Excavations at Trecastell, Powys, south Wales, in 2007 yielded a copper halberd complete with its haft-grip. This has major implications for the mode of hafting halberds, but the discovery has also prompted a reconsideration of insular halberds in their north-west European context. Understanding the relationships between different types of halberd and different regional groups continues to be hampered by the dearth of good dating evidence, but the creation of better classifications for British and Irish weapons and new radiocarbon dates on two examples, one being Trecastell, have allowed a new developmental scheme to be advanced.

The emergence of metal-headed halberds is considered more generally. While it is acknowledged that halberd-like implements pre-existed in other materials in some parts of Europe, it is argued that the appearance of metal-headed halberds depended on the transmission of a particular set of metallurgical and related skills. A new model for the vigorous uptake of halberds on a regional basis helps explain the patchiness and anachronism of halberd hotspots.

The Trecastell halberd adds to one of the significant concentrations of the weapon type in Britain and prompts a more general review of the earliest metalwork from Wales and the Marches. For the Chalcolithic, halberds are instrumental in identifying a major contrast in depositional behaviour; this contrast dissolves at the beginning of the Early Bronze Age when a ‘new deposition ground’ is established. The former is attributed to the existence of a regional group across much of the region for whom the halberd served as a cultural icon, while the latter may relate to the demise of this enshrined value for the halberd.

In the course of making a digital record of a bow engraved on the lower face of a capstone in the Déhus passage grave, on Guernsey, several new motifs were observed, necessitating a reinterpretation of the composition as a whole.

While the presence of a bow and two arrows is confirmed by photogrammetry and images obtained under directional lighting, the anthropomorphic figure can now be better defined, and compared to figures recently recognised in the Paris Basin. The presence of ‘hands’, however, cannot be confirmed, and these engravings may instead represent two horned animals in contact with two further motifs, one of which is certainly a throwing stick.

This paper explores how geophysical survey, undertaken in conjunction with landscape and historical analysis, is contributing to a deeper understanding of prehistoric focal centres and landscape organisation in the wider ‘hinterland’ of the Hill of Tara, Co. Meath. Arising out of the Discovery Programme’s ‘Late Iron Age and ‘Roman’ Ireland’ (LIARI) Project, the present investigations targeted a number of prominent hilltop sites in the Meath–north Dublin region suspected, on the basis of archaeological, topographical, and early documentary evidence, to have been important ceremonial/political centres in later prehistory. Foremost among these are the Hill of Lloyd (Co. Meath), the location of a prehistoric enclosure overlooking the early monastic foundation at Kells; Faughan Hill (Co. Meath), the traditional burial place of Niall of the Nine Hostages; and Knockbrack (Co. Dublin), whose summit is crowned by a large, internally-ditched enclosure with central burial mound. The discovery through this multi-disciplinary study of additional large-scale enclosures, burial monuments, and other significant archaeological features serves to further corroborate the deep historical importance of these sites, and opens up new avenues for exploring such themes as territoriality, social organisation, and identity in the wider Tara region.

As a result of the exclusive use of extremely small megaliths (miniliths), the prehistoric stone settings of Exmoor, south-west England, challenge current approaches to the interpretation of monumental stone architecture during the later Neolithic and Early Bronze Age. Whilst the broader context of the practice of erecting tiny upright stones (a seemingly diverse and widespread phenomenon) and the reasons why this diminutive architecture has tended to escape sustained critical comment have been explored (smaller stone elements being relegated to a generalised background or subsidiary role such as ‘packing’), attempts to explain the settings have been remarkably few. Drawing upon the results of ten years of piecemeal fieldwork on the moor the present paper seeks to rectify this, arguing that far from being generalised ritual structures or metaphorical expressions of hunting groups, the tiny stones were, instead, an integral part of a dynamic human–animal landscape of movement and pause.

The implications of pit-deposits containing aurochs/Bos primigenius skulls dating to the Bronze Age, found in two recent excavations in Bedfordshire are outlined. Involving a review of related findings in south-eastern England, these serve as a platform to consider the dynamics of aurochs extinction, which is held to have occurred in Britain by the middle–later centuries of the 2nd millennium bc. It should be stressed that, although consulting many ‘expert’ colleagues, this paper is not written from a faunal remains-specialist perspective. It is essentially discursive and primarily intended to highlight a significant site-recovery trend. It reflects, moreover, on issues of broad social relevance. Holocene human-induced extinctions have both an inherent curiosity and poignancy. Indeed now, faced with currently threatened mass-species loss, they can even involve – beyond regret – a sense of cumulative guilt.

Non-invasive survey in the Stonehenge ‘Triangle’, Amesbury, Wiltshire, has highlighted a number of features that have a significant bearing on the interpretation of the site. Geophysical anomalies may signal the position of buried stones adding to the possibility of former stone arrangements, while laser scanning has provided detail on the manner in which the stones have been dressed; some subsequently carved with axe and dagger symbols. The probability that a lintelled bluestone trilithon formed an entrance in the north-east is signposted. This work has added detail that allows discussion on the question of whether the sarsen circle was a completed structure, although it is by no means conclusive in this respect. Instead, it is suggested that it was built as a façade, with other parts of the circuit added and with an entrance in the south.

Lead isotope analyses of 50 Irish Chalcolithic and Early Bronze Age gold artefacts favour a gold source in southern Ireland. However when combined with major element analysis, the artefacts are not consistent with any Irish gold deposit analysed to date. Understanding the lead isotope signatures of ore deposits within a study region allows informed inferences to be drawn regarding the likelihood that an unanalysed ore deposit was exploited in the past. If an Irish gold source is assumed, then the gold is most likely to have originated from deposits hosted by Old Red Sandstone in the Variscan ore field of south-west Ireland. However, based on our current understanding of mineralisation in the region, this scenario is considered unlikely. A non-Irish source for the gold is therefore preferred – a scenario that may favour cosmologically-driven acquisition, ie, the deliberate procurement of a material from distant or esoteric sources. Available geochemical data, combined with current archaeological evidence, favour the alluvial deposits of south-west Britain as the most likely source of the gold.

Neolithic ditched enclosures appear to be widely distributed across Central and Western Europe, and from the Mediterranean area to Scandinavia. They have been known in areas of Europe for a long time, but particularly in the last 25 years studies on British, French, Central European, and Scandinavian ditched enclosures have flourished. In line with this, a number of international meetings occurred in the last three decades. In southern Iberia, by contrast, ditched enclosures only began to be known in the 1970s, and even then methodological deficiencies and lack of funding hampered their characterisation. As a consequence of this, Iberian Neolithic and Copper Age ditched enclosures were largely unknown outside Portugal and Spain. They were not represented in any of the international meetings above, nor included in any of the syntheses made about the topic. Not only that, for decades, Spanish and Portuguese archaeologists were not aware of the potential analogies themselves, and the research that was being carried out elsewhere in Europe had almost no influence on the way ditched enclosures were surveyed, excavated, and interpreted in the peninsula. The main objective of this article is to advance the recognition of the southern Iberian evidence by other European researchers and the integration of the Iberian conversation into the general discussion. The focus will be on how these sites have been studied by several generations of Iberian archaeologists, in an attempt to explain why it has taken Portuguese and Spanish archaeologists so long to realise that Iberian enclosures should not be understood in isolation.

Recent radiocarbon dating of a skeleton from Balevullin, Tiree, excavated in the early twentieth century, demonstrates that it dates to the Neolithic period, rather than the Iron Age as originally expected. Osteological examination suggests that the individual was a young adult woman, exhibiting osteological deformities consistent with vitamin D deficiency, most likely deriving from childhood rickets; an exceptionally early identification of the disease in the UK with potentially significant social implications. Isotopic analysis supports the osteological evidence for physiological stress in childhood and further suggests that the woman was most probably local to the islands. Analysis of the surviving written archive reveals that the surviving skeleton was one of several originally recovered from the site, making Balevullin an exceptionally rare example of a British Neolithic inhumation cemetery.

Excavations in 2008 on the site of a proposed new prison at Belmarsh West, London Borough of Greenwich, found the heavily decayed remains of two superimposed Early Neolithic trackways. These structures, which are radiocarbon dated to the first quarter of the 4th millennium cal BC comprise some of the earliest structures yet encountered in the London Basin. The trackways were found towards the base of a peat sequence, immediately above the underlying Devensian gravels. The associated palaeoenvironmental record suggests that they were constructed in response to rising base levels, within a local floodplain environment dominated by alder carr, in order to maintain mobility across an expanding wetland landscape. The archaeological and geomorphological background to the excavations and a description of the results of the excavations are presented, with a particular emphasis on the Neolithic structures. The significance and wider context of the structures are examined through a consideration of their construction, wider palaeoenvironmental context, and the ways in which the structures can shed light on the nature of Early Neolithic subsistence strategies and land-use within the Thames floodplain.

Based on recent evidence from both archaeological and natural sciences, in this paper we would like to sketch a historical geography of Europe and the Mediterranean around the year 1600 bc and then discuss the changes observed during the 16th century bc in relation to a possible correspondence with the Thera eruption. Our point of departure will be the sequence of events that took place during the months and years just before, during, and immediately after the Thera eruption. The available archaeological evidence permits us to explore the response of the local and regional communities, the logistics that were mobilised, and the political decisions adopted in light of these events. From this local and regional scenario we will move on to discuss the changes occurring in Europe, the Mediterranean, and the Near East during the 16th century bc. At least four different socio-economic and political scenarios can be sketched, showing that the responses of Bronze Age societies were highly variable. At that point, we can ask how different political structures existing at the time reacted or were affected by the ecological and/or social dynamics. Basically, our itinerary concludes that the Thera eruption did not cause a severe climatic or environmental change, but touched the ideological realm particularly of those socio-political entities which were more dependent on complex ideological superstructures in order to legitimate extreme economic exploitation.

This paper presents new AMS dating of organic finds from the Shigir (Shigirsky) peat bog, located in the Sverdlovsk Province, Kirovgrad District of the Urals. The bog is located immediately south of the river Severnaya Shuraly, with the Urals to the west. Intermittent survey and excavation has been undertaken at this location since 1879, resulting in the recovery of in excess of 3000 cultural artefacts, including oars, sculptures of birds, snake figurines, wooden skis, arrowheads, and fish hooks. The dates presented here indicate that not only is there a long duration of human use of the wetlands at Shigir, but that the artefact forms also appear to have a significant duration of use throughout the earlier prehistoric periods considered here.

New radiocarbon dates for the Neolithic settlement at Pool on Sanday, Orkney, are interpreted in a formal chronological framework. Phases 2.2 and 2.3, during which flat-based Grooved Ware pottery with incised decoration developed, have been modelled as probably dating to between the 31st and 28th centuries cal bc. There followed a hiatus of a century or so, before the resumption of occupation in Phase 3, which has a different Grooved Ware style featuring the use of applied decoration. This has been modelled as probably dating from the 26th to the 24th centuries cal bc. The implications of these results are discussed for the emergence and development of Grooved Ware, and for the trajectory of settlement and monumentality on Sanday.

Iron Age tankards are stave-built wooden vessels completely covered or bound in copper-alloy sheet. The distinctive copper-alloy handles of these vessels frequently display intricate ‘Celtic’ or La Tène art styles. They are characterised by their often highly original designs, complex manufacturing processes, and variety of find contexts. No systematic analysis of this artefact class has been undertaken since Corcoran’s (1952a) original study was published in Volume 18 of these Proceedings. New evidence from the Portable Antiquities Scheme for England and Wales and recent excavations have more than quadrupled the number of known examples (139 currently). It is therefore necessary and timely to re-examine tankards, and to reintegrate them into current debates surrounding material culture in later prehistory. Tankards originate in the later Iron Age and their use continued throughout much of the Roman period. As such, their design was subject to varying influences over time, both social and aesthetic. Their often highly individual form and decoration is testament to this fact and has created challenges in developing a workable typology (Corcoran 1952a; 1952b; 1957; Spratling 1972; Jackson 1990). A full examination of the decoration, construction, wear and repair, dating, and deposition contexts will allow for a reassessment of the role of tankards within the social and cultural milieu of later prehistoric and early Roman Britain.

Over 40 years of archaeological investigations along the south coast of Papua New Guinea has identified a rapid succession of cultural changes during the late Holocene. The so-called ‘Papuan Hiccup’ (c. 1200–800 cal bp) is a poorly understood period of socio-economic upheaval along the coast, identified mainly from changes in archaeological ceramic styles and settlement patterns. During this period, the region-wide Early Papuan Pottery (EPP) tradition diverges into separate, localised ceramic sequences that have generic associations with local ethnographic wares. A correspondence between the timing of the Papuan Hiccup and a period of peak El Niño-Southern Oscillation (ENSO) activity implies a link between cultural and climate change. This paper explores this relationship further by examining changes in interaction networks along the south coast of Papua New Guinea, specifically focusing on chert artefacts. Chemical characterisation (portable X-Ray Fluorescence; pXRF) and technological analysis are used to map changes in lithic technology over time, including access to raw materials and technological organisation, at the site of Taurama, a prehistoric coastal village site that was occupied both prior to and after the Papuan Hiccup. Although the sample sizes are small and the interpretations necessarily circumscribed, it is argued that changes in the number of chert sources being exploited and in the intensity of core reduction at Taurama may be related to climate change in the region.

The Bronze Age was the first epoch in which societies became irreversibly linked in their co-dependence on ores and metallurgical skills that were unevenly distributed in geographical space. Access to these critical resources was secured not only via long-distance physical trade routes, making use of landscape features such as river networks, as well as built roads, but also by creating immaterial social networks, consisting of interpersonal relations and diplomatic alliances, established and maintained through the exchange of extraordinary objects (gifts). In this article, we reason about Bronze Age communication networks and apply the results of use-wear analysis to create robust indicators of the rise and fall of political and commercial networks. In conclusion, we discuss some of the historical forces behind the phenomena and processes observable in the archaeological record of the Bronze Age in Europe and beyond.