Environmental changes in the pre-Andean valleys and Chaco Plain (Northwest Argentina) during the Late Pleistocene and Holocene
- Autores
- Sayago, Jose Manuel; Zinck, J.; Collantes, Mirian Mabel; Toledo, M.
- Año de publicación
- 2005
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Thick loess deposits interbedded with paleosols in the intermountain valleys of Tafí (Tucumán province) and Balcozna (Catamarca province) in north-western Argentina were assigned to late Pleistocene age on the basis of radiocarbon, biostratigraphic and soil evidence. The mechanisms of loess transport and soil formation are related to recurrent northward shifts of the polar front, with a temporal frequency that is in phase with the Dansgaard-Oerscher cycles. In the western Chaco plain, paleosol sequences developed during the Holocene show a general coincidence with the cold periods of glaciochemical increase detected in the Greenland GISP2 ice core. Moreover, the Greenland cold events also parallel the Holocene glacial advances in the southern Patagonian Andes. In conclusion, the regional pattern of loess-paleosol sequences developed in the subtropical pre-Andean valleys and in the western Chaco plain of northwest Argentina during Late Pleistocene and Holocene suggests that the perturbations affecting air and ocean circulation over the North Atlantic might have also influenced the climatic conditions in sub-tropical South America. © 2005 E. Schweizerbart'sche Verlagsbuchhandlung.
Fil: Sayago, Jose Manuel. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Instituto de Geociencias y Medio Ambiente; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; Argentina
Fil: Zinck, J.. Universidad Nacional de Tucumán; Argentina
Fil: Collantes, Mirian Mabel. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Instituto de Geociencias y Medio Ambiente; Argentina
Fil: Toledo, M.. Fundación Miguel Lillo; Argentina - Materia
-
DANSGAARD-OERSCHER CYCLES
HOLOCENE COLD PERIODS
LOESS-PALEOSOLS
PALEOCLIMATIC CYCLICITY - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/100861
Ver los metadatos del registro completo
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Environmental changes in the pre-Andean valleys and Chaco Plain (Northwest Argentina) during the Late Pleistocene and HoloceneSayago, Jose ManuelZinck, J.Collantes, Mirian MabelToledo, M.DANSGAARD-OERSCHER CYCLESHOLOCENE COLD PERIODSLOESS-PALEOSOLSPALEOCLIMATIC CYCLICITYhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Thick loess deposits interbedded with paleosols in the intermountain valleys of Tafí (Tucumán province) and Balcozna (Catamarca province) in north-western Argentina were assigned to late Pleistocene age on the basis of radiocarbon, biostratigraphic and soil evidence. The mechanisms of loess transport and soil formation are related to recurrent northward shifts of the polar front, with a temporal frequency that is in phase with the Dansgaard-Oerscher cycles. In the western Chaco plain, paleosol sequences developed during the Holocene show a general coincidence with the cold periods of glaciochemical increase detected in the Greenland GISP2 ice core. Moreover, the Greenland cold events also parallel the Holocene glacial advances in the southern Patagonian Andes. In conclusion, the regional pattern of loess-paleosol sequences developed in the subtropical pre-Andean valleys and in the western Chaco plain of northwest Argentina during Late Pleistocene and Holocene suggests that the perturbations affecting air and ocean circulation over the North Atlantic might have also influenced the climatic conditions in sub-tropical South America. © 2005 E. Schweizerbart'sche Verlagsbuchhandlung.Fil: Sayago, Jose Manuel. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Instituto de Geociencias y Medio Ambiente; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; ArgentinaFil: Zinck, J.. Universidad Nacional de Tucumán; ArgentinaFil: Collantes, Mirian Mabel. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Instituto de Geociencias y Medio Ambiente; ArgentinaFil: Toledo, M.. Fundación Miguel Lillo; ArgentinaE Schweizerbartsche Verlags2005-08info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/100861Sayago, Jose Manuel; Zinck, J.; Collantes, Mirian Mabel; Toledo, M.; Environmental changes in the pre-Andean valleys and Chaco Plain (Northwest Argentina) during the Late Pleistocene and Holocene; E Schweizerbartsche Verlags; Neues Jahrbuch für Geologie und Palaontologie - Abhandlungen; 236; 1-2; 8-2005; 245-2650077-7749CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1127/njgpa/236/2005/245info:eu-repo/semantics/altIdentifier/url/https://www.schweizerbart.de/shop/cart/add?artno=155023601012info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:53:27Zoai:ri.conicet.gov.ar:11336/100861instacron: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:34982025-09-03 09:53:27.321CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Environmental changes in the pre-Andean valleys and Chaco Plain (Northwest Argentina) during the Late Pleistocene and Holocene |
title |
Environmental changes in the pre-Andean valleys and Chaco Plain (Northwest Argentina) during the Late Pleistocene and Holocene |
spellingShingle |
Environmental changes in the pre-Andean valleys and Chaco Plain (Northwest Argentina) during the Late Pleistocene and Holocene Sayago, Jose Manuel DANSGAARD-OERSCHER CYCLES HOLOCENE COLD PERIODS LOESS-PALEOSOLS PALEOCLIMATIC CYCLICITY |
title_short |
Environmental changes in the pre-Andean valleys and Chaco Plain (Northwest Argentina) during the Late Pleistocene and Holocene |
title_full |
Environmental changes in the pre-Andean valleys and Chaco Plain (Northwest Argentina) during the Late Pleistocene and Holocene |
title_fullStr |
Environmental changes in the pre-Andean valleys and Chaco Plain (Northwest Argentina) during the Late Pleistocene and Holocene |
title_full_unstemmed |
Environmental changes in the pre-Andean valleys and Chaco Plain (Northwest Argentina) during the Late Pleistocene and Holocene |
title_sort |
Environmental changes in the pre-Andean valleys and Chaco Plain (Northwest Argentina) during the Late Pleistocene and Holocene |
dc.creator.none.fl_str_mv |
Sayago, Jose Manuel Zinck, J. Collantes, Mirian Mabel Toledo, M. |
author |
Sayago, Jose Manuel |
author_facet |
Sayago, Jose Manuel Zinck, J. Collantes, Mirian Mabel Toledo, M. |
author_role |
author |
author2 |
Zinck, J. Collantes, Mirian Mabel Toledo, M. |
author2_role |
author author author |
dc.subject.none.fl_str_mv |
DANSGAARD-OERSCHER CYCLES HOLOCENE COLD PERIODS LOESS-PALEOSOLS PALEOCLIMATIC CYCLICITY |
topic |
DANSGAARD-OERSCHER CYCLES HOLOCENE COLD PERIODS LOESS-PALEOSOLS PALEOCLIMATIC CYCLICITY |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
Thick loess deposits interbedded with paleosols in the intermountain valleys of Tafí (Tucumán province) and Balcozna (Catamarca province) in north-western Argentina were assigned to late Pleistocene age on the basis of radiocarbon, biostratigraphic and soil evidence. The mechanisms of loess transport and soil formation are related to recurrent northward shifts of the polar front, with a temporal frequency that is in phase with the Dansgaard-Oerscher cycles. In the western Chaco plain, paleosol sequences developed during the Holocene show a general coincidence with the cold periods of glaciochemical increase detected in the Greenland GISP2 ice core. Moreover, the Greenland cold events also parallel the Holocene glacial advances in the southern Patagonian Andes. In conclusion, the regional pattern of loess-paleosol sequences developed in the subtropical pre-Andean valleys and in the western Chaco plain of northwest Argentina during Late Pleistocene and Holocene suggests that the perturbations affecting air and ocean circulation over the North Atlantic might have also influenced the climatic conditions in sub-tropical South America. © 2005 E. Schweizerbart'sche Verlagsbuchhandlung. Fil: Sayago, Jose Manuel. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Instituto de Geociencias y Medio Ambiente; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; Argentina Fil: Zinck, J.. Universidad Nacional de Tucumán; Argentina Fil: Collantes, Mirian Mabel. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Instituto de Geociencias y Medio Ambiente; Argentina Fil: Toledo, M.. Fundación Miguel Lillo; Argentina |
description |
Thick loess deposits interbedded with paleosols in the intermountain valleys of Tafí (Tucumán province) and Balcozna (Catamarca province) in north-western Argentina were assigned to late Pleistocene age on the basis of radiocarbon, biostratigraphic and soil evidence. The mechanisms of loess transport and soil formation are related to recurrent northward shifts of the polar front, with a temporal frequency that is in phase with the Dansgaard-Oerscher cycles. In the western Chaco plain, paleosol sequences developed during the Holocene show a general coincidence with the cold periods of glaciochemical increase detected in the Greenland GISP2 ice core. Moreover, the Greenland cold events also parallel the Holocene glacial advances in the southern Patagonian Andes. In conclusion, the regional pattern of loess-paleosol sequences developed in the subtropical pre-Andean valleys and in the western Chaco plain of northwest Argentina during Late Pleistocene and Holocene suggests that the perturbations affecting air and ocean circulation over the North Atlantic might have also influenced the climatic conditions in sub-tropical South America. © 2005 E. Schweizerbart'sche Verlagsbuchhandlung. |
publishDate |
2005 |
dc.date.none.fl_str_mv |
2005-08 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 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://hdl.handle.net/11336/100861 Sayago, Jose Manuel; Zinck, J.; Collantes, Mirian Mabel; Toledo, M.; Environmental changes in the pre-Andean valleys and Chaco Plain (Northwest Argentina) during the Late Pleistocene and Holocene; E Schweizerbartsche Verlags; Neues Jahrbuch für Geologie und Palaontologie - Abhandlungen; 236; 1-2; 8-2005; 245-265 0077-7749 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/100861 |
identifier_str_mv |
Sayago, Jose Manuel; Zinck, J.; Collantes, Mirian Mabel; Toledo, M.; Environmental changes in the pre-Andean valleys and Chaco Plain (Northwest Argentina) during the Late Pleistocene and Holocene; E Schweizerbartsche Verlags; Neues Jahrbuch für Geologie und Palaontologie - Abhandlungen; 236; 1-2; 8-2005; 245-265 0077-7749 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1127/njgpa/236/2005/245 info:eu-repo/semantics/altIdentifier/url/https://www.schweizerbart.de/shop/cart/add?artno=155023601012 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
E Schweizerbartsche Verlags |
publisher.none.fl_str_mv |
E Schweizerbartsche Verlags |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
reponame_str |
CONICET Digital (CONICET) |
collection |
CONICET Digital (CONICET) |
instname_str |
Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.name.fl_str_mv |
CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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1842269225895329792 |
score |
13.13397 |