Soil genesis and landscape evolution in the Parana River Delta
The relationships between landscapes features evolution and soil genesis and distribution are studied. The area is located in southern Entre Rios province (33o00'-33o45'S and 58o30'-59o17'W). The Parana River Delta, has a complex genetic evolution, due to river processes, marine...
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2004
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paper:paper_00044822_v59_n2_p229_Pereyra2023-06-08T14:25:45Z Soil genesis and landscape evolution in the Parana River Delta Pereyra, Fernando X. Baumann, Valérie Altinier, María Victoria Tchilinguirian, Pablo Landscape evolution Parana River Delta Pedogenesis landscape evolution pedogenesis soil drainage spatial distribution Argentina Parana Delta South America Western Hemisphere World The relationships between landscapes features evolution and soil genesis and distribution are studied. The area is located in southern Entre Rios province (33o00'-33o45'S and 58o30'-59o17'W). The Parana River Delta, has a complex genetic evolution, due to river processes, marine ingressions and aeolian actions. These processes resulted in an unstable landscape, that imprinted its particular features in soils. Nine geomorphic units were recognized: 1) Gualeguay river alluvial plain and terraces, 2) Arroyo Ñancay aluvial plain and terrazes, 3) Minor streams aluvial plains, 4) Gualeguay river delta, 5) Deltaic plain, 6) Beach ridges, 7) Old lagoon and tidal plain, 8) Loessic plain and 9) Dunes. Soils are mainly Entisols, Inceptisols and Mollisols, and a spatial trend is recognized in the Delta Region. Soil evolution is controlled by a) an active morphodynamic, b) soil landscape features that resulted in a dominant aquic regime of soils and c) Late Quaternary climatic fluctuations that resulted in sea level variations. Finally, soil development, soil features and distribution and soil drainage are studied in relation with landscape main features and evolution. © 2004 Asociación Geológica Argentina. Fil:Pereyra, F.X. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Baumann, V. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Altinier, V. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Tchilinguirian, P. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2004 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v59_n2_p229_Pereyra http://hdl.handle.net/20.500.12110/paper_00044822_v59_n2_p229_Pereyra |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-134 |
collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
topic |
Landscape evolution Parana River Delta Pedogenesis landscape evolution pedogenesis soil drainage spatial distribution Argentina Parana Delta South America Western Hemisphere World |
spellingShingle |
Landscape evolution Parana River Delta Pedogenesis landscape evolution pedogenesis soil drainage spatial distribution Argentina Parana Delta South America Western Hemisphere World Pereyra, Fernando X. Baumann, Valérie Altinier, María Victoria Tchilinguirian, Pablo Soil genesis and landscape evolution in the Parana River Delta |
topic_facet |
Landscape evolution Parana River Delta Pedogenesis landscape evolution pedogenesis soil drainage spatial distribution Argentina Parana Delta South America Western Hemisphere World |
description |
The relationships between landscapes features evolution and soil genesis and distribution are studied. The area is located in southern Entre Rios province (33o00'-33o45'S and 58o30'-59o17'W). The Parana River Delta, has a complex genetic evolution, due to river processes, marine ingressions and aeolian actions. These processes resulted in an unstable landscape, that imprinted its particular features in soils. Nine geomorphic units were recognized: 1) Gualeguay river alluvial plain and terraces, 2) Arroyo Ñancay aluvial plain and terrazes, 3) Minor streams aluvial plains, 4) Gualeguay river delta, 5) Deltaic plain, 6) Beach ridges, 7) Old lagoon and tidal plain, 8) Loessic plain and 9) Dunes. Soils are mainly Entisols, Inceptisols and Mollisols, and a spatial trend is recognized in the Delta Region. Soil evolution is controlled by a) an active morphodynamic, b) soil landscape features that resulted in a dominant aquic regime of soils and c) Late Quaternary climatic fluctuations that resulted in sea level variations. Finally, soil development, soil features and distribution and soil drainage are studied in relation with landscape main features and evolution. © 2004 Asociación Geológica Argentina. |
author |
Pereyra, Fernando X. Baumann, Valérie Altinier, María Victoria Tchilinguirian, Pablo |
author_facet |
Pereyra, Fernando X. Baumann, Valérie Altinier, María Victoria Tchilinguirian, Pablo |
author_sort |
Pereyra, Fernando X. |
title |
Soil genesis and landscape evolution in the Parana River Delta |
title_short |
Soil genesis and landscape evolution in the Parana River Delta |
title_full |
Soil genesis and landscape evolution in the Parana River Delta |
title_fullStr |
Soil genesis and landscape evolution in the Parana River Delta |
title_full_unstemmed |
Soil genesis and landscape evolution in the Parana River Delta |
title_sort |
soil genesis and landscape evolution in the parana river delta |
publishDate |
2004 |
url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v59_n2_p229_Pereyra http://hdl.handle.net/20.500.12110/paper_00044822_v59_n2_p229_Pereyra |
work_keys_str_mv |
AT pereyrafernandox soilgenesisandlandscapeevolutionintheparanariverdelta AT baumannvalerie soilgenesisandlandscapeevolutionintheparanariverdelta AT altiniermariavictoria soilgenesisandlandscapeevolutionintheparanariverdelta AT tchilinguirianpablo soilgenesisandlandscapeevolutionintheparanariverdelta |
_version_ |
1768544529204379648 |