The Forgotten Kingdom.: New investigations in the prehistory of Eswatini

The kingdom of Eswatini provides a rich archaeological sequence covering all time periods from the Early Stone Age to the Iron Age. For over 27 years though, no or very little archaeological research was conducted in the country. In the scope of a new project funded by the German Research Foundation (DFG) we aim to re-excavate and re-date Lion Cavern, the potentially oldest ochre mine in the world. In addition, we conduct a largescale geological survey for outcrops of ochre and test their geochemical signatures for comparative studies with archaeological ochre pieces from MSA and LSA assemblages in Eswatini. Here we present a review of the research history of the kingdom and some preliminary results from our ongoing project

Between the Deseado Massif and the north Santa Cruz river basin (Patagonia, Argentina): geochemical analysis on obsidian artifacts and human circulation models

El objetivo de este trabajo es evaluar la posibilidad de la existencia de una fuente desconocida de obsidiana entre el sur del Macizo del Deseado y la margen norte de la cuenca del río Santa Cruz (Patagonia, Argentina). La alta frecuencia de obsidiana en algunos sectores de este espacio y la mención de pobladores locales acerca de la existencia de fuentes desconocidas hasta el momento llevaron a la necesidad de explorar esta hipótesis. Se realizaron análisis geoquímicos mediante fluorescencia de rayos X a una muestra de 20 artefactos de obsidiana. Los resultados indican una composición geoquímica similar a las fuentes secundarias de Pampa del Asador, su cono aluvial y 17 de Marzo o sectores intermedios entre ellas, lo que debilita la hipótesis acerca de la existencia de una fuente de obsidiana con una composición diferente en este sector del espacio. Por otra parte, a efectos de comenzar a evaluar cuál de las fuentes habría sido utilizada en cada caso, se hicieron análisis de frecuencia artefactual y se modelaron caminos óptimos entre cañadones que desembocan al norte del río Santa Cruz y las fuentes de obsidiana negra conocidas. Si bien se requieren análisis adicionales, los resultados sugieren la utilización de obsidiana de 17 de Marzo en los espacios más orientales (cañadón Yaten Guajen).The purpose of this paper is to analyze the possibility of the existence of an unknown obsidian source between the south of the Deseado Massif and the northern shore of the Santa Cruz River basin (Patagonia, Argentina). The high frequency of obsidian in some of the analyzed spaces and the information provided by local inhabitants about the existence of an unknown obsidian source in the area, pointed to the need of evaluating this hypothesis. Geochemical analysis, through X-ray fluorescence, were performed on 20 obsidian artifacts recovered in different spaces of the study area. The results indicate a geochemical composition similar to the secondary sources of Pampa del Asador, its alluvial cone, and 17 de Marzo or intermediate sectors between them, which weakens the hypothesis of the existence of an unknown obsidian source with a different composition in this area. In addition, in order to evaluate which of the obsidian sources was used, obsidian artifacts frequencies were utilized and least cost paths were modeled between canyons in the northern shore of Santa Cruz river and the known black obsidian sources. Although further analysis need to be performed, results suggest the utilization of the 17 Marzo source in easterly spaces (Yaten Guajen canyon).Fil: Franco, Nora Viviana. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Saavedra 15. Instituto Multidisciplinario de Historia y Ciencias Humanas; ArgentinaFil: Glascock, Michael D. University of Missouri; Estados UnidosFil: MacDonald, Brandi L.. University of Missouri; Estados UnidosFil: Gilio, Brenda Ludmila. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro de Investigaciones y Transferencia de Santa Cruz. Universidad Tecnológica Nacional. Facultad Regional Santa Cruz. Centro de Investigaciones y Transferencia de Santa Cruz. Universidad Nacional de la Patagonia Austral. Centro de Investigaciones y Transferencia de Santa Cruz; Argentin

Varvarco obsidian: a new source in northwestern Patagonia (Neuquén, Argentina)

En el norte neuquino existen depósitos piroclásticos que contienen nódulos de obsidianas. Las investigaciones en la región dieron a conocer las principales fuentes utilizadas por las poblaciones que allí habitaron. Para profundizar el conocimiento de cada fuente de obsidiana se adoptó un programa de estudio geoarqueológico y geoquímico. Así, se han descubierto nuevas ocurrencias de obsidianas, la más destacable de las cuales es la obsidiana Varvarco que aquí se presenta. Se dan a conocer los muestreos realizados en el valle del río Varvarco, su contexto geológico y geomorfológico, la presencia de obsidiana, el tipo de yacimiento, forma de presentación, distribución y abundancia. Luego, se describen las principales características observadas bajo microscopio petrográfico. Por último, se presentan los resultados de análisis geoquímicos de fluorescencia de rayos X y activación neutrónica. A partir de los primeros la obsidiana Varvarco se diferencia de la de Cerro Huenul, pero no de la obsidiana Maule 1 y 2. Los segundos análisis discriminan bien esta nueva obsidiana de las ya conocidas para Neuquén. Los resultados obtenidos permiten reinterpretar la disponibilidad de recursos líticos de buena calidad para la talla y revisar las interpretaciones de movilidad e interacción de poblaciones en esta región.In northern Neuquén there are pyroclastic deposits containing obsidian nodules. The researches in the region revealed the main sources used by the people that lived there. A program of geoarchaeological and geochemical study was adopted to extend the knowledge of each source of obsidian. Thus, new occurrences of obsidian have been discovered, the most notable of which is the Varvarco obsidian presented here. We present the samples points conducted in the valley of Varvarco river, its geological and geomorphological context, the presence of obsidian, the type of deposit, presentation form, distribution and abundance. Then, we described the main characteristics observed under a petrographic microscope. Finally, we present the results of X-ray fluorescence and neutron activation geochemical analysis. The Varvarco obsidian differs from that of Cerro Huenul, but not from the obsidian Maule 1 and 2 from the XRF. NAA discriminates well this new obsidian from those already known in Neuquén. The results obtained allow to reinterpret the availability of good quality lithic resources and to revise the interpretations of mobility and interaction of populations in this region.Fil: Fernández, María Victoria. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Diversidad Cultural y Procesos de Cambio. Universidad Nacional de Río Negro. Instituto de Investigaciones en Diversidad Cultural y Procesos de Cambio; ArgentinaFil: Leal, Pablo Rodrigo. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaFil: Della Negra, Claudia. No especifíca;Fil: Klesner, Catherine. University of Arizona; Estados UnidosFil: MacDonald, Brandi L.. University of Missouri; Estados UnidosFil: Glascock, Michael D.. University of Missouri; Estados UnidosFil: Barberena, Ramiro. Universidad Nacional de Cuyo. Facultad de Ciencias Exactas y Naturales. Laboratorio de Paleoecología Humana; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Interdisciplinario de Ciencias Básicas. - Universidad Nacional de Cuyo. Instituto Interdisciplinario de Ciencias Básicas; Argentin

Hope in dirt: report of the Fort Apache Workshop on Forensic Sedimentology Applications to Cultural Property Crime, 15—19 October 2018

A 2018 workshop on the White Mountain Apache Tribe lands in Arizona examined ways to enhance investigations into cultural property crime (CPC) through applications of rapidly evolving methods from archaeological science. CPC (also looting, graverobbing) refers to unauthorized damage, removal, or trafficking in materials possessing blends of communal, aesthetic, and scientific values. The Fort Apache workshop integrated four generally partitioned domains of CPC expertise: (1) theories of perpetrators’ motivations and methods; (2) recommended practice in sustaining public and community opposition to CPC; (3) tactics and strategies for documenting, investigating, and prosecuting CPC; and (4) forensic sedimentology—uses of biophysical sciences to link sediments from implicated persons and objects to crime scenes. Forensic sedimentology served as the touchstone for dialogues among experts in criminology, archaeological sciences, law enforcement, and heritage stewardship. Field visits to CPC crime scenes and workshop deliberations identified pathways toward integrating CPC theory and practice with forensic sedimentology’s potent battery of analytic methods

Genetic determinants of heel bone properties: genome-wide association meta-analysis and replication in the GEFOS/GENOMOS consortium

Quantitative ultrasound of the heel captures heel bone properties that independently predict fracture risk and, with bone mineral density (BMD) assessed by X-ray (DXA), may be convenient alternatives for evaluating osteoporosis and fracture risk. We performed a meta-analysis of genome-wide association (GWA) studies to assess the genetic determinants of heel broadband ultrasound attenuation (BUA; n = 14 260), velocity of sound (VOS; n = 15 514) and BMD (n = 4566) in 13 discovery cohorts. Independent replication involved seven cohorts with GWA data (in silico n = 11 452) and new genotyping in 15 cohorts (de novo n = 24 902). In combined random effects, meta-analysis of the discovery and replication cohorts, nine single nucleotide polymorphisms (SNPs) had genome-wide significant (P < 5 × 10(-8)) associations with heel bone properties. Alongside SNPs within or near previously identified osteoporosis susceptibility genes including ESR1 (6q25.1: rs4869739, rs3020331, rs2982552), SPTBN1 (2p16.2: rs11898505), RSPO3 (6q22.33: rs7741021), WNT16 (7q31.31: rs2908007), DKK1 (10q21.1: rs7902708) and GPATCH1 (19q13.11: rs10416265), we identified a new locus on chromosome 11q14.2 (rs597319 close to TMEM135, a gene recently linked to osteoblastogenesis and longevity) significantly associated with both BUA and VOS (P < 8.23 × 10(-14)). In meta-analyses involving 25 cohorts with up to 14 985 fracture cases, six of 10 SNPs associated with heel bone properties at P < 5 × 10(-6) also had the expected direction of association with any fracture (P < 0.05), including three SNPs with P < 0.005: 6q22.33 (rs7741021), 7q31.31 (rs2908007) and 10q21.1 (rs7902708). In conclusion, this GWA study reveals the effect of several genes common to central DXA-derived BMD and heel ultrasound/DXA measures and points to a new genetic locus with potential implications for better understanding of osteoporosis pathophysiology

Paleoindian ochre mines in the submerged caves of the Yucatán Peninsula, Quintana Roo, Mexico

Investigations in the now-submerged cave systems on the Yucatán Peninsula continue to yield evidence for human presence during the Pleistocene-Holocene transition. Skeletal remains are scattered throughout the caves of Quintana Roo, most representing individuals who died in situ. The reasons why they explored these underground environments have remained unclear. Here, we announce the discovery of the first subterranean ochre mine of Paleoindian age found in the Americas, offering compelling evidence for mining in three cave systems on the eastern Yucatán over a ~2000-year period between ~12 and 10 ka. The cave passages exhibit preserved evidence for ochre extraction pits, speleothem digging tools, shattered and piled flowstone debris, cairn navigational markers, and hearths yielding charcoal from highly resinous wood species. The sophistication and extent of the activities demonstrate a readiness to venture into the dark zones of the caves to prospect and collect what was evidently a highly valued mineral resource

Sources, circulation, and use of obsidian in central Chile

A geochemical analysis of 382 obsidian samples from different archeological sites in Central Chile (32°–35° Lat. South) has identified the preferential use of three known sources in the Andean mountain range, Arroyo Paramillos and Laguna del Diamante located in the Maipo Volcano area, and Las Cargas located ca 120 km further south. The analysis of the circulation and use of this raw material from the beginning of the Archaic period until the arrival of the Inka to this territory reveals differences in how obsidian from these three main sources was used, both spatially and temporally. The hunter-gatherers occupying the Andean mountain range preferred the obsidian source from the Maipo Volcano area, while the hunter gatherer and horticulturalist groups from the central valley used more frequently the obsidian from Las Cargas source. These differences are linked to the quality of the obsidian, its suitability for the intended use and the distance of the users from the source.Fil: Sanhueza, Lorena. Universidad de Chile; ChileFil: Cornejo Bustamante, Luis Eduardo. Universidad Alberto Hurtado; ChileFil: Duran, Victor Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Interdisciplinario de Ciencias Básicas. - Universidad Nacional de Cuyo. Instituto Interdisciplinario de Ciencias Básicas; ArgentinaFil: Cortegoso, Valeria. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Interdisciplinario de Ciencias Básicas. - Universidad Nacional de Cuyo. Instituto Interdisciplinario de Ciencias Básicas; ArgentinaFil: Yebra, Lucía Gabriela. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Interdisciplinario de Ciencias Básicas. - Universidad Nacional de Cuyo. Instituto Interdisciplinario de Ciencias Básicas; ArgentinaFil: Glascock, Michael D.. University of Missouri; Estados UnidosFil: MacDonald, Brandi L.. University of Missouri; Estados UnidosFil: Giesso, Martín. Southern Illinois University; Estados Unido

Obsidian sources from the southern Andean highlands (Laguna del Diamante, Argentina and Chile): geochemical insights on geological complexity and human biogeography

New geochemical results for two obsidian types, Laguna del Diamante and Arroyo Paramillos, naturally available in the Laguna del Diamante locality, a seasonally accessible highland wetland emplaced in the current border between Argentina and Chile at 3300 masl (34°S), are presented. A total of 1219 archeological artifacts from 41 sites located on both sides of the Andes have been assigned to these sources. The artifacts were analyzed by non-destructive, energy-dispersive X-ray fluorescence (ED-XRF). Archeological distributions of these obsidian types are assessed through GIS spatial analysis. Results show a great asymmetry in the distribution of these sources toward the two Andean slopes: the Laguna de Diamante chemical type shows a fairly local use pattern, being concentrated almost entirely in Cordillera sites, but the Paramillos shows a less homogeneous distribution and tends to be more concentrated in the sites that are in the western natural corridor. Although these lands were accessed and occupied from diverse demographic nodes in lower-altitude settings, the spatial analysis of obsidian artifacts reinforces the argument of dominant geographic vectors of access connecting with the western valleys and lowlands of Chile.Fil: Cortegoso, Valeria. Consejo Nacional de Investigaciones Cientificas y Tecnicas. Centro Cientifico Tecnologico Conicet - Mendoza. Instituto Interdisciplinario de Ciencias Basicas. - Universidad Nacional de Cuyo. Instituto Interdisciplinario de Ciencias Basicas.; ArgentinaFil: Yebra, Lucía Gabriela. Consejo Nacional de Investigaciones Cientificas y Tecnicas. Centro Cientifico Tecnologico Conicet - Mendoza. Instituto Interdisciplinario de Ciencias Basicas. - Universidad Nacional de Cuyo. Instituto Interdisciplinario de Ciencias Basicas.; ArgentinaFil: Durán, Víctor. Consejo Nacional de Investigaciones Cientificas y Tecnicas. Centro Cientifico Tecnologico Conicet - Mendoza. Instituto Interdisciplinario de Ciencias Basicas. - Universidad Nacional de Cuyo. Instituto Interdisciplinario de Ciencias Basicas.; ArgentinaFil: Barberena, Ramiro. Consejo Nacional de Investigaciones Cientificas y Tecnicas. Centro Cientifico Tecnologico Conicet - Mendoza. Instituto Interdisciplinario de Ciencias Basicas. - Universidad Nacional de Cuyo. Instituto Interdisciplinario de Ciencias Basicas.; ArgentinaFil: Lucero Ferreyra, Gustavo Fernando. Universidad Nacional de Cuyo. Facultad de Ciencias Exactas y Naturales. Laboratorio de Paleoecología Humana; ArgentinaFil: Cornejo Bustamante, Luis Eduardo. Universidad de Chile; ChileFil: Giesso, Martín. Northeastern University; Estados UnidosFil: MacDonald, Brandi L.. University of Missouri; Estados UnidosFil: Glascock, Michael D. University of Missouri; Estados Unido