[en] In order to evaluate the role of heterotrophic bacteria on carbon flow in food chains of an Amazonian floodplain lake, monthly collections of these organisms were made during the hydrological year from December 2007 to November 2008. Littoral, pelagic, and aquatic macrophyte regions of the Catalao Lake in central Amazonia were sampled and bacteria were multiplied in vitro, using dissolved organic carbon (COD) of each one of the regions studied as a substrate. The bacterial biomass obtained was used for stable isotope analyses of carbon and nitrogen. These data were confronted with COD values of the four hydrological periods of the lake (dry, rising, flood and fall). In general, it was found that the main source of carbon for heterotrophic bacteria was that of C4 origin, which presented a minimum contribution of 75% of bacterial biomass, to the extent that the bacteria D13C average value -17.72 Per Mille ± 2.25 was comparing this value with the D13C of zooplankton in the same period (-33.04 Per Mille ± 3.81) permit concludes that the contribution of heterotrophic bacteria in the carbon flow to higher trophic levels in the Catalao lake is minimal.

[en] To evaluate the seasonal variation and isotopic composition of phytoplankton, water samples were collected monthly between October 2007 and November 2008 in Lake Catalao, a floodplain lake at the confluence between rivers Negro and Amazon. Analyses of total chlorophyll concentration and δ"13C and δ"15N isotopic abundances were made from particulate size fractions of 30-60, 10-30 and <10 μm in the littoral, pelagic, and floating meadows regions. Chlorophyll concentration was found to be inversely associated to lake depth, and high concentrations of chlorophyll in the floating meadows zone were significant. The fraction <10 μm was the most abundant representing in average more than 40% of the particulate matter. The δ3 13C values were relatively constant during the study (-25.1% -34.0%), whereas the δ"15N values showed strong variability (15.6% 2.4%), which has been attributed to the resuspension of sediments during mixing of the water column. Mixing associated to the sudden drop in temperature during the rising water period was an important event in the trophic and isotopic dynamics of the lake. Variations in chlorophyll content were generally associated with the dilution process, in which concentration was inversely correlated to the water level, whereas abundance was directly correlated to the water level.

[en] Increased awareness about the toxicity of mercury (Hg) has during the latest decades resulted in reduced Hg use in industrialised countries. Developing countries, on the contrary, have largely increased their anthropogenic Hg emissions caused by its use in gold mining, transfer of Hg emitting factories from developed countries, and increased burning of coal without appropriate flue gas cleaning. These increased emissions occur mainly in the tropics, where the fate of Hg is not well documented. The aim of the present study is to increase the knowledge about Hg levels and transformations in two tropical areas affected by anthropogenic Hg emissions - the Pantanal wetland in Brazil, housing gold miners using the amalgamation method, and Lake Xolotilan (Managua) in Nicaragua, where a chlor-alkali plant relocated from the USA has emitted much Hg. Actual Hg content in water, biota, and sediment will be determined by atomic fluorescence spectrophotometry and atomic absorption spectrophotometry. Mercury inethylation capacity in sediments and selected biota will be determined with in-situ incubations with ²⁰³Hg and subsequent radiological measurements. Factors affecting the methylation and demethylation rates will be identified by varying environmental conditions such as pH, redox potential, conductivity, light, temperature, geochemical factors and population of bacteria. Sediment turnover will be studied by determining fallout cesium (¹³⁷Cs) in sediment profiles. The study is expected to increase the knowledge about Hg-transformations in the tropics and point out proper measures to reduce health hazards due to Hg-exposure. (author)

[en] Increased awareness about the toxicity of mercury (Hg) has during the latest decades resulted in reduced use of Hg in industrialised countries. Developing countries, on the contrary, have largely increased their anthropogenic Hg emissions caused by its use in gold mining, transfer of Hg emitting factories from developed countries, and increased burning of coal without appropriate flue gas cleaning. The contribution of global Hg sources and the importance of other parameters to increased Hg levels encountered in hydroelectric reservoirs and other areas after flooding is not well understood, especially not in the tropics. The aim of the present study is to increase the knowledge about Hg transformations in tropical areas. Total Hg content in water, biota, and sediment will be determined by atomic absorption and fluorescence spectrophotometry and methyl Hg content in biota by gaschromatography after extraction with acids, hydroxides, and organic solvents. Mercury methylation capacity in sediments, water, and selected biota will be determined with ²⁰³Hg and subsequent radiological measurements of insitu incubations. Factors affecting the methylation and demethylation rates will be identified with laboratory incubations with ²⁰³Hg at varying environmental conditions such as organic matter, pH, redox potential, conductivity, light, temperature, geochemical factors and populations of bacteria. The populations of bacteria will be determined to quantity by isotope techniques. The first experiments indicate markedly larger methylation capacity as well as bacterial production of incubated samples of Eichhornia crassipes, originating from Brazil, compared to Myriophyllum spicatum from Sweden. The results are the first step to better understand the importance of environmental parameters and bacterial production for methylation of Hg. (author)

[en] Highlights: • Large diel variations on CO₂ dynamics • Higher plankton metabolism associated with wind mediated mixing. • Phytoplankton consumption of CO₂ derived from macrophyte decomposition. • Planktonic respiration is greater in solar exposed chambers. • CO₂ emissions enhanced during exceptional drought. We investigated plankton metabolism and its influence on carbon dioxide (CO₂) dynamics in a central Amazon floodplain lake (Janauacá, 3°23′ S, 60°18′ W) from September 2015 to May 2016, including a period with exceptional drought. We made diel measurements of CO₂ emissions to the atmosphere with floating chambers and depth profiles of temperature and CO₂ partial pressure (pCO₂) at two sites with differing wind exposure and proximity to vegetated habitats. Dissolved oxygen (DO) concentrations were monitored continuously during day and night in clear and dark chambers with autonomous optical sensors to evaluate plankton metabolism. Overnight community respiration (CR), and gross primary production (GPP) rates were higher in clear chambers and positively correlated with chlorophyll-a (Chl-a). CO₂ air-water fluxes varied over 24-h periods with changes in thermal structure and metabolism. Most net daily CO₂ fluxes during low water and mid-rising water at the wind exposed site were into the lake as a result of high rates of photosynthesis. All other measurements indicated net daily release to the atmosphere. Average GPP rates (6.8 gC m⁻² d⁻¹) were high compared with other studies in Amazon floodplain lakes. The growth of herbaceous plants on exposed sediment during an exceptional drought led to large carbon inputs when these areas were flooded, enhancing CR, pCO₂, and CO₂ fluxes. During the period when the submerged herbaceous vegetation decayed phytoplankton abundance increased and photosynthetic uptake of CO₂ occurred. While planktonic metabolism was often autotrophic (GPP:CR > 1), CO₂ out-gassing occurred during most periods investigated indicating other inputs of carbon such as sediments or soils and wetland plants.