Evidence of the earliest humans in the Southern Deseado Massif (Patagonia, Argentina), Mylodontidae, and changes in water availability

Autores
Brook, G. A.; Franco, Nora Viviana; Ambrustolo, Pablo; Mancini, Maria Virginia; Wang, L.; Fernández, Pablo Marcelo
Año de publicación
2015
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Mylodontidae bones from La Gruta 3 rockshelter, which date to 11,077-10,571calBP (9560 ± 30-9470 ± 3014CBP) and 9539-9466calBP (8540 ± 3014CBP), indicate that the extinct giant ground sloth was in the area after it was first occupied by humans during the late Pleistocene at 12,799-12,049calBP (10,845 ± 61-10,477 ± 5614CBP). Sediment characteristics at La Gruta 1 and 3 rockshelters (LG1 and LG3) suggest that conditions were wetter during major periods of human occupation and this is supported by pollen data. Lacustrine silts and clays in La Barda, and La Gruta Lagoons 1 and 3, provide evidence of an arid interval prior to about 6500calBP (5690 ± 3514CBP) followed by wetter conditions. This may explain why there is no evidence of humans between ca. 7760 and 5583calBP (7500 ± 250 and 4770 ± 2514CBP) either at La Gruta or at La Martita and Viuda Quenzana, which are ca. 25km away. There is considerable evidence for occupation at Viuda Quenzana after 5581calBP and scanty evidence for occupation at La Gruta around 3800calBP with more abundant evidence after 1880calBP. In the last 1500 years, six radiocarbon ages show that humans occupied LG1 and LG3 before (1372-1271calBP) and after (539-156calBP), but not during, the Medieval Climate Anomaly, which may have been a time of increased aridity in the area. The findings at La Gruta show that Mylodontidae was probably present in the southern Deseado Massif after the first humans arrived but data from southern Patagonia show that it became extinct soon afterwards.
Fil: Brook, G. A.. University of Georgia; Estados Unidos
Fil: Franco, Nora Viviana. Universidad de Buenos Aires; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Ambrustolo, Pablo. Universidad Nacional de La Plata; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Mancini, Maria Virginia. Universidad Nacional de Mar del Plata; Argentina
Fil: Wang, L.. University of Georgia; Estados Unidos
Fil: Fernández, Pablo Marcelo. Secretaría de Cultura de la Nación. Dirección Nacional de Cultura y Museos. Instituto Nacional de Antropología y Pensamiento Latinoamericano; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Materia
Caves
Early Humans
Mylodontidae
Paleoclimate
Patagonia
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/50075

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network_name_str CONICET Digital (CONICET)
spelling Evidence of the earliest humans in the Southern Deseado Massif (Patagonia, Argentina), Mylodontidae, and changes in water availabilityBrook, G. A.Franco, Nora VivianaAmbrustolo, PabloMancini, Maria VirginiaWang, L.Fernández, Pablo MarceloCavesEarly HumansMylodontidaePaleoclimatePatagoniahttps://purl.org/becyt/ford/6.1https://purl.org/becyt/ford/6Mylodontidae bones from La Gruta 3 rockshelter, which date to 11,077-10,571calBP (9560 ± 30-9470 ± 3014CBP) and 9539-9466calBP (8540 ± 3014CBP), indicate that the extinct giant ground sloth was in the area after it was first occupied by humans during the late Pleistocene at 12,799-12,049calBP (10,845 ± 61-10,477 ± 5614CBP). Sediment characteristics at La Gruta 1 and 3 rockshelters (LG1 and LG3) suggest that conditions were wetter during major periods of human occupation and this is supported by pollen data. Lacustrine silts and clays in La Barda, and La Gruta Lagoons 1 and 3, provide evidence of an arid interval prior to about 6500calBP (5690 ± 3514CBP) followed by wetter conditions. This may explain why there is no evidence of humans between ca. 7760 and 5583calBP (7500 ± 250 and 4770 ± 2514CBP) either at La Gruta or at La Martita and Viuda Quenzana, which are ca. 25km away. There is considerable evidence for occupation at Viuda Quenzana after 5581calBP and scanty evidence for occupation at La Gruta around 3800calBP with more abundant evidence after 1880calBP. In the last 1500 years, six radiocarbon ages show that humans occupied LG1 and LG3 before (1372-1271calBP) and after (539-156calBP), but not during, the Medieval Climate Anomaly, which may have been a time of increased aridity in the area. The findings at La Gruta show that Mylodontidae was probably present in the southern Deseado Massif after the first humans arrived but data from southern Patagonia show that it became extinct soon afterwards.Fil: Brook, G. A.. University of Georgia; Estados UnidosFil: Franco, Nora Viviana. Universidad de Buenos Aires; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Ambrustolo, Pablo. Universidad Nacional de La Plata; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Mancini, Maria Virginia. Universidad Nacional de Mar del Plata; ArgentinaFil: Wang, L.. University of Georgia; Estados UnidosFil: Fernández, Pablo Marcelo. Secretaría de Cultura de la Nación. Dirección Nacional de Cultura y Museos. Instituto Nacional de Antropología y Pensamiento Latinoamericano; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaPergamon-Elsevier Science Ltd2015-03info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/50075Brook, G. A.; Franco, Nora Viviana; Ambrustolo, Pablo; Mancini, Maria Virginia; Wang, L.; et al.; Evidence of the earliest humans in the Southern Deseado Massif (Patagonia, Argentina), Mylodontidae, and changes in water availability; Pergamon-Elsevier Science Ltd; Quaternary International; 363; 3-2015; 107-1251040-6182CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.quaint.2014.04.022info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S1040618214002304info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:45:06Zoai:ri.conicet.gov.ar:11336/50075instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 10:45:07.08CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Evidence of the earliest humans in the Southern Deseado Massif (Patagonia, Argentina), Mylodontidae, and changes in water availability
title Evidence of the earliest humans in the Southern Deseado Massif (Patagonia, Argentina), Mylodontidae, and changes in water availability
spellingShingle Evidence of the earliest humans in the Southern Deseado Massif (Patagonia, Argentina), Mylodontidae, and changes in water availability
Brook, G. A.
Caves
Early Humans
Mylodontidae
Paleoclimate
Patagonia
title_short Evidence of the earliest humans in the Southern Deseado Massif (Patagonia, Argentina), Mylodontidae, and changes in water availability
title_full Evidence of the earliest humans in the Southern Deseado Massif (Patagonia, Argentina), Mylodontidae, and changes in water availability
title_fullStr Evidence of the earliest humans in the Southern Deseado Massif (Patagonia, Argentina), Mylodontidae, and changes in water availability
title_full_unstemmed Evidence of the earliest humans in the Southern Deseado Massif (Patagonia, Argentina), Mylodontidae, and changes in water availability
title_sort Evidence of the earliest humans in the Southern Deseado Massif (Patagonia, Argentina), Mylodontidae, and changes in water availability
dc.creator.none.fl_str_mv Brook, G. A.
Franco, Nora Viviana
Ambrustolo, Pablo
Mancini, Maria Virginia
Wang, L.
Fernández, Pablo Marcelo
author Brook, G. A.
author_facet Brook, G. A.
Franco, Nora Viviana
Ambrustolo, Pablo
Mancini, Maria Virginia
Wang, L.
Fernández, Pablo Marcelo
author_role author
author2 Franco, Nora Viviana
Ambrustolo, Pablo
Mancini, Maria Virginia
Wang, L.
Fernández, Pablo Marcelo
author2_role author
author
author
author
author
dc.subject.none.fl_str_mv Caves
Early Humans
Mylodontidae
Paleoclimate
Patagonia
topic Caves
Early Humans
Mylodontidae
Paleoclimate
Patagonia
purl_subject.fl_str_mv https://purl.org/becyt/ford/6.1
https://purl.org/becyt/ford/6
dc.description.none.fl_txt_mv Mylodontidae bones from La Gruta 3 rockshelter, which date to 11,077-10,571calBP (9560 ± 30-9470 ± 3014CBP) and 9539-9466calBP (8540 ± 3014CBP), indicate that the extinct giant ground sloth was in the area after it was first occupied by humans during the late Pleistocene at 12,799-12,049calBP (10,845 ± 61-10,477 ± 5614CBP). Sediment characteristics at La Gruta 1 and 3 rockshelters (LG1 and LG3) suggest that conditions were wetter during major periods of human occupation and this is supported by pollen data. Lacustrine silts and clays in La Barda, and La Gruta Lagoons 1 and 3, provide evidence of an arid interval prior to about 6500calBP (5690 ± 3514CBP) followed by wetter conditions. This may explain why there is no evidence of humans between ca. 7760 and 5583calBP (7500 ± 250 and 4770 ± 2514CBP) either at La Gruta or at La Martita and Viuda Quenzana, which are ca. 25km away. There is considerable evidence for occupation at Viuda Quenzana after 5581calBP and scanty evidence for occupation at La Gruta around 3800calBP with more abundant evidence after 1880calBP. In the last 1500 years, six radiocarbon ages show that humans occupied LG1 and LG3 before (1372-1271calBP) and after (539-156calBP), but not during, the Medieval Climate Anomaly, which may have been a time of increased aridity in the area. The findings at La Gruta show that Mylodontidae was probably present in the southern Deseado Massif after the first humans arrived but data from southern Patagonia show that it became extinct soon afterwards.
Fil: Brook, G. A.. University of Georgia; Estados Unidos
Fil: Franco, Nora Viviana. Universidad de Buenos Aires; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Ambrustolo, Pablo. Universidad Nacional de La Plata; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Mancini, Maria Virginia. Universidad Nacional de Mar del Plata; Argentina
Fil: Wang, L.. University of Georgia; Estados Unidos
Fil: Fernández, Pablo Marcelo. Secretaría de Cultura de la Nación. Dirección Nacional de Cultura y Museos. Instituto Nacional de Antropología y Pensamiento Latinoamericano; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
description Mylodontidae bones from La Gruta 3 rockshelter, which date to 11,077-10,571calBP (9560 ± 30-9470 ± 3014CBP) and 9539-9466calBP (8540 ± 3014CBP), indicate that the extinct giant ground sloth was in the area after it was first occupied by humans during the late Pleistocene at 12,799-12,049calBP (10,845 ± 61-10,477 ± 5614CBP). Sediment characteristics at La Gruta 1 and 3 rockshelters (LG1 and LG3) suggest that conditions were wetter during major periods of human occupation and this is supported by pollen data. Lacustrine silts and clays in La Barda, and La Gruta Lagoons 1 and 3, provide evidence of an arid interval prior to about 6500calBP (5690 ± 3514CBP) followed by wetter conditions. This may explain why there is no evidence of humans between ca. 7760 and 5583calBP (7500 ± 250 and 4770 ± 2514CBP) either at La Gruta or at La Martita and Viuda Quenzana, which are ca. 25km away. There is considerable evidence for occupation at Viuda Quenzana after 5581calBP and scanty evidence for occupation at La Gruta around 3800calBP with more abundant evidence after 1880calBP. In the last 1500 years, six radiocarbon ages show that humans occupied LG1 and LG3 before (1372-1271calBP) and after (539-156calBP), but not during, the Medieval Climate Anomaly, which may have been a time of increased aridity in the area. The findings at La Gruta show that Mylodontidae was probably present in the southern Deseado Massif after the first humans arrived but data from southern Patagonia show that it became extinct soon afterwards.
publishDate 2015
dc.date.none.fl_str_mv 2015-03
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
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info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/50075
Brook, G. A.; Franco, Nora Viviana; Ambrustolo, Pablo; Mancini, Maria Virginia; Wang, L.; et al.; Evidence of the earliest humans in the Southern Deseado Massif (Patagonia, Argentina), Mylodontidae, and changes in water availability; Pergamon-Elsevier Science Ltd; Quaternary International; 363; 3-2015; 107-125
1040-6182
CONICET Digital
CONICET
url http://hdl.handle.net/11336/50075
identifier_str_mv Brook, G. A.; Franco, Nora Viviana; Ambrustolo, Pablo; Mancini, Maria Virginia; Wang, L.; et al.; Evidence of the earliest humans in the Southern Deseado Massif (Patagonia, Argentina), Mylodontidae, and changes in water availability; Pergamon-Elsevier Science Ltd; Quaternary International; 363; 3-2015; 107-125
1040-6182
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quaint.2014.04.022
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S1040618214002304
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
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dc.publisher.none.fl_str_mv Pergamon-Elsevier Science Ltd
publisher.none.fl_str_mv Pergamon-Elsevier Science Ltd
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