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| Registros recuperados : 13 | |
| 3. |  | EINLOFT, R.; RUIZ, H. A.; GRIFFITH, J. J.; PEREIRA, P. R. G.; ABRAHAO, W. A. P. Crescimento de gramineas e leguminosas em substrato rico em manganes proveniente de area de emprestimo. Revista Arvore, Vicosa, v.23, n.2, 204-212, abr./jun. 1999.| Biblioteca(s): Embrapa Florestas. |
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| 6. | | FREITAS, G. A. de; SILVA, R. R. da; BARROS, H. B.; VAZ-DE-MELO, A.; ABRAHÃO, W. A. P. Produção de mudas de alface em função de diferentes combinações de substratos. Revista Ciência Agronômica, Fortaleza, v. 44, n. 1, p. 159-166, jan./mar. 2013.| Biblioteca(s): Embrapa Hortaliças. |
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| 7. | | STRINGHETA, A. C. O.; ABRAHAO, W. A. P.; CARDOSO, A. A.; COSTA, L. M. da; SANTANA FILHO, S. Recomposicao da paisagen em areas degradadas utilizando composto de lixo urbano e leguminosas da regiao de Vicosa, Minas Gerais. Revista Ceres, Vicosa, v.46, n.265, p.321-334, maio/jun. 1999.| Biblioteca(s): Embrapa Florestas. |
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| 8. | | BORGES JÚNIOR, M.; MELLO, J. W. V. de; SCHAEFER, C. E. G. R.; DUSSIN, T. M.; ABRAHÃO, W. A. P. Valores de referência local e avaliação da contaminação por zinco em solos adjacentes a área mineradas no município de Vazante-MG. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 32, número especial, p. 2883-2893, nov./dez., 2008. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 32, número especial, nov./dez., 2008.| Biblioteca(s): Embrapa Solos / UEP-Recife. |
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| 9. | | OLIVEIRA, F. S. de; SCHAEFER, C. E. G. R.; ABRAHÃO, W. A. P.; ALMEIDA, E. de P. C.; SIMAS, F. N. B. Soil-geomorphology interactions and paleoclimatic implications of an ornithogenic soil toposequence on Rata Island, Fernando de Noronha Archipelago, South Atlantic. Journal of South American Earth Sciences, v. 52, p. 119-128, Jul. 2014.| Biblioteca(s): Embrapa Solos. |
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| 10. | | SOUZA, J. J. L. L. de; ABRAHÃO, W. A. P.; MELLO, J. W. V. de; SILVA, J. da; COSTA, L. M. da; OLIVEIRA, T. S. de. Geochemistry and spatial variability of metal (loid) concentrations in soils of the state of Minas Gerais, Brazil. Science of the Total Environment, Amsterdam, v. 505, p. 338-349, Feb. 2015| Biblioteca(s): Embrapa Hortaliças. |
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| 11. | | SILVA, J. da; ROSADO, C. B.; MELLO, J. W. V. de; ABRAHÃO, W. A. P.; FERREIRA, V. de P.; SANTOS JUNIOR, L. dos. Variabilidade de elementos traço em alguns latossolos de Minas Gerais. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 33., 2011, Uberlândia. Solos nos biomas brasileiros: sustentabilidade e mudanças climáticas: anais. Uberlândia: Sociedade Brasileira de Ciência do Solo, 2011. 1 CD-ROM. Resumo expandido.| Biblioteca(s): Embrapa Hortaliças. |
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| 12. | | SOUZA, J. J. L. L. de; SCHAEFER, C. E. G. R.; ABRAHÃO, W. A. P.; MELLO, J. W. V. de; SIMAS, F. N. B.; SILVA, J. da; FRANCELINO, M. R. Hydrogeochemistry of sulfate-affected landscapes in keller peninsula, maritime antarctica. Geomorphology, Amsterdam, v. 165/156, p. 55-56, Jun. 2012.| Biblioteca(s): Embrapa Hortaliças. |
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| 13. | | DEMATTÊ, J. A. M.; DOTTO, A. C.; PAIVA, A. F. S.; SATO, M. V.; DALMOLIN, R. S. D.; ARAÚJO, M. do S. B. de; SILVA, E. B. da; NANNI, M. R.; CATEN, A. ten; NORONHA, N. C.; LACERDA, M. P. C.; ARAUJO FILHO, J. C. de; RIZZO, R.; BELLINASO, H.; FRANCELINO, M. R.; SCHAEFER, C. E. G. R.; VICENTE, L. E.; SANTOS, U. J. dos; SAMPAIO, E. V. de S. B.; MENEZES, R. S. C.; SOUZA, J. J. L. L. de; ABRAHÃO, W. A. P.; COELHO, R. M.; GREGO, C. R.; LANI, J. L.; FERNANDES, A. R.; GONÇALVES, D. A. M.; SILVA, S. H. G.; MENEZES, M. D. de; CURI, N.; COUTO, E. G.; ANJOS, L. H. C. dos; CEDDIA, M. B.; PINHEIRO, E. F. M.; GRUNWALD, S.; VASQUES, G. de M.; MARQUES JÚNIOR, J.; SILVA, A. J. da; BARRETO, M. C. de V.; NÓBREGA, G. N.; SILVA, M. Z. da; SOUZA, S. F. de; VALLADARES, G. S.; VIANA, J. H. M.; TERRA, F. da S.; HORÁK-TERRA, I.; FIORIO, P. R.; SILVA, R. C. da; FRADE JÚNIOR, E. F.; LIMA, R. H. C.; FILIPPINI ALBA, J. M.; SOUZA JUNIOR, V. S. de; BREFIN, M. de L. M. S.; RUIVO, M. de L. P.; FERREIRA, T. O.; BRAIT, M. A.; CAETANO, N. R.; BRINGHENTI, I.; MENDES, W. de S.; SAFANELLI, J. L.; GUIMARÃES, C. C. B.; POPPIEL, R. R.; SOUZA, A. B. e; QUESADA, C. A.; COUTO, H. T. Z. do. The Brazilian Soil Spectral Library (BSSL): a general view, application and challenges. Geoderma, v. 354, 113793, 2019. Na publicação: Gustavo M. Vasques.| Biblioteca(s): Embrapa Agricultura Digital; Embrapa Clima Temperado; Embrapa Cocais; Embrapa Meio Ambiente; Embrapa Milho e Sorgo; Embrapa Solos. |
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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. |
Registro Completo
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
15/08/2014 |
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Data da última atualização: |
10/11/2021 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 1 |
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Autoria: |
OLIVEIRA, F. S. de; SCHAEFER, C. E. G. R.; ABRAHÃO, W. A. P.; ALMEIDA, E. de P. C.; SIMAS, F. N. B. |
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Afiliação: |
Fábio Soares de Oliveira, Departamento de Geografia, Instituto de Geociências, Universidade Federal de Minas Gerais, UFMG.; Carlos Ernesto G.R. Schaefer, Departamento de Solos, Universidade Federal de Viçosa, UFV.; Walter Antônio Pereira Abrahão, Departamento de Solos, Universidade Federal de Viçosa, UFV.; ELIANE DE PAULA CLEMENTE ALMEIDA, CNPS; Felipe Nogueira Bello Simas, Departamento de Solos, Universidade Federal de Viçosa, UFV. |
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Título: |
Soil-geomorphology interactions and paleoclimatic implications of an ornithogenic soil toposequence on Rata Island, Fernando de Noronha Archipelago, South Atlantic. |
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Ano de publicação: |
2014 |
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Fonte/Imprenta: |
Journal of South American Earth Sciences, v. 52, p. 119-128, Jul. 2014. |
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DOI: |
https://doi.org/10.1016/j.jsames.2014.02.007 |
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Idioma: |
Inglês |
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Conteúdo: |
The formation of highly phosphatized soils on sites of avian activity is a common feature of oceanic islands. We characterized a toposequence of phosphatic soils on Rata Island, to evaluate the soil genesis based on local topographic variations. For this purpose, four soils ranging from the upper hill down to the lowest landscape position on the island, representing a range of parent materials (basalt and calcareous sands), were analyzed. In the lowest landscape position a shallow Regosol was identified, strongly influenced by birds and marine sprays, developed on 'karstified' Pleistocene calcarenites; the three other soils in the upper part of the toposequence are Ornithogenic Cambisols, ranging from a deep Cambisol profile on Basalt lava to intermediate Cambisols on mixed colluvial sediments of the basalt/ calcareous. The lowermost Regosol is associated with a rugged landscape with strong calcarenite dissolution and karstification. The soil phosphatization is clearly an inherited process of the Late Quaternary age, when climate conditions were different. Initial weathering took place in the last interglacial period, under wetter conditions during which the Tertiary basalts were strongly weathered, leaving corestones in a saprolitic, oxidized mass. In the late Pleistocene, a gentle surface distributed these weathering products along the pediment slopes as colluvial materials, whereas in the coastal areas aeolian processes formed large sand dunes composed of reworked calcareous sands from marine sources during a time of very low sea level. During this time, widespread bird activity accounted for secondary apatite formation on the surface of calcareous oolites. Finally, the Holocene warming was accompanied by increasing sea level, enhanced tropical weathering, Fe and Al mobility and variscite formation superimposed on degraded Ca-phosphates, forming two phase phosphatic aggregates. MenosThe formation of highly phosphatized soils on sites of avian activity is a common feature of oceanic islands. We characterized a toposequence of phosphatic soils on Rata Island, to evaluate the soil genesis based on local topographic variations. For this purpose, four soils ranging from the upper hill down to the lowest landscape position on the island, representing a range of parent materials (basalt and calcareous sands), were analyzed. In the lowest landscape position a shallow Regosol was identified, strongly influenced by birds and marine sprays, developed on 'karstified' Pleistocene calcarenites; the three other soils in the upper part of the toposequence are Ornithogenic Cambisols, ranging from a deep Cambisol profile on Basalt lava to intermediate Cambisols on mixed colluvial sediments of the basalt/ calcareous. The lowermost Regosol is associated with a rugged landscape with strong calcarenite dissolution and karstification. The soil phosphatization is clearly an inherited process of the Late Quaternary age, when climate conditions were different. Initial weathering took place in the last interglacial period, under wetter conditions during which the Tertiary basalts were strongly weathered, leaving corestones in a saprolitic, oxidized mass. In the late Pleistocene, a gentle surface distributed these weathering products along the pediment slopes as colluvial materials, whereas in the coastal areas aeolian processes formed large sand dunes composed of reworked calcare... Mostrar Tudo |
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Palavras-Chave: |
Paleogeograph; Phosphatization; Volcanic islands. |
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Thesaurus NAL: |
ornithogenic soils. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02738naa a2200229 a 4500
001 1992705
005 2021-11-10
008 2014 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1016/j.jsames.2014.02.007$2DOI
100 1 $aOLIVEIRA, F. S. de
245 $aSoil-geomorphology interactions and paleoclimatic implications of an ornithogenic soil toposequence on Rata Island, Fernando de Noronha Archipelago, South Atlantic.$h[electronic resource]
260 $c2014
520 $aThe formation of highly phosphatized soils on sites of avian activity is a common feature of oceanic islands. We characterized a toposequence of phosphatic soils on Rata Island, to evaluate the soil genesis based on local topographic variations. For this purpose, four soils ranging from the upper hill down to the lowest landscape position on the island, representing a range of parent materials (basalt and calcareous sands), were analyzed. In the lowest landscape position a shallow Regosol was identified, strongly influenced by birds and marine sprays, developed on 'karstified' Pleistocene calcarenites; the three other soils in the upper part of the toposequence are Ornithogenic Cambisols, ranging from a deep Cambisol profile on Basalt lava to intermediate Cambisols on mixed colluvial sediments of the basalt/ calcareous. The lowermost Regosol is associated with a rugged landscape with strong calcarenite dissolution and karstification. The soil phosphatization is clearly an inherited process of the Late Quaternary age, when climate conditions were different. Initial weathering took place in the last interglacial period, under wetter conditions during which the Tertiary basalts were strongly weathered, leaving corestones in a saprolitic, oxidized mass. In the late Pleistocene, a gentle surface distributed these weathering products along the pediment slopes as colluvial materials, whereas in the coastal areas aeolian processes formed large sand dunes composed of reworked calcareous sands from marine sources during a time of very low sea level. During this time, widespread bird activity accounted for secondary apatite formation on the surface of calcareous oolites. Finally, the Holocene warming was accompanied by increasing sea level, enhanced tropical weathering, Fe and Al mobility and variscite formation superimposed on degraded Ca-phosphates, forming two phase phosphatic aggregates.
650 $aornithogenic soils
653 $aPaleogeograph
653 $aPhosphatization
653 $aVolcanic islands
700 1 $aSCHAEFER, C. E. G. R.
700 1 $aABRAHÃO, W. A. P.
700 1 $aALMEIDA, E. de P. C.
700 1 $aSIMAS, F. N. B.
773 $tJournal of South American Earth Sciences$gv. 52, p. 119-128, Jul. 2014.
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