A paleomagnetic study of basaltic lava flows exposed in the northern Neuquén Cordillera, southernmost Central Andes, along the Antiñir-Copahue fault zone (ACFZ), involved 25 sites of the Cola de Zorro Formation (Pliocene–Early Pleistocene) along two different sections. The sites show exclusive normal polarity, corresponding to the Late Pliocene Gauss chron (3.6–2.6 Ma). The angular standard deviation of virtual geomagnetic poles (VGPs; ASD = 14.8°) is consistent with the expected values from recent geomagnetic models, in opposition to anomalously low dispersion found in previous studies in Pleistocene VGPs of reverse polarity from neighboring areas to our study zone. Mean paleomagnetic directions for Bella Vista (Dec = 0.0°, Inc = −50.0°, α₉₅ = 7.6°, K = 36.7, N = 11) and Río Huaraco sections (Dec = 354.9°, Inc = −57.0°, α₉₅ = 7.5°, K = 55.7, N = 8) do not show tectonic rotation around vertical axes. Combining and regrouping our and previous data by area confirmed the absence of tectonic rotations in the Huaraco-Trohunco block and a statistically significant clockwise rotation of 14.4° ± 10.3° of three adjacent tectonic blocks located south of our study locality in Pleistocene times. These results suggest that strike-slip deformation along some sections of the ACFZ was significant in the Pleistocene structural evolution of this region.

What does it mean to teach and work in a corporate university with colonial roots, today? The on-going events in Palestine – what have been described by many specialists and international organizations as a genocidal campaign – have brought to the surface the historical undercurrents, the tensions and the contradictions of such an institution as a nested sensorial assemblage of actors, memories, affects and interests. Starting from the events that happened in the context of teaching an archaeology course on social justice while a student encampment was in place on campus, in the spring of 2024, I reflect on the materiality of protest, on teaching as a transgressive undertaking and on the retooling of colonial and decolonial structures to advance emancipation. In the midst of a rather dark moment, this is ultimately a hopeful reflection.

Significant thicknesses, a large number of paleosols, and an impressive chronological framework place the loess–paleosol series of the Afghan-Tajik depression on a par with the famous sections of the Chinese Loess Plateau. Based on the results of field stratigraphy, description of the macro- and micromorphological structure, field magnetic susceptibility measurements, and study of the chemical and grain-size compositions, a comprehensive characterization of the structure, properties, and formation conditions of paleosol horizons and loess layers was carried out. Three loess units and two pedocomplexes are distinguished in the late and upper middle Pleistocene deposits of the Obi-Mazar section. These sediments are characterized by high silt and carbonate content and the presence of loess with pedogenic features. Pedocomplex PC1, consisting of three paleosols, according to the stratigraphic position and absolute dating, corresponds to MIS 5. Pedocomplex PC2, consisting of two developed paleosols separated by loess, is correlated with MIS 7. The properties of the studied paleosols together with modern soil distribution in the region allow for the reconstruction of the soil type of PC1 and PC2 of the Obi-Mazar section with the genesis of the Calcisols–Kastanozems groups.

States have the sovereign right to pursue their social and economic development, often involving urbanization, industrialization, infrastructure development, and tourism promotion. Regrettably, these endeavors frequently lead to destruction or damage to the authenticity and integrity of their cultural heritage. In light of this, one might wonder whether and to what extent, under customary international law, states’ right to development must be harmonized with the need to preserve their own cultural heritage for the benefit of future generations. The present contribution examines various elements of international practice, including treaty practice, resolutions of international organizations, national legislation, and states’ conduct in actual cases to determine the existence of a customary prohibition or clear limits on damaging cultural heritage for social and economic development. It also reflects more broadly on the international regime for protecting cultural heritage during peacetime and the ambiguous relationship between the World Heritage Convention and customary law.

In the present discussion, I will focus on the creation of baby warriors in Mesoamerica in a twofold manner: as human beings and as blade stones. The emphasis will be on central Mexico, complemented with essential data from other parts of Postclassic Mesoamerica. By juxtaposing information from historical sources in a novel way, this investigation seeks to offer new insights that should reinforce the idea that warriors captured on the battlefield were considered to be children. Although this idea has been suggested before, this article aims to contribute new historical evidence that not only confirms this notion but also widens our understanding of the creation of nonbiological offspring. Making kin out of Others aims to satisfy a cosmological need to incorporate vital energy and elements for individual and collective personhood from outside of the community. The second idea of this investigation focuses on a related productive variant of this gestational dynamic, suggesting that by stone flaking and chipping, children (of stone) were fabricated. Some of them were indeed “child blade stones” who personified warriors and fed themselves with sacrificial victims, securing sustenance for the hungry gods. I argue that the birth of these warriors should be integrated into a major mythological theme—namely, the Child Hero and the Old Adoptive Mother.

Continental-scale patterns of morphological and biological change represent broad time- and spatially averaged interpretations. Conversely, regionally focused studies of morphological variability offer an opportunity to consider patterns of biological change at more refined spatial scales, where nuanced histories may be identified. That approach is particularly applicable for areas known to have dynamic biogeographic and glacial landscapes (e.g., western Canada). We studied proboscideans from Alberta, Canada, an area thought to represent a zone of sympatry between extinct forms of mammoth (i.e., Mammuthus columbi, Mammuthus primigenius) in order to test existing taxonomic hypotheses and chronologically contextualize the regional record of mammoths through the Late Pleistocene. Morphometric analysis of sixth molars of mammoths from Alberta (n = 17) support identification of three distinct morphologies that we assign to M. columbi, M. primigenius, and intermediates of those taxa. The presence of intermediate forms is perhaps unsurprising, given both the recognition of hybridization in M. columbi and M. primigenius and the previously documented occurrence of both taxa in Alberta. Some records of M. columbi may document a broader northern geographic incursion for that taxon than previously recognized, but could also represent a much deeper time component to the history of Mammuthus in Alberta (i.e., Mammuthus trogontherii).

As historic drought conditions become more common in western North America, Late Quaternary hydroclimate records become vital for putting present anthropogenic conditions into a longer-term context. Here, we establish a high-resolution record of drought for the eastern Sierra Nevada (California) using lacustrine carbonates from well-dated sediment cores. We used oxygen and carbon stable-isotope ratios, combined with high-resolution scanning X-ray fluorescence counts of calcium (Ca) and titanium (Ti), to reconstruct the drought record over the last 4600 years in June Lake. We found elevated δ18O and δ13C carbonate isotope values coinciding with peaks in both total inorganic carbon and Ca/Ti, suggesting enhanced carbonate precipitation in response to evaporative concentration of lake water. At least six intervals of prolonged (centennial-scale) carbonate deposition were identified, including three pulses during the Late Holocene Dry Period (LHDP; ~3500–2000 cal yr BP), the Medieval Climate Anomaly (~1200–800 cal yr BP), and the Current Warm Period, which began around 100 cal yr BP. This record highlights the complexities of the LHDP, an interval that was more variable at June Lake than has been previously described in regional records.