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There is a long history in the use of osseous materials from some of the earliest contexts of the Andes, yet most technology studies have focused on durable materials of ceramic, metal, and stone. In this paper, we present evidence for the continual use of osseous raw materials before and during Wari state expansion in the 1st millennium CE in the Cusco region of Peru. Results indicate that, at the site of Ak'awillay, communities were exploiting osseous raw material to produce artifacts used in textile manufacture, food processing, and ceremonial activities. We argue that wide-scale access to bone and antler raw material fostered social interactions that mediated emergent power dynamics in private and public spaces. This key line of evidence reveals that communal practices in public spaces at Ak'awillay involved food processing activities, while private settings were reserved for sharing of familial knowledge around textile production. We emphasize the greater need in the Andes for a close look at osseous technology to detect these subtle, yet integral patterns to understand social and power relations in the past. [ABSTRACT FROM AUTHOR]

The aim of this study is to assess the variability of the stable carbon and nitrogen isotope composition of herbivores -guanaco and huemul-in southern Patagonia. The study area extends from the eastern slopes of the Andes to the Atlantic Coast between 47° and 49° S. The ultimate aim of the research was to generate an isotopic ecology with an adequate spatial resolution that allows the incorporation and development of stable isotope studies in discussions of the population dynamics of hunter-gatherers in continental Patagonia. This paper presents the δ13C and δ15N values of 159 guanaco and huemul specimens, both modern and archaeological. This space was divided into three areas: Western area, Central Plateau and Eastern Area. Isotopic variability within groups was analyzed using the SIBER, from which the isotopic niches of the different groups are compared. The results show a spatial pattern of isotopic variability in herbivores, i.e. lower δ13C and δ15N values associated with forest environments in the western end of the transect and higher values, especially δ15N, towards the east, with maximum values observed near the Atlantic coast. Our results support the stated expectations on herbivore stable isotope composition variability and its association with environmental variables in a longitudinal transect across the southern Argentinean Patagonia. [ABSTRACT FROM AUTHOR]

High-altitude hypoxia is one of many environmental stressors affecting human populations in the highland Andes. Living highland Andeans show adaptive physiological responses to these conditions through both developmental plasticity and natural selection. Given the longevity of human settlement in this region, these same responses ought to have affected ancient Andeans. This paper tests whether developmental plasticity or natural selection best explains the morphological signatures of adaptations to high-altitude hypoxia in ancient highland Andeans. I compare four groups of skeletons: two groups from lowland regions and two groups from high elevations. Previous work shows that the two highland groups have small bodies and voluminous ribs compared with the lowland groups indicating morphological adaptations to high-altitude environments. This paper compares patterns of intrinsic variation and sexual dimorphism in body size, limb lengths, and rib morphology in highland and lowland groups to test if developmental plasticity or natural selection underlies these morphological differences. The four groups share similar patterns of sexual dimorphism and intrinsic variation in body size and limb lengths. The two highland samples show greater degrees of sexual dimorphism in rib morphology than the lowlanders. Patterns of intrinsic variation in rib morphology do not sort by altitude. Both natural selection and developmental plasticity in response to high-altitude hypoxia likely shaped skeletal morphology in ancient highland Andeans. [ABSTRACT FROM AUTHOR]

We have carried out long-term comparative in a wide latitudinal range of the Andes (29°–37° south), encompassing selected areas that differ in ecology and biogeography. This latitudinal span shows diversity in subsistence modes across time and space, ranging from Andean agro-pastoralists in the north to Patagonian hunter-gatherers in the south. As part of this research, a program of geochemical and archaeological characterization of obsidian sources and distributions is being developed, attempting to assess connections between different biogeographical contexts. This work has allowed recognizing five Andean sources with different geological and topographical properties. Stemming from this macro-regional endeavor, in this paper we present a comparative analysis of the human use of two sources that, based on the intensity of human use on a macro-regional scale, can be interpreted as ‘minor’ sources. This study is framed on GIS least-cost models for human circulation across rugged landscapes allowing access to the sources. We assess temporal and spatial patterns of human occupation of high-altitude Andean deserts and neighboring areas comparing two of obsidian sources: Laguna del Diamante (34° S) and Cerro Huenul (36° S). The results indicate the existence of asymmetric distributions, particularly in the case of Laguna del Diamante. This evidence is used to assess the existence of dominant geographic vectors of human access and use of the Andean highlands. On this basis, we explore the analytical potential of minor sources for the study of human biogeography and organization of technology. [ABSTRACT FROM AUTHOR]

A large (>0.1 km 2 ) and complex mass movement in the Central Andes of Argentina (final portion of Cordillera de Olivares, Frontal Cordillera), was studied to identify the triggering factors and understand their relationship with geomorphic, cryogenic and climatic dynamics. This debris-rockslide is composed of clast supported blocks of Permian–Triassic volcanic breccias. In order to characterize this feature, high resolution satellite imagery interpretation was carried out, together with the study of the landslide detachment zones and landslide bodies. These debris-rockslide events could have originated as a consequence of the combination of internal slow deformation and fragmentation under periglacial conditions, followed by a sudden collapse of the rock mass. Pre- and post-slide digital elevation models (DEMs) were created from topographical data with the help of a Geographic Information System (GIS) tool. Approximately 14.89 M m 3 of rock and debris travelled nearly 2 km from an elevation of 5023 m–4325 m asl. Although usually the origin of such catastrophic movements is related to seismically active areas with earthquakes whose magnitude frequently exceed Ms 6, our hypothesis is that this debris-rockslide event has a climatic origin caused by large snow accumulations during winters and subsequent fast meltdown processes during spring, which would have facilitated the sliding. The paper outlines the important role that snowmelt can play in the genesis and evolution of rock displacements and the importance of meteorological data, seismic catalogues, historical aerial photography and satellite images in geomorphological back-analysis. [ABSTRACT FROM AUTHOR]

Abstract: This paper presents a synthesis of geological, geochemical, and archaeological information for the Huenul obsidian source located in northern Patagonia (Neuquén Province, Argentina). Important information recently published on other obsidian sources in the South-Central Andes of Argentina and Chile provide the context for this endeavor, allowing evaluation of the role of this lithic source within the network of human mobility and interaction on different spatial scales. It is suggested here that Huenul obsidian is genetically related with the Tilhué Formation, already been mapped in detail. This regional information provides a search model for geoarchaeological surveys. This raw material displays a remarkable supra-regional distribution in the archaeological record, although it is regionally under-represented. Three alternative hypotheses explaining the distribution of Huenul obsidians allow evaluation of technological decisions, marginal vs. nuclear role of certain spaces for past human societies, and territorial organization. [Copyright &y& Elsevier]

Abstract: While the Ensenadan Stage/Age (ca. 2.1 to 0.5Ma) was characterized by certain mammal associations in the Pampean plains, the Andean ranges of Patagonia and Tierra del Fuego, their piedmont areas and, in some cases, the adjacent lowlands were undergoing a well-defined alternating sequence of glacial and interglacial stages driven by the regional climate of Southernmost South America and Antarctica. This paper reviews the available geographical, geological and chronological evidence of glaciation during the Ensenadan stage/age, with perhaps more than 15 distinct glacial events, including the Great Patagonian Glaciation (GPG) and other cold episodes that took place before and after it. Finally, a tentative correlation of Patagonian glacial episodes and the Pampean biostratigraphic stages, based on radiometric dating and paleomagnetic studies, is herein presented. [Copyright &y& Elsevier]

This paper discusses basic tendencies in the characteristics of the early archaeological record corresponding to human occupation near the eastern flank of the Andean range, at the southern end of South America. Lithic artifacts are analyzed within an organization of technology perspective and are discussed according to Borrero''s ecological model of the peopling of Patagonia. The characteristics of the lithic artifacts along with raw material provenience at the oldest levels at sites Cerro Casa de Piedra 7 and Chorrillo Malo 2, match our expectations for an exploration or early colonization phase in the peopling of the space. In addition, the range of variation of tools is similar to that present at early sites located to the east of the area. Some differences at these sites are already evident. Among these are the higher tool deposition rates at sites located close to Pampa del Asador, a known source of black obsidian that was used by early inhabitants of Patagonia. This poses some new questions that should be addressed regionally, taking into account the regional availability of lithic resources. [Copyright &y& Elsevier]