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Registro Completo |
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Biblioteca(s): |
Embrapa Agrossilvipastoril; Embrapa Trigo. |
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Data corrente: |
27/11/2024 |
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Data da última atualização: |
27/11/2024 |
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Tipo da produção científica: |
Capítulo em Livro Técnico-Científico |
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Autoria: |
COUTO, E. G.; CORRÊA, G. R.; OLIVEIRA, V. A.; NASCIMENTO, A. F. do; VIDAL-TORRADO, P.; BEIRIGO, R.; SCHAEFER, C. E. G. R. |
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Afiliação: |
EDUARDO G. COUTO, UNIVERSIDADE FEDERAL DO MATO GROSSO; GUILHERME RESENDE CORRÊA, UNIVERSIDADE FEDERAL DE UBERLÂNDIA; VIRLEI A. OLIVEIRA, FUNDAÇÃO INSTITUTO BRASILEIRO DE GEOGRAFIA E ESTATÍSTICA; ALEXANDRE FERREIRA DO NASCIMENTO, CNPT; PABLO VIDAL-TORRADO, UNIVERSITY OF SÃO PAULO; RAPHAEL BEIRIGO, UNIVERSIDADE FEDERAL DA PARAÍBA; CARLOS E. G. R. SCHAEFER, UNIVERSIDADE FEDERAL DE VIÇOSA. |
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Título: |
Soils of Pantanal: the largest continental wetland. |
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Ano de publicação: |
2024 |
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Fonte/Imprenta: |
In: SCHAEFER, C. E. G. R. (ed.). The soils of Brazil. Cham: Springer, 2023. |
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Páginas: |
p. 239-267. |
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Série: |
(World soils book series). |
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Idioma: |
Inglês |
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Conteúdo: |
The Pantanal is a large tectonic depression located between the Andean slopes and the Brazilian Central Plateau, and the largest continental wetland worldwide, with great biodiversity and pedodiversity, driven by alternating cycles of flood and drought. In this rich Brazilian biome, subtle changes in relief and hydrological condition change soil properties, and affect the distribution of the highly diverse flora and fauna. The wetland soils of Pantanal are closely related to the nature of sediments, and vary according to changes in erosion and deposition/sedimentation rates. Depending on the amount of sand, primary minerals and watertable level, many different types of soils are formed. Quaternary Climatic changes associated with various glacial/interglacial periods occurred in the region, allowing changing pedoclimates with contrasting soil formation processes. The pedoenvironments and soils present in the Pantanal subregions strongly vary according to small topographical variations. Altimetric differences, even a few centimeters, have great influence in soil formation, determining the flood and drought periods at different parts of the landscape. Some soil characteristics also influence the internal flow of water, both vertical and lateral. These differences result in varying intensities of hydromorphism, present in all soils of Pantanal. Even at the highest landscape, soils show signs of hydromorphism, identified by the presence of grayish colors, and Fe3+ reduction process. Paludization, gleying, laterization (plinthite formation), solodization, salinization, argilluviation and podzolization are common pedogenic processes in Pantanal, and are strongly driven by the flooding regime. The main soils in Pantanal are (in decreasing order of total area): Planossolos Nátricos (23%) > Plintossolos (21%) > Espodossolos Ferrilúvicos (19%) > Planossolos Háplicos (11,8%) > Gleissolos (11,7%) > Vertissolos (5,8%) > Argissolos Vermelho-Amarelos (4,8%) > Other minor soils (Neossolos Litólicos, Neossolos Quartzarênicos, Chernossolos Argilúvicos, Neossolos Flúvicos, all with less than 5% in total). The Pantanal wetlands, one of the richest biomes in the neotropics, are under severe threat of vegetation loss and widespread burning due to the intensification of land use, with replacement of the traditional cattle ranching, and climate changes. MenosThe Pantanal is a large tectonic depression located between the Andean slopes and the Brazilian Central Plateau, and the largest continental wetland worldwide, with great biodiversity and pedodiversity, driven by alternating cycles of flood and drought. In this rich Brazilian biome, subtle changes in relief and hydrological condition change soil properties, and affect the distribution of the highly diverse flora and fauna. The wetland soils of Pantanal are closely related to the nature of sediments, and vary according to changes in erosion and deposition/sedimentation rates. Depending on the amount of sand, primary minerals and watertable level, many different types of soils are formed. Quaternary Climatic changes associated with various glacial/interglacial periods occurred in the region, allowing changing pedoclimates with contrasting soil formation processes. The pedoenvironments and soils present in the Pantanal subregions strongly vary according to small topographical variations. Altimetric differences, even a few centimeters, have great influence in soil formation, determining the flood and drought periods at different parts of the landscape. Some soil characteristics also influence the internal flow of water, both vertical and lateral. These differences result in varying intensities of hydromorphism, present in all soils of Pantanal. Even at the highest landscape, soils show signs of hydromorphism, identified by the presence of grayish colors, and Fe3+ reduction proce... Mostrar Tudo |
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Thesagro: |
Solo. |
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Thesaurus Nal: |
Pantanal. |
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Categoria do assunto: |
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P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 03080naa a2200241 a 4500
001 2169686
005 2024-11-27
008 2024 bl uuuu u00u1 u #d
100 1 $aCOUTO, E. G.
245 $aSoils of Pantanal$bthe largest continental wetland.$h[electronic resource]
260 $c2024
300 $ap. 239-267.
490 $a(World soils book series).
520 $aThe Pantanal is a large tectonic depression located between the Andean slopes and the Brazilian Central Plateau, and the largest continental wetland worldwide, with great biodiversity and pedodiversity, driven by alternating cycles of flood and drought. In this rich Brazilian biome, subtle changes in relief and hydrological condition change soil properties, and affect the distribution of the highly diverse flora and fauna. The wetland soils of Pantanal are closely related to the nature of sediments, and vary according to changes in erosion and deposition/sedimentation rates. Depending on the amount of sand, primary minerals and watertable level, many different types of soils are formed. Quaternary Climatic changes associated with various glacial/interglacial periods occurred in the region, allowing changing pedoclimates with contrasting soil formation processes. The pedoenvironments and soils present in the Pantanal subregions strongly vary according to small topographical variations. Altimetric differences, even a few centimeters, have great influence in soil formation, determining the flood and drought periods at different parts of the landscape. Some soil characteristics also influence the internal flow of water, both vertical and lateral. These differences result in varying intensities of hydromorphism, present in all soils of Pantanal. Even at the highest landscape, soils show signs of hydromorphism, identified by the presence of grayish colors, and Fe3+ reduction process. Paludization, gleying, laterization (plinthite formation), solodization, salinization, argilluviation and podzolization are common pedogenic processes in Pantanal, and are strongly driven by the flooding regime. The main soils in Pantanal are (in decreasing order of total area): Planossolos Nátricos (23%) > Plintossolos (21%) > Espodossolos Ferrilúvicos (19%) > Planossolos Háplicos (11,8%) > Gleissolos (11,7%) > Vertissolos (5,8%) > Argissolos Vermelho-Amarelos (4,8%) > Other minor soils (Neossolos Litólicos, Neossolos Quartzarênicos, Chernossolos Argilúvicos, Neossolos Flúvicos, all with less than 5% in total). The Pantanal wetlands, one of the richest biomes in the neotropics, are under severe threat of vegetation loss and widespread burning due to the intensification of land use, with replacement of the traditional cattle ranching, and climate changes.
650 $aPantanal
650 $aSolo
700 1 $aCORRÊA, G. R.
700 1 $aOLIVEIRA, V. A.
700 1 $aNASCIMENTO, A. F. do
700 1 $aVIDAL-TORRADO, P.
700 1 $aBEIRIGO, R.
700 1 $aSCHAEFER, C. E. G. R.
773 $tIn: SCHAEFER, C. E. G. R. (ed.). The soils of Brazil. Cham: Springer, 2023.
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Registro original: |
Embrapa Trigo (CNPT) |
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| Registros recuperados : 3 | |
| 1. |  | REBEQUI, A. M.; FERREIRA, A. C. de B.; BOGIANI, J. C.; SOFIATTI, V.; ALVES, U. P. C.; ALVES, G. L. Produtividade do algodoeiro em diferentes sistemas de cultivo e manejo do solo. In: CONGRESSO BRASILEIRO DO ALGODÃO, 12., 2019, Goiânia, GO. Anais... Goiânia: Abrapa, 2019. 1 p. 1 p.| Tipo: Resumo em Anais de Congresso |
| Biblioteca(s): Embrapa Territorial. |
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| 2. | | REBEQUI, A. M.; FERREIRA, A. C. de B.; BOGIANI, J. C.; SOFIATTI, V.; ALVES, U. P. C.; ALVES, G. L. Produtividade do algodoeiro em diferentes sistemas de cultivo e manejo do solo. In: CONGRESSO BRASILEIRO DO ALGODÃO, 12., 2019, Goiânia, GO. Anais... Goiânia: Abrapa, 2019. 1 p. 1 p.| Tipo: Resumo em Anais de Congresso |
| Biblioteca(s): Embrapa Algodão. |
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| 3. | | REBEQUI, A. M.; FERREIRA, A. C. de B.; BOGIANI, J. C.; ALVES, U. P. C.; ALVES, G. L.; VICENTE, N. G. Perda de água em solo com diferentes sistemas de cultivo e manejo do algodoeiro. In: CONGRESSO BRASILEIRO DO ALGODÃO, 12., 2019, Goiânia, GO. Anais... Goiânia: Abrapa, 2019. 1 p. 1 p.| Tipo: Resumo em Anais de Congresso |
| Biblioteca(s): Embrapa Territorial. |
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| Registros recuperados : 3 | |
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