A growing number of institutions that hold cultural heritage artifacts are now considering voluntary repatriations in which they choose to return an artifact despite unfilled gaps in their knowledge of its ownership history. But how are institutions to judge whether it is more probable that such gaps conceal theft and illicit export or are innocuous? Attempting to answer this question for Nepal, we examine published and archival records to trace the history of the growth in collecting of Nepali cultural heritage in the United States, with special attention to a 1964 exhibition at New York’s Asia Society Gallery, “The Art of Nepal,” and the activity of the New York dealers Nasli and Alice Heeramaneck. We conclude that the majority of Nepali heritage items in America entered after Nepal prohibited their export.

The formation and evolution of large-scale deposits generated by mass movement are often closely related to tectonic and climatic conditions. Investigating deposits under the influence of complex geological conditions can aid in reconstructing paleoenvironmental characteristics and fluvial geomorphic evolution. The First Bend of the Yangtze River (FBYR), located in the Jinsha River basin in southwest China, represents a significant section characterized by abundant allochthonous deposits. We conducted a detailed investigation of the Hongwen allochthonous deposit (HAD) and the river sediments in the First Bend. Through terrain interpretation, dating, and paleoenvironmental analysis, the HAD was determined to be a complex deposit with multiple sources and stages (46.4–33.5 ka), formed under the combined influence of tectonic activity and climate. Three mass-movement events occurred during the interglacial stage of the last glacial period or its transitional period, coinciding with the rapid uplift stage of the Tibetan Plateau since the late Pleistocene. Prominent features of this period include significant rainfall and tectonic activities. By dating fluvial sediments and examining the evolution of the HAD, we revealed a river incision rate of 2.30 mm/yr for the Jinsha River, providing a basis for analyzing periodic river cutting and the development pattern of surface processes.

To investigate long-term relationships between climate, vegetation, landscape geochemistry and fires in the boreal forest zone of Western Siberia, a sediment core of 345 cm was collected from Shchuchye Lake (located in south taiga zone of southeast part of West Siberian plain) and investigated by spore-pollen, radiocarbon, LOI and charcoal analyses. Quantitative palaeoclimate was reconstructed based on pollen data. Investigation revealed 13.2 cal ka history of vegetation, climate, landscapes and fires. In the dry climate of Late Glacial, the landscape was treeless. Continuous permafrost existed in the soil. In the middle of the YD cooling 12.4–12.2 cal ka BP, our data showed warming that caused degradation of permafrost in soils and settlement of spruce in moist places. Later, thawing and accumulation of moisture in a local lowering in relief increased and a lake was formed. With the beginning of the Holocene, the climate sharply changed to warmer and wetter. Intensified surface flow caused accumulation of mineral and carbonate fraction in the lake. Dense birch forests spread on drylands. As a result, the leaching regime initiated the formation of podzols in the soil. At about 10.0 cal ka BP, Scots pine (Pinus sylvestris) quickly spread in the area of investigation. Fires became more frequent and more intense during the dry Late Glacial time, sharply decreasing with increased precipitation in the Early Holocene, and again moderately increasing with spread of pine forests in the mid Holocene. With the transition to Late Holocene (after 6.0 cal ka BP), the intensity of regional background fires and number of local fires decreased.

Oral traditions describing details of ancient volcanic eruptions and their effects survive throughout the inhabited world. Many such eruptions, especially those having catastrophic environmental and societal consequences, proved sufficiently memorable to form the basis of enduring oral traditions. Using global databases, we identified 2306 such eruptions from 477 inhabited locations that occurred before the start of the Common Era (CE) and are therefore likely to have been the subject of oral traditions. Of these, we selected 20 events (‘remembered’ Holocene eruptions) for which there are extant oral (-derived) traditions that demonstrate how such traditions can reveal details of past volcanism that often are undetectable by retrodictive geoscientific enquiry. We also selected 20 events (‘forgotten’ Holocene eruptions) about which no oral traditions are known and discuss the possible reasons for this. Such oral traditions, while often challenging for conventionally trained geoscientists to interpret, are valuable yet largely overlooked sources of information about the nature and effects of Holocene volcanism that can usefully complement geoscientific enquiry. In particular, we identified locations where memories of such volcanism appear ‘forgotten’ in the hope that scientists might focus their attention on revealing, identifying, and analyzing local traditions.

People are often assumed to expand existing mechanisms—kinship in particular—to include others when they form communities. These models (con)fuse similarity with sameness, as we argue based on Husserl's concept of empathy. People recognize others without overlooking differences. They form community by negotiating belonging. We ask how individuals materialize community, how they create unity in a political process, and how they employ bordering and bonding social interactions. Our case study is Dos Ceibas, a Late Preclassic (350 b.c. to a.d. 250) Maya hamlet in the Petexbatun region. The North Plaza originated as a residential group—possibly of the hamlet's founder—and was transformed over multiple construction episodes into a public and ceremonial place. By a.d. 250, Dos Ceibas consisted of a small pyramid overlooking a plaza and two likely residential buildings. Its growth pattern sets the North Plaza apart from nearby Group MP16 and magnified internal differences. At the same time, Dos Ceibas's pyramid and plaza were likely communal constructions that project a shared community identity. The comparison with contemporary settlements nearby identifies distinct settlement layouts and suggests localized community identities.

This study aims to discuss the chronology of the Egyptian 5th dynasty of the Old Kingdom and the tentative date of accession of king Djedkare based on material from his royal necropolis at South Saqqara and non-royal cemetery of Abusir South, Egypt. A series of radiocarbon (14C) dates were established through analysis of archaeological material from several monuments at the necropolis, including the king’s pyramid complex, pyramid complex of his queen, and two elite tombs (Isesiankh and Khuwy). In addition, two samples from non-royal tombs in the Abusir South cemetery, were taken into consideration for further precision during the modeling, associated with king Huni (end 3rd dynasty) and king Niuserre (5th dynasty). The contextualized 14C dates together with re-evaluation of historical evidence on Djedkare’s rule, results in a new model of temporal probability density which can be further refined with any new data from archaeological research. It shows that Djedkare’s reign can be currently modelled between 2503 and 2449 BCE (95.4%), thus slightly older than expected by literature. This presented model provides a more precise chronological frame for the late 5th dynasty period of Egyptian history, which was period of a significant socio-economic transformation.

This paper presents new radiocarbon dates for two Aboriginal archaeological complexes situated on the cliff-lines of the Murray River in South Australia (SA); at Pooginook Flat and Tanamee. These dates represent the first age estimates for archaeological sites within the Upper Gorge section of the Murray River. The dates ranged from ca. 11 cal ka to the Late Holocene. The research supports previous evidence which has indicated that sites located along the Murray cliffs preserve much of the oldest evidence of Aboriginal peopling along the Murray River corridor in SA. The new dates also allow us to contribute to discussions concerning broader chronological trends in Aboriginal lifeways within the Murray-Darling Basin (MDB). Specifically, the new ages add some insight into the nature and timing of early Aboriginal occupation along the Murray River corridor in SA and further evidence that the LGM acted as a significant inhibitive factor for intensive occupation of this riverscape. The conservation of these significant and informative cliff-top sites remains precarious, however, and there is an imperative to continue to record and sample the extant sites.

Drawing on insights from contemporary urban theory, this contribution questions where medieval urbanization took place. It is proposed that urbanization is a process which extends beyond towns and cities, which are merely a representation of a more expansive and transformative process. Through discussion of building stone, grain production, salt extraction, woodland management and mineral exploitation, it is argued that medieval urbanization was generative of political ecological relations which challenge prevailing understandings of the rural/urban divide and re-frame urbanization as a metabolic process. The discussion utilizes contemporary concepts of ‘extended urbanization’, ‘urban metabolism’ and ‘political ecology’ to re-frame perceptions of medieval–urban relations and the notion of urban hinterland.

This article uses tensions over the construction of a flow-regulation infrastructure built to control outflow from Lake Titicaca into the Desaguadero River, on the border between Peru and Bolivia, as a case study to explore the ways that relationships to water emerge and are contested. We argue that a nuanced understanding of tensions arising from this infrastructure requires us to recognize the long-term history of how the river accumulated practices, meanings and materials. Adapting the work of Arturo Escobar, we use the concept of ‘water regime’ to think about how engagements with the river are based in different spatiotemporal frameworks that have developed transhistorically and come into tension around the materiality and dynamism of the river itself.

This study considers the role played by Teotihuacan in the emergence of the office of the Classic Maya ajawtaak, or ‘lords’. I argue that the synthesis of this office at the site of Tikal was influenced by the building of Teotihuacan's Pyramid of the Feathered Serpent between about 180 and 230 ce. Prior to and in concert with this building's construction, Teotihuacanos orchestrated the sacrifice of an estimated 200 or more individuals, some number of whom resided beyond the Basin of Mexico before burial. Osteological traits consistent with origins in the Maya region are present among these sacrifices. The Pyramid of the Feathered Serpent features mirror and obsidian icons, which later grew to prominence in the self-presentations of the ajawtaak. I note that around the time of this monument's construction, Tikal's obsidian corpus changed in ways that paralleled similar, earlier changes that had occurred to obsidian procurement strategies at Teotihuacan. I conclude that from about 200 ce, some Classic ajawtaak observed the religion that cohered with the building of Teotihuacan's Temple of the Feathered Serpent. The ajawtaak occupied a unique positionality in Early Classic Mesoamerica that was neither essentially Teotihuacan nor essentially Maya, but a dynamic syncretism of the two ethnicities.