| |
|
|
|
Registro Completo |
|
Biblioteca(s): |
Embrapa Pantanal. |
|
Data corrente: |
08/02/2000 |
|
Data da última atualização: |
11/04/2017 |
|
Autoria: |
SAN JOSE, J. J.; MEDINA, E. |
|
Título: |
Effect of fire on organic matter production and water balance in a tropical savanna. |
|
Ano de publicação: |
1975 |
|
Fonte/Imprenta: |
In: GOLLEY, F.B.; MEDINA, E., ed. Tropical ecological systems: trends in terrestrial and aquatic research. New York: Springer-Verlag, 1975. p.251-264. |
|
Série: |
(Ecological studies; analysis and synthesis, 11) |
|
Idioma: |
Inglês |
|
Conteúdo: |
Lowland savannas in northern South America (llanos) occupy a region with a pronounced rainfall seasonality with four to six months dry season and 600 to 1,500 mm rainfall. This seasonality is considered to be determinant in savanna phenology, although species with divergent rhythms have been reported (Monasterio, 1968) due to water availability during the dry season (Vareschi, 1960). Savanna vegetation growing under high rainfall regimes is a puzzling phytogeographic problem, and hypotheses on its origin have produced an extensive literature (see the chapter by Sarmiento and Monasterio). Savanna vegetation can be formed in response to several limiting factors, such as soil, geomorphology, and fire. The human factor also plays an important role (Walter, 1970; Blydenstein, 1962; Monasterio and Sarmiento, 1968; Bourliere and Hadley, 1970; Daubenmire, 1968). |
|
Palavras-Chave: |
Fire; Forest; Savanna. |
|
Thesagro: |
Floresta; Fogo; Matéria Orgânica; Queimada. |
|
Thesaurus Nal: |
burning; organic matter. |
|
Categoria do assunto: |
-- |
|
Marc: |
LEADER 01647naa a2200253 a 4500
001 1799783
005 2017-04-11
008 1975 bl --- 0-- u #d
100 1 $aSAN JOSE, J. J.
245 $aEffect of fire on organic matter production and water balance in a tropical savanna.
260 $c1975
490 $a(Ecological studies; analysis and synthesis, 11)
520 $aLowland savannas in northern South America (llanos) occupy a region with a pronounced rainfall seasonality with four to six months dry season and 600 to 1,500 mm rainfall. This seasonality is considered to be determinant in savanna phenology, although species with divergent rhythms have been reported (Monasterio, 1968) due to water availability during the dry season (Vareschi, 1960). Savanna vegetation growing under high rainfall regimes is a puzzling phytogeographic problem, and hypotheses on its origin have produced an extensive literature (see the chapter by Sarmiento and Monasterio). Savanna vegetation can be formed in response to several limiting factors, such as soil, geomorphology, and fire. The human factor also plays an important role (Walter, 1970; Blydenstein, 1962; Monasterio and Sarmiento, 1968; Bourliere and Hadley, 1970; Daubenmire, 1968).
650 $aburning
650 $aorganic matter
650 $aFloresta
650 $aFogo
650 $aMatéria Orgânica
650 $aQueimada
653 $aFire
653 $aForest
653 $aSavanna
700 1 $aMEDINA, E.
773 $tIn: GOLLEY, F.B.; MEDINA, E., ed. Tropical ecological systems: trends in terrestrial and aquatic research. New York: Springer-Verlag, 1975. p.251-264.
Download
Esconder MarcMostrar Marc Completo |
|
Registro original: |
Embrapa Pantanal (CPAP) |
|
|
Biblioteca |
ID |
Origem |
Tipo/Formato |
Classificação |
Cutter |
Registro |
Volume |
Status |
URL |
Voltar
|
|
|
| Registros recuperados : 3 | |
| Registros recuperados : 3 | |
|
| Nenhum registro encontrado para a expressão de busca informada. |
|
|
