[1] This study analyzes evapotranspiration data for three wet and two seasonally dry rain forest sites in Amazonia. The main environmental (net radiation, vapor pressure deficit, and aerodynamic conductance) and vegetation (surface conductance) controls of evapotranspiration are also assessed. Our research supports earlier studies that demonstrate that evapotranspiration in the dry season is higher than that in the wet season and that surface net radiation is the main controller of evapotranspiration in wet equatorial sites. However, our analyses also indicate that there are different factors controlling the seasonality of evapotranspiration in wet equatorial rain forest sites and southern seasonally dry rain forests. While the seasonality of evapotranspiration in wet equatorial forests is driven solely by environmental factors, in seasonally dry forests, it is also biotically controlled with the surface conductance varying between seasons by a factor of approximately 2. The identification of these different drivers of evapotranspiration is a major step forward in our understanding of the water dynamics of tropical forests and has significant implications for the future development of vegetation-atmosphere models and land use and conservation planning in the region.

O presente trabalho teve como objetivo verificar a variação da produção de serrapilheira de diferentes biomas: Cerrado (com as fitofisionomias Cerrado sensu stricto e Cerradão) e Floresta de Transição Amazônia-Cerrado, em clima tropical. Para a determinação da produção de serrapilheira foram utilizados coletores de tela em náilon. Dados micrometereológicos foram coletados nas áreas de estudo. A produção de serrapilheira nos dois biomas mostrou acentuada sazonalidade, com as maiores produções ocorrendo durante a estação seca e menor durante a estação chuvosa. A maior produção de serrapilheira ocorreu na Floresta de Transição, seguida do bioma Cerrado. A fração de folhas foi mais representativa do que as frações de galhos, flores, frutos em ambas as áreas estudadas.

RESUMOEm função de se analisar a produção, dinâmica e decomposição de serrapilheira em busca da sazonalidade do microclima em uma floresta tropical de transição Amazônia Cerrado, propõe-se estimar a produção de serrapilheira, por meio de caixas de coleta de 1 m 2 e o acúmulo de serrapilheira sobre o solo por meio de quadrantes de 25 x 25 cm, distribuídos aleatoriamente. Determinaram-se a constante de decaimento (K), o coeficiente de retorno de serrapilheira (K L ) e a constante de decomposição (K'). Com o emprego de bolsas de nylon preenchidas com folhas de espécies de relevância na floresta (Tovomita schomburgkki e Brosimium lactescens) estudou-se a decomposição de folhas e se monitaram os fatores ambientais por meio de equipamentos instalados em uma torre micrometeorológica. A produção de serrapilheira não só se apresentou de forma sazonal, com significativa influência da umidade relativa do ar e da precipitação, em uma floresta de transição, mas foi majoritariamente composta de folhas seguidas de galhos e miscelânea (flores e frutos). A decomposição de folhas em florestas tropicais foi acelerada em ambas as estações, seca-úmida e úmida-seca, sendo a velocidade de decomposição das folhas maior na estação úmida-seca.Palavras-chave: acúmulo de serrapilheira no solo, Amazônica, decomposição de folhas Seasonal dynamics of the litterfall production and decomposition in tropical transitional forest ABSTRACTThe objective of this study was to analyze the production, dynamics and litter decomposition as a function of the seasonality of the microclimate in a transitional tropical forest of Amazonia Cerrado. Estimate of litterfall was carried out with collection boxes of 1 m 2 and floor forest mass with quadrants of 25 x 25 cm distributed randomly. The decline constant (K), litter turnover rate (K L ) and litter decomposition rate (K') were determined by estimation of litterfall and forest floor litter mass. Leaf decomposition was studied by litter bags with leaves of species of relevance (Tovomita schomburgkki and Brosimium lactescens) in the forest. The analysis of the environmental factors was measured through micrometeorological equipments. The litterfall was seasonal in nature, with significant influence from relative air humidity and rainfall in a transitional forest. Litterfall was mainly composed of leaves, followed by twigs, and miscellany (flowers and fruits). The leaf decomposition in tropical forests was accelerated in seasons, dry-wet and wet-dry, being the leaf decomposition higher in the wet-dry season.

[1] This study analyzed how seasonal and interannual variations in climate alter litter dynamics, including production, decomposition, and accumulation. Monthly measurements of leaf, stem, and reproductive (flower plus fruit) litter and the forest floor litter mass were combined with a mass balance model to determine rates of litter decomposition for a semideciduous tropical forest located in the rain forest-savanna ecotone of the southern Amazon Basin for [2001][2002][2003][2004][2005][2006][2007]. Annual rates of litter production varied between 8 and 10.5 Mg ha À1 a À1 , and leaf litter production accounted for the majority ($70%) of the total litter production. Leaf litter production peaked at the end of the May-August dry season while stem litter production peaked during the wet season and reproductive litter production peaked during the dry-wet season transition. Forest floor litter mass ranged between 5 and 8 Mg ha À1 over the study period and generally declined as litter inputs declined. Litter decomposition rates were remarkably stable from year-toyear and varied between 10.8 and 12.4 Mg ha À1 a À1 . On average, rates of litter decomposition were highest during the dry-wet season transition. Overall, our results suggest that rainfall variability directly altered litter production dynamics and indirectly altered forest floor litter mass and decomposition kinetics through its effect on litter production. Future changes in seasonal and/or interannual rainfall patterns, whether in response to El Niño or to anthropogenic climate change, will likely have important consequences for the litter dynamics of Amazonian semideciduous forest.

RESUMOEste estudo foi desenvolvido numa área de floresta de transição Amazônia-Cerrado no norte de Mato Grosso. Teve como objetivo quantificar a dinâmica da produção e acúmulo e as partes constituintes da serrapilheira, bem como a participação das folhas no retorno do nitrogênio, fósforo e carbono ao solo por meio da decomposição. Foram coletados mensalmente durante um ano dados de serrapilheira total produzida, serrapilheira total acumulada no solo e avaliada a decomposição de folhas no período de seca e de chuvas. A produção de serrapilheira apresentou variações sazonais com maiores valores no período seco e predomínio da fração foliar durante todo o ano. Por outro lado, a serrapilheira acumulada não apresentou diferenças significativas entre o período de seca e o chuvoso como também correlação significativa com a serrapilheira produzida. A decomposição da serrapilheira exclusiva de folhas foi mais intensa no período chuvoso e em ordem decrescente de espécies, em T. schomburgkii, Thyrsodium sp, B. lactescens e P. sagotianum. A espécie P. sagotianum tanto no período seco quanto no chuvoso apresentou maior resistência à decomposição. O potencial de retorno de nitrogênio ao solo foi da ordem de 70,3 kg.ha -1 .ano -1 , para o fósforo, de 76,1 kg.ha -1 .ano -1 e para o carbono, de 3,5 ton.ha -1 .ano -1 . Houve uma correlação entre a decomposição exclusiva de folhas e o retorno de nitrogênio e fósforo para todas as espécies estudadas no período de seca. No período chuvoso foi registrada correlação significativa somente para nitrogênio e o carbono para a espécie P. sagotianum.PALAVRAS-CHAVE: ciclagem de nutrientes, serrapilheira, floresta de transição. Leaf contribution to litterfall and litterpool and nutrients recycling in transition forest in Mato Grosso ABSTRACTThis study was conducted in an area of Amazonia-Cerado transition forest in the noirth of Mato Grosso state, Brazil. The main objectives of the study was to quantify the variability of litter fall and litter pool biomass (leaves, flowers, fruits, and wood), and the participation of the leaves in the return of nitrogen, phosphorus and carbon to the soil through decomposition. Litter was collected monthly during one year and leaves decomposition was analyzed during the dry and rainy seasons. Litter fall varied along the year with higher values in the dry season and predominance of the leaf fraction. Nevertheless, there was no significant difference between dry and rainy seasons for litter pool as well as significant correlation between litter pool and litter fall. Decomposition of leaves was more intense in the rainy season in order of decreasing species: T. schomburgkii, Thyrsodium sp, B. lactescens and P. sagotianum. The species P. sagotianum in both dry and rainy seasons showed most slowly decomposition. The potential return was 70.3 kg.ha -1 .year -1 for nitrogen, 76.1 kg.ha -1 .years -1 for phosphorus, 3.5 ton.ha -1 . years -1 for carbon. There was significant correlation between leave decomposition and nitrogen and phosphorus return for all species ana...

The recent and widespread expansion of the pioneer tree species Vochysia divergens Pohl into western Brazil has the potential to significantly alter the structure and function of the Pantanal-a UNESCO World Heritage Site and the World's largest tropical wetland. Here we assess the seasonal pattern of evapotranspiration (ET) and micrometeorological variables of V. divergens (locally known as cambarazal), located in the Northeast of the Brazilian Pantanal. ET was calculated from a number of micrometeorological measurements recorded between January 2007 and January 2008. The results indicate that ET was the dominant sink for net radiation (R n ) during the wet and dry seasons, primarily because the forest was either flooded (December-May) or retained a high level of soil moisture. ET decreased during the dry season due to a decline in R n and surface water availability, and an increase in atmospheric vapor pressure deficit. Based on this analysis we conclude that the spread of V. divergens into the Pantanal and the associated high rates of ET are due in part to high water availability, even during the dry season, and the consistently high leaf area index that increases the transpiration surface area when the water table is below the soil surface.

RESUMOO estudo do balanço de energia de uma superfície vegetada e a atmosfera é importante para caracterizar o microclima local, identificar interações entre variáveis ambientais e a vegetação, e identificar efeitos das atividades antropogênicas. O objetivo deste trabalho foi estimar a variação sazonal do balanço de energia pelo método da razão de Bowen em uma área de vegetação monodominante de Cambará na RPPN SESC-Pantanal e uma área de pastagem na Fazenda Experimental da UFMT. Os componentes do balanço de energia apresentaram sazonalidade, com maiores médias na estação chuvosa nas duas áreas de estudo. No cambarazal houve maior variação do fluxo de calor latente da estação seca para a chuvosa que na pastagem. Entretanto, a variação sazonal do fluxo de calor sensível foi menor no cambarazal que na pastagem, devido ao efeito termo-regulador do cambarazal, em função da maior biomassa. A energia disponível aos dois sítios foi destinada prioritariamente em fluxo de calor latente, 80,0% no cambarazal e 56,6% na pastagem, seguido pelo fluxo de calor sensível, 19,1 e 42,9%, e pelo fluxo de calor no solo, 0,3 e 7,2%. Palavras-chave: razão de Bowen; sazonalidade; floresta tropical; microclima. ABSTRACT: ESTIMATE OF ENERGY BALANCE IN CAMBARAZAL AND PASTURE IN THE NORTH OF PANTANAL BY BOWEN RATIO METHOD.The energy balance study of a vegetated surface and atmosphere is important to characterize the local microclimate, identify interactions among environmental variables and the vegetation and to identify anthropogenic activities effects. The objective of this work was estimate the seasonality of energy balance by Bowen ratio method in a monodominant vegetation of Cambará area in the RPPN SESC-Pantanal and a pasture area in UFMT's Experimental Farm. The energy balance components presented seasonality, with larger averages at the rainy station in two areas of study. In the cambarazal was a higher variation of the latent heat flux of the dry season for the rainy season that in the pasture. However, the seasonal variation of the sensible heat flux in the cambarazal was lower than in the pasture, due to the thermo-regulatory effect in the cambarazal, according to the largest biomass. The available energy at two ranches was partitioned priority in latent heat flux, 80,0% in the cambarazal and 56,6% in the pasture, followed by the sensible heat flux, 19,1 and 42,9%, and by the soil heat flux, 0,3 and 7,2%.

[1] Measurements of soil CO 2 efflux, litter production, and the surface litter pool biomass were made over a 1 year period in a tropical transitional forest near Sinop, Mato Grosso, Brazil with the aim of quantifying the seasonal variation in soil respiration and litter decomposition and the annual contribution of litter decomposition to soil CO 2 efflux. Average annual soil CO 2 efflux (±95% confidence interval (CI)) was 7.91 ± 1.16 g C m À2 d À1 . Soil CO 2 efflux was highest during the November-February wet season (9.15 ± 0.90 g C m À2 d À1 ) and lowest during the May-September dry season (6.19 ± 1.40 g C m À2 d À1 ), and over 60% of the variation in seasonal soil CO 2 efflux was explained by seasonal variations in soil temperature and moisture. Mass balance estimates of mean (±95% CI) decomposition rates were statistically different between the wet and dry seasons (0.66 ± 0.08 and 1.65 ± 0.10 g C m À2 d À1 , respectively), and overall, decomposition of leaf litter comprised 16% of the average annual soil respiration. Leaf litter production was higher during the dry season, and mean (±95% CI) leaf litter fall (5.6 ± 1.7 Mg ha À1