Did the megafauna range to 4300 BP in South America?
- Autores
- Cione, Alberto Luis; Figini, Aníbal Juan; Tonni, Eduardo Pedro
- Año de publicación
- 2001
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- A date of 4300 ± 90 BP for extinct megafauna in Argentina is discussed. The fossil remains come from the Guerrero Member (area) of the Luján Formation near the city of Luján, Buenos Aires Province. The age of the top of the Guerrero Member is constrained by more than 60 radiocarbon dates obtained from the overlying Río Salado Member of Luján Formation, Las Escobas Formation, and Puesto Callejón Viejo Soil, most of them older than 4300 BP. In view of its low collagen content, the 14C measurement of bone sample from Luján should not be accepted uncritically. Because of the poor bone preservation and the possible introduction of "young" contaminants that were not completely eliminated, the 14C date of 4300 ± 90 BP is not reliable. Both biostratigraphic and 14C dating evidence indicates that the date of 4300 BP for the last representative of extinct megafauna in South America is unsupported.
Facultad de Ciencias Naturales y Museo - Materia
-
Ciencias Naturales
Carbono 14
Datación por radiocarbono
megafauna
Argentina - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- http://creativecommons.org/licenses/by-nc-sa/4.0/
- Repositorio
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/83533
Ver los metadatos del registro completo
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Did the megafauna range to 4300 BP in South America?Cione, Alberto LuisFigini, Aníbal JuanTonni, Eduardo PedroCiencias NaturalesCarbono 14Datación por radiocarbonomegafaunaArgentinaA date of 4300 ± 90 BP for extinct megafauna in Argentina is discussed. The fossil remains come from the Guerrero Member (area) of the Luján Formation near the city of Luján, Buenos Aires Province. The age of the top of the Guerrero Member is constrained by more than 60 radiocarbon dates obtained from the overlying Río Salado Member of Luján Formation, Las Escobas Formation, and Puesto Callejón Viejo Soil, most of them older than 4300 BP. In view of its low collagen content, the <SUP>14</SUP>C measurement of bone sample from Luján should not be accepted uncritically. Because of the poor bone preservation and the possible introduction of "young" contaminants that were not completely eliminated, the <SUP>14</SUP>C date of 4300 ± 90 BP is not reliable. Both biostratigraphic and <SUP>14</SUP>C dating evidence indicates that the date of 4300 BP for the last representative of extinct megafauna in South America is unsupported.Facultad de Ciencias Naturales y Museo2001info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdf69-75http://sedici.unlp.edu.ar/handle/10915/83533enginfo:eu-repo/semantics/altIdentifier/issn/0033-8222info:eu-repo/semantics/altIdentifier/doi/10.1017/S0033822200031647info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-09-29T11:15:50Zoai:sedici.unlp.edu.ar:10915/83533Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-29 11:15:50.974SEDICI (UNLP) - Universidad Nacional de La Platafalse |
dc.title.none.fl_str_mv |
Did the megafauna range to 4300 BP in South America? |
title |
Did the megafauna range to 4300 BP in South America? |
spellingShingle |
Did the megafauna range to 4300 BP in South America? Cione, Alberto Luis Ciencias Naturales Carbono 14 Datación por radiocarbono megafauna Argentina |
title_short |
Did the megafauna range to 4300 BP in South America? |
title_full |
Did the megafauna range to 4300 BP in South America? |
title_fullStr |
Did the megafauna range to 4300 BP in South America? |
title_full_unstemmed |
Did the megafauna range to 4300 BP in South America? |
title_sort |
Did the megafauna range to 4300 BP in South America? |
dc.creator.none.fl_str_mv |
Cione, Alberto Luis Figini, Aníbal Juan Tonni, Eduardo Pedro |
author |
Cione, Alberto Luis |
author_facet |
Cione, Alberto Luis Figini, Aníbal Juan Tonni, Eduardo Pedro |
author_role |
author |
author2 |
Figini, Aníbal Juan Tonni, Eduardo Pedro |
author2_role |
author author |
dc.subject.none.fl_str_mv |
Ciencias Naturales Carbono 14 Datación por radiocarbono megafauna Argentina |
topic |
Ciencias Naturales Carbono 14 Datación por radiocarbono megafauna Argentina |
dc.description.none.fl_txt_mv |
A date of 4300 ± 90 BP for extinct megafauna in Argentina is discussed. The fossil remains come from the Guerrero Member (area) of the Luján Formation near the city of Luján, Buenos Aires Province. The age of the top of the Guerrero Member is constrained by more than 60 radiocarbon dates obtained from the overlying Río Salado Member of Luján Formation, Las Escobas Formation, and Puesto Callejón Viejo Soil, most of them older than 4300 BP. In view of its low collagen content, the <SUP>14</SUP>C measurement of bone sample from Luján should not be accepted uncritically. Because of the poor bone preservation and the possible introduction of "young" contaminants that were not completely eliminated, the <SUP>14</SUP>C date of 4300 ± 90 BP is not reliable. Both biostratigraphic and <SUP>14</SUP>C dating evidence indicates that the date of 4300 BP for the last representative of extinct megafauna in South America is unsupported. Facultad de Ciencias Naturales y Museo |
description |
A date of 4300 ± 90 BP for extinct megafauna in Argentina is discussed. The fossil remains come from the Guerrero Member (area) of the Luján Formation near the city of Luján, Buenos Aires Province. The age of the top of the Guerrero Member is constrained by more than 60 radiocarbon dates obtained from the overlying Río Salado Member of Luján Formation, Las Escobas Formation, and Puesto Callejón Viejo Soil, most of them older than 4300 BP. In view of its low collagen content, the <SUP>14</SUP>C measurement of bone sample from Luján should not be accepted uncritically. Because of the poor bone preservation and the possible introduction of "young" contaminants that were not completely eliminated, the <SUP>14</SUP>C date of 4300 ± 90 BP is not reliable. Both biostratigraphic and <SUP>14</SUP>C dating evidence indicates that the date of 4300 BP for the last representative of extinct megafauna in South America is unsupported. |
publishDate |
2001 |
dc.date.none.fl_str_mv |
2001 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Articulo http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
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article |
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publishedVersion |
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http://sedici.unlp.edu.ar/handle/10915/83533 |
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http://sedici.unlp.edu.ar/handle/10915/83533 |
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eng |
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eng |
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info:eu-repo/semantics/altIdentifier/issn/0033-8222 info:eu-repo/semantics/altIdentifier/doi/10.1017/S0033822200031647 |
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info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) |
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openAccess |
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http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) |
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