefore, has a very limited availability in parts of Co. Antrim as well as parts of Counties Down and Deny. As a contrast, erratic and beach flint is available in some quantity down the east coast of Ireland from Co. Down to Wexford. A second potential constraining factor is that unlike Britain, where flint was exploited for axe manufacture in the east and other rocks in the west, flint sources and porcellanite for axe manufacturing are both found adjacent to each other in the same corner of Co. Antrim. In particular, a number of more substantial chipping floors of Neolithic age are known, e.g. the opencast quarry sites at Ballygalley Head. The purpose of this study is to assess the role of flint production on the Antrim coast with particular reference to its significance in the Neolithic. This topic will be developed in the context of an analysis of the material found at Mad Mans Window near Glenarm.

A comprehensive study of flint materials peat site Old Voykovichi 1 includes technological, trasological and planigrafy analysis of flint. For the study were selected trasological all products retouched typologically decorated tools, plates and fragments thereof. The ratio between these typological and trasological analysis shows that using trasology we can get almost five times more guns and more complete picture of economic activity in the parking lot. On the excavation plan 2004-2005, all guns were applied separated by the trasological analysis. The basic amount of guns concentrated in the excavation in 2004 in several squares, arranged in an elongated spots. This suggested that this place was inhabited space site. Two more spots guns concentrations may be associated with production sites in the plaza parking lot. Thus, we can say that the study materials trasological archaeological monuments of the Stone Age enable us to refine the chronological past affiliation to recruit economic complex and to determine the type of hardware and guess the location of the monument of the living space. Site Old Voykovichi 1 can be defined as a seasonal hunting camp the final transition to the Mesolithic and Early Neolithic.

AbstractThe article describes the results of the interdisciplinary studies of a unique bone slotted point from Tłokowo, north-eastern Poland. The artefact was discovered in 1989, and indirect dating suggested an Early Mesolithic date. In this article we present the results of direct radiocarbon dating of the point, which shows that it is almost 2000 years younger than previously suggested. In addition, physical-chemical studies of the adhesive used to mount the flint inserts inside the point were conducted. The results of gas chromatography mass spectrometry (GC-MS) and attenuated total reflectance Fourier transform infrared spectroscopy (ATR-FT-IR) analysis indicate that the adhesive is birch tar. Finally, the article presents the results of detailed traceological studies that allow interpretation of the technology of production and possible function of the point. For the analysis, as well as various types of microscopes, optical coherence tomography (OCT) was used. In the discussion the results of all the analyses are considered alongside our current knowledge of this type of Mesolithic points in Europe.

The occurrence of mesolithic artefacts around Malham Tarn and Great Close Mire has been noted from the 1920s onwards. Pollen analysis at Tarn Moss to the west of Malham Tarn in the 1950s indicated that forest clearance had begun during Zone VI (c. 7000–5500 bc). Between 1972 and 1982, five prolific flint sites and a sixth, minor site were located in this area. The sites are of ‘Narrow Blade’ affinities and may have formed a summer base camp for hunter/gatherer groups operating in the Craven Pennines. Some artefacts of neolithic date have been found on the sites and this may indicate continuity. There is evidence for forest clearance and settlement in the later neolithic and this was well established by the Early Bronze Age.

Archaeological fieldwork preceding housing development revealed a Mesolithic site in a primary context. A central hearth was evident from a cluster of calcined flint and bone, the latter producing a modelled date for the start of occupation at 8220–7840 calbcand ending at 7960–7530 calbc(95% probability). The principal activity was the knapping of bladelets, the blanks for microlith production. Impact-damaged microliths indicated the re-tooling of hunting weaponry, while microwear analysis of other tools demonstrated hide working and butchery activity at the site. The lithics can be classified as a Honey Hill assemblage type on the basis of distinctive leaf-shaped microlithic points with inverse basal retouch.Such assemblages have a known concentration in central England and are thought to be temporally intermediate between the conventional British Early and Late Mesolithic periods. The lithic assemblage is compared to other Honey Hill type and related Horsham type assemblages from south-eastern England. Both assemblage types are termed Middle Mesolithic and may be seen as part of wider developments in the late Preboreal and Boreal periods of north-west Europe. Rapid climatic warming at this time saw the northward expansion of deciduous woodland into north-west Europe. Emerging new ecosystems presented changes in resource patterns and the Middle Mesolithic lithic typo-technological developments reflect novel foraging strategies as adaptations to the new opportunities of Boreal forest conditions. While Honey Hill-type assemblages are seen as part of such wider processes their distinctive typological signature attests to autochthonous, regional developments of human groups infilling the landscape. Such cultural insularity may reflect changing social boundaries with reduction in mobility range and physical isolation caused by rising sea level and the creation of the British archipelago.

The results of archaeological works carried out in 2017 at the Priyut Sukacheva 2 site (Irkutsk) and analysis of the Mesolithic stone industry are presented. During the excavation, we uncovered the Pleistocene and Holocene deposits and identified two cultural layers. Mixed and poorly informative materials were found in the 1th layer, which is dated, in accordance with the ceramics, to a wide period from Neolithic to the Middle Ages. The most interesting finds of this layer are a flint zoomorphic figurine and a sandstone bait fish. The most representative is the collection of the 2nd layer. Three fireplaces made of pebbles were found here, which were severely destroyed because of cryogenic processes at the end of the Early – beginning of the Middle Holocene. The collection includes almost 6 thousand finds, among which were noted: debitage, cores and precors, end-scrapers (the most numerous category), incisors, borers, points, combined and notched tools, abrasive tools, preforms of tools, a knife, a side-scraper, pebbles and pieces of rock. The collection also consist of a few faunal remains (Equus ferus, Cervidae and ungulates). According to the specificity of lithic assemblage and the presence of large fireplaces, we can assume that there was a short-term settlement of hunter-gatherers. Here, the primary stone knapping was carried out, that indicated by the finds of cores, precors, flakes, and pieces of rock. Along with this, intensive economic activities were carried out, which was probably associated with various works on skin dressing, processing bone and wood. Despite of the lack of radiocarbon dates, the lithic assemblage of the 2nd layer is sufficiently expressive for a detailed comparison with materials from other sites. As a result of the collection analysis, the greatest similarity with the Late Mesolithic complexes of the Lisikha site, located on the opposite bank of Angara river, was found. Both sites have a similarity in the preferences of the inhabitants in the choice of raw materials (mudstone), the shape of cores and tools, and the stratigraphic position of the archaeological materials. Taking into account all the data, the age of complexes from the 2nd layer at the Priyut Sukacheva 2 site should be determined by the Final Mesolithic (~9.5–8.5 ka cal BP). The results of stratigraphic analysis do not contradict these conclusions.

AbstractThis paper describes the rediscovery of the exact location for the Isleham hoard (tl 63197253) and presents the results of related fieldwork; it briefly reviews the metallurgical significance of the hoard, and discusses its local environmental and social context, as well as the distribution of founder's hoards within the Fenland region.The hoard was found to have been placed in a pit dug into a filled-in Bronze Age boundary ditch, next to a rectangular building, and adjacent to the edge of low-lying wetland bordering a palaeochannel which revealed an environmental sequence stretching from the Mesolithic to the Bronze Age. This area is also in proximity to a possible ringwork. Mesolithic and Neolithic activity is evidenced by residual flint tools and pottery. By the Bronze Age the tongue of fen next to the hoard had begun to be invaded by ferns and terrestrial vegetation and its latest peat phase was radiocarbon dated to 4045 ± 62 bp. Molluscs within the boundary ditch show an open landscape with a mixture of dryland and wetland taxa, and the presence of Vertigo angustior, a rare British species no longer known from Cambridgeshire, and one indicative of transitional habitats between wet and dry land. This landscape was probably contemporary with the deposition of the hoard.Current typological and radiocarbon analysis for Wilburton metalwork would suggest a date within the period 1150 to 1000 bc for the hoard, whilst a typological assessment of the pot in which the hoard was found suggests an affinity with Post-Deverel-Rimbury (PDR) Plainware dated currently from around 1150 to 800 bc. OSL dating of a sample of the pot containing the hoard yielded a date of 1460 ± 230 bc at 1 sigma.The locations of other founder's hoards within the region suggest a clustering in the southern fens and South Cambridgeshire, apparently related to ancient routeways.

Archaeological research in Jasień site no. 38 was conducted in 2013. The site was discovered and excavated during construction of a road junction and exit on the A4 motorway towards Brzesko. It is located on the western verge of the culmination of a dune, within the ridges of the marshy valley of the Uszewka River. As a result of the investigation, fourteen archaeological features were discovered, and 357 artefacts were obtained from features and layers. Most of them were fragments of vessels and flint artefacts. Based on the analysis of the materials, several phases of human activity were identified. The oldest artefacts can be linked with two Mesolithic cultural units, namely the Komornica culture with post-Maglemosian elements, and the Janisławice culture (?). Other archaeological materials dated to younger phases are equally scarce in terms of their quantity and are represented by pottery fragments associated with the Mierzanowice and Lusatian cultures. Amongst the artefacts from Jasień, materials referring to the Trzciniec culture are predominant. In terms of style and formal and technological characteristics they are extremely uniform, and they reveal features typical of the classical phase of the Trzciniec culture development.

Geometric microliths are inherent in almost all the Mesolithic and Neolithic monuments in the Lower Volga Region. For the sites of the territory they play a key role. With the help of this type of tools, it is possible to determine the cultural affiliation and chronological position of the studied monuments. In this paper we mainly consider the Neolithic sites on the territory of the Lower Volga and Lower Donets, which have geometric microliths in stone implements. Most of these monuments have a fairly stable series of tools of a geometric type, which makes it possible to compare them among themselves and draw parallels. The results of radiocarbon dating for Neolithic monuments of the Lower Volga and Lower Donets are presented. There is a typological comparison of these sites. The paper discusses similarities and differences, as well as possible contacts, or the lack of population on the two territories - the Lower Volga and the Lower Donets. The author comes to the conclusion that based on the analysis of geometric microliths it is not possible to trace a significant connection between the population of the Lower Volga and the Lower Donets. In the development of the flint industries of these regions there are more differences than similarities.

The rediscovery of human remains, correspondence and other unpublished excavation archival material in the Glasgow Museums collection of Ludovic McLellan Mann prompted the reappraisal of a short archaeological investigation undertaken in April 1931 at Holm Park, near Ballantrae, Ayrshire, by a schoolboy, Eric French and his biology teacher, William Hoyland. This article offers a re-evaluation of their fieldwork which exposed two inhumation burials, named ‘Tuesday Morning’ and ‘Tuesday Afternoon’. Eight dog whelk shells remain from an overlying diffuse shell midden spread that may reflect the remnants of a dye-processing site. The skeletons and marine shells went on temporary display at Bryanston School, Dorset. The area south of Ballantrae is well known for prehistoric flint scatter sites and the finds presented the intriguing possibility that the burials might be Mesolithic in age, the excavators believing they might even be Palaeolithic. A collection of flint cores, initially associated with the archive, now appears unrelated to this excavation for it was found with a note written by a local lithic collector, William Edgar. New osteological analysis confirmed the presence of at least two adult individuals, and one bone sample returned an early medieval radiocarbon date. This evidence contributes to national understandings of early historic burial practices in unenclosed cemeteries during the transition from Iron Age pagan to Christian burial rites, important given the paucity of 1st millennium evidence in south-west Scotland. It also offers insight into an earlier account of multiple inhumation burials, found in the general vicinity in 1879, although aspects of the precise location and relationship between the two discoveries is currently unresolved. Mann’s correspondence with French’s father, a prominent Glasgow industrialist, and with Hoyland reveals the character of archaeological social networks in western Scotland during the 1930s which have been a neglected aspect of research to date. Canmore ID 60957 Canmore ID 60935 Canmore ID 275902

In 2016 during the inventory and transportation of the archaeological finds from temporary archaeological storage at Pheophania to the present-day storage facility of the Institute of Archaeology, the materials of the excavations of the expeditions of 1980 and 1985 were selected and processed. The excavations and surveys were conducted by expeditions under the lead of O. G. Shaposhnikova and D. Ya. Telehin on the territory of the Starobilsk district of the Luhansk region. The surveys in 1980 were conducted at only two locations located close to each other — the settlements of Aidar-Bila and Pidhorivka. Aydar-Bila. Because the location plan is missing (it is also missing from the 1986 report), it was not possible to locate the settlement on the map. However, it can be assumed that the multilayered settlement of Aydar-Bila is located in the eastern part of the village Pidhorivka of the Starobilsk district of the Lugansk region, on the low floodplain terrace of the right bank of the river Bila (the right tributary of the Aydar river). At the location of the settlement, the width of the valley of both rivers is 2.23 km. In 1986, additional research was conducted and the site was named Hyrlo Biloyi. In fact, this name is more common and widely used in the scientific literature. The settlement is multilayered, as indicated by the code on the finds. The largest number of finds is associated with layer 4. Given the vertical distribution of the finds, it can be assumed that there are at least three episodes of occupation in the history of the settlement, two of which, given the peculiarities of the finds, occurred in the Neolithic Period and one in the Late Bronze Age. Pidhorivka. The multilayered settlement of Pidhorivka is located on the off-shore terrace of the right bank of the Aydar River, at the point where the coast recedes to the west, thus forming a sufficiently wide floodplain, on which the depressions of the old-aged lakes are noticeable. In total, about 10 different settlements were found within the specified floodplain, 5 of which are known from the research of S. O. Loktushev in 1939. In 1963, the Pidhorivka settlement was investigated by V. M. Gladilin, however, no report or publication on the results of the research appeared, as correctly pointed out by Y. G. Gurin in 1998. It is only known that the expedition V. M. Gladilin cleaned up the coastline of the Aydar River, where the Neolithic materials were discovered. Some findings revealed by the expedition led by V. M. Gladilin appear in the monograph V. M. Danilenko as an example of the material culture of the Azov culture he identified. In 1980, the expedition of the Academy of Sciences of the USSR under the direction of O. G. Shaposhnikova laid out an excavation area on the Pidhorivka settlement. The results of these studies are unknown (missing report, field documentation, and findings). In the same year an expedition led by D. Y. Telegin excavated a trench with a total area of 5 m2. Later (in 1984), the site was explored by an expedition under the general guidance of K. I. Krasilnikov and Y. G. Gurin. The total number of findings revealed as a result of the research by O. G. Shaposhnikova reached 295 units. The material analysis demonstrates the settlement is multi-layered. The upper horizons with the Middle and Late Bronze Age materials being the latest. In the conditional horizon of 0.8/0.9 m, a rather informative fragment of the Late Copper Age vessel was found, and at the same time, it is accompanied by a flint complex, which has the appearance of the Early Copper Age or Neolithic. The artifacts found in the conditional horizons of 0.9/1.0—1.1/1.2 m appear to be relatively «pure» in that the cultural and chronological terms clearly define their affiliation with the Early Neolithic Period and allow them to be associated with the Lower Don culture/Nizhnedonska culture of the Mariupol Cultural and Historical Area. At the same time, the presence of earlier artifacts, such as a conical single-platform core and multiple-truncated burin, makes one more cautious to interpret the complexes. Both the core and the burin look more logical in the flint complexes of the lower horizons of the site. In this sense, it is important to pay attention to the description of the stratigraphic section of the excavation area 2 of the settlement Pidhorivka, presented by Y. G. Gurin in a monograph about the Early Copper age sites of the Siversky Donets Basin. It states that, at a depth of 1.7/2.0 m and below, the layer of floodplain alluvium contains «Mesolithic materials». Y. G. Gurin did not publish the materials themselves that he claimed were from the Mesolithic era. In 2006, O. F. Gorelik issued a publication dedicated to the interpretation of the materials of the lower layer of Pidhorivka. In this work, he linked the affiliation of the flint complex with the early stage of Donetsk culture, and considered the site one of the centers of the Mesolithic industries with the yanishlavitsa type of projectile points. This conclusion is based on the similarity of the materials of the lower layer of Pidhoryvka with the flint complex of the site Shevchenko hamlet, one of the features of which is the presence of a yanislavitsa type of projectile point. In 1999, the materials of the site Zelena Hornitsa 5 were published, which is located on the second floodplain terrace of the lake on the left bank of the Siversky Donets River. In the material culture of this site, even if there are multiple elements, they in no way affect the overall situation. The complex of projectile points of the site consists of trapezes, a yanislavitsa type, points with truncated edges, and so on. The presence of the collapse of the stucco vessel along with these flint products, gave rise to criticism of the idea of O. F. Gorelik about the Mesolithic character of complexes with a yanislavitsa type of projectile points. Later V. O. Manko, in a more detailed form, questioned the theory of O. F. Gorelik. To the present day we can state that there has been some stagnation in this issue. The surveys in 1985 were conducted at the valley of Aidar river from v. Lyman to v. Losovivka. In this area, sites lots have been found, which in chronological terms date back to the Paleolithic—Medieval times. For this reason, we believe that the introduction into scientific circulation of even a small amount of archaeological materials, allows the creation of a more complete picture of the processes that took place in the basin of the middle stream of the Siversky Donets River during the Neolithic—Copper Age.

Abstract Sowinki is a village located 35 km south of Poznań, where archaeological research has revealed the remains of settlement from different archaeological periods, ranging from the Mesolithic (ca. six thousand years BC) to the Late Medieval period (ca. 15th century AD). This area, therefore, provides a record of the history of Greater Poland (Poznań) region, tracing back to about seven and a half thousand years ago. Samples of bones and wood were collected from different features, including mostly cellar pits, refuse pits and grave pits. Eight of the samples, all collected from grave pits, were selected for radiocarbon dating. The obtained 14C measurements have confirmed previous findings concerning different cultures registered in the studied area, and additionally, they have helped to clarify chronology of the early medieval cemetery. The presented results are the first isotopic measurements taken for the site of Sowinki. Previously, chronological frameworks of this site were determined on the basis of relative chronology, according to stratigraphy of sediments, examination of metal finds, pottery and flint objects. The deposition depth of the analysed charcoals did not exceed 100 cm below ground level. According to the analysis, all the samples date to the time of the early Piasts’ dynasty. The obtained data have allowed for defining two chronological phases of the early medieval cemetery. This is an important archaeological site both in terms of its spread and the long time of existence. In addition, it provides a valuable background for the study on the emergence of early medieval elites and the formation of the Polish “early feudal” state.

Šventoji 43 is one of eight Comb Ware culture sites known in Lithuania at present. The site was excavated in 2013 and 2014 and revealed a homogeneous pottery assemblage, which was classified as Comb Ware and was radiocarbon dated to 3900–3650 cal BC. As a result of this dating, it has been found that Comb Ware is the oldest pottery type to have been produced in coastal Lithuania. In fact, the pottery assemblage of Šventoji 43 also suggests that Comb Ware originates from a distinct phase in the pottery sequence of coastal Lithuania that both predates all other phases from Šventoji pottery bearing sites and has not been previously recognised in other assemblages. Zooarchaeological analysis has revealed that the site was occupied during the early spring and mostly used for fishing zander and pike in the lagoonal lake and for hunting seals and forest game. The unique character of the flint industry, which combined hard hammer percussion and bipolar knapping that resulted in the production of microliths on irregular blades, suggests that the local Šventoji 43 community had Mesolithic roots. Furthermore, this evidence supports the hypothesis that Comb Ware had reached Lithuania through intense contact between East Baltic hunter-gatherers rather than due to a mass migration of the population from the Northeastern Baltic. The much wider distribution of Finno-Ugric hydronyms, compared to that of Comb Ware sites gives an impression that some other Subneolithic pottery types in addition to Comb Ware might have been produced by Finno-Ugric speaking people. Keywords: Comb Ware, Šventoji 43, coastal Lithuania, beginning of pottery production, Finno-Ugric hydronyms

An excavation was undertaken by CFA Archaeology Ltd (CFA) between August and November 2010 on the site of the new Musselburgh Primary Health Care Centre. The site, which lies to the south of Inveresk Road, is centred on NGR 33430 67224. Until its demolition, the area had been occupied by Brunton Wireworks. The Scheduled Monument of Inveresk Roman Fort lies at the top of the steep slope c 50m to the south of the excavation site. The excavation identified six phases of activity on the site, the earliest being a Mesolithic flint scatter (Clarke & Kirby forthcoming). The area was used as a burial ground in the Iron Age and a ring ditch may also be of prehistoric date. Later, six Roman inhumation burials (four of which had been decapitated) and a horse burial were interred, and a possible Roman fortlet was constructed. Across the site, a network of interconnected ditches formed part of a Roman-period field system, which cut through the rampart of the possible fortlet, and through a number of the graves. Along the southern boundary of the site a large accumulation of Roman midden deposits overlay features associated with the field system, although it may have started to build up while the latter was still in use. A post-built structure was also found, one post of which cut a ditch of the field system. The midden deposits extended along the full length of the southern boundary of the site, measuring 110m long by up to 20m wide. Numerous artefacts were recovered, representing the rubbish and discarded personal belongings of the fort occupants. The pottery included samian bowls with personal names scratched on the bases. Evidence from these, together with isotopic analysis of the human skeletons, shows that the ethnic origin of those living in the fort was diverse, as would be expected for the Roman army.

Over a period of 14 years, and as part of the Polish Archaeological Record research project, the author directed a field survey of the whole of the Lega river basin (NE Poland) – an area of over 850 km2. As a result of the survey of this hitherto poorly investigated area, almost 1100 archaeological sites were discovered, 748 of which contained lithic materials. The most interesting sites were initially studied by detailed mapping of surface-find distribution and later by excavation. A complete study of the whole drainage basin was very important for settlement research. The large number of the surface lithic assemblages enables reliable statistical analyses and accurate cartographic studies supported by palaeo-environmental reconstructions. Lithic assemblages were analysed from the point of production techniques and typology, dispelling some doubts about chronological-cultural affiliations of flint inventories from north-east Poland and neighbouring countries, but also raising new questions. It was possible to observe clear and changing settlement preferences in the late Palaeolithic and Mesolithic in the zone of late Glacial lakes and their adjacent outwash territories to the south. Six concentrations of sites were discovered, associated with communication routes and zones of economic activity.

Any new knowledge that goes beyond the stone tools and techniques used in the Palaeolithic and Mesolithic is most significant as it reveals the cultural and technical capabilities of the people living in these periods. In 1963, two pitch finds were discovered in a lignite open-mining pit in the northern foothills of the Harz Mountains, in a layer the geological age of which was dated as being older than 80,000 years. The great significance of these finds was therefore immediately apparent. One of the finds showed a fingerprint as well as the imprints of a flint stone tool and the structure of wood cells. This was indicative of the pitch piece having served as an adhesive to secure a wooden haft to a flint stone blade.Over 30 years later these finds were transferred to the Doerner Institut for investigation. The GC and GC/MS analyses revealed that, in both cases, birch pitches, well-known historical adhesives, had been used. These consist predominantly of pentacyclic triterpenoid components of the lupane type, with betulin forming the major component. The comparison with birch bark extracts showed that the biological peak profile (bio-marker) was surprisingly well preserved in these pitch finds and that hardly any degradation products were present.Today, comparable pitches can easily be produced with modern technical methods, i.e. using airtight laboratory flasks and temperature control facilities. However, any attempt at simulating the conditions of the Neandertal period and at producing these birch pitches without any of these modern facilities will soon be met with many difficulties. This implies that the Neandertals did not come across these pitches by accident but must have produced them with intent. Conscious action is, however, always a clear sign of considerable technical capabilities.

The crystalline geological substratum of the Armorican Massif, in the West of France, is devoid of flint nodules in primary position. As a result, during Prehistory, humans developed different strategies for making their toolkits, either by adapting production methods to local rocks from diverse sources, or by importing materials from the sedimentary margins. This article proposes to analyse the distribution of lithic materials during the Mesolithic as the consequence of a succession of collective choices. Many sedimentary, metamorphic or plutonic rocks of local origin were used, and considerably increased in quantity from the Early Mesolithic to the Late Mesolithic. After the identification of the geological origin of the rocks, a series of mechanical analyses were carried out to define their properties. Then, the social integration process of these rocks was addressed. The lithic assemblages of Beg-er-Vil (Quiberon) and la Presqu’île (Brennilis) were then described to tangibly explain the intentions of productions in coastal and continental economies respectively during the Late Mesolithic (end of the seventh and sixth millennia BCE). The toolkits in both economies are strictly identical, but two different lithic management systems were clearly in place. The first, on the coast, consisted exclusively of production on pebbles, whereas, the other, inland, used a wide range of materials of mediocre quality. During the Mesolithic (and unlike Neolithic practices), and in this context of geological paucity, sacrificing technical standards always seemed preferable to long-distance acquisitions by means of imports or exchanges.