Back to the bases: Building a terrestrial water δ18O baseline for archaeological studies in North Patagonia (Argentina)

Autores
Serna, Alejandro; Prates, Luciano Raúl; Valenzuela, Luciano O.; Salazar García, Domingo C.
Año de publicación
2020
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Archaeology has been using stable oxygen as an isotopic tracer linked with water consumption for decades, and it has been demonstrated to be a powerful tool to assess paleomobility in bioarchaeology. Central-eastern North Patagonia (Argentina) is an especially appropriate region to apply it since it presents a high density of huntergatherer burials, it was a nodal zone criss-crossed by an extensive network of important routes, and it is characterized by a high environmental fragmentation due to the scarcity of fresh water sources. The aim of this paper is to build an empirical stable oxygen isotope baseline of terrestrial surface waters to assess the potentiality of tracing past human movement. We analyzed 46 water samples from 13 locations with permanent sources (rivers, springs, streams), compared it with predictions of precipitation and evaluated it considering seasonal variation, altitude and distance from the coast. Our results show that different post-precipitation processes change the isotopic signal from the sources with respect to the local precipitation, and highlight the relevance of analyzing terrestrial water sources. According to their oxygen isotope values we defined five hydrologic zones: Colorado River, Negro River, Closed Basins and Plains, Eastern and Western Somuncurá Foothills. Their identification shows the potential to address past human movement using stable oxygen water baselines in central-eastern North Patagonia.
Facultad de Ciencias Naturales y Museo
Materia
Ciencias Naturales
Oxygen isotopes
Isotopic baseline
Paleomobility
Archaeology
Patagonia
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/128301

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spelling Back to the bases: Building a terrestrial water δ18O baseline for archaeological studies in North Patagonia (Argentina)Serna, AlejandroPrates, Luciano RaúlValenzuela, Luciano O.Salazar García, Domingo C.Ciencias NaturalesOxygen isotopesIsotopic baselinePaleomobilityArchaeologyPatagoniaArchaeology has been using stable oxygen as an isotopic tracer linked with water consumption for decades, and it has been demonstrated to be a powerful tool to assess paleomobility in bioarchaeology. Central-eastern North Patagonia (Argentina) is an especially appropriate region to apply it since it presents a high density of huntergatherer burials, it was a nodal zone criss-crossed by an extensive network of important routes, and it is characterized by a high environmental fragmentation due to the scarcity of fresh water sources. The aim of this paper is to build an empirical stable oxygen isotope baseline of terrestrial surface waters to assess the potentiality of tracing past human movement. We analyzed 46 water samples from 13 locations with permanent sources (rivers, springs, streams), compared it with predictions of precipitation and evaluated it considering seasonal variation, altitude and distance from the coast. Our results show that different post-precipitation processes change the isotopic signal from the sources with respect to the local precipitation, and highlight the relevance of analyzing terrestrial water sources. According to their oxygen isotope values we defined five hydrologic zones: Colorado River, Negro River, Closed Basins and Plains, Eastern and Western Somuncurá Foothills. Their identification shows the potential to address past human movement using stable oxygen water baselines in central-eastern North Patagonia.Facultad de Ciencias Naturales y Museo2020info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdf4-12http://sedici.unlp.edu.ar/handle/10915/128301enginfo:eu-repo/semantics/altIdentifier/issn/1040-6182info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quaint.2019.06.008info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/4.0/Creative Commons Attribution 4.0 International (CC BY 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-10-22T17:11:56Zoai:sedici.unlp.edu.ar:10915/128301Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-10-22 17:11:56.788SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv Back to the bases: Building a terrestrial water δ18O baseline for archaeological studies in North Patagonia (Argentina)
title Back to the bases: Building a terrestrial water δ18O baseline for archaeological studies in North Patagonia (Argentina)
spellingShingle Back to the bases: Building a terrestrial water δ18O baseline for archaeological studies in North Patagonia (Argentina)
Serna, Alejandro
Ciencias Naturales
Oxygen isotopes
Isotopic baseline
Paleomobility
Archaeology
Patagonia
title_short Back to the bases: Building a terrestrial water δ18O baseline for archaeological studies in North Patagonia (Argentina)
title_full Back to the bases: Building a terrestrial water δ18O baseline for archaeological studies in North Patagonia (Argentina)
title_fullStr Back to the bases: Building a terrestrial water δ18O baseline for archaeological studies in North Patagonia (Argentina)
title_full_unstemmed Back to the bases: Building a terrestrial water δ18O baseline for archaeological studies in North Patagonia (Argentina)
title_sort Back to the bases: Building a terrestrial water δ18O baseline for archaeological studies in North Patagonia (Argentina)
dc.creator.none.fl_str_mv Serna, Alejandro
Prates, Luciano Raúl
Valenzuela, Luciano O.
Salazar García, Domingo C.
author Serna, Alejandro
author_facet Serna, Alejandro
Prates, Luciano Raúl
Valenzuela, Luciano O.
Salazar García, Domingo C.
author_role author
author2 Prates, Luciano Raúl
Valenzuela, Luciano O.
Salazar García, Domingo C.
author2_role author
author
author
dc.subject.none.fl_str_mv Ciencias Naturales
Oxygen isotopes
Isotopic baseline
Paleomobility
Archaeology
Patagonia
topic Ciencias Naturales
Oxygen isotopes
Isotopic baseline
Paleomobility
Archaeology
Patagonia
dc.description.none.fl_txt_mv Archaeology has been using stable oxygen as an isotopic tracer linked with water consumption for decades, and it has been demonstrated to be a powerful tool to assess paleomobility in bioarchaeology. Central-eastern North Patagonia (Argentina) is an especially appropriate region to apply it since it presents a high density of huntergatherer burials, it was a nodal zone criss-crossed by an extensive network of important routes, and it is characterized by a high environmental fragmentation due to the scarcity of fresh water sources. The aim of this paper is to build an empirical stable oxygen isotope baseline of terrestrial surface waters to assess the potentiality of tracing past human movement. We analyzed 46 water samples from 13 locations with permanent sources (rivers, springs, streams), compared it with predictions of precipitation and evaluated it considering seasonal variation, altitude and distance from the coast. Our results show that different post-precipitation processes change the isotopic signal from the sources with respect to the local precipitation, and highlight the relevance of analyzing terrestrial water sources. According to their oxygen isotope values we defined five hydrologic zones: Colorado River, Negro River, Closed Basins and Plains, Eastern and Western Somuncurá Foothills. Their identification shows the potential to address past human movement using stable oxygen water baselines in central-eastern North Patagonia.
Facultad de Ciencias Naturales y Museo
description Archaeology has been using stable oxygen as an isotopic tracer linked with water consumption for decades, and it has been demonstrated to be a powerful tool to assess paleomobility in bioarchaeology. Central-eastern North Patagonia (Argentina) is an especially appropriate region to apply it since it presents a high density of huntergatherer burials, it was a nodal zone criss-crossed by an extensive network of important routes, and it is characterized by a high environmental fragmentation due to the scarcity of fresh water sources. The aim of this paper is to build an empirical stable oxygen isotope baseline of terrestrial surface waters to assess the potentiality of tracing past human movement. We analyzed 46 water samples from 13 locations with permanent sources (rivers, springs, streams), compared it with predictions of precipitation and evaluated it considering seasonal variation, altitude and distance from the coast. Our results show that different post-precipitation processes change the isotopic signal from the sources with respect to the local precipitation, and highlight the relevance of analyzing terrestrial water sources. According to their oxygen isotope values we defined five hydrologic zones: Colorado River, Negro River, Closed Basins and Plains, Eastern and Western Somuncurá Foothills. Their identification shows the potential to address past human movement using stable oxygen water baselines in central-eastern North Patagonia.
publishDate 2020
dc.date.none.fl_str_mv 2020
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
Articulo
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info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quaint.2019.06.008
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International (CC BY 4.0)
eu_rights_str_mv openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International (CC BY 4.0)
dc.format.none.fl_str_mv application/pdf
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