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 | Acesso ao texto completo restrito à biblioteca da Embrapa Solos. Para informações adicionais entre em contato com cnps.biblioteca@embrapa.br. |
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Registro Completo |
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
27/04/2023 |
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Data da última atualização: |
05/12/2023 |
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Tipo da produção científica: |
Capítulo em Livro Técnico-Científico |
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Autoria: |
VIDAL-TORRADO, P.; BUURMAN, P.; MARTINEZ, P.; LOPES-MAZZETTO, J. M.; SCHELLEKENS, J.; COELHO, M. R.; GOMES, F. H. |
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Afiliação: |
PABLO VIDAL-TORRADO, UNIVERSIDADE DE SÃO PAULO; PETER BUURMAN, WAGENINGEN UNIVERSITY; PEDRO MARTINEZ, OREGON STATE UNIVERSITY; JOSIANE MILLANI LOPES-MAZZETTO, LINCOLN UNIVERSITY; JUDITH SCHELLEKENS, KU LEUVEN; MAURICIO RIZZATO COELHO, CNPS; FELIPE HAENEL GOMES, UNIVERSIDADE FEDERAL DE LAVRAS. |
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Título: |
Soils of restingas. |
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Ano de publicação: |
2023 |
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Fonte/Imprenta: |
In: SCHAEFER, C. E. G. R. (ed.). The soils of Brazil. Cham: Springer, 2023. cap. 14, p. 393-410. (World soils book series). |
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DOI: |
https://doi.org/10.1007/978-3-031-19949-3_14 |
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Idioma: |
Inglês |
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Conteúdo: |
The Restinga is one of the ecosystems of the Atlantic Rainforest biome in Brazil. It is characterized by extremely nutrient-poor soils formed in sandy coastal sediments from the Quaternary age. The highly dynamic environment of sandy coasts causes landforms with different microrelief. This, in combination with the poor and harsh conditions strongly influence both vegetation composition and ecological succession. Consequently soil formation and vegetation has remarkable variation at short distances within the Restinga ecosystem. This variation strongly depends on (i) geomorphological evolution (deposition/ erosion and age), (ii) particle size of the sediment (sand or clay), (iii) drainage conditions, and (iv) organic matter inputs. Soils from the Restinga ecosystem include Espodossolos (Podzols), Neossolos Quartzarênicos (Arenosols), Organossolos (Histosols), and Gleissolos (Gleysols). However, poorly drained Espodossolos (Podzols) dominate this forested landscape due to the low and flat relief of the shoreline and large amounts of dissolved organic matter (DOM) produced upon decomposition of litter and roots in H, O, and A horizons. The morphology of Espodossolos in the Restinga ecosystem is complex, with a large short-distance variability in depths and shapes of the E- and B-horizons. In order to interpret soil-forming processes in the context of the landscape, transects of related profiles are studied in detail in the different geomorphic units. We connect soil morphology, micromorphology, organic matter chemistry, and microbiology with geomorphology at the ecosystem level. MenosThe Restinga is one of the ecosystems of the Atlantic Rainforest biome in Brazil. It is characterized by extremely nutrient-poor soils formed in sandy coastal sediments from the Quaternary age. The highly dynamic environment of sandy coasts causes landforms with different microrelief. This, in combination with the poor and harsh conditions strongly influence both vegetation composition and ecological succession. Consequently soil formation and vegetation has remarkable variation at short distances within the Restinga ecosystem. This variation strongly depends on (i) geomorphological evolution (deposition/ erosion and age), (ii) particle size of the sediment (sand or clay), (iii) drainage conditions, and (iv) organic matter inputs. Soils from the Restinga ecosystem include Espodossolos (Podzols), Neossolos Quartzarênicos (Arenosols), Organossolos (Histosols), and Gleissolos (Gleysols). However, poorly drained Espodossolos (Podzols) dominate this forested landscape due to the low and flat relief of the shoreline and large amounts of dissolved organic matter (DOM) produced upon decomposition of litter and roots in H, O, and A horizons. The morphology of Espodossolos in the Restinga ecosystem is complex, with a large short-distance variability in depths and shapes of the E- and B-horizons. In order to interpret soil-forming processes in the context of the landscape, transects of related profiles are studied in detail in the different geomorphic units. We connect soil morphology,... Mostrar Tudo |
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Palavras-Chave: |
Bh degradation; Brazilian coastal plain; Ichnofossil; Podzol micromorphology; Podzol morphology; Podzolization; Tropical podzol. |
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Thesagro: |
Podzólico; Restinga; Solo Tropical. |
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Thesaurus Nal: |
Podzols; Tropical soils. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02619naa a2200349 a 4500
001 2153407
005 2023-12-05
008 2023 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1007/978-3-031-19949-3_14$2DOI
100 1 $aVIDAL-TORRADO, P.
245 $aSoils of restingas.$h[electronic resource]
260 $c2023
520 $aThe Restinga is one of the ecosystems of the Atlantic Rainforest biome in Brazil. It is characterized by extremely nutrient-poor soils formed in sandy coastal sediments from the Quaternary age. The highly dynamic environment of sandy coasts causes landforms with different microrelief. This, in combination with the poor and harsh conditions strongly influence both vegetation composition and ecological succession. Consequently soil formation and vegetation has remarkable variation at short distances within the Restinga ecosystem. This variation strongly depends on (i) geomorphological evolution (deposition/ erosion and age), (ii) particle size of the sediment (sand or clay), (iii) drainage conditions, and (iv) organic matter inputs. Soils from the Restinga ecosystem include Espodossolos (Podzols), Neossolos Quartzarênicos (Arenosols), Organossolos (Histosols), and Gleissolos (Gleysols). However, poorly drained Espodossolos (Podzols) dominate this forested landscape due to the low and flat relief of the shoreline and large amounts of dissolved organic matter (DOM) produced upon decomposition of litter and roots in H, O, and A horizons. The morphology of Espodossolos in the Restinga ecosystem is complex, with a large short-distance variability in depths and shapes of the E- and B-horizons. In order to interpret soil-forming processes in the context of the landscape, transects of related profiles are studied in detail in the different geomorphic units. We connect soil morphology, micromorphology, organic matter chemistry, and microbiology with geomorphology at the ecosystem level.
650 $aPodzols
650 $aTropical soils
650 $aPodzólico
650 $aRestinga
650 $aSolo Tropical
653 $aBh degradation
653 $aBrazilian coastal plain
653 $aIchnofossil
653 $aPodzol micromorphology
653 $aPodzol morphology
653 $aPodzolization
653 $aTropical podzol
700 1 $aBUURMAN, P.
700 1 $aMARTINEZ, P.
700 1 $aLOPES-MAZZETTO, J. M.
700 1 $aSCHELLEKENS, J.
700 1 $aCOELHO, M. R.
700 1 $aGOMES, F. H.
773 $tIn: SCHAEFER, C. E. G. R. (ed.). The soils of Brazil. Cham: Springer, 2023. cap. 14, p. 393-410. (World soils book series).
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Registro original: |
Embrapa Solos (CNPS) |
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| Registros recuperados : 47 | |
| 4. |  | COELHO, M. R.; VIDAL-TORRADO, P.; MARTINS, V. M.; OTERO PÉREZ, X. L.; MACÍAS VÁZQUEZ, F. Avaliação de cloretos não tamponados como extratores de alumínio associado à matéria orgânica em Espodossolos do estado de São Paulo. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 33., 2011, Uberlândia. Solos nos biomas brasileiros: sustentabilidade e mudanças climáticas: anais. [Uberlândia]: SBCS: UFU, ICIAG, 2011. 1 CD-ROM.| Tipo: Artigo em Anais de Congresso |
| Biblioteca(s): Embrapa Solos. |
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| 8. | | CAMPOS, J. R. da R.; SILVA, A. C.; SILVA, E. de B.; VIDAL-TORRADO, P. Extração e quantificação de alumínio trocável em Organossolos. Pesquisa Agropecuária Brasileira, Brasília, DF, v. 49, n. 3, p. 207-214, mar. 2014. Título em inglês: Extraction and quantification of exchangeable aluminum in Fibric Histosol.| Biblioteca(s): Embrapa Unidades Centrais. |
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| 12. | | GONZÁLEZ-PÉREZ, M.; BUURMAN, P.; VIDAL-TORRADO, P.; MARTIN NETO, L. Pyrolysis-gas chromatography/mass spectrometry characterization of humic acids in spodosols under tropical rain forest in southeastern Brazil. In: MEETING OF THE INTERNATIONAL HUMIC SUBSTANCES SOCIETY, 15., 2010, Puerto de la Cruz, ES. Advances in natural organic matter and humic substances research 2008-2010: proceedings. [S. l.: s. n.], 2010. v. 2. p. 329-332. J. A. González-Pérez, F. J. González-Vila, G. Almendros, Eds.| Tipo: Artigo em Anais de Congresso |
| Biblioteca(s): Embrapa Instrumentação. |
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| 14. | | MACEDO, R. S.; TEIXEIRA, W. G.; CORRÊA, M. M.; MARTINS, G. C.; VIDAL-TORRADO, P. Micromorphological evidences of pedogenetic changes due to anthropic action in Amazonian Dark Earth in the Central Amazon, Brazil. In: INTERNATIONAL CONFERENCE ON SOIL MICROMORPHOLOGY, 15., 2016, México, DF. Abstracts... México, DF: Universidad Nacional Autónoma de México, 2016.| Tipo: Resumo em Anais de Congresso |
| Biblioteca(s): Embrapa Amazônia Ocidental. |
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| 15. | | MACEDO, R. S.; TEIXEIRA, W. G.; CORRÊA, M. M.; MARTINS, G. C.; VIDAL-TORRADO, P. Micromorphological evidences of pedogenetic changes due to anthropic action in Amazonian Dark Earth in the Central Amazon, Brazil. In: INTERNATIONAL CONFERENCE ON SOIL MICROMORPHOLOGY, 15., 2016, México, DF. Abstracts... México, DF: Universidad Nacional Autónoma de México, 2016.| Tipo: Resumo em Anais de Congresso |
| Biblioteca(s): Embrapa Solos. |
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| 17. | | MACEDO, R. S.; TEIXEIRA, W. G.; CORRÊA, M. M.; MARTINS, G. C.; VIDAL-TORRADO, P. Pedogenetic processes in anthrosols with pretic horizon (Amazonian Dark Earth) in Central Amazon, Brazil. Plos One, v. 12, n. 5, e0178038, May 2017.| Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
| Biblioteca(s): Embrapa Amazônia Ocidental; Embrapa Solos. |
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| 20. | | MACEDO, R. S.; MADELLA, M.; CALEGARI, M. R.; TEIXEIRA, W. G.; MARTINS, G. C.; VIDAL-TORRADO, P. Coleção de referência de fitólitos de plantas como subsídio para identificação e classificação de fitólitos em solos. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 35., 2015, Natal. O solo e suas múltiplas funções: anais. Natal: Sociedade Brasileira de Ciência do Solo, 2015.| Tipo: Artigo em Anais de Congresso |
| Biblioteca(s): Embrapa Amazônia Ocidental. |
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| Registros recuperados : 47 | |
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| Nenhum registro encontrado para a expressão de busca informada. |
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