Research published in the last decade, which has provided data from both technological and morphometrical analyses of lithic points from southeastern and southern Brazil and Uruguay, suggests that there is much more cultural diversity among hunter-gatherers during the Early to Mid-Holocene than previously suggested by the Umbu Tradition model. Some of these studies have suggested new archaeological cultures and new definitions of lithic industries. In this article we present new data on another lithic assemblage that we associate with the Garivaldinense lithic industry and is found at the Pedro Fridolino Schmitz site. We also present, for the first time, the definition of two new types of lithic bifacial stemmed points. Our data suggest a low-density occupation of the site from the Middle to Late Holocene (8000–1000 BP) and some variability within the Garivaldinense industry throughout time and space.

This article presents a case of osteomyelitis variolosa from a skeleton excavated in the Western Cemetery at Cirencester (Corinium) in Britain, dated to the 3rd or 4th c. CE. This osteological condition is caused by the variola virus, the causative agent of smallpox, and is found in some individuals who have survived a childhood smallpox infection, the condition manifesting many years later. The significance of this discovery is that it indicates that smallpox had been introduced into the Roman world, and to Britain in particular, by the late 3rd or 4th c. CE. Rather than postulating a separate and unrecorded introduction of smallpox into the Roman empire, we suggest that this discovery strengthens the case for seeing the 2nd-c. Antonine Plague as an early form of smallpox.

This article reports from an interdisciplinary, archaeological and philosophical research project developing and using an analogue model in archaeological research. With prominent uses outside of archaeology, analogue models can offer a unique participatory perspective to prehistoric processes. As such the paper contributes to recent discussions in this journal and elsewhere on the role of games, play and gamification in archaeological research, teaching and cultural heritage. Our analogue model critically discusses cultural-evolution-based models of selected European Neolithic and Bronze Age models and develops a perspective based on the life history and the Capability Approaches. In times of climate and war stress, our model can offer a hopeful perspective of the human past, present and future without compromising on scientific insights.

On the upper reaches of the Tigris and Euphrates, archaeologists encounter evidence that challenges conventional understandings of early state formation as a transition from ‘small-scale, egalitarian’ to ‘large-scale, stratified’ societies. One such location is the Early Bronze Age cemetery of Başur Höyük, which presents evidence of grand funerary rituals—including ‘retainer burials’ and spectacular deposits of metallic wealth—in an otherwise small-scale, egalitarian setting. A further, puzzling feature of this cemetery is the preponderance of teenagers in the richest tombs. Here we describe the combined results of archaeological and anthropological analysis at Başur Höyük, including ancient DNA, and consider the challenges they pose to traditional accounts of early state formation.

Highly precise and reproducible radiocarbon (14C) measurements are regularly performed at the Heidelberg Institute for Environmental Physics, Heidelberg, Germany, in collaboration with the radiocarbon laboratory of the Curt-Engelhorn-Center Archaeometry in Mannheim, Germany. Here, we report an update of the technical details, focusing on the analysis of cold-water corals (CWC), and present an improved long-term blank value with a mean of (0.190 ± 0.064) pMC (n = 138) and excellent reproducibility of the IAEA-C2 standard with a mean of (41.15 ± 0.16) pMC (n = 75), consistent with its certified consensus value. Furthermore, 33 duplicates of the CWC 14C measurements agree within 2σ, 85% even within the 1σ range. This provides excellent conditions for accurate 14C measurements. As an application example, we present combined 230Th/U and 14C ages of a coral-bearing sediment core from the upper Mauritanian slope. The resulting ventilation age record confirms decreasing ventilation between 30 and 25 kyr BP, most likely reflecting a northward propagation of a water mass originating from the south. During the LGM, we confirm a previously hypothesized southward displacement of the Cap Verde Frontal Zone. With the onset of the deglaciation, our record documents again an advance of a southern-sourced water mass into the subtropical North Atlantic. During the Bølling-Allerød warm period, strong ventilation fluctuations possibly indicate temporal influence of southern-sourced water.

Earthworm biospheroids are a useful alternative to radiocarbon (14C) soil dating. In this study, we undertook a series of measurements to test the 14C dating potential/performance of recent earthworm biospheroid granules. A novel sample preparation protocol for 14C in biospheroids was developed and elaborated at Atomki (Institute for Nuclear Research) and tested on IAEA reference materials. 24 natural biospheroid samples were extracted from five different location/environment-eight topsoils (A-horizon soils). Bomb-peak-based, high-resolution 14C dating show very uniform 14C results at 105.6 ± 2.6 pMC (1σ) and none of the biospheroids are older than 30 yr. It also shows that no biospheroid with a 14C bomb-peak as high as that observed in the 1960s and 1990s were observed. The results confirmed that earthworms do indeed consume almost exclusively recent biogenic carbon, not other organic compounds or inorganic carbonates previously bound in the soil. The calendar age of their biospheroids were extremely close to the real (zero) age of the surface. Thus, no “reservoir effect” is seen for these macrofossils. We conclude that a biospheroid-based 14C age determination method may be suitable to measure the burial time as long as earthworm biospheroids can be found in the soil.

Throughout the Pleistocene, valley glaciers repeatedly advanced into the forelands of the European Alps. However, the corresponding geological record is highly fragmentary and the regional glaciation history, especially prior to the last glacial maximum, is still poorly documented. We explored the archives of the Lower Aare Valley in the confluence area of the Aare river with Reuss and Limmat, focusing on the overdeepened Gebenstorf-Stilli Trough. In four scientific boreholes, ∼350 m of drill cores were recovered, and complemented with investigations of outcrops and reflection seismics in the nearby glaciofluvial Habsburg-Rinikerfeld Palaeochannel. The integrative interpretation of these data provides new insights into the local landscape evolution: We identified two generations of glacial basin infill in the Gebenstorf-Stilli Trough that are overlain by glaciofluvial gravels, and two distinct glaciofluvial gravel bodies in the neighboring paleochannel. In this specific local setting, gravel petrographic compositions and their statistical analysis prove to be powerful tools to identify inputs from the confluent catchments, to aid in lithostratigraphic classification, and to interpret the depositional and landscape histories. We suggest that it is mainly the penultimate glaciation, characterized by three separate ice advances, that shaped the present-day study area, and whose deposits are preserved in the Middle Pleistocene archives.

Terrestrial proxies of wind direction spanning the last deglaciation suggest easterly winds were present near the Laurentide Ice Sheet margin in the North American midcontinent. However, the existence and spatial extent of such easterly winds have not been investigated with transient paleoclimate model simulations, which could provide improved dynamical context for interpreting the causes of these winds. Here we assess near-surface winds near the retreating southern Laurentide Ice Sheet margin using iTRACE, a transient simulation of deglacial climate from 20–11 ka. Near the south-central margin, simulated near-surface winds are northeasterly to easterly through the deglaciation, due to katabatic flow off the ice sheet and anticyclonic circulation. As the ice sheet retreats and the Laurentide High moves northeastward and weakens, near-surface northeasterly winds weaken. Meltwater fluxes also influence temperature and sea level pressure over the North Atlantic, leading to easterly wind anomalies over eastern to midwestern North America. The agreement between proxy and model wind directions is promising, although simulated easterly to northeasterly winds extend too far south in iTRACE relative to the proxy data. Agreement is also strongest in winter, spring, and fall, suggesting these may have been seasons with greater aeolian activity.

Integral to the fabric of human technology, knots have shaped survival strategies since their first invention. As the ties that bind, their evolution and diversity have afforded human cultural change and expression. This study examines knotting traditions over time and space. We analyse a sample of 338 knots from 86 ethnographically or archaeologically documented societies over 12 millennia. Utilizing a novel approach that combines knot theory with computational string matching, we show that knotted structures can be precisely represented and compared across cultures. This methodology reveals a staple set of knots that occur cross-culturally, and our analysis offers insights into their cultural transmission and the reasons behind their ubiquity. We discuss knots in the context of cultural evolution, illustrating how the ethnographic and archaeological records suggest considerable know-how in knot-tying across societies spanning from the deep past to contemporary times. The study also highlights the potential of this methodology to extend beyond knots, proposing its applicability to a broader range of string and fibre technologies.