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
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/83533

id SEDICI_6da373cc7621d1c6c64a29d3a072eb44
oai_identifier_str oai:sedici.unlp.edu.ar:10915/83533
network_acronym_str SEDICI
repository_id_str 1329
network_name_str SEDICI (UNLP)
spelling 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
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://sedici.unlp.edu.ar/handle/10915/83533
url http://sedici.unlp.edu.ar/handle/10915/83533
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/issn/0033-8222
info:eu-repo/semantics/altIdentifier/doi/10.1017/S0033822200031647
dc.rights.none.fl_str_mv 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)
eu_rights_str_mv openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by-nc-sa/4.0/
Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
dc.format.none.fl_str_mv application/pdf
69-75
dc.source.none.fl_str_mv reponame:SEDICI (UNLP)
instname:Universidad Nacional de La Plata
instacron:UNLP
reponame_str SEDICI (UNLP)
collection SEDICI (UNLP)
instname_str Universidad Nacional de La Plata
instacron_str UNLP
institution UNLP
repository.name.fl_str_mv SEDICI (UNLP) - Universidad Nacional de La Plata
repository.mail.fl_str_mv alira@sedici.unlp.edu.ar
_version_ 1844616030664523776
score 13.070432