Recent Excavation and Recording at the New Neolithic Rock Art Site of Vallée Aux Noirs,Buthiers (Seine‐et‐Marne,France)

Following the exceptional discovery of Neolithic engravings on a boulder at Vallée aux Noirs in the Fontainebleau forest, south of Paris, an excavation trench was opened in order to access the buried part of the decorated rock panel and explore the stratigraphic context of the artwork. A palaeosol was found two metres below the modern ground level, underneath multiple layers of sterile sandy soil forming a very compact sequence from which only one archaeological artefact was recovered – an Iron Age fibula (c.200–300 BC). Dating of the palaeosol was attempted through two different methods: AMS dates from charcoal suggest a significant span from the Early Bronze Age to the Iron Age, while two more consistent OSL dates point to formation of the palaeosol during the Late Neolithic (3500–3000 cal BC). The entire engraved rock surface (16 m²), including its buried part, was fully recorded. Four main semiotic groups were identified: a typical fifth‐millennium crook‐hafted axe with a ring, two boats with steering oars, and a central, very tall human figure dominating the composition from its 3.5‐metre height.     

Neolithic and Bronze-Age Herders of Pupićina Cave,Croatia

Abstract

Pupi?ina Cave (Croatia) preserves an important archaeological sequence spanning 12,000 years. Here we present and discuss the results of extensive excavations in post-Mesolithic deposits.Pupi?ina Cave,located in NE Istria in a region rich in caves and in prehistoric settlement, has well-dated evidence from the Middle Neolithic, Late Neolithic, Middle Bronze Age, Iron Age, and Roman periods. Visitors to the cave in the Middle Neolithic ca. 5500–5000 in calibrated years B.C (cal B.C.) left typical Danilo/Vla?ka pottery and kept herds of sheep and goats during the spring. Mortality profiles suggest that herds were managed for milk production. During the Late Neolithic (ca. 4550–4150 cal B.C.) Hvar pottery appears along with lithic artifacts from great distances (e.g.,Lipari). Herds of sheep and goats were managed for meat as were cattle and pigs. There was a major hiatus in occupation between the Late Neolithic and the Middle Bronze Age. Middle Bronze Age (ca. 1775–1400 cal B.C.) deposits are found only in one large pit. Pottery is dominated by drinking vessels, and faunal use is the same as in the Late Neolithic. The cave was used primarily as an animal pen during the Iron Age (1st millennium B.C.).     

Impulses of agro-pastoralism in the 4th and 3rd millennia BC on the south-western coastal rim of Norway

Abstract

A review of the available archaeological and palaeoecological evidence from the coastal heathlands of south-western Norway was compiled to reveal the processes of neolithisation proceeding from the Early Neolithic towards the generally accepted breakthrough in the Late Neolithic, 2500/2350 cal. BC. South-western Norway then became part of the Scandinavian, and thus the European, agricultural complex. Three phases of forest clearance are recorded — from 4000–3600 cal. BC, 2500–2200 cal. BC and 1900–1400 cal. BC. Deforestation was intentional and followed a regional pattern linked to the geology and topography of the land. In the first period (4000–2500 cal. BC), forage from broad-leaved trees was important, while cereal cultivation was scarcely recorded. Agro-Neolithic (here referring to agriculturally-related Neolithic) artefacts and eco-facts belonging to the Funnel Beaker and Battle Axe culture are rare, but pervasive. They must primarily be considered to be status indicators with a ritual function; the hunter-gatherer economy still dominated. The breakthrough in agro-pastoral production in the Late Neolithic was complex and the result of interactions between several variables, i.e. a) deforestation resulting from agriculture being practised for nearly 1500 years b) experience with small-scale agriculture through generations and c) intensified exchange systems with other South Scandinavian regions. From 2500/2350 cal. BC onwards, two distinct environmental courses are noticeable in all pollen diagrams from the study area, indicating expansion in pastoralism, either towards heath or towards grassland and permanent fields.     

Mid- to late-Holocene vegetational and land-use change in the Hadrian's Wall region: a radiocarbon-dated pollen sequence from Crag Lough,Northumberland, England

Pollen, charcoal and sedimentological analyses of a radiocarbon-dated sediment sequence from Crag Lough, by Hadrian's Wall, northern England, are used to reconstruct vegetational and land-use change since ca. 3000 cal BC. Clearance of Quercus and Corylus avellana woodland began at ca. 2600 cal BC, followed by a substantial decline of Alnus glutinosa and spread of Calluna vulgaris at ca. 400 cal BC. Local cereal cultivation occurred sporadically from ca. 2200 cal BC, with a decline (perhaps associated with climatic deterioration) at ca. 900 cal BC, then an increase at ca. 600 cal BC. Secale cereale was grown in the area from approximately the first to fifth centuries AD, followed by a second phase from ca. AD 1250–1700, when it was accompanied by Cannabis sativa.The sequence is interpreted in the light of the archaeological record, particularly in relation to the impact of Roman military activity in the area. The most significant episodes of woodland clearance occurred in the late Neolithic/early Bronze Age period and then in the middle Iron Age, creating a patchwork of woodland, heather moorland, pasture and arable land by the Roman period. The main changes in the Roman period were a decline in the extent of Betula woodland and perhaps the local introduction of Secale cereale cultivation. Local land management practices involving fire seem to have been suspended in the Roman period, but resumed afterwards. The end of the Roman period may have been accompanied by a shift towards pastoral land-use and abandonment of less favourable agricultural land, but the effect was minor compared to that at other sites in the region. Later shifts in land use may relate to climate variability, as reconstructed from several mires in northern England.     

Vegetation history at the multi-period prehistoric complex at Ballynahatty,Co. Down,Northern Ireland

Palaeoecological methods can provide an environmental context for archaeological sites, enabling the nature of past human activity to be explored from an indirect but alternative perspective. Through a palynological study of a small fen peatland located within the catchment of a multi-period prehistoric complex at Ballynahatty, Co. Down, Northern Ireland, we reconstruct the vegetation history of the area during the early prehistoric period. The pollen record reveals tentative evidence for Mesolithic activity in the area at 6410–6220 cal BC, with woodland disturbance identified during the Mesolithic–Neolithic transitional period ca. 4430–3890 cal BC. A more significant impact on the landscape is observed in the Early Neolithic from 3950 to 3700 cal BC, with an opening up of the forest and the establishment of a mixed agricultural economy. This activity precedes and continues to be evident through the Mid-Neolithic during which megalithic tombs and related burial sites were constructed at Ballynahatty. Due to chronological uncertainties and a possible hiatus in peat accumulation in the fen, the contemporary environment of the Ballynahatty timber circle complex (constructed and used ca. 3080–2490 cal BC) and henge (dating to the third millennium cal BC) cannot certainly be established. Nevertheless, the pollen record suggests that the landscape remained open through to the Bronze Age, implying a long continuity of human activity in the area. These findings support the idea that the Ballynahatty prehistoric complex was the product of a gradual and repeated restructuring of the ritual and ceremonial landscape whose significance continued to be recognised throughout the early prehistoric period.     

Dietary changes and millet consumption in northern France at the end of Prehistory: Evidence from archaeobotanical and stable isotope data

Diachronic changes of dietary human habits between the Neolithic and the Bronze Age are mainly identified through archaeological artefacts and archaeozoological and archaeobotanical studies. This paper aims to demonstrate the importance of a multi-disciplinary approach for palaeodietary studies and to identify the food changes between Neolithic and Bronze Age human groups in northern France. These changes are probably linked to the introduction of new crops, such as millet, and the use of stable isotope analysis on bones and teeth proves to be an effective method for assessing the role of this specific cereal in the diet and the economy. Stable isotope analyses were performed on bone and tooth collagen and apatite from eight humans and five domestic animals from a Late Bronze Age site (LBA; Barbuise; 15th–13th c. BC; Aube). The studied corpus is compared with isotopic data from human and animal bones from a nearby Neolithic site (Gurgy; 5th mill. BC; Yonne) and regional Neolithic to Iron sites located in northern France. Moreover, Barbuise data are supplemented by information from an important archaeobotanical study carried out on 21 LBA and Early Iron Age sites in the region. Neolithic and LBA human collagen isotopic ratios (δ¹³C, δ¹⁵N) differ statistically, as do those of some animals. Carbon isotopic ratios of human apatite corroborate collagen results indicating the consumption of ¹³C enriched food by LBA humans and animals compared to Neolithic samples. The high number of occurrences of plant remains in the Bronze Age settlements near the site points to the consumption of C₄ plants, such as millet, and would account for these results.     

Settlement and environmental history of a multilayered settlement mound in Niederröblingen (central Germany) – a multi-proxy approach

A multi-disciplinary palaeoecological approach on a sequence of dated archaeosediments was accomplished. The sediments derive from a multilayered prehistoric settlement mound in central Germany, representing the remnants of a prehistoric village. Based on the analysis of biological remains and geochemical/physical analysis of the settlement layers its environment was reconstructed. There is a trend to increasing anthropogenic activities and impact on the environment represented through a rise of indicators for productive surplus from the Early Neolithic (5300–4900 BC) until the Roman Times (400 AD). During the Early Neolithic, shifting flat settlements were situated in a locally opened landscape. The immediate surrounding of the floodplain was used by the settlers for their economic requirements (e.g. wood from the riparian forest). After a hiatus of ca. 1900 years, a multilayered settlement mount rose from Late Neolithic Times (3000 BC) to Roman Times. Since the Middle Bronze Age (approximately 1500 BC) the riparian forest was obviously replaced by agricultural fields and meadows and henceforward the hinterland used by the settlers probably grew in size. The continuing demand of wood was maintained by the acquisition of more distant sources. The onset of house constructions substituting wood by loam (wattle and daub) might be a possible societal response to this shortfall. This is reflected in the growing thickness and composition of the settlement layers, as well as in the archaeological record (e.g. tumbled wattle and daub house walls). The rising of the groundwater table and the start of severe floods of the adjacent river Helme during pre-Roman Iron Age (approx. 800–100 BC) might reflect a geomorphological response to the increased land use intensity at a regional scale.     

Agricultural and household activities in Vestfold,Southeast Norway,as illustrated by pollen data and the charred remains of crops and wild plants

This paper presents and interprets two data sets from Vestfold, Southeast Norway: the pollen record is from a small lake basin, isolated from the sea in Mid Mesolithic (8100–6400 cal BC), and with a record of sediment deposition up to recent time. Charred plant remains from six settlement sites ranging in date from the Late Neolithic (2400–1800 cal BC) to the Merovingian Period (cal AD 570–800). Soil from archaeological contexts that was recovered from several prehistoric settlement features (two- and three-aisled houses, a rock shelter and a pit) has also been investigated. The number and concentrations of identifiable charred macro remains are low from all features except one, but the records contribute to the interpretation of agriculture and wild plant use. Carbonised cereals dated to the Late Neolithic/Early Bronze Age are reported from a two-aisled house. Naked barley was the main cereal identified and a few weed seeds were found with the cereal grains. In a rock shelter nearby, cereals and seeds of flax were found, demonstrating cultivation in the Late Bronze Age. Pollen of ribwort plantain recorded in lake deposits in Nordbytjern, 0·5?km to the southwest, also indicates agricultural activity in the southern part of Vestfold during the Late Bronze Age. Archaeobotanical samples from Early Iron Age houses contained low concentrations of carbonised cereal remains, mainly hulled barley, but also wheat and oat. Seeds/fruits of weeds, plants of moist/wet habitats and grasses increase in abundance from the end of Roman Period. The high concentration of hulled barley found in a pit at the site of Ringdal 13 confirms that hulled barley was a cereal used in the Iron Age. Throughout the Iron Age, cereal pollen has a continuous curve in the Nordbytjern pollen diagram, demonstrating the significance of cereal cultivation in Vestfold. Flax was also cultivated in the vicinity of and probably processed in Nordbytjern. Large numbers of rush seeds and sedge nutlets indicate a possible involvement in basketry and cordage making and/or as animal fodder.     

The Living and The Dead,Memory and Transition: Bayesian Modelling of Mesolithic and Neolithic Deposits from Vlasac,the Danube Gorges

The paper applies Bayesian statistical modelling to radiocarbon dates obtained for a stratigraphic sequence comprising occupation features and superimposed burials from the Late Mesolithic (c.7400–6200 cal BC) to the Mesolithic–Neolithic transition (c.6200–5900 cal BC), from Vlasac in the Danube Gorges region of the north‐central Balkans. This sequence, investigated in the course of excavations at the site in 2006–9, yielded stratigraphic evidence of the transformation of local forager populations as a result of contact with Neolithic communities. Our paper provides a reliable chronological framework for changes from Late Mesolithic burial rites to new, Neolithic types of ornamental beads at the top of the sequence. The use of the same burial location and continuities in burial rites over a considerable period of time raise significant questions about the role of tradition and the potential for enduring practices in prehistoric societies.     

Political economic reorganization among non-state societies: A case study using Middle Holocene mortuary data from the Cis-Baikal,Russia

The extraordinary record of prehistoric funeral activities in Russia’s Cis-Baikal region provides an opportunity to study changes in political strategies that boreal forest hunter–gatherers employed at these events in the Middle Holocene. I use published data on burial treatments (quantities of grave goods, presence of exotic materials, burial layouts) from 10 Late Neolithic (henceforth referred to as “LN,” 4000–3000 BC) and 11 Early Bronze Age (“EBA,” 3000–2000 BC) cemeteries to explore important and previously undetected shifts in the ways that funerals during these periods articulated with political life. LN groups used funerals to emphasize affiliation with corporate institutions, while EBA funeral participants employed political strategies focused on displaying wealth. Current evidence indicates that groups on the western peripheries of the Cis-Baikal started employing semi-nomadic pastoral subsistence practices at the time of the LN-EBA transition, and I suggest that these groups presented new opportunities for Cis-Baikal inhabitants. Interactions with mobile, food-producing groups may have indirectly stimulated indigenous populations to redefine funeral gatherings as venues appropriate for cultivating long-distance economic and political support through competitive displays of wealth.     

Evaluation of radiocarbon dates from the Middle Holocene hunter-gatherer cemetery Khuzhir-Nuge XIV,Lake Baikal,Siberia

A data set of 87 radiocarbon determinations obtained for the Bronze Age Khuzhir-Nuge XIV cemetery in the Cis-Baikal region of Siberia is analyzed from the perspective of data quality and within the local archaeological context. Bone preservation, expressed in terms of collagen yields, is a very important factor affecting both the accuracy and precision of ¹⁴C dates and, therefore, publication of this information should be adopted as a required standard. According to the calibrated high-collagen dates, after a single Serovo interment the cemetery was used continuously by Glazkovo peoples for up to 700 years (∼2700–2000 BC), and 70% of all burials were interred within a relatively short peak period between approximately 2500 and 2300 BC. The extensive radiocarbon data from KN XIV allow for the re-evaluation of existing models and perspectives on the place of the Glazkovo culture within the Cis-Baikal Neolithic and Bronze Age.     

Golden Biographies: The Production,Curation, Fragmentation and Deposition of the Armorican-Type Rolled-Gold Bead-Like Ornaments found at Pendleton,Lancashire

A rare Chalcolithic rolled-gold bead-like ornament dated to c. 2400–2200 cal. BC was found in association with sherds of early Beaker ware in an Early Bronze Age Collared Urn burial dated to c. 1545–1450 cal. BC. The grave was located at Pendleton, Lancashire. This paper reports on the AMS radiocarbon dates for the burial context along with X-ray composition analysis of the gold ornament, which shows the object had a high platinum content consistent with alluvial, placer, deposits possibly originating in Brittany, France rather than the British Isles. This unparalleled rolled-gold ornament is compared to the corpus of British and French rolled-gold ornaments and contemporary goldwork and a provenance, manufacture and biography of the find is explored. Both curation and fragmentation are considered in the context of a dated Beaker ware assemblage from the local domestic site of Lower Brockholes, Preston, as well as existing corpora of Beaker and Collared Urn ware from the region.     

The emergence of rice agriculture in Korea: archaeobotanical perspectives

This paper reviews archaeobotanical records on the beginning and spread of rice agriculture in the Korean peninsula. Argument for the earliest evidence of domesticated rice at the Sorori site, 15,000 years ago, is invalid. The evidence for rice cultivation in the Neolithic (Chulmun) is still insufficient although rice remains have been reported from a few late Neolithic sites in central-western Korea which dated to about 3000 BC. The existence of rice agriculture in the Bronze Age (Early and Middle Mumun: c.1300 ∼ 300 BC), on the other hand, is demonstrated by the high percentage and/or frequency of rice remains among crops recovered from various sites, as well as through the numerous findings of paddy fields. Rice appears to have been introduced from the Liaodong region, China, while so called 'southern diffusion route' that the beginning of rice cultivation was first stimulated by influences from Southeast Asia or South China is no more valid. Charred rice remains recovered from the Bronze Age dwellings consist of dehusked clean grains and weedy seeds are very rare among samples containing rice grains, which could be related with the harvesting and processing methods of rice. Measurements of charred rice grains also will be reported in this paper. Agricultural villages disappear from the archaeological records from the third century BC, which corresponds to the beginning of the Early Iron Age (Late Mumun), and reappear from the late first century with the emergence of urban societies.     

Hunter–gatherer foraging ranges, migrations, and travel in the middle Holocene Baikal region of Siberia: Insights from carbon and nitrogen stable isotope signatures

Foraging ranges, migrations, and travel among Middle Holocene hunter–gatherers in the Baikal region of Siberia are examined based on carbon and nitrogen stable isotope signatures obtained from 350 human and 203 faunal bone samples. The human materials represent Early Neolithic (8000–6800 cal BP), Late Neolithic (6000–5000 cal BP), and Early Bronze Age periods (∼5000–4000 cal BP) and come from the following four smaller areas of the broader region: the Angara and upper Lena valleys, Little Sea of Baikal’s northwest coast, and southwest Baikal. Forager diets from each area occupy their own distinct position within the stable isotope spectrum. This suggests that foraging ranges were not as large as expected given the distances involved and the lack of geographic obstacles between the micro-regions. All examined individuals followed a similar subsistence strategy: harvesting game and local fishes, and on Lake Baikal also the seal, and to a more limited extent, plant foods. Although well established in their home areas, exchange networks with the other micro-regions appear asymmetrical both in time and direction: more travel and contacts between some micro-regions and less between others. The Angara valley seems to be the only area with the possibility of a temporal change in the foraging strategy from more fishing during the Early Neolithic to more ungulate hunting during the Late Neolithic–Early Bronze Age. However, the shift in stable isotope values suggesting this change can be viewed also as evidence of climate change affecting primary productivity of the Baikal–Angara freshwater system.     

LAND USE IN THE EASTERN ALPS DURING THE BRONZE AGE—AN ARCHAEOBOTANICAL CASE STUDY OF A HILLTOP SETTLEMENT IN THE MONTAFON (WESTERN AUSTRIA)*

Investigations of the oldest prehistoric settlement in the western Austrian county of the Vorarlberg reveal a deeper insight into the colonization of the Alps. The human presence is recorded from the Late Neolithic (c. 3000 cal. bc ) onwards, reflecting farming and possible mining activities. Three distinct settlement phases are recognized palynologically: (1) in the Early and Middle Bronze Ages (c. 1700 cal. bc ), (2) during the Iron Age (c. 500 cal. bc ) and (3) at the beginning of the medieval era (c. cal. ad 800). In addition plant macrofossil analyses of soil samples from the archaeological excavation of the Bronze Age settlement of Friaga indicate a complex subsistence strategy of the Middle Bronze Age settlers, whereby cereals and pulses reveal a balanced diet.     

Palaeodiet of Mesolithic and Neolithic populations of Meuse Basin (Belgium): evidence from stable isotopes

The human diet was investigated using the carbon and nitrogen isotopic signatures of 93 Mesolithic and Neolithic specimens (∼10,000–2000 BC) from the Meuse Basin (Belgium). During the Ancient Mesolithic period (∼9300–8000 BC), the environment was generally open and the main dietary protein was provided by hunted terrestrial mammals, with the possible addition of freshwater resources. Human remains are not available in the Meuse Basin from around 8000 BC to 4300 BC, thus preventing the study of the Mesolithic-Neolithic dietary transition in this region. Throughout the Middle Neolithic (∼4300–3000 BC), hunting was more difficult and less productive due to a densely forested environment. The contribution of freshwater resources to the diet increased, with the remaining proteins provided by terrestrial wild and/or domestic mammals, indicating that non-agricultural resources were not eliminated in this region during the Middle Neolithic period. The contribution of freshwater resources seems negligible in the Middle/Late and Late Neolithic periods (∼3300–1700 BC), with isotopic results revealing a diet composed of agricultural products. The δ¹⁵N values of infants are compatible with a weaning age at around 2 years. This study documents the dietary changes that occurred in Belgium during the first part of the Holocene, and reveals the subtle dietary distinction between wild and domestic terrestrial resources and freshwater resources.     

Isotopic dietary reconstruction of humans from Middle Bronze Age Lerna,Argolid, Greece

This study presents the results of a carbon and nitrogen stable isotope analysis of 39 human bone and 8 animal samples from Middle Bronze Age (or Middle Helladic, MH, ca. 2100–1700 BC) Lerna, Greece. The isotopic data indicate that the humans had a C₃ terrestrial diet while certain individuals appear to have significant amounts of animal protein in their diet. With regard to weaning age, the isotopic values and the estimated age of early enamel disruptions suggest that solid foods were starting to be used as a substitute for breast milk at or before the ages of 2.5 and 3 years old.     

Archaeology in Gabon, 1886–1988

This is the first attempt at synthesis of archaeological research conducted in Gabon between 1982 and 1988. Middle Stone Age, Late Stone Age, Neolithic, Early and Late Iron Age data are discussed in the context of earlier discoveries and of current research in Central Africa as a whole.Though the Middle Stone Age remains undated, its earliest component clearly preceded 40,000 bp. The Late Stone Age is datedca 9000–2500 bp, with an early Neolithic perhaps as old as 5000–3000 bp. A late Neolithic is firmly dated to 2600–2200 bp. Iron smelting is shown to have begunca 2500 bp in inland areas of Gabon andca 2000 bp near the coast.

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Résumé On présente ici une première synthèse des données scientifiques obtenues au cours des travaux de 1982–1988 au Gabon. Les éléments relatifs au Middle Stone Age, au Late Stone Age, au Néolithique, aux Ages du Fer ancien et récent sont présentés. A chaque fois une discussion s'engage les mettant en relation avec le contexte global de l'Afrique Centrale ainsi qu'avec les découvertes antérieures.Quoique le MSA reste mal daté, il peut être démontré que les plus vieux outils ont au moins 40,000 ans d'âge. Le LSA quant à lui est circonscrit à la périodeca 9000–2500 bp, alors qu'un Néolithique ancien est peut-être situé vers 5000–3000 bp. Un Néolithique final est, lui, correctement daté vers 2600–2200 bp. Enfin, la fonte du fer est attestée à l'intérieur des terres dès 2500 bp alors que le littoral ne semble pas connaitre cette technologie avant 2000 bp.

     

Economic Change in the Prehistoric Hexi Corridor (4800–2200 bp), North‐West China

It is widely known that the Hexi Corridor in North‐West China lies at a hub of trans‐Eurasian cultural exchange. Its role became increasingly important during the late prehistoric period, particularly as the ancient Silk Road began to be used. While the profound transformation of local cultural characteristics in the late Neolithic and the Bronze Age is well documented, the detailed economic dynamics of cultural evolution have not yet been clearly illustrated. In this paper, we report on significant new zooarchaeological and faunal isotopic data from the Neolithic and Bronze Age sites in the Hexi Corridor. The primary objective is to systematically reconstruct the prehistoric economic context of this area by combining these new data with previous archaeological studies and radiocarbon dates. We argue that the primary economic activities of local inhabitants changed dramatically in the prehistoric Hexi Corridor. This was marked by agricultural production at c.4800–4000 bp , agro‐pastoral production at c.4000–3000 bp and animal husbandry at c.3000–2200 bp , respectively. The major subsistence strategies of these three periods show considerable variation. It is very likely that these transformations of economic patterns in the prehistoric Hexi Corridor were primarily triggered by transcontinental cultural exchange and, to a lesser extent, by climate change.     

Genesis,age and archaeological significance of a pedosediment in the depression around Tell Mozan,Syria

A pedosedimentological profile from the ditch surrounding the lower town of the Bronze Age site of Mozan is investigated for its soil and sedimentological characteristics and has been dated in order to gain information on the use of the ditch and on the landscape development surrounding the settlement. The depression did not contain large amounts of water (flowing or stagnant) and probably was used for agricultural purposes. Accumulation – that in part includes anthropogenically-derived, redeposited, and bioturbated debris – started at around 2800 cal. BC or later, and was especially intensive at some time between 2800 and 1000 cal. BC. Deposition may have been caused by intensive agricultural use of the landscape during the urban explosion of the Early Bronze Age or in the early Middle Bronze Age.