Balance of the nutrients Ca+2, Mg+2, Na+, K+ e NO3 on a first order catchment covered with Natural vegetation in Central Amazonia

The study was conducted on a first-order catchment of about 3.5 km2 located on an experimental site 16 km west of the Manaus - Boa Vista highway, and 60 km north of Manaus. The main purpose was to quantify the balance of the nutrients Ca+2, Mg+2 Na+, K and NO3 through the comparison of the values of rainfall input versus streamflow output. Water sampling and nutrient flux determinations were carried out on a monthly basis for a one year period. Ionic concentrations showed low variation along the period. The highest concentrations in the rainfall were related to the accumulation of aerosols in the atmosphere, after a long rainless period. The vegetation exerted, apparently, more influence on nitrate, over the other nutrients. The nutrient flux varied, where their total input was attributed to individual storms of great magnitude. The balance, expressed in kg.ha-1,year1, was positive for all nutrients, with the following net gain values: Ca+2 (2,33); Mg+2 (1,66); Na+ (2,07); K+ (1,80) and NO3 (5,84).O estudo foi conduzido em uma bacia hidrográfica experimental de primeira ordem de aproximadamente 3,5 km2 localizada próximo ao km 16 da estrada secundária ZF-02, do km 60 da rodovia BR-174 que liga Manaus - Boa Vista. O principal objetivo foi quantificar o balanço dos nutrientes Ca+2, Mg+2 Na+, K+e NO3 através da entrada via precipitação e saída via deflúvio. As coletas de água e os cálculos do fluxo de nutrientes foram feitos em base mensal por um período de um ano. Observou-se que as concentrações iônicas apresentaram pouca variação ao longo do tempo. As maiores concentrações na precipitação ocorreram em função do acúmulo de aerosóis na atmosfera, após um período longo sem chuva. Aparentemente a vegetação exerceu influência mais evidente sobre o nitrato em relação aos demais nutrientes. O fluxo dos nutrientes foi variável, onde principalmente a entrada total destes deu-se em função de eventos individuais de chuva de grande magnitude. O balanço em kg.ha-1.ano-1 foi positivo para todos os nutrientes com os seguintes ganhos líquidosCa+2 (2,33); Mg+2 (1,66); Na+ (2,07); K+ (l,80) e NO3 (5,84)

Spatio-temporal dynamics of soil bacterial communities as a function of Amazon forest phenology

Abstract Most tropical evergreen rain forests are characterised by varying degrees of precipitation seasonality that influence plant phenology and litterfall dynamics. Soil microbes are sensitive to soil water:air ratio and to nutrient availability. We studied if within-year seasonality in precipitation and litterfall-derived nutrient input resulted in predictable seasonal variation in soil bacterial diversity/microbial functional groups in an Amazonian forest. We characterised the spatio-temporal dynamics of microbial communities from the plot to the stand scales and related them to precipitation seasonality and spatial variability in soil characteristics. Community composition and functional diversity showed high spatial heterogeneity and was related to variability in soil chemistry at the stand level. Large species turnover characterised plot level changes over time, reflecting precipitation seasonality-related changes in soil nutrient and moisture regimes. The abundance of decomposers was highest during the rainy season, characterised also by anaerobic saprophytes and N2-fixers adapted to fluctuating redox conditions. In contrast, Beijerinckiaceae, likely derived from the phyllosphere, were found at higher abundances when litter inputs and accumulation were highest. We showed that in a mildly seasonal rain forest, the composition of soil microbial communities appears to be following canopy phenology patterns and the two are interlinked and drive soil nutrient availability

Seasonality modulates the direct and indirect influences of forest cover on larval anopheline assemblages in western Amazônia

Serious concerns have arisen regarding urbanization processes in western Amazônia, which result in the creation of artificial habitats, promoting the colonization of malaria vectors. We used structural equation modelling to investigate direct and indirect effects of forest cover on larval habitats and anopheline assemblages in different seasons. We found 3474 larvae in the dry season and 6603 in the rainy season, totalling ten species and confirming the presence of malaria vectors across all sites. Forest cover had direct and indirect (through limnological variables) effects on the composition of larval anopheline assemblages in the rainy season. However, during the dry season, forest cover directly affected larval distribution and habitat variables (with no indirect affects). Additionally, artificial larval habitats promote ideal conditions for malaria vectors in Amazonia, mainly during the rainy season, with positive consequences for anopheline assemblages. Therefore, the application of integrated management can be carried out during both seasons. However, we suggest that the dry season is the optimal time because larval habitats are more limited, smaller in volume and more accessible for applying vector control techniques

Perspectivas de pesquisas na relação entre clima e o funcionamento da Floresta Amazônica

Pesquisas recentes do programa LBA (Programa de\ud Grande Escala da Biosfera‑Atmosfera na Amazônia)\ud demonstram ligações entre o clima e o uso da terra\ud na Amazônia e o funcionamento do bioma (1). A\ud vegetação tem uma estreita relação com a atmosfera,\ud controlando uma série de processos físico‑químicos que influenciam\ud a taxa de formação de nuvens, quantidade de núcleos de condensação\ud de nuvens, quantidade de vapor de água, balanço de radiação, emissão\ud de gases biogênicos e de efeito estufa entre tantas outras propriedades.\ud A Amazônia, por sua localização tropical e grande área (Figura 1), é\ud uma importante fonte de vapor de água para nosso planeta. Ela também\ud contém o maior reservatório de carbono entre os ecossistemas\ud terrestres, e tem um papel fundamental na mitigação das mudanças\ud climáticas em curso. A mobilização de pequena fração do carbono\ud acumulado na biomassa da floresta pode perturbar o ciclo de carbono\ud global. A Amazônia também é parte do mais intenso ciclo hidrológico\ud de nosso planeta, com um sofisticado processamento e reciclagem de\ud vapor de água, que alimenta a maior bacia hidrológica. Estes aspectos\ud fazem da região amazônica uma questão central em pesquisas de clima\ud e nas mudanças globais. Desde seu início, o programa LBA focou no\ud relacionamento entre clima, ciclos biogeoquímicos e o papel da mudança\ud de uso do solo em curso, alterando o funcionamento do bioma