Effects of a native and a non-native macrophyte species of Hydrocharitaceae on Chironomidae and Oligochaeta assemblages structure / Efeitos de uma espécie de macrófita nativa e uma invasora de Hydrocharitaceae sobre a estrutura das assembleias de Chironomidae e Oligochaeta

This study investigated the structure of the Oligochaeta and Chironomidae assemblages associated with monospecific stands of two submerged macrophyte species: Egeria najas and Hydrilla verticillata. Samplings were carried out in Leopoldo Backwater and Paraná river, in August 2008. To assess the structure of Oligochaeta and Chironomidae assemblage in each macrophyte we calculated: species density, richness, diversity, and evenness. A detrended correspondence analysis (DCA) was used to summarize Oligochaeta and Chironomidae assemblages composition. The highest values of species density and richness for the two groups were recorded in H. verticillata. Although there were no significant differences in density, richness and Shannon diversity, the assemblage composition of these groups was significantly different between plant species. These results suggest that despite being a recent colonizer in the upper Paraná river habitats, the non-native species H. verticillata seems to provide favorable conditions for the establishment of native assemblages of Chironomidae and Oligochaeta. Moreover, differences in the species composition of Oligochaeta and Chironomidae arose from peculiar characteristics of each plant, as attached microorganisms and organic matter, so that other factors, rather than plant architecture can also influence the assemblage of these groups.

Este estudo objetivou investigar a estrutura da assembleia de Oligochaeta e Chironomidae em associação com bancos puros de duas espécies de macrófitas submersas: Hydrilla verticillata e Egeria najas. As coletas foram realizadas no ressaco do Leopoldo e no rio Paraná, em agosto de 2008. Para avaliar a estrutura da assembleia de Oligochaeta e Chironomidae em cada macrófita foram calculados: densidade, riqueza, diversidade de Shannon e equitabilidade. Uma análise de correspondência destendenciada (DCA) foi usada para sumarizar a composição da assembleia de Oligochaeta e Chironomidae. Os maiores valores de densidade e riqueza para os dois grupos foram registrados na H. verticillata. Embora não houvesse nenhuma diferença significativa na densidade, riqueza e diversidade de Shannon, a composição da assembleia desses grupos foi significativamente diferente entre as macrófitas. Esses resultados sugerem que apesar de ser uma colonizadora recente dos habitats do alto rio Paraná, H. verticillata parece prover condições favoráveis para o estabelecimento das assembleias de Oligochaeta e Chironomidae. Além disso, diferenças na composição de espécies desses grupos ocorreram devido às características peculiares de cada planta, como micro-organismos e matéria orgânica aderidos, de forma que outros fatores, em vez de arquitetura da planta, podem também influenciar a assembleia desses grupos.

Photo-degradation effect on dissolved organic carbon availability to bacterioplankton in a lake in the upper Paraná river floodplain / Photo-degradation effect on dissolved organic carbon availability to bacterioplankton in a lake in the upper Paraná river floodplain

Dissolved organic carbon (DOC) is nowadays recognized as the main substrate and source of energy for aquatic microbial community. The great part of available organic carbon for bacterioplankton might be formed after photolytic degradation of humic material, which constitutes the major part of DOC in almost all natural waters. The effects of DOC photo-degradation were evaluated, as was its utilization by bacterioplankton, through a two-step experiment, one involving photo-degradation of DOC and the other bacterial growth on the photo-degraded substrate. Photo-degradation was responsible for the consumption of 19% of DOC, reduced SUVA254, an increase in the E2/E3 and E3/E4 ratios, in addition to modifications in the fluorescence spectra that indicated a rise in the labile fraction of DOC. However, these alterations on DOC were not reflected in differences in bacterioplankton growth, as shown by the fact that there were no significant differences in density, biomass, bacterial production, bacterial respiration and bacterial growth efficiency between treatment and control.

O carbono orgânico dissolvido (COD) é reconhecido atualmente como o principal substrato e fonte de energia para a comunidade microbiana aquática. Grande parte do COD biodisponível para o bacterioplâncton pode ser gerada após degradação fotolítica do material húmico dissolvido, que constitui a maior parte do carbono orgânico total. Neste trabalho foram avaliados os efeitos da fotodegração no COD de um ambiente húmico e a sua posterior utilização pelo bacterioplâncton, por meio de um experimento em duas etapas, uma de fotodegradação do COD e outra de crescimento microbiano sobre o substrato fotodegradado. A fotodegradação causou consumo de 19% do COD, diminuição na SUVA254, aumento nas razões E2/E3 e E3/E4 e modificações nos espectros de fluorescência apontando aumento da fração lábil. No entanto, as alterações no COD não se refletiram em diferenças no crescimento do bacterioplâncton, não havendo diferenças significativas com relação à densidade, biomassa, produção, respiração e eficiência de crescimento bacteriano.

Bacterioplankton features and its relations with doc characteristics and other limnological variables in Paraná river floodplain environments (PR/MS-Brazil)

Since the introduction of the Microbial Loop concept, many studies aimed to explain the role of bacterioplankton and dissolved organic carbon (DOC) in aquatic ecosystems. Paraná River floodplain system is a very complex environment where these subjects were little explored. The aim of this work was to characterize bacterial community in terms of density, biomass and biovolume in some water bodies of this floodplain and to verify its temporal variation and its relation with some limnological variables, including some indicators of DOC quality, obtained through Ultraviolet-visible (UV-VIS) and fluorescence spectroscopic analysis. Bacterial density, biomass and biovolume are similar to those from other freshwater environments and both density and biomass were higher in the period with less rain. The limnological and spectroscopic features that showed any relation with bacterioplankton were the concentrations of N-NH4 and P-PO4, water transparency, and some indicators of DOC quality and origin. The analysis of these relations showed a possible competition between bacterioplankton and phytoplankton for inorganic nutrients and that the DOC used by bacterioplankton is labile and probably from aquatic macrophytes.

Bacterioplankton features and its relations with doc characteristics and other limnological variables in Paraná river floodplain environments (PR/MS-Brazil).

Since the introduction of the Microbial Loop concept, many studies aimed to explain the role of bacterioplankton and dissolved organic carbon (DOC) in aquatic ecosystems. Paraná River floodplain system is a very complex environment where these subjects were little explored. The aim of this work was to characterize bacterial community in terms of density, biomass and biovolume in some water bodies of this floodplain and to verify its temporal variation and its relation with some limnological variables, including some indicators of DOC quality, obtained through Ultraviolet-visible (UV-VIS) and fluorescence spectroscopic analysis. Bacterial density, biomass and biovolume are similar to those from other freshwater environments and both density and biomass were higher in the period with less rain. The limnological and spectroscopic features that showed any relation with bacterioplankton were the concentrations of N-NH4 and P-PO4, water transparency, and some indicators of DOC quality and origin. The analysis of these relations showed a possible competition between bacterioplankton and phytoplankton for inorganic nutrients and that the DOC used by bacterioplankton is labile and probably from aquatic macrophytes.