While recent genomic and isotopic information show that migration has been pervasive along human history, southern Andean archaeology has largely overlooked its importance in shaping human trajectories of sociocultural change. Building on previous isotopic research that identified the presence of migrant farmers in the Uspallata Valley (Mendoza, Argentina), we present chronological and bioarchaeological results that help to characterize the timing and mode of human migrations in the southern Andes. The burials with migrants show the representation of the different age classes, including a high abundance of children, as well as both men and women, suggesting that family groups were likely involved. The Bayesian modeling of 16 direct dates for migrants indicates that these migrations started between 1210–1275 CE (median 1255 CE) and finished at 1320–1425 CE (median 1360 CE), indicating that there is nearly no overlap between the commencement of this migration phase and the southwards expansion of the Inka Empire. The model defines a diachronic process that lasted between 55 and 195 years, implying that migration to Uspallata was a multi-generational process that involved between two and eight generations (median of four generations). Our contextual, bioarchaeological and chronological evidence indicates that the conditions fostering migration to Uspallata were sustained through time, inviting to explore persisting push-pull dynamics acting during this period. 87Sr/86Sr results show that migration occurred across the daily territories of these groups and may have involved movement across social or ethnic frontiers.

Between 1969 and 1975 the excavations promoted by the Soprintendenza alle Antichità dell'Etruria Meridionale in the area to the east of the church of Santa Maria of Falleri identified a building in opus quadratum, located at the intersection between the main east–west and north–south urban road axes. As part of the Falerii Novi Project, this area has been systematically surveyed and (re)studied, applying an interdisciplinary approach. This has allowed the identification in this area of a monumental republican temple, linked to the forum, which should be placed in the context of the earliest development of the town, which has been known to us up to now only via literary sources. The identification of the republican temple of Falerii Novi contributes to fresh insights into the foundation of the town and its urban development.

Although Greek was the dominant epigraphic language in Cyrenaica throughout the Classical period, Latin was introduced by Roman merchants and administrators at the time of the formation of the province of Crete and Cyrene c. 67 BC, and remained in use, albeit by a constant minority, until at least the fourth century AD, with the last well-dated Latin inscription dating from the Valentinian dynasty. The aim of this article is to provide an overview of Latin inscriptions in the region, based on the IR Cyrenaica 2020 corpus, which brings together hitherto scattered documents and also includes many texts published for the first time. After a general overview of the corpus in terms of geographical, typological and chronological distribution, we will look at the linguistic landscape of ancient Cyrenaica, focusing on the multilingualism of the region, the literacy of the populations, the borrowings from one language to another (Latinisms), and the influences of the western provinces on the Latin of the region, among other topics. Lastly, a series of Latin funerary inscriptions allow us to examine the multiple identities claimed by the populations, as well as the cultural influences between Greek-, Latin- and Libyan-speaking populations.

The dietary habits of Neanderthals are considered an issue of great interest in the literature and have opened an important number of fruitful debates. Indeed, understanding diets can provide important information regarding issues of palaeoenvironmental reconstructions and subsistence strategies. In this respect, dental remains can play a vital role in the conducted efforts to reconstruct the palaeoecological niches securely and accurately since dental microwear analyses have precisely detected dietary patterns of the populations in the past. In this context, the Iberian Peninsula forms an interesting model for examining Neanderthal populations, their subsistence strategies, and adaptive skills. This study aims the examination of already published data in order to provide a holistic approach regarding the dietary habits of H. neanderthalensis populations in the Iberian Peninsula, along with the importance of the utilization of dental microwear analysis in the archaeological record.

Egyptology has been changing. At least in the way its practitioners present their findings to a broad public audience. A selection of recent publications for general-interest readership represents something of a reorientation of perspectives on the (Western-led) archaeological ‘discovery’ of Pharaonic Egyptian remains, and the opening up of a subtle counter-narrative, which is something of an anti-archaeology. Rather than attempting to reconstruct what might positively be said of ancient events, their causes and motivations, Egyptologists are increasingly owning up to what is not known or what happened in the aftermath of the ‘main event’ that conditions the nature of the evidence we have at our disposal.

The mountain communities of late-first millennium bc Italy have been regarded as non-urban societies that reverted to city life mainly owing to Roman intervention. A growing body of archaeological evidence is uncovering the diversity of settlement forms and dynamics in the region's pre-Roman past, which included sites encompassing a range of functions and social agents. This article presents an in-depth, microscale analysis of one such site, Monte Vairano in Samnium, drawing on perspectives from comparative urbanism. Monte Vairano developed urban characteristics such as a complex socioeconomic profile and political cohesion, as well as potentially more unique features such as an apparently balanced distribution of wealth. These results can shed further light on the diversity of ancient urbanization and its sociopolitical implications in late-first millennium bc Italy and the Mediterranean.

The fluvial capture of endorheic basins represents a milestone in basin chronology, implying a profound disequilibrium that triggers critical geomorphological, sedimentological, paleogeographic, and even paleoecological transformations. The primary goal of many geomorphological studies is to determine the timing of endorheic-to-exorheic transitions with the objective of unveiling the dynamics that follow the capture event. The age of the Guadix-Baza Basin capture in the Central Betic Cordillera (S Spain) remains a subject of controversy, with proposed estimates ranging from 17 to 600 ka. In this study, we present new 234U/230Th and optically stimulated luminescence ages from exorheic deposits exposed within the basin's main fluvial valley, the Guadiana Menor River. We acquired the oldest numerical age recorded to date for a postcapture deposit within the basin. This age corresponds to a travertine platform formed 240.8 ± 25 ka on a surface level that was already incised into the glacis surface at approximately 250 m. Using these data, we estimate that basin capture took place earlier than ca. 240 ka, plus the time required for the river to incise 250 m to the position of the travertine. Furthermore, the proximity of the Matuyama-Brunhes reversal (781 ka) to the top of the endorheic succession and the ages of the paleontological sites (> ca. 750 ka) throughout the basin suggest that the capture could have occurred earlier than the oldest previously proposed age of 600 ka.

The present study offers an epistemological and ontological historiographical review of the concept of the unit of analysis using island archaeology as a case study. We carry out a critical investigation to lay out the main ideas used to define units of analysis, and we consider the discourse that has emerged between this and other fields when defining such a concept. From an epistemological point of view, we can define three distinct strategies: first, those that define units of analysis by their outer limits, their borders; secondly, those that make the definition based on the internal dynamics taking place within the units of study; and in third place, strategies that focus on defining the analytical unit as a set of interactions between agents. From a more ontological point of view, we can differentiate between strategies that take on a categorical perspective and those that take on a more relational perspective. Ultimately, we reflect on the conceptualization and function of the unit of analysis in the process of interpretation, and in so doing, we provide evidence of the great theoretical richness of the concept and the multiple interrelated factors involved in its development.

Western Anatolian ritual pits provide valuable insights into socio-cultural, economic and symbolic practices during the Early to Middle Bronze Age. Findings in feasting pits, such as carbonized seeds and animal bones, indicate a strong link between ritual and food. Standing stones, altars and carefully arranged artefacts suggest a symbolic and sacred dimension beyond mere ceremonies. The pits from this period contain carbonized seeds and fragments of wood, indicating the presence of small fires during certain rituals. Changing features in ritual pits from the Early to Middle Bronze Age reveal a dynamic relationship between spatial arrangements and religious practices. The study shows that in the first half of the second millennium bce several ritual activities known from different regions reached western Anatolia for the first time. Interregional trade involved not only goods, but also the dissemination of rituals over a wide geographical area. This cultural interaction reveals western Anatolia as a dynamic and influential centre in this historical period. By exploring the ritual practices of second-millennium bce western Anatolia, this paper presents new perspectives on the rituals of the region.

This study explores patterning in δ18O values of tooth enamel in contemporary African herbivores from mainly C3-dominated ecosystems. Evapotranspiration causes plants to lose H216O to a greater extent than H218O, leaving leaves enriched in 18O. In eastern Africa, ES species (evaporation-sensitive species: those obtaining water from food) tend to have more positive δ18Oenamel values than EI species (evaporation-insensitive species: those heavily dependent on drinking water); the magnitude of the difference increases with increasing aridity. We find the same pattern applies in the winter and year-round rainfall region of southern Africa, allowing us to use δ18Oenamel in fossil animals to examine paleo-aridity. We apply this approach to infer aridity at Quaternary fossil assemblages from present-day winter and year-round rainfall zones, including Elandsfontein (ca. 1–0.6 Ma), Hoedjiespunt (ca. 300–130 ka), and Nelson Bay Cave (23.5–3 ka). This analysis suggests that (1) at various times during the Pleistocene, Elandsfontein and Hoedjiespunt environments were wetter than last glacial maximum (LGM) to Holocene environments at Nelson Bay Cave (year-round rainfall zone); and (2) considered alongside other evidence from the year-round rainfall zone, wetter conditions across the Pleistocene–Holocene transition at Nelson Bay Cave suggests that climate changes at near-coastal sites may be out of phase with the adjacent interior.