Geomorphologic units of the Middle São Francisco River alluvial plain, Northeastern Brazil

Detalhes bibliográficos
Autor(a) principal: Santos, Landerlei Almeida [UNESP]
Data de Publicação: 2022
Outros Autores: Latrubesse, Edgardo Manuel
Tipo de documento: Artigo
Idioma: por
Título da fonte: Repositório Institucional da UNESP
Texto Completo: http://dx.doi.org/10.20502/RBG.V23I1.1999
http://hdl.handle.net/11449/223377
Resumo: The Sao Francisco rivers is the largest river draining the cratonic areas of Cerrado savanas and semiarid Caatinga environments in NE Brazil. This study presents the first geomorphologic map of the Middle Sao Francisco River, and describe the main morphosedimentary units of the alluvial plain. The use of high-resolution satellite images, digital elevation models, cores data from previous studies, and morphosedimentary field descriptions were the procedures applied. The morphological composition indicates that the alluvial plain is a mosaic of morphosedimentary units. Eight geomorphological units were recognized. The unit classified as Impeded Floodplain is the richest in terms of diversity of geomorphological features, and was sub-classify in seven morphosedimentary subunits. At least three fluvial stages must be responsible for building the current mosaic of morphologies displayed on the floodplain. It is likely that a braided channel is the oldest type of system that operated in the region and left marks on the preserved floodplain. Subsequently, an important wetter stage induced a change in the behavior of the main river to a multichannel type, responsible for the main features observed current. Finally, the current, drier stage, with lower river flow, has controlled the development of the bank accretion floodplain and fluvial-aeolian floodplain during the Late Holocene. Therefore, these paleohidrological variations of the São Francisco River must play a key role in the construction of the complex and floodplain relic of the Middle São Francisco River.
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spelling Geomorphologic units of the Middle São Francisco River alluvial plain, Northeastern BrazilUnidades geomorfológicas da planície aluvial do Médio Rio São Francisco, Nordeste do BrasilAlluvial plainGeomorphologyMiddle São Francisco RiverThe Sao Francisco rivers is the largest river draining the cratonic areas of Cerrado savanas and semiarid Caatinga environments in NE Brazil. This study presents the first geomorphologic map of the Middle Sao Francisco River, and describe the main morphosedimentary units of the alluvial plain. The use of high-resolution satellite images, digital elevation models, cores data from previous studies, and morphosedimentary field descriptions were the procedures applied. The morphological composition indicates that the alluvial plain is a mosaic of morphosedimentary units. Eight geomorphological units were recognized. The unit classified as Impeded Floodplain is the richest in terms of diversity of geomorphological features, and was sub-classify in seven morphosedimentary subunits. At least three fluvial stages must be responsible for building the current mosaic of morphologies displayed on the floodplain. It is likely that a braided channel is the oldest type of system that operated in the region and left marks on the preserved floodplain. Subsequently, an important wetter stage induced a change in the behavior of the main river to a multichannel type, responsible for the main features observed current. Finally, the current, drier stage, with lower river flow, has controlled the development of the bank accretion floodplain and fluvial-aeolian floodplain during the Late Holocene. Therefore, these paleohidrological variations of the São Francisco River must play a key role in the construction of the complex and floodplain relic of the Middle São Francisco River.Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)Universidade de São PauloUNESP Instituto de Geociência e Ciências Exatas Programa de Pós-Graduação em Geociências e Meio Ambiente, SPUFG Programa de Pós-Graduação em Ciências Ambientais, GOUNESP Instituto de Geociência e Ciências Exatas Programa de Pós-Graduação em Geociências e Meio Ambiente, SPUniversidade Estadual Paulista (UNESP)Programa de Pós-Graduação em Ciências AmbientaisSantos, Landerlei Almeida [UNESP]Latrubesse, Edgardo Manuel2022-04-28T19:50:16Z2022-04-28T19:50:16Z2022-01-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/article1097-1115http://dx.doi.org/10.20502/RBG.V23I1.1999Revista Brasileira de Geomorfologia, v. 23, n. 1, p. 1097-1115, 2022.2236-56641519-1540http://hdl.handle.net/11449/22337710.20502/RBG.V23I1.19992-s2.0-85123838045Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPporRevista Brasileira de Geomorfologiainfo:eu-repo/semantics/openAccess2022-04-28T19:50:16Zoai:repositorio.unesp.br:11449/223377Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462022-04-28T19:50:16Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false
dc.title.none.fl_str_mv Geomorphologic units of the Middle São Francisco River alluvial plain, Northeastern Brazil
Unidades geomorfológicas da planície aluvial do Médio Rio São Francisco, Nordeste do Brasil
title Geomorphologic units of the Middle São Francisco River alluvial plain, Northeastern Brazil
spellingShingle Geomorphologic units of the Middle São Francisco River alluvial plain, Northeastern Brazil
Santos, Landerlei Almeida [UNESP]
Alluvial plain
Geomorphology
Middle São Francisco River
title_short Geomorphologic units of the Middle São Francisco River alluvial plain, Northeastern Brazil
title_full Geomorphologic units of the Middle São Francisco River alluvial plain, Northeastern Brazil
title_fullStr Geomorphologic units of the Middle São Francisco River alluvial plain, Northeastern Brazil
title_full_unstemmed Geomorphologic units of the Middle São Francisco River alluvial plain, Northeastern Brazil
title_sort Geomorphologic units of the Middle São Francisco River alluvial plain, Northeastern Brazil
author Santos, Landerlei Almeida [UNESP]
author_facet Santos, Landerlei Almeida [UNESP]
Latrubesse, Edgardo Manuel
author_role author
author2 Latrubesse, Edgardo Manuel
author2_role author
dc.contributor.none.fl_str_mv Universidade Estadual Paulista (UNESP)
Programa de Pós-Graduação em Ciências Ambientais
dc.contributor.author.fl_str_mv Santos, Landerlei Almeida [UNESP]
Latrubesse, Edgardo Manuel
dc.subject.por.fl_str_mv Alluvial plain
Geomorphology
Middle São Francisco River
topic Alluvial plain
Geomorphology
Middle São Francisco River
description The Sao Francisco rivers is the largest river draining the cratonic areas of Cerrado savanas and semiarid Caatinga environments in NE Brazil. This study presents the first geomorphologic map of the Middle Sao Francisco River, and describe the main morphosedimentary units of the alluvial plain. The use of high-resolution satellite images, digital elevation models, cores data from previous studies, and morphosedimentary field descriptions were the procedures applied. The morphological composition indicates that the alluvial plain is a mosaic of morphosedimentary units. Eight geomorphological units were recognized. The unit classified as Impeded Floodplain is the richest in terms of diversity of geomorphological features, and was sub-classify in seven morphosedimentary subunits. At least three fluvial stages must be responsible for building the current mosaic of morphologies displayed on the floodplain. It is likely that a braided channel is the oldest type of system that operated in the region and left marks on the preserved floodplain. Subsequently, an important wetter stage induced a change in the behavior of the main river to a multichannel type, responsible for the main features observed current. Finally, the current, drier stage, with lower river flow, has controlled the development of the bank accretion floodplain and fluvial-aeolian floodplain during the Late Holocene. Therefore, these paleohidrological variations of the São Francisco River must play a key role in the construction of the complex and floodplain relic of the Middle São Francisco River.
publishDate 2022
dc.date.none.fl_str_mv 2022-04-28T19:50:16Z
2022-04-28T19:50:16Z
2022-01-01
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://dx.doi.org/10.20502/RBG.V23I1.1999
Revista Brasileira de Geomorfologia, v. 23, n. 1, p. 1097-1115, 2022.
2236-5664
1519-1540
http://hdl.handle.net/11449/223377
10.20502/RBG.V23I1.1999
2-s2.0-85123838045
url http://dx.doi.org/10.20502/RBG.V23I1.1999
http://hdl.handle.net/11449/223377
identifier_str_mv Revista Brasileira de Geomorfologia, v. 23, n. 1, p. 1097-1115, 2022.
2236-5664
1519-1540
10.20502/RBG.V23I1.1999
2-s2.0-85123838045
dc.language.iso.fl_str_mv por
language por
dc.relation.none.fl_str_mv Revista Brasileira de Geomorfologia
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv 1097-1115
dc.source.none.fl_str_mv Scopus
reponame:Repositório Institucional da UNESP
instname:Universidade Estadual Paulista (UNESP)
instacron:UNESP
instname_str Universidade Estadual Paulista (UNESP)
instacron_str UNESP
institution UNESP
reponame_str Repositório Institucional da UNESP
collection Repositório Institucional da UNESP
repository.name.fl_str_mv Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)
repository.mail.fl_str_mv
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