This paper considers the shift from the practice of collective burials to individual (or double) burials in western Europe at the end of the Neolithic/Copper Age, around 2500–2000 BC, through the lens of a particular mortuary site—the artificial cave of Bolores (Torres Vedras, Portugal). It suggests that the practices involved in making and using collective burials played an important role in this transformation towards increasing social differentiation. It explores how a focus on materiality at different scales, both temporal and spatial, might contribute new insights into geographically widespread and relatively co-synchronous social change.

This study reconstructs the Alfredian network as consisting of twelve actors. This network is termed a coalition, within which a cluster of Mercian actors is further hypothesised. Historical sources and charter evidence suggest that Mercian scribes worked for West Saxon kings and may even have taken part in the establishment of a proto-chancery at the royal court. This writing office can be conjectured to have ties with the Alfredian coalition and described as a community of practice. The whole sociolinguistic reconstruction is supported by three case studies: Angelcynn ‘the English people’ and here ‘band, troop’ in historical-political genres, and gretan freondlice in epistolary genres. The diffusion of these Alfredian norms across time, place and genres is linked to the royal chancery and its distribution channels, as well as to the diachronic sustainability of linguistic practices within professional discourse communities and their archives.

This article aims to provide an interpretation of the structure and spatial patterning of the non-ceramic refuse from the Neolithic site of Bylany. The data are considered at three levels: tackling questions of refuse management and deposition in the vicinity of houses; the spatial distribution of refuse within the settlement area as a whole; and the quantity and structure of non-ceramic refuse from a long-term settlement perspective. The analysed assemblage of non-ceramic finds is divided into five categories: chipped stone, polished stone, whetstones, manos/metates, and other stones without use-wear traces. The analysis is based on GIS and multivariate statistics. The spatial distribution and quantity of refuse are analysed with respect to space (in terms of proximity to Neolithic houses and the whole of the excavated settlement area) and time (the duration of settlement in six chronological stages). No deliberate pattern of refuse management was identified in the vicinity of the houses, but the refuse was found to have a tendency towards peripheral grouping within the settled area as a whole. Refuse quantity depends on the number of houses and settlement duration. The negative correlation between the mean density of non-ceramic artefacts per house and the number of houses in corresponding chronological stages may be explained by the interpretation that refuse was commonly deposited within abandoned houses, which would be consistent with ethnoarchaeological observations.

Accurate mapping of the 78-ha Roman town of Viroconium (modern-day Wroxeter in Shropshire, UK) in preparation for detailed research and site management proved a task that requires the use of modern information techniques. This article describes the creation of high spatial accuracy maps by the use of GPS-located gradiometer survey data in order to georeference available aerial photographs, and the use of digital processing of aerial photographs to obtain additional information invisible to the unaided eye. A GIS is being used to build a vectorized interpreted map of the town with a spatial error typically less than one metre. The results compare favourably with previous mapping efforts based on traditional methods.

Considerable debate persists concerning the origins of those involved in the adventus Saxonum: the arrival of Germanic peoples in Britain during the fifth century AD. This question was investigated using oxygen and strontium isotope ratios obtained from archaeological dental samples from individuals in the ‘Migration Period’ cemetery, Ringlemere, Kent (n = 7) and three continental European sites (n = 17). Results demonstrated that strontium alone is unable to distinguish between individuals from south-east England and north-west Europe. Although 87Sr/86Sr values from Ringlemere fell within local biosphere parameters and suggest a spatially and temporally related group, δ18O values were inconsistent with origins in eastern England or on the North German plain. Results from the European sites negate past climate change as an explanation. It is possible that culturally mediated behaviour has obscured geographical relationships. Further work to characterize water sources and human δ18O values in the putative European homelands is required.