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
.jpg)
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/128301
Ver los metadatos del registro completo
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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. |
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2020 |
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2020 |
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