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Registro Completo |
Biblioteca(s): |
Embrapa Café. |
Data corrente: |
08/12/2011 |
Data da última atualização: |
08/12/2011 |
Tipo da produção científica: |
Resumo em Anais de Congresso |
Autoria: |
SOARES, F. Q.; REIS, R. B. dos; EIRA, M. T. S. da; FAZUOLI, L. C. |
Afiliação: |
FABIO QUEZADO SOARES, CENARGEN; RAIMUNDA BARREIRAS DOS REIS, CENARGEN; MIRIAN THEREZINHA SOUZA DA EIRA, SAPC; LUIZ CARLOS FAZUOLI, IAC. |
Título: |
Viabilidade de sementes de Coffea arabica e Coffea canephora. |
Ano de publicação: |
2003 |
Fonte/Imprenta: |
In: SIMPÓSIO DE PESQUISA DOS CAFÉS DO BRASIL, 3., 2003, Porto Seguro. Resumos... Brasília, DF: Embrapa Café, 2003. |
Idioma: |
Português |
Palavras-Chave: |
Café arabica; Café canephora; Viabilidade. |
Thesagro: |
Conservação; Germoplasma; Longevidade. |
Categoria do assunto: |
-- |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/49776/1/Viabilidade-de-sementes.pdf
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Marc: |
LEADER 00660nam a2200205 a 4500 001 1909107 005 2011-12-08 008 2003 bl uuuu u00u1 u #d 100 1 $aSOARES, F. Q. 245 $aViabilidade de sementes de Coffea arabica e Coffea canephora.$h[electronic resource] 260 $aIn: SIMPÓSIO DE PESQUISA DOS CAFÉS DO BRASIL, 3., 2003, Porto Seguro. Resumos... Brasília, DF: Embrapa Café$c2003 650 $aConservação 650 $aGermoplasma 650 $aLongevidade 653 $aCafé arabica 653 $aCafé canephora 653 $aViabilidade 700 1 $aREIS, R. B. dos 700 1 $aEIRA, M. T. S. da 700 1 $aFAZUOLI, L. C.
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Embrapa Café (CNPCa) |
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Registro Completo
Biblioteca(s): |
Embrapa Solos. |
Data corrente: |
15/08/2014 |
Data da última atualização: |
10/11/2021 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Circulação/Nível: |
A - 1 |
Autoria: |
OLIVEIRA, F. S. de; SCHAEFER, C. E. G. R.; ABRAHÃO, W. A. P.; ALMEIDA, E. de P. C.; SIMAS, F. N. B. |
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. |
Título: |
Soil-geomorphology interactions and paleoclimatic implications of an ornithogenic soil toposequence on Rata Island, Fernando de Noronha Archipelago, South Atlantic. |
Ano de publicação: |
2014 |
Fonte/Imprenta: |
Journal of South American Earth Sciences, v. 52, p. 119-128, Jul. 2014. |
DOI: |
https://doi.org/10.1016/j.jsames.2014.02.007 |
Idioma: |
Inglês |
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 |
Palavras-Chave: |
Paleogeograph; Phosphatization; Volcanic islands. |
Thesaurus NAL: |
ornithogenic soils. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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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