Detalhes bibliográficos
| Ano de defesa: |
2010 |
| Autor(a) principal: |
Castrillon, Solange Kimie Ikeda |
| Orientador(a): |
Silva, Carolina Joana da
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| Banca de defesa: |
Não Informado pela instituição |
| Tipo de documento: |
Tese
|
| Tipo de acesso: |
Acesso aberto |
| Idioma: |
por |
| Instituição de defesa: |
Universidade Federal de São Carlos
|
| Programa de Pós-Graduação: |
Programa de Pós-Graduação em Ecologia e Recursos Naturais - PPGERN
|
| Departamento: |
Não Informado pela instituição
|
| País: |
BR
|
| Palavras-chave em Português: |
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| Palavras-chave em Inglês: |
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| Área do conhecimento CNPq: |
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| Link de acesso: |
https://repositorio.ufscar.br/handle/ufscar/1686
|
Resumo: |
Several studies have evaluated the mechanisms that determine the different landscapes in the Pantanal, there are multiple factors that are working together on the islands of the Pantanal contributing to the maintenance of its current state. Surveys have been conducted on six islands in the river between Paraguay and Cáceres Taiamã Ecological Station, Pantanal, comparing the diversity of islands from two geomorphological processes: from the rupture of the neck of meander and sedimentation. This study aimed to determine the effects of soil characteristics and flood levels in tree diversity. The samples consisted of 22 plots per island of 10m by 20m down the center and edge, and depositional and eroded sides of the islands. The topographical differences between the plots were measured from the River. We recorded 40 species belonging to 34 genera and 21 families. The indices of Shannon- Weaver diversity ranged from H 'from 1.08 to 2.77. The floristic communities were distinct between the islands of different origins, which are subjected to different periods of flooding. The islands formed by breaking the neck of meander abundace and have higher species richness. The soils of the islands, had an average of clayey to very clayey. The group formed by the most frequent and abundant species in the islands were positively correlated with soil properties that were high on the islands, such as magnesium and saturation of magnesium, and aluminum, clay and silte.O center of the islands is subject to a period of more flooding . There were differences in height between local depositional and erosion occurred in five islands, and the erosional side is higher than the deposition |
