Abstract:In Argentine Patagonia, the type of archaeological burial "in pit" has been only identified on the coast of Lángara Bay. This modality is characterized by the presence of single and multiple primary burials. Studies on five human burials in pits are presented in this article. The aim is to compare the contexts of burials in pit at the site level and the spatial characteristics of their distribution in the Lángara Bay locality from a diachronic perspective. The approach focuses on mortuary practices and social … Show more
“…Regardless of the ecological and/or social motivations, the recurrent use of specific locations is expected in Patagonia. The archaeological and bioarchaeological records show that Late Holocene hunter-gatherers often re-used the same locations (“persistent places”, sensu [ 66 ]) for settlement and inhumation through time (see examples in [ 49 , 67 , 68 ]). As long as critical resources are available, the daily circulation around the same area for an indefinite amount of time is one possible landscape exploitation strategy among hunter-gatherer groups [ 15 , 69 – 71 ].…”
During the Late Holocene, hunter-gatherer interaction networks significantly grew in intensity and extension across Patagonia. Although this growth is evidenced by the increased flow of exotic items across the region, the mechanisms behind these strengthening social networks remain unclear. Since evidence suggests that some individuals might have performed long-distance trips, this article aims to address the potential relationship between these individuals and the flows of exotic items in North Patagonia. We analyzed 54 enamel teeth for strontium isotopes and reconstructed their probable mobility using mixed-effect models and isotope-based geographic assignments. We inferred population and individual mobility trends and compared them against the flow of exotic items built from a standardized compilation. Our results indicate that most individuals have isotopic composition compatible with residence within their burial and surrounding areas. However, a few individuals show isotopic composition incompatible with their burial areas, which suggests axes -from the burial location to the most likely isotope integration area- of extraordinary mobility. At the same time, the flows of exotic items overlap with these axes around the eastern sector of the study area suggesting that this location could have been a central point of convergence for people and items. We argue that small-scale socially driven mobility could have played a relevant role as a general mechanism of interaction that fostered and materialized Patagonian interaction networks during the Late Holocene.
“…Regardless of the ecological and/or social motivations, the recurrent use of specific locations is expected in Patagonia. The archaeological and bioarchaeological records show that Late Holocene hunter-gatherers often re-used the same locations (“persistent places”, sensu [ 66 ]) for settlement and inhumation through time (see examples in [ 49 , 67 , 68 ]). As long as critical resources are available, the daily circulation around the same area for an indefinite amount of time is one possible landscape exploitation strategy among hunter-gatherer groups [ 15 , 69 – 71 ].…”
During the Late Holocene, hunter-gatherer interaction networks significantly grew in intensity and extension across Patagonia. Although this growth is evidenced by the increased flow of exotic items across the region, the mechanisms behind these strengthening social networks remain unclear. Since evidence suggests that some individuals might have performed long-distance trips, this article aims to address the potential relationship between these individuals and the flows of exotic items in North Patagonia. We analyzed 54 enamel teeth for strontium isotopes and reconstructed their probable mobility using mixed-effect models and isotope-based geographic assignments. We inferred population and individual mobility trends and compared them against the flow of exotic items built from a standardized compilation. Our results indicate that most individuals have isotopic composition compatible with residence within their burial and surrounding areas. However, a few individuals show isotopic composition incompatible with their burial areas, which suggests axes -from the burial location to the most likely isotope integration area- of extraordinary mobility. At the same time, the flows of exotic items overlap with these axes around the eastern sector of the study area suggesting that this location could have been a central point of convergence for people and items. We argue that small-scale socially driven mobility could have played a relevant role as a general mechanism of interaction that fostered and materialized Patagonian interaction networks during the Late Holocene.
“…En el año 2014 se visitó el lugar y se observó la presencia de escasos restos óseos los cuales se encontraban a una profundidad de 1 m aproximadamente. Una reconstrucción del contexto de hallazgo permitió inferir que el o los individuo/s presentes en el entierro habrían sido depositados en una fosa realizada sobre una terraza costera (Zilio y Hammond 2017).…”
Section: Los Entierros Humanos Analizadosunclassified
“…AP, por último los chenques se ubican en el rango cronológico de entre 1000 y 300 cal. AP(Zilio 2015(Zilio , 2016(Zilio , 2017aZilio y Hammond 2017; Zubimendi et al 2011).En trabajos previos(Zilio 2015(Zilio , 2017b, a partir del análisis de las dataciones radiocarbónicas de los entierros humanos en la CNSC, se pudo observar que muchos de los rangos de las edades calibradas se superponen permitiendo inferir la posible…”
En este trabajo se analizan tres entierros humanos procedentes de la costa norte de Santa Cruz, los cuales presentan edades radiocarbónicas similares. Los contextos arqueológicos, denominados El Zanjón 3 (2850 ± 60 años AP), Shag (2670 ± 70 años AP) y El Amanecer (2890 ± 60 años AP) presentan distintas modalidades de entierro; en fosa, en anillo y en médano, respectivamente. Se plantea la pregunta de si los tres tipos de entierro podrían representar una multiplicidad de tratamientos mortuorios llevados a cabo por un mismo grupo socio-cultural en esta franja de costa, o si por lo contrario, los mismos podrían pertenecer a distintos grupos humanos. Se desarrollan distintas vías analíticas tendientes a reconocer diferencias y similitudes entre los contextos mortuorios a fin de generar información que permita realizar una aproximación al problema. Se caracterizaron los tres entierros; se calibraron las dataciones radiocarbónicas y se realizó una suma de probabilidades; además se efectuaron determinaciones bioarqueológicas y se establecieron las tendencias paleodietarias inferidas a partir del análisis de isótopos estables de carbono, nitrógeno (δ13C y δ15N, colágeno y apatita) y oxígeno (δ18O). Finalmente, se presenta nueva información que permite profundizar acerca de la variabilidad mortuoria de las poblaciones cazadoras recolectoras que habitaron en Patagonia.
“…This type of burial was found only in Bahía Lángara archaeological locality in the coast of San Jorge gulf (Figure ). This type of inhumation is characterized by the presence of primary burials, both single and multiple (Zilio & Hammond, ).…”
The aim of this paper is to provide information on the analysis of stable isotopes obtained from bones of marine and terrestrial fauna used as potential food by hunter‐gatherers on the northern coast of Santa Cruz province (Argentine Patagonia). The results from the isotopic ecology are analysed to contribute to dietary interpretations of the human populations who lived in this area. The mean of terrestrial resources is −19.1‰ ± 1.8‰ and 9.2‰ ± 2.6‰ for δ13C and δ15N, respectively. Meanwhile, marine resources recorded a mean of δ13C −12.5‰ ± 1.2‰ and δ15N of 19.4‰ ± 2.4‰. The analysed human samples come from different types of burials dated mainly in the Late Holocene. The δ13C and δ15N isotopic values on human remains suggest the existence of different diets during the Late Holocene, including people who consumed mainly marine, terrestrial, and mixed proteins, with a range between −18‰ to −10.4‰ and 12.4‰ to 23.4‰ for δ13C and δ15N, respectively. Some of these isotopic values, which indicate marine diets, are the highest recorded for Patagonia. The influence of the marine spray on the terrestrial trophic chains is suggested for the Patagonian Atlantic coast, evidenced by higher values in the δ15N of guanacos from the coast in relation to others studied from the hinterland.
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