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
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/281207
Ver los metadatos del registro completo
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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. |
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2025 |
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2025-07 |
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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 |
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http://hdl.handle.net/11336/281207 |
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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 |
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eng |
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