Physical violence and social conflict have been widely studied in the ancient societies of the Andes. However, studies about violence are scarce for the Formative period of northern Chile (1000 BC–AD 900). Evidence from these investigations is generally interpreted as interpersonal violence, whose protagonists are mostly men. Here, we present the case of an adult female recovered from the Tarapacá 40 cemetery (Tarapacá region, Chile) displaying lesions suggestive of trauma. We reconstruct her life and death in the context of this era's social and political conditions. Results of our bioanthropological characterization, cranial trauma analysis, carbon and nitrogen isotope analysis, and recording of the funerary offerings suggest she was a local member of the Formative community buried in the Tarapacá 40 cemetery and that she suffered intentional lethal lesions. Her death is unusual because there are no previous bioarchaeological records of lethal violence against women in the Tarapacá region. The osteobiography of this woman reflects a context characterized by an increase in inequality and social complexity, whereby physical violence could be used as a mechanism of internal regulation and exercise of power during the Formative period.

Se presentan los resultados de los análisis técnicos de manufactura en fibra vegetal de esteras o mantas funerarias, ampliamente usadas entre los cazadores, pescadores y recolectores de la tradición cultural Chinchorro, que habitaron la costa del norte de Chile y sur de Perú entre los 10.000 y 3500 aP. Se analizaron 153 fragmentos de esteras de 12 sitios funerarios de Arica y Camarones. Se describen y grafican los atributos de las dos técnicas identificadas: twining o torzal (94%) y técnica de estera cosida (6%) y sus rasgos estéticos de pintados y bordados. Estas técnicas fueron muy conservadoras y no variaron a través del tiempo y el espacio. La excepción es la técnica de estera cosida, que aparece hacia fines del Arcaico Tardío (4000-3500 aP). La aplicación de diseños pintados se registra desde el Arcaico Temprano (10.000-7000 aP) con ajedrezados y franjas bicolor (rojo y negro), a lo que se agregan en el Arcaico Tardío diseños más complejos (escalonados y círculos) además de esteras con aplicación de bordados. No detectamos diferencias en la manufactura de las esteras en relación con la edad, sexo y tipo de tratamiento funerario de los individuos que portaban estas esteras.

Un trabajo de rescate arqueológico en la cuenca alta del Río Loa (norte de Chile) resultó en el hallazgo de una inhumación prehispánica de un infante asociado a variados atavíos y ofrendas, junto a los restos óseos parciales de una adolescente. Ambos individuos fueron sometidos a análisis de isótopos estables para establecer paleodieta (δ13C y δ15N) y movilidad (δ18O y 87Sr/86Sr). Además, se efectuaron dataciones radiocarbónicas pareadas de los restos bioantropológicos y culturales con el fin establecer la cronología de la inhumación y, a la vez, evaluar la existencia de un posible efecto reservorio marino. Los resultados isotópicos sugieren consumo de dieta principalmente terrestre y un origen local para los individuos, aunque con una ingesta moderada de recursos marinos. Los fechados radiocarbónicos presentan una inesperada diferencia entre las edades de las ofrendas y los restos humanos, indicando la existencia de un importante efecto reservorio. Dichos resultados dan nuevas luces sobre el consumo de alimentos marinos durante el Formativo temprano en la región, a la vez que permiten ejemplificar los alcances de efectuar dataciones pareadas de restos humanos y culturales.

The marine subsistence economy of the prehistoric people of northern Chile was heavily reliant on fiber technology for the components of nets, lines, and tethers. Despite the significance and the remarkable preservation of fiber artifacts along the arid Atacama coastline, these components have received little direct attention. This case study of fiber artifacts from the Caleta Vitor archaeological complex is the first broad overview of techniques, material usage/preference, and fiber-processing conventions at a northern Chilean Archaic period site. The data presented in this paper indicate gradual change in material preferences over time, shifting from locally available vegetal fiber, which dominates the Archaic period, with small amounts of camelid fiber, to the predominance of camelid fiber in the Late Formative period. This change coincides with the appearance of more complex weaving techniques indicating participation in the previously established textile tradition proposed by Ulloa (2008) as stretching from the Azapa Valley to the Loa River.

The use of rodent middens from northern Chile as paleoecological archives has at times been questioned due to concerns about their biogenic origin and the degree to which their record represents vegetation composition rather than rodent habits. To address such concerns, we carried out a modern calibration study to assess the representation of vegetation by pollen records from rodent middens. We compared vegetation censuses with soil-surface and midden (matrix and feces) pollen samples from sites between 21° and 28°S. The results show that (1) the pollen signal from the midden matrix provides a more realistic reflection of local vegetation than soil-surface samples due to the pollen-deposition processes that occur in middens; and (2) in contrast to feces pollen assemblages, which feature some biases, rodent dietary habits do not seem to influence midden matrix pollen assemblages, probably because midden agents are dietary generalists. Our finding that modern pollen data from rodent middens reflect vegetation patterns confirms the reliability of midden pollen records as paleoecological archives in northern Chile.

We present a fossil pollen analysis from a swamp forest in the semiarid coast of Chile (32°05′S; 71°30′W), at the northern influence zone of southern westerly wind belt. A ∼10,000 cal yr BP (calendar years before 1950) palynological sequence indicates a humid phase characterized by dense swamp forest taxa dated between ∼9900 and 8700 cal yr BP. The presence of pollen-starved sediments with only scant evidence for semiarid vegetation indicates that extreme aridity ensued until ∼5700 cal yr BP. The swamp forest recovered slowly afterwards, helped by a significant increase in moisture at ∼4200 cal yr BP. A new swamp forest contraction suggests that another slightly less intense drought occurred between ∼3000 and 2200 cal yr BP. The swamp forest expansion begins again at ∼2200 cal yr BP, punctuated by a highly variable climate. Comparisons between the record presented here with other records across the region imply major variations in the extent of the southern westerlies during the Holocene. This variability could have been caused either by latitudinal displacements from the present mean position of southern westerlies wind belt or by changes in the intensity of the South Pacific Subtropical Anticyclone, both of which affect winter precipitation in the region.

Plant macrofossils from 33 rodent middens sampled at three sites between 2910 and 3150 m elevation in the main canyon of the Río Salado, northern Chile, yield a unique record of vegetation and climate over the past 22,000 cal yr BP. Presence of low-elevation Prepuna taxa throughout the record suggests that mean annual temperature never cooled by more than 5°C and may have been near-modern at 16,270 cal yr BP. Displacements in the lower limits of Andean steppe and Puna taxa indicate that mean annual rainfall was twice modern at 17,520–16,270 cal yr BP. This pluvial event coincides with infilling of paleolake Tauca on the Bolivian Altiplano, increased ENSO activity inferred from a marine core near Lima, abrupt deglaciation in southern Chile, and Heinrich Event 1. Moderate to large increases in precipitation also occurred at 11,770–9550 (Central Atacama Pluvial Event), 7330–6720, 3490–2320 and at 800 cal yr BP. Desiccation occurred at 14,180, 8910–8640, and 4865 cal yr BP. Compared to other midden sites in the region, early Holocene desiccation seems to have happened progressively earlier farther south. Emerging trends from the cumulative midden record in the central Atacama agree at millennial timescales with improved paleolake chronologies for the Bolivian Altiplano, implying common forcing through changes in equatorial Pacific sea-surface temperature gradients.

Sky observation in sub-tropical Andean areas, part of ancient Collasuyu, during the Inca empire (ca. 1470 A.D.) was characterized by the combined use of geographical, social, psychological and natural elements of the entorno (environment or landscape). From a phenomenological perspective, it would be understood as: the place (point of observation), the path (line or relation), the horizon (calendrical marker) and the zenith/anti-zenith (vertical projection) as an expression of ‘dwelling or living in the world’. I present results obtained from a spatio-temporal analysis of mountain worship which took place at the Atacama Indian community of Socaire, northern Chile (23° 35′ 28″S, 67° 52′ 36″W, 3274m AMSL). These indicate the existence of an animistic relationship between astronomical observations, the worship of mountains, and agricultural practices. The psychological phenomena of pareidolia, apophenia and hierophany also contribute to explain the mimetolith of the ‘Hand of God’ (formed by the Tumisa, Lausa, Chiliques, Ipira and Miñiques mountains) and the social categories of space and time in Socaire: ‘above, here, and down’; ‘right and left’; ‘female and male’; ‘noon and midnight’; ‘north and south’; and ‘visible and invisible’ (as complementary opposites or yanantin).