Aeolian Landscapes and Paleoclimatic Legacy in the Southern Chacopampean Plain, Argentina

Autores
Fucks, Enrique Eduardo; Rico, Yamile; Galone, Luciano; Lorente, Malena; D'Amico, Sebastiano; Pisano, Maria Florencia
Año de publicación
2025
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The Chacopampean Plain is a major physiographic unit in Argentina, bounded by theColorado River to the south, the Sierras Pampeanas and Subandinas to the west, and theParaná River, Río de la Plata Estuary, and the Argentine Sea to the east. Its subsurfacepreserves sediments from the Miocene marine transgression, while the surface hosts someof the country’s most productive soils. Two main geomorphological domains are recognized:fluvial systems dominated by alluvial megafans in the north, and aeolian systemscharacterized by loess accumulation and wind erosion in the south. The southern sectorexhibits diverse landforms such as deflation basins, ridges, dune corridors, lunettes, andmantiform loess deposits. Despite their regional extent, the origin and chronology of manyaeolian features remain poorly constrained, as previous studies have primarily focusedon depositional units rather than wind-sculpted erosional features. This study integratesremote sensing data, field observations, and a synthesis of published chronometric andsedimentological information to characterize these aeolian landforms and elucidate theirgenesis. Our findings confirm wind as the dominant morphogenetic agent during LateQuaternary glacial stadials. These aeolian morphologies significantly influence the region’shydrology, as many permanent and ephemeral water bodies occupy deflation basins orintermediate low-lying sectors prone to flooding under modern climatic conditions, whichare considerably wetter than during their original formation.
Fil: Fucks, Enrique Eduardo. Centro En Estudios Integrales de la Dinamica Exogeno (ceide) ; Facultad de Cs.agrarias y Forestales ; Universidad Nacional de la Plata;
Fil: Rico, Yamile. Provincia de Buenos Aires. Gobernación. Comisión de Investigaciones Científicas; Argentina
Fil: Galone, Luciano. University of Malta; Malta
Fil: Lorente, Malena. Universidad Nacional de la Plata. Facultad de Cs.naturales y Museo. Centro de Estudios Integrales de la Dinamica Exogeno.; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: D'Amico, Sebastiano. University of Malta; Malta
Fil: Pisano, Maria Florencia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de la Plata. Facultad de Cs.naturales y Museo. Centro de Estudios Integrales de la Dinamica Exogeno.; Argentina
Materia
wind processes
Pampas Plain
paleoclimate
loess
geomorphology
Argentina
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/281207

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network_name_str CONICET Digital (CONICET)
spelling Aeolian Landscapes and Paleoclimatic Legacy in the Southern Chacopampean Plain, ArgentinaFucks, Enrique EduardoRico, YamileGalone, LucianoLorente, MalenaD'Amico, SebastianoPisano, Maria Florenciawind processesPampas PlainpaleoclimateloessgeomorphologyArgentinahttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Chacopampean Plain is a major physiographic unit in Argentina, bounded by theColorado River to the south, the Sierras Pampeanas and Subandinas to the west, and theParaná River, Río de la Plata Estuary, and the Argentine Sea to the east. Its subsurfacepreserves sediments from the Miocene marine transgression, while the surface hosts someof the country’s most productive soils. Two main geomorphological domains are recognized:fluvial systems dominated by alluvial megafans in the north, and aeolian systemscharacterized by loess accumulation and wind erosion in the south. The southern sectorexhibits diverse landforms such as deflation basins, ridges, dune corridors, lunettes, andmantiform loess deposits. Despite their regional extent, the origin and chronology of manyaeolian features remain poorly constrained, as previous studies have primarily focusedon depositional units rather than wind-sculpted erosional features. This study integratesremote sensing data, field observations, and a synthesis of published chronometric andsedimentological information to characterize these aeolian landforms and elucidate theirgenesis. Our findings confirm wind as the dominant morphogenetic agent during LateQuaternary glacial stadials. These aeolian morphologies significantly influence the region’shydrology, as many permanent and ephemeral water bodies occupy deflation basins orintermediate low-lying sectors prone to flooding under modern climatic conditions, whichare considerably wetter than during their original formation.Fil: Fucks, Enrique Eduardo. Centro En Estudios Integrales de la Dinamica Exogeno (ceide) ; Facultad de Cs.agrarias y Forestales ; Universidad Nacional de la Plata;Fil: Rico, Yamile. Provincia de Buenos Aires. Gobernación. Comisión de Investigaciones Científicas; ArgentinaFil: Galone, Luciano. University of Malta; MaltaFil: Lorente, Malena. Universidad Nacional de la Plata. Facultad de Cs.naturales y Museo. Centro de Estudios Integrales de la Dinamica Exogeno.; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: D'Amico, Sebastiano. University of Malta; MaltaFil: Pisano, Maria Florencia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de la Plata. Facultad de Cs.naturales y Museo. Centro de Estudios Integrales de la Dinamica Exogeno.; ArgentinaMDPI2025-07info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/281207Fucks, Enrique Eduardo; Rico, Yamile; Galone, Luciano; Lorente, Malena; D'Amico, Sebastiano; et al.; Aeolian Landscapes and Paleoclimatic Legacy in the Southern Chacopampean Plain, Argentina; MDPI; Geographies; 5; 3; 7-2025; 1-242673-7086CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.mdpi.com/2673-7086/5/3/33info:eu-repo/semantics/altIdentifier/doi/10.3390/geographies5030033info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2026-02-26T10:26:58Zoai:ri.conicet.gov.ar:11336/281207instacron: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:34982026-02-26 10:26:59.248CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Aeolian Landscapes and Paleoclimatic Legacy in the Southern Chacopampean Plain, Argentina
title Aeolian Landscapes and Paleoclimatic Legacy in the Southern Chacopampean Plain, Argentina
spellingShingle Aeolian Landscapes and Paleoclimatic Legacy in the Southern Chacopampean Plain, Argentina
Fucks, Enrique Eduardo
wind processes
Pampas Plain
paleoclimate
loess
geomorphology
Argentina
title_short Aeolian Landscapes and Paleoclimatic Legacy in the Southern Chacopampean Plain, Argentina
title_full Aeolian Landscapes and Paleoclimatic Legacy in the Southern Chacopampean Plain, Argentina
title_fullStr Aeolian Landscapes and Paleoclimatic Legacy in the Southern Chacopampean Plain, Argentina
title_full_unstemmed Aeolian Landscapes and Paleoclimatic Legacy in the Southern Chacopampean Plain, Argentina
title_sort Aeolian Landscapes and Paleoclimatic Legacy in the Southern Chacopampean Plain, Argentina
dc.creator.none.fl_str_mv Fucks, Enrique Eduardo
Rico, Yamile
Galone, Luciano
Lorente, Malena
D'Amico, Sebastiano
Pisano, Maria Florencia
author Fucks, Enrique Eduardo
author_facet Fucks, Enrique Eduardo
Rico, Yamile
Galone, Luciano
Lorente, Malena
D'Amico, Sebastiano
Pisano, Maria Florencia
author_role author
author2 Rico, Yamile
Galone, Luciano
Lorente, Malena
D'Amico, Sebastiano
Pisano, Maria Florencia
author2_role author
author
author
author
author
dc.subject.none.fl_str_mv wind processes
Pampas Plain
paleoclimate
loess
geomorphology
Argentina
topic wind processes
Pampas Plain
paleoclimate
loess
geomorphology
Argentina
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv The Chacopampean Plain is a major physiographic unit in Argentina, bounded by theColorado River to the south, the Sierras Pampeanas and Subandinas to the west, and theParaná River, Río de la Plata Estuary, and the Argentine Sea to the east. Its subsurfacepreserves sediments from the Miocene marine transgression, while the surface hosts someof the country’s most productive soils. Two main geomorphological domains are recognized:fluvial systems dominated by alluvial megafans in the north, and aeolian systemscharacterized by loess accumulation and wind erosion in the south. The southern sectorexhibits diverse landforms such as deflation basins, ridges, dune corridors, lunettes, andmantiform loess deposits. Despite their regional extent, the origin and chronology of manyaeolian features remain poorly constrained, as previous studies have primarily focusedon depositional units rather than wind-sculpted erosional features. This study integratesremote sensing data, field observations, and a synthesis of published chronometric andsedimentological information to characterize these aeolian landforms and elucidate theirgenesis. Our findings confirm wind as the dominant morphogenetic agent during LateQuaternary glacial stadials. These aeolian morphologies significantly influence the region’shydrology, as many permanent and ephemeral water bodies occupy deflation basins orintermediate low-lying sectors prone to flooding under modern climatic conditions, whichare considerably wetter than during their original formation.
Fil: Fucks, Enrique Eduardo. Centro En Estudios Integrales de la Dinamica Exogeno (ceide) ; Facultad de Cs.agrarias y Forestales ; Universidad Nacional de la Plata;
Fil: Rico, Yamile. Provincia de Buenos Aires. Gobernación. Comisión de Investigaciones Científicas; Argentina
Fil: Galone, Luciano. University of Malta; Malta
Fil: Lorente, Malena. Universidad Nacional de la Plata. Facultad de Cs.naturales y Museo. Centro de Estudios Integrales de la Dinamica Exogeno.; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: D'Amico, Sebastiano. University of Malta; Malta
Fil: Pisano, Maria Florencia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de la Plata. Facultad de Cs.naturales y Museo. Centro de Estudios Integrales de la Dinamica Exogeno.; Argentina
description The Chacopampean Plain is a major physiographic unit in Argentina, bounded by theColorado River to the south, the Sierras Pampeanas and Subandinas to the west, and theParaná River, Río de la Plata Estuary, and the Argentine Sea to the east. Its subsurfacepreserves sediments from the Miocene marine transgression, while the surface hosts someof the country’s most productive soils. Two main geomorphological domains are recognized:fluvial systems dominated by alluvial megafans in the north, and aeolian systemscharacterized by loess accumulation and wind erosion in the south. The southern sectorexhibits diverse landforms such as deflation basins, ridges, dune corridors, lunettes, andmantiform loess deposits. Despite their regional extent, the origin and chronology of manyaeolian features remain poorly constrained, as previous studies have primarily focusedon depositional units rather than wind-sculpted erosional features. This study integratesremote sensing data, field observations, and a synthesis of published chronometric andsedimentological information to characterize these aeolian landforms and elucidate theirgenesis. Our findings confirm wind as the dominant morphogenetic agent during LateQuaternary glacial stadials. These aeolian morphologies significantly influence the region’shydrology, as many permanent and ephemeral water bodies occupy deflation basins orintermediate low-lying sectors prone to flooding under modern climatic conditions, whichare considerably wetter than during their original formation.
publishDate 2025
dc.date.none.fl_str_mv 2025-07
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/11336/281207
Fucks, Enrique Eduardo; Rico, Yamile; Galone, Luciano; Lorente, Malena; D'Amico, Sebastiano; et al.; Aeolian Landscapes and Paleoclimatic Legacy in the Southern Chacopampean Plain, Argentina; MDPI; Geographies; 5; 3; 7-2025; 1-24
2673-7086
CONICET Digital
CONICET
url http://hdl.handle.net/11336/281207
identifier_str_mv Fucks, Enrique Eduardo; Rico, Yamile; Galone, Luciano; Lorente, Malena; D'Amico, Sebastiano; et al.; Aeolian Landscapes and Paleoclimatic Legacy in the Southern Chacopampean Plain, Argentina; MDPI; Geographies; 5; 3; 7-2025; 1-24
2673-7086
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://www.mdpi.com/2673-7086/5/3/33
info:eu-repo/semantics/altIdentifier/doi/10.3390/geographies5030033
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
application/pdf
dc.publisher.none.fl_str_mv MDPI
publisher.none.fl_str_mv MDPI
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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