987 resultados para WET TROPICAL FORESTS
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Este trabalho teve como objetivo estudar a composição e estrutura de um estrato arbóreo da floresta tropical úmida em Alta Floresta - MT, determinando os padrões de semelhança com outras regiões da Amazônia brasileira. O estudo foi realizado em uma área de 2 hectares, dividida em 20 parcelas de 10x 100m, onde foram mensurados a altura e o DAP ≥ 10 cm de todos os indivíduos. Para avaliação do grau de similaridade entre a composição florística e estrutura arbórea de Alta Floresta com as nove regiões pertencentes à Amazônia Legal brasileira, utilizou-se o método de agrupamento hierárquico aglomerativo com ligações pela média dos grupos (UPGMA), por meio do índice de Sorensen (qualitativo). Para a ordenação, foi utilizado o mesmo programa, utilizando a Escalonamento Multidimensional não-métrica (NMS) por meio do índice de Jaccard aplicado à presença e ausência de famílias e gêneros. Para análise de similaridade entre as 10 regiões, comparando a matriz de distâncias físicas entre elas com as matrizes de composição de famílias e gêneros, utilizou-se o programa PATN por meio do Teste de Mantel com o índice de Jaccard. A região apresentou 1101 indivíduos, pertencentes a 32 famílias, 54 gêneros e 68 espécies. A família com maior riqueza de espécie foi Leguminosae. A espécie Helicostilys podogyne e o gênero Cecropia sp. foram as mais importantes no levantamento. A floresta tropical úmida de Alta Floresta não se assemelhou com nenhuma das nove regiões comparadas neste estudo.
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Foi avaliado o crescimento diamétrico de uma população de Sterculia pruriens (Aublet) Schumann (axixá) após exploração florestal seletiva, na Estação Experimental da Embrapa Amazônia Oriental, Moju, Pará, localizada entre as coordenadas geográficas 02º 07' 30" e 2º 12' 06" de Latitude Sul e 48º 46' 57" e 48º 48' 30" de Longitude Oeste. Em cada uma das nove clareiras selecionadas foram instaladas faixas de 10m x 50m, começando na bordadura da clareira para o interior da floresta, nas direções Norte, Sul, Este e Oeste. Cada faixa foi dividida em parcelas quadradas de 10m de lado, que foram numeradas de 1 a 5 da borda para o interior da floresta e constituem o nível II de abordagem. Foi analisado a distribuição diamétrica da espécie com amplitude de DAP e" 5cm em intervalos de 5cm de diâmetro, até o valor máximo de 66,8cm encontrado no início do monitoramento. Na área de estudo foi encontrado densidade elevada da espécie, logo após a exploração florestal e após três anos desta. Ao final do estudo, foi observado um acréscimo de 9,8% na densidade dos indivíduos acima de 5cm de diâmetro. O crescimento diamétrico da espécie em três anos de observação foi de 0,37cm. Embora baixo ele é crescente, justificado pela abertura do dossel. A análise da distribuição diamétrica mostra que a abertura do dossel foi benéfica para o incremento diamétrico da espécie, aumentando o número de indivíduos em cinco das oito classes de diâmetro analisadas, mantendo-se ainda como uma distribuição decrescente.
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Foram avaliadas as respostas hematológicas de 20 búfalas, criadas ao sol (grupo - SS) e à sombra (grupo - CS), em Belém, Pará. Os animais do grupo CS (n = 10) estavam em sistema silvipastoril, com Racosperma mangium e os do SS (n = 10), em piquetes sem sombra, em pastagem de Brachiaria humidicola, água para beber e sal mineral. Foram mensuradas temperatura do ar (TA), umidade relativa do ar (UR) e temperatura de globo negro, em cada tratamento. A coleta de sangue para eritrograma e número total de leucócitos foi realizada a cada 14 dias, às 13 h, durante o ano de 2009. Através da análise de variância constatou-se que em todos os períodos do ano, a TA e índice de temperatura de globo e umidade (ITGU) foram diferentes (P < 0,05), com níveis mais elevados no grupo SS. No período mais chuvoso, o grupo CS apresentou valores elevados de leucócitos, enquanto nos períodos de transição e menos chuvoso, foram maiores no grupo SS. No período menos chuvoso do ano, o grupo SS apresentou maiores valores de hemácias. O teor de hemoglobina teve maiores níveis (P < 0,05) nos períodos de transição e menos chuvoso. Somente a hemoglobina teve correlação significativa e negativa (P < 0,05) com a UR. Conclui-se que as novilhas búfalas Murrah estão sujeitas a um ambiente hostil e o período menos chuvoso é o mais propício a causar estresse térmico.
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The high tree diversity and vast extent of Amazonian forests challenge our understanding of how tree species abundance and composition varies across this region. Information about these parameters, usually obtained from tree inventories plots, is essential for revealing patterns of tree diversity. Numerous tree inventories plots have been established in Amazonia, yet, tree species composition and diversity of white-sand and terra-firme forests of the upper Rio Negro still remain poorly understood. Here, we present data from eight new one-hectare tree inventories plots established in the upper Rio Negro; four of which were located in white-sand forests and four in terra-firme forests. Overall, we registered 4703 trees > 10 cm of diameter at breast height. These trees belong to 49 families, 215 genera, and 603 species. We found that tree communities of terra-firme and white-sand forests in the upper Rio Negro significantly differ from each other in their species composition. Tree communities of white-sand forests show a higher floristic similarity and lower diversity than those of terra-firme forests. We argue that mechanisms driving differences between tree communities of white-sand and terra-firme forests are related to habitat size, which ultimately influences large-scale and long-term evolutionary processes.
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The objective of this work was to assess the fine-root (≤ 2 mm diameter) production dynamics of two forest regrowths at different ages. Fine-root production was monitored by the ingrowth core method in one 18-year-old site (2 ha) and one 10-year-old site (0.5 ha), both localized in the Apeú region, Northern Pará State, Brazil. The sites were abandoned after successive shifting cultivation, beginning in 1940. Monthly production of live fine-root was similar between sites and was influenced by rainfall seasonality, with higher production during the dry season than the wet season for mass and length. However, mortality in terms of mass was higher in the 10-year-old site than in the 18-year-old site. The seasonality influenced mortality only in the 18-year old site following the pattern observed for live fine-root. The influence seasonal on mortality in terms of length was different between sites, with higher mortality during the wet season in the 10-year-old site and higher mortality during the dry season in the 18-year-old site. Specific root length was higher during the wet season and at the 10-year-old site. Fine-root production was not influenced by the chronosequence of the sites studied, probably fine-root production may have already stabilized in the sites or it depended more on climate and soil conditions. The production of fine-roots mass and length were indicators that generally showed the same pattern.
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White sand forests, although low in nutrients, are characterized not only by several endemic species of plants but also by several monodominant species. In general, plants in this forest have noticeably thin stems. The aim of this work was to elaborate a parallel dichotomous key for the identification of Angiosperm tree species occurring on white sand forests at the Allpahuayo Mishana National Reserve, Loreto, Peru. We compiled a list of species from several publications in order to have the most comprehensive list of species that occur on white sand forest. We found 219 species of Angiosperm, the more abundant species were Pachira brevipes (26.27%), Caraipa utilis (17.90%), Dicymbe uaiparuensis (13.27%), Dendropanax umbellatus (3.28%), Sloanea spathulata (2.52%), Ternstroemia klugiana (2.30%), Haploclathra cordata (2.28%), Parkia igneiflora (1.20%), Emmotum floribundum (1.06%), Ravenia biramosa (1.04%) among others. Most species of white sand forests can be distinguished using characteristics of stems, branches and leaves. This key is very useful for the development of floristic inventories and related projects on white sand forests from Allpahuayo Mishana National Reserve.
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Nutrient recycling in the forest is linked to the production and decomposition of litter, which are essential processes for forest maintenance, especially in regions of nutritionally poor soils. Human interventions in forest such as selecttive logging may have strong impacts on these processes. The objectives of this study were to estimate litterfall production and evaluate the influence of environmental factors (basal area of vegetation, plant density, canopy cover, and soil physicochemical properties) and anthropogenic factors (post-management age and exploited basal area) on this production, in areas of intact and exploited forest in southern Amazonia, located in the northern parts of Mato Grosso state. This study was conducted at five locations and the average annual production of litterfall was 10.6 Mg ha-1 year-1, higher than the values for the Amazon rainforest. There were differences in litterfall productions between study locations. Effects of historical logging intensity on litterfall production were not significant. Effects of basal area of vegetation and tree density on litterfall production were observed, highlighting the importance of local vegetation characteristics in litterfall production. This study demonstrated areas of transition between the Amazonia-Cerrado tend to have a higher litterfall production than Cerrado and Amazonia regions, and this information is important for a better understanding of the dynamics of nutrient and carbon cycling in these transition regions.
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The Bananal Island is regarded the largest fluvial island in the world, bounded by Araguaia and Javaés rivers, being located in southwest of Tocantins. The objectives of this work were to provide information about the vegetational changes that occurred at the Bananal Island, in order to contribute to the understanding the dynamics of past and current savanna and areas of ecotones with forests. Thus, a sedimentary core collected from a small lake at the Bananal Island plain was submitted to pollen and radiocarbon dating analyses. The results showed that the last millennium was dominated by forest reflecting a wet climate. At the beginning of the record (920-770 yr cal BP) the wet climate and high rainfall produced flooding during long rainy seasons that maintained the Javaés River connected to the studied lake, and hence, this environment was marked by the presence of a homogenous forest rich in Moraceae/Urticaceae, due to flooded soils occurrence. During the following period (770-304 yr cal BP) the reduced rainfall and shortening of the rainy seasons isolated the lake from the Javaés River for long periods, which caused a diversification of the forest and gave rise to the appearance of the components of floodplain forest and marsh vegetation adapted to waterlogged soils. Since 304 years cal BP to the present day this environment remained dominated by this diverse forest and the lacustrine conditions were also similar to previous phase, with a slight increase of moisture in the last 84 years that caused the increase of Piranhea.
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Forest structure determines light availability for understorey plants. The structure of lowland Amazonian forests is known to vary over long edaphic gradients, but whether more subtle edaphic variation also affects forest structure has not beenresolved. In western Amazonia, the majority of non-flooded forests grow on soils derived either from relatively fertile sediments of the Pebas Formation or from poorer sediments of the Nauta Formation. The objective of this study was to compare structure and light availability in the understorey of forests growing on these two geological formations. We measured canopy openness and tree stem densities in three size classes in northeastern Peru in a total of 275 study points in old-growth terra firme forests representing the two geological formations. We also documented variation in floristic composition (ferns, lycophytes and the palm Iriartea deltoidea) and used Landsat TM satellite image information to model the forest structural and floristic features over a larger area. The floristic compositions of forests on the two formations were clearly different, and this could also be modelled with the satellite imagery. In contrast, the field observations of forest structure gave only a weak indication that forests on the Nauta Formation might be denser than those on the Pebas Formation. The modelling of forest structural features with satellite imagery did not support this result. Our results indicate that the structure of forest understorey varies much less than floristic composition does over the studied edaphic difference.
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In this paper, Isopropanol (IPA) availability during the anisotropic etching of silicon in Potassium Hydroxide (KOH) solutions was investigated. Squares of 8 to 40 m were patterned to (100) oriented silicon wafers through DWL (Direct Writing Laser) photolithography. The wet etching process was performed inside an open HDPE (High Density Polyethylene) flask with ultrasonic agitation. IPA volume and evaporation was studied in a dynamic etching process, and subsequent influence on the silicon etching was inspected. For the tested conditions, evaporation rates for water vapor and IPA were determined as approximately 0.0417 mL/min and 0.175 mL/min, respectively. Results demonstrate that IPA availability, and not concentration, plays an important role in the definition of the final structure. Transversal SEM (Scanning Electron Microscopy) analysis demonstrates a correlation between microloading effects (as a consequence of structure spacing) and the angle formed towards the (100) plane.
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v. 1 1868 - Ranuncul-Connar
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v. 2 1871 - Leguminosae-Ficoideae
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v. 3 1877 - Umbelliferae-Eben
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v. 4 (1-4) 1902-04 - Ola-Gentianeae