Late Pleistocene-Holocene paleoenvironments in the middle basin of the Salado river, province of Buenos Aires, Argentina
- Autores
- Pommarés, Nicole Nadín; Fucks, Enrique Eduardo; Pisano, María Florencia; Luengo, Mariel Samanta; Ramos, Nicolás Andrés; Di Lello, Claudia Viviana
- Año de publicación
- 2020
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The Salado river basin is the largest one in the Buenos Aires province, with an area near 170,000 km2. This work aims to perform a stratigraphic analysis of the middle sector of this basin to provide information on the paleoenvironmental evolution during the end of the Quaternary. Results indicate that the evolution of this basin occurred largely in water deficit conditions. Different aeolian lithostratigraphic units are recognized and grouped into three units, as follows: La Postrera, Laguna Las Barrancas, and De la Riestra Formations. New lithological, paleontological, and chronological information is provided regarding the fluvial deposits, which allows for a deeper understanding of the paleoenvironmental conditions that prevailed during deposition. The integrated study of all these deposits with an adjusted chronological control suggests a paleoenvironmental model that is directly associated with the climatic conditions that prevailed at the end of the Quaternary.
Centro de Estudios Integrales de la Dinámica Exógena
Consejo Nacional de Investigaciones Científicas y Técnicas - Materia
-
Ciencias Naturales
Fluvial deposits
Paleoclimate
Loess
Lunettes
Deflation basins
Paleoenvironmental reconstruction - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- http://creativecommons.org/licenses/by/4.0/
- Repositorio
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/169206
Ver los metadatos del registro completo
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Late Pleistocene-Holocene paleoenvironments in the middle basin of the Salado river, province of Buenos Aires, ArgentinaPommarés, Nicole NadínFucks, Enrique EduardoPisano, María FlorenciaLuengo, Mariel SamantaRamos, Nicolás AndrésDi Lello, Claudia VivianaCiencias NaturalesFluvial depositsPaleoclimateLoessLunettesDeflation basinsPaleoenvironmental reconstructionThe Salado river basin is the largest one in the Buenos Aires province, with an area near 170,000 km2. This work aims to perform a stratigraphic analysis of the middle sector of this basin to provide information on the paleoenvironmental evolution during the end of the Quaternary. Results indicate that the evolution of this basin occurred largely in water deficit conditions. Different aeolian lithostratigraphic units are recognized and grouped into three units, as follows: La Postrera, Laguna Las Barrancas, and De la Riestra Formations. New lithological, paleontological, and chronological information is provided regarding the fluvial deposits, which allows for a deeper understanding of the paleoenvironmental conditions that prevailed during deposition. The integrated study of all these deposits with an adjusted chronological control suggests a paleoenvironmental model that is directly associated with the climatic conditions that prevailed at the end of the Quaternary.Centro de Estudios Integrales de la Dinámica ExógenaConsejo Nacional de Investigaciones Científicas y Técnicas2020-11-13info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfhttp://sedici.unlp.edu.ar/handle/10915/169206enginfo:eu-repo/semantics/altIdentifier/issn/0895-9811info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsames.2020.103001info: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:UNLP2025-09-29T11:45:01Zoai:sedici.unlp.edu.ar:10915/169206Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-29 11:45:02.03SEDICI (UNLP) - Universidad Nacional de La Platafalse |
dc.title.none.fl_str_mv |
Late Pleistocene-Holocene paleoenvironments in the middle basin of the Salado river, province of Buenos Aires, Argentina |
title |
Late Pleistocene-Holocene paleoenvironments in the middle basin of the Salado river, province of Buenos Aires, Argentina |
spellingShingle |
Late Pleistocene-Holocene paleoenvironments in the middle basin of the Salado river, province of Buenos Aires, Argentina Pommarés, Nicole Nadín Ciencias Naturales Fluvial deposits Paleoclimate Loess Lunettes Deflation basins Paleoenvironmental reconstruction |
title_short |
Late Pleistocene-Holocene paleoenvironments in the middle basin of the Salado river, province of Buenos Aires, Argentina |
title_full |
Late Pleistocene-Holocene paleoenvironments in the middle basin of the Salado river, province of Buenos Aires, Argentina |
title_fullStr |
Late Pleistocene-Holocene paleoenvironments in the middle basin of the Salado river, province of Buenos Aires, Argentina |
title_full_unstemmed |
Late Pleistocene-Holocene paleoenvironments in the middle basin of the Salado river, province of Buenos Aires, Argentina |
title_sort |
Late Pleistocene-Holocene paleoenvironments in the middle basin of the Salado river, province of Buenos Aires, Argentina |
dc.creator.none.fl_str_mv |
Pommarés, Nicole Nadín Fucks, Enrique Eduardo Pisano, María Florencia Luengo, Mariel Samanta Ramos, Nicolás Andrés Di Lello, Claudia Viviana |
author |
Pommarés, Nicole Nadín |
author_facet |
Pommarés, Nicole Nadín Fucks, Enrique Eduardo Pisano, María Florencia Luengo, Mariel Samanta Ramos, Nicolás Andrés Di Lello, Claudia Viviana |
author_role |
author |
author2 |
Fucks, Enrique Eduardo Pisano, María Florencia Luengo, Mariel Samanta Ramos, Nicolás Andrés Di Lello, Claudia Viviana |
author2_role |
author author author author author |
dc.subject.none.fl_str_mv |
Ciencias Naturales Fluvial deposits Paleoclimate Loess Lunettes Deflation basins Paleoenvironmental reconstruction |
topic |
Ciencias Naturales Fluvial deposits Paleoclimate Loess Lunettes Deflation basins Paleoenvironmental reconstruction |
dc.description.none.fl_txt_mv |
The Salado river basin is the largest one in the Buenos Aires province, with an area near 170,000 km2. This work aims to perform a stratigraphic analysis of the middle sector of this basin to provide information on the paleoenvironmental evolution during the end of the Quaternary. Results indicate that the evolution of this basin occurred largely in water deficit conditions. Different aeolian lithostratigraphic units are recognized and grouped into three units, as follows: La Postrera, Laguna Las Barrancas, and De la Riestra Formations. New lithological, paleontological, and chronological information is provided regarding the fluvial deposits, which allows for a deeper understanding of the paleoenvironmental conditions that prevailed during deposition. The integrated study of all these deposits with an adjusted chronological control suggests a paleoenvironmental model that is directly associated with the climatic conditions that prevailed at the end of the Quaternary. Centro de Estudios Integrales de la Dinámica Exógena Consejo Nacional de Investigaciones Científicas y Técnicas |
description |
The Salado river basin is the largest one in the Buenos Aires province, with an area near 170,000 km2. This work aims to perform a stratigraphic analysis of the middle sector of this basin to provide information on the paleoenvironmental evolution during the end of the Quaternary. Results indicate that the evolution of this basin occurred largely in water deficit conditions. Different aeolian lithostratigraphic units are recognized and grouped into three units, as follows: La Postrera, Laguna Las Barrancas, and De la Riestra Formations. New lithological, paleontological, and chronological information is provided regarding the fluvial deposits, which allows for a deeper understanding of the paleoenvironmental conditions that prevailed during deposition. The integrated study of all these deposits with an adjusted chronological control suggests a paleoenvironmental model that is directly associated with the climatic conditions that prevailed at the end of the Quaternary. |
publishDate |
2020 |
dc.date.none.fl_str_mv |
2020-11-13 |
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/10915/169206 |
url |
http://sedici.unlp.edu.ar/handle/10915/169206 |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/issn/0895-9811 info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsames.2020.103001 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International (CC BY 4.0) |
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openAccess |
rights_invalid_str_mv |
http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International (CC BY 4.0) |
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application/pdf |
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SEDICI (UNLP) - Universidad Nacional de La Plata |
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