At the turn of the twentieth century, American logging companies backed by the US colonial regime initiated extensive extraction in Bikol, Philippines. Industrial infrastructure and the involvement of a newly assembled Bikolano workforce left a profound imprint on the region's landscape. This article discusses a collaborative archaeological project that used archival materials, place-name analysis, ethnographic interviews, discussions with local scholars, satellite mapping, and drone-mounted lidar scans of former industrial sites. Findings shed light on the enduring ramifications of American logging in the early 1900s on settlement patterns, the infrastructure of routes and mobility, the state of industries from Philippine independence in 1946 through the 1980s, and ongoing environmental hazards. These findings emphasize the legacy of American empire, reveal the role of Filipino logging workers in shaping the landscape through settlement decisions, and uncover intricate connections across a pan-Pacific American colonial frontier that was shaped by both extractive and settler colonialism. This article adds to an emerging trend in Americanist archaeology in which archaeology investigates recent historical and even contemporary events.

The Deliblato (Banat) Sand Sea, which is one of the largest areas of аeolian sand in Europe, is located near the Iron Gate, which marks the crossing of the Danube River through the biggest gorge of this river. Here, Danubian alluvium has served as the sand source for the Banat Sand Sea, which was formed primarily through southeasterly (Košava) winds. Utilizing a multi-proxy approach, the objective of this study is to gain a better understanding of the environmental dynamics of the Banat Sand Sea. To achieve this goal, we conducted an analysis of an archive representing an approximately 20-m-thick dune formation on the northern edge of this dune field. Using optically stimulated luminescence (OSL) dating, we calculated aeolian sedimentation rates and dune ages. Sand was deposited here approximately between 17 ka and 13 ka. Magnetic susceptibility, grain size, and colorimetric analyses were interpreted in terms of local paleoenvironmental conditions. Calculated sedimentation rates (SR) indicate intensive aeolian deposition during the study period that range from 483 cm/ka to 502 cm/ka. We compared our data with regional and other European archives, as well as with climatic variations recorded in the Greenland ice core North Greenland Ice Core Project (NGRIP).

This paper tests a new model to study the Roman conquest and colonization of the Western Mediterranean. This recent model depicts Roman expansion as a more sustainable process than previously assumed, which tapped into, reinforced and integrated wider Mediterranean settlement trends. Contrary to what is assumed by traditional narratives, colonization did not entail the immediate destruction and restructuring of native landscapes — but rather the integration, opportunistic reuse, appropriation and development of previous land-uses and settlements. Two legacy datasets collected through pedestrian survey in the colonial territories of Cosa (Italy) and Tarraco (Spain) were used to test this model on a supranational scale. The analysis indicated that certain portions of the native landscape were possibly integrated into the Roman Empire without initial drastic changes being reflected in the settlement patterns or the landscape.

Focusing on the late prehistoric southern Levant, we recently suggested that the diffused low-frequency distribution of large predator bones (lion, leopard and bear) coalesces into a coherent temporal pattern when observed at a sufficiently long timescale. While in the previous research we sought to determine what sort of sociocultural mechanism might explain this pattern, effectively drawing it into the orbit of the familiar, in this brief provocation, we push in the other direction, towards the unfamiliar: how can a process or phenomenon be culturally significant yet meaningless at the human and societal levels? How is a phenomenon substantial in the long term and insubstantial in the short term?

In the summer of 2022, Tulane University, in collaboration with archaeologists from other institutions, began excavations at the site of Pompeii. The archaeological work was focused on Insula 14 of Region 1, located in the southeastern sector of the site. To overcome the challenges of recording a complex urban excavation, and of working with a collaborative team, we designed and implemented a unique workflow that combines paperless and 3D data-capture methods through the use of GIS technologies. The final product of our documentation workflow was a robust and easy-to-use online geodatabase where archaeologists can revisit, explore, visualize, and analyze each excavated context using virtual tools. We present our workflow for digitally documenting observational and spatial data in the field, and how we made these data available to project archaeologists during and after the field season. First, we describe the development of digital forms in ESRI's Survey123. Then, we explain our procedures for 3D documentation through SfM photogrammetric methods and discuss how we integrated the data and transformed it into an accessible format by using interactive dashboards and online 3D web scenes. Finally, we discuss the components of our workflow that are broadly applicable and that can easily be adapted to other projects.

El objetivo principal de este trabajo es presentar importantes novedades sobre el marco histórico y productivo de la explotación minera de la sierra de Corduba en época romana, así como de la gestión de sus recursos. Desde hace años y a partir de la documentación epigráfica disponible, se ha venido apuntando una posible presencia en este territorio de la societas Sisaponensis y de la explotación de plomo y plata por su parte, a pesar de la afamada vinculación con el beneficio del cinabrio que recoge un conocido pasaje de Plinio. Nuestras investigaciones en el norte de Córdoba y los análisis arqueométricos realizados sobre tres lingotes de plomo recuperados en el paraje de Los Escoriales de Doña Rama, situado en la Sierra de Gata (Belmez-Córdoba), suponen una superación de la frontera del conocimiento sobre los aspectos reseñados, ya que permiten contrastar estas dos hipótesis tradicionales y proponer nuevas cuestiones sobre la explotación de estos parajes y la actividad de esta societas. Estos lingotes fueron encontrados en una instalación minero-metalúrgica romana, algo que es excepcional, y conservan una inscripción, S S, que los vincula sin duda con la societas Sisaponensis.

The production and distribution of ceramic building materials (CBM) in the Roman period have long attracted the attention of archaeologists, as they provide clues to aspects of trade, identity, and technological and architectural traditions. However, there has been a notable scarcity of studies focusing on plain CBM in the southern Levant, particularly in the Mediterranean coastal region. This study concentrates on CBM (bricks, tubuli, drainage pipes, and roof tiles) from a Roman-period wealthy farmstead (Khirbat Khaur el-Bak) near the city of Ashqelon/Ascalon, apparently owned by a serving member of the military or a veteran. The petrographic analyses indicate that apart from the locally produced drainage pipes, the CBM were imported from overseas, namely Cilicia and Beirut. The results shed light on CBM trade in the Eastern Mediterranean, and on the complex nature of the population and material life in and around Roman Ashqelon, which included local and foreign elements.

This article focuses on the ancestral human remains of Indigenous peoples that were taken by European invaders during the colonial era. It begins by considering the notion of human remains. It then describes the two types of heritage that result from the removal of human remains: the tangible heritage made of the remains exhibited or stored in the museums or universities of former colonial States, and the intangible heritage made of the collective memories of the surviving communities and their descendants about the removal (and the absence) of the stolen remains. The article next examines the role of national and international laws with respect to the restitution of human remains by exploring the concept of transitional justice. This article argues that transitional justice can facilitate the meaningful repatriation of ancestral human remains and hence the healing of past injustice.

The results of radiocarbon variation studies observed in annual tree rings from the NW Pacific (USA Northwest) (Stuiver and Braziunas 1993) and Europe (England, Brehm et al. 2021; Slovakia, Povinec 1977, 1987) are reviewed with the aim of better understanding the 11-year radiocarbon cycle and possible impacts of solar proton events on 14C levels in the atmosphere and biosphere. The average Δ14C amplitude in tree rings for the period of 1798–1944 was 1.3 ± 0.3‰, the average periodicity was 11 ± 1 years, and the average time shift between the sunspot numbers and Δ14C records was 3 ± 1 years. A new solar activity minimum (Gleissberg minimum, 1878–1933) has been identified in the Δ14C data sets from the NW Pacific and England, showing Δ14C excess of 7‰, comparable to the Dalton minimum (1797–1823). No significant changes in Δ14C levels were identified that could be associated with solar proton events during 1800–1950.

The AMS Golden Valley laboratory is equipped with two accelerator mass spectrometers: the AMS facility from the Budker Institute of Nuclear Physics (BINP) and the Mini Carbon Dating System (MICADAS-28) from Ionplus AG and two graphitization systems: the Automated Graphitization Equipment (AGE-3) from Ionplus AG and the Absorption-catalytic setup (ACS) developed at the Boreskov Institute of Catalysis (BIC). The ACS was designed for graphite preparation from labeled biomedical samples, dissolved organics, and dissolved or gaseous carbon dioxide but has proven to be suitable for the traditional dating of objects no older than 35,000 years. Here we present two series of AMS data for the samples from Glasgow International Radiocarbon Inter-comparison (GIRI), prepared using AGE-3 and ACS, and then measured on MICADAS-28. The mean value of the background F14C was 0.0024 ± 0.0009 and 0.012 ± 0.003 for AGE-3 and ACS, respectively, and both methods gave reproducible results for the OXI.

This article traces a statue, which Zenon of Aphrodisias carved, from Syracuse to its discovery at the Palace of Cogolludo in 2007. The study of this statue of the Muse Euterpe broadly demonstrates the appreciation for a figure from the classical world to Early Modern Europe and focuses attention on two understudied moments in the history of sculpture. It shows that Zenon carved the figure in the 4th c. CE, and its story reveals new connections between sculptors of Aphrodisias and specific patrons of the period. The statue's subsequent history attests to the high regard for ancient art and epigraphy in the Iberian Peninsula in 1500–1700. Since the statue probably belonged to Luis de la Cerda, ninth Duke of Medinaceli, it draws attention to a remarkable patron and a neglected aspect of Spanish cultural history.