Old collections, real or fake, are a basic part of the collection history of an antiquity or artwork. This article is a starting point for a study of the concept: how old collections are employed, what functions they have, and how fictitious old collections are chosen and constructed. To explore these concepts, the article considers the example of Cumberland Clark, an early 20th-century collector who serves as the putative origin of cuneiform tablets in a handful of present-day collections, most notably the Schøyen Collection. This article looks at the life and collections of Cumberland Clark, then argues that the Clark provenance for current collections is a fabrication, and concludes by looking at Clark in the context of other old collections in order to draw some lessons about fabricated provenance.

Sudden annual rises in radiocarbon concentration have proven to be valuable assets for achieving exact-year calibration of radiocarbon measurements. These extremely precise calibrations have usually been obtained through the use of classical χ2 tests in conjunction with a local calibration curve of single-year resolution encompassing a rapid change in radiocarbon levels. As the latest Northern Hemisphere calibration curve, IntCal20, exhibits single-year resolution over the last 5000 years, in this study we investigate the possibility of performing calibration of radiocarbon dates using the classical χ2 test and achieving high-precision dating more extensively, examining scenarios without the aid of such abrupt changes in radiocarbon concentration. In order to perform a broad analysis, we simulated 171 sets of radiocarbon measurements over the last two millennia, with different set lengths and sample spacings, and tested the effectiveness of the χ2 test compared to the most commonly used Bayesian wiggle-matching technique for temporally ordered sequences of samples such as tree-rings sequences, the OxCal D_Sequence. The D_Sequence always produces a date range, albeit in certain cases very narrow; the χ2 test proves to be a viable alternative to Bayesian wiggle-matching, as it achieves calibrations of comparable precision, providing also a highest-likelihood estimate within the uncertainty range.

Ocean radiocarbon (14C) is a proxy for air-sea exchange, vertical and horizontal mixing, and water mass identification. Here, we present five pre- to post-bomb coral Δ14C records from West Flower Garden Bank and Santiaguillo reefs in the Gulf of Mexico, Boca de Medio, and Isla Tortuga near the Cariaco Basin north of Venezuela. To assess basin-wide Δ14C variability, we compiled the Atlantic Ocean reef-building surface coral Δ14C records (24 corals and 28 data sets in total) with these new records. Cumulatively, the Δ14C records, on their independent age models, reveal the onset of post-bomb Δ14C trends in 1958 ±1 to 2 years. A general decrease in maximum Δ14C values occurs with decreasing latitude reflecting the balance between air-sea gas exchange and surface water residence time, vertical mixing, and horizontal advection. A slightly larger atmospheric imprint in the northern sites and relatively greater vertical mixing and/or advection of low-14C waters influence the southern Caribbean and eastern Atlantic sites. The eastern Atlantic sites, due to upwelling, have the lowest post-bomb Δ14C values. Equatorial currents from the eastern Atlantic transport low Δ14C water towards the western South Atlantic and southern Caribbean sites. Decadal Δ14C averages for the pre-bomb interval (1750–1949) for the low latitude western Atlantic are relatively constant within analytical (3–5‰) and chronological uncertainties (∼1–2 years) due to mixing and air-sea exchange. The compiled Δ14C records provide updated regional marine Δ14C values for marine reservoir corrections.

The Cunene region of southern Angola, especially the area around Xangongo, hosts a large number of African baobabs, including several superlative specimens. Our research reports the investigation of the three biggest specimens from Xangongo Grove, named XG-1 (11 stems; circumference 26.34 m), XG-2 (5 stems; 22.70 m) and XG-3 (9 stems; 27.73 m), and of the largest baobab from Xangongo town, named XT-1 (7 stems; 21.02 m). Several wood samples were collected from these four baobabs mainly as cores from trunks and/or primary branches and then radiocarbon-dated by AMS. The two oldest samples were extracted from two primary branches of baobab XG-1. These have practically identical radiocarbon dates of 1822 ± 19 BP and 1822 ± 10 BP, which correspond to identical calibrated ages of 1785 ± 15 and 1785 ± 10 calendar years. The calculated age of baobab XG-1 is 2100 ± 50 years. Thus, XG-1, which is called by the locals “The biggest baobab of Africa”, becomes the oldest living African baobab with accurate dating results. The results indicate ages of 1100 years for baobab XG-2, 850 years for baobab XG-3 and 550 years for baobab XT-1.

We report a set of radiocarbon dating of prehistoric settlements located on the paleolake Baruun Khuree shores in the Gobi-Altai area, southern Mongolia. The obtained series of 11 AMS 14C measurements on charcoal and other charred plant macro-remains can be associated with one of the earliest episodes of the Holocene highly mobile desert-adapted hunter-gatherers activities from the Gobi desert (ca. 11,250–10,500 cal BP). Exploiting a wide range of environments, including dune fields, they are characterized by pottery usage and microblade core technology with wedge-shaped cores as well as osteological materials. These preliminary results are part of a project analyzing the nature of long-lasting prehistoric occupation around Tsakhiurtyn Hundi (Eng. Flint Valley)—one of the most extensive early prehistoric sites of Central Asia owing its name to the presence of abundant flint outcrops, lithic workshops and their innumerable flint artifacts.

The archaeological settlements of the Early Neolithic Urfa region in Türkiye have garnered academic and public interest since the 1990s due to their large-scale stone architecture and rich iconography, particularly featuring phallic imagery. While mainstream narratives suggest a male-centred society in the region, feminist and queer theory approach such interpretations with a critical eye. By challenging traditional ‘male-centred society’ narratives through the lens of queer and feminist theories, this study offers a critique of existing methodologies that fail to historicize archaeological data. By recontextualizing the phallic iconography through the lens of sexuality, this study proposes a new interpretation: the phallus was not a symbol of male power, but an agent facilitating spiritual transcendence, enabling ecstatic experiences and serving as a conduit between the material and spiritual realms.

Within this paper, glocalization is presented to explain the heterogeneity of the Uruk Expansion/Phenomenon, a process which saw extensive interactions and cultural integration across Mesopotamia during the fourth millennium bce, characterized by the spread of southern Mesopotamian material culture and cultural practices. Through close examination of archaeological data from the Adhaim-Sirwan Drainage Basin, southern Iraqi Kurdistan, a region which is emerging as a focus of intense culture-contact during the Uruk Phenomenon, I contend that a glocalized perspective of this phenomenon better illuminates its regional nuances and complexities, as well as the interactions between local and Uruk communities within the Adhaim-Sirwan. By employing a glocalizing framework, this paper demonstrates that cultural interactions led to varied adaptations of the Uruk Phenomenon and illustrates the dynamic interplay between global influences and local responses. Ultimately, this paper advocates for a nuanced understanding of the Uruk Phenomenon, highlighting its regional variability and the importance of local agency in shaping cultural outcomes, thereby framing it as a distinctly glocalized process rather than an expression of globalization.

Migration is an established topic in archaeology, approached by researchers in multiple ways. We argue, however, that new ways of thinking are needed to understand migration in new ways in relation to new results coming from ancient DNA studies and other archaeometric analysis. We apply a transdisciplinary approach and engage with (critical) migration studies, critical heritage studies and archaeology to unwrap essential theoretical aspects of migration. Based on our results, we propose a conceptual/theoretical framework as our contribution to migration studies in archaeology.

The Late Neolithic and Early Bronze Age (c. 2900–1600 bc) of Central Europe are characterized by burial practices that strongly differentiate between men and women through body placement and orientation in the grave, as well as through grave goods. The osteological sex estimation of the individuals from the cemeteries of Franzhausen I and Gemeinlebarn F corresponds to the gender expressed in the funerary practice in 98 per cent of cases. In this study, we investigate the remaining minority by applying ultra-high-performance liquid chromatography–high-resolution mass spectrometry (UHPLC-HRMS) to identify sex-specific peptides in the dental enamel of 34 individuals, for which the published osteological sex estimation did not fit the gendered burial practice. The results reveal sex estimation and transcription errors, demonstrating that the chromosomal sex of the individuals usually aligns with the gendered burial treatment. We found burials with internally inconsistent gendered patterns (‘mixed-message burials’), but there is no evidence to suggest that a biologically male individual was deliberately buried as a woman or a biologically female individual was buried as a man.