Diazotrophic community in the sediments of Poyang Lake in response to water level fluctuations.

Water level fluctuations (WLFs) are typical characteristic of floodplain lakes and dominant forces regulating the structure and function of lacustrine ecosystems. The sediment diazotrophs play important roles in contributing bioavailable nitrogen to the aquatic environment. However, the relationship between the diazotrophic community and WLFs in floodplain lakes is unknown. In this paper, we carried out a comprehensive investigation on the alpha diversity, abundance, composition and co-occurrence network of the sediment diazotrophs during different water level phases in Poyang Lake. There were no regular variation patterns in the alpha diversity and abundance of the sediment diazotrophs with the water level phase transitions. The relative abundance of some diazotrophic phyla (including Alphaproteobacteria, Deltaproteobacteri, Euryarchaeota, and Firmicutes) and genera (including Geobacter, Deferrisoma, Desulfuromonas, Rivicola, Paraburkholderia, Methylophilus, Methanothrix, Methanobacterium, and Clostridium) was found to change with the water level phase transitions. The results of ANOSIM, PerMANOVA, and DCA at the OTU level showed that the diazotrophic community structure in the low water level phase was significantly different from that in the two high water level phases, while there was no significant difference between the two high water level phases. These results indicated that the diazotrophic community was affected by the declining water level in terms of the composition, while the rising water level contributed to the recoveries of the diazotrophic community. The diazotrophs co-occurrence network was disrupted by the declining water level, but it was strengthened by the rising water level. Moreover, redundancy analysis showed that the variation of the diazotrophic community composition was mostly related to sediment total nitrogen (TN) and total phosphorous (TP). Interestingly, the levels of sediment TN and TP were also found to vary with the water level phase transitions. Therefore, it might be speculated that the WLFs may influence the sediment TN and TP, and in turn influence the diazotrophic community composition. These data can contribute to broadening our understanding of the ecological impacts of WLFs and the nitrogen fixation process in floodplain lakes.

Spatiotemporal heterogeneity of inundation pattern of floodplain lake wetlands and impact on wetland vegetation.

The inundation pattern is an important ecohydrological indicator for studying floodplain lake wetlands, as it is the key factor affecting the wetland vegetation distribution patterns. Poyang Lake, the largest freshwater lake in China, is a typical floodplain lake wetland. This study presents a hydrodynamic model and vegetation survey of Poyang Lake, analyzed the spatiotemporal heterogeneity of the inundation pattern (inundation duration and depth), assessed the response patterns of wetland vegetation concerning the inundation pattern, and examined the impact of the proposed Poyang Lake Water Conservancy Hub (PLWCH) on the inundation pattern and wetland vegetation. The results revealed that the inundation pattern of Poyang Lake had significant spatial heterogeneity. Inundation pattern was found to have a significant impact on the vegetation succession. The response relationship between the distribution areas of different wetland vegetation types and inundation pattern was in accordance with the Gaussian curve, and the ecological threshold range of the Carex spp. community was the greatest. Owing to factors such as climate change and anthropogenic activities, the inundation pattern of Poyang Lake varied significantly since 2003, with the average inundation duration and average inundation depth decreasing by 15 d and 0.32 m, respectively. Consequently, the spatial distribution of wetland vegetation changed significantly, whereby the Carex spp., Polygonum criopolitanum, and Phalaris arundinacea communities extended down to the lower elevation zone. In the future, the PLWCH may result in increases in the inundation duration and depth, restrain the downward vegetation extension trend, and promote the vegetation to move to higher elevations similar to the status prior to 2003. These findings provide a detailed description of the spatiotemporal heterogeneity of the inundation pattern and the drivers of wetland vegetation distribution patterns in floodplain lake wetlands, serving as a scientific basis for conservation and restoration of these ecosystems.

Chlorophyll a variations and responses to environmental stressors along hydrological connectivity gradients: Insights from a large floodplain lake.

Understanding the key drivers of eutrophication in floodplain lakes has long been a challenge. In this study, the Chlorophyll a (Chla) variations and associated relationships with environmental stressors along the temporal hydrological connectivity gradient were investigated using a 11-year dataset in a large floodplain lake (Poyang Lake). A geostatistical method was firstly used to calculate the hydrological connectivity curves for each sampling campaign that was further classified by K-means technique. Linear mixed effect (LME) models were developed through the inclusion of the site as a random effect to identify the limiting factors of Chla variations. The results identified three clear hydrological connectivity variation patterns with remarkable connecting water area changes in Poyang Lake. Furthermore, hydrological connectivity changes exerted a great influence on environmental variables in Poyang Lake, with a decrease in nutrient concentrations as the hydrological connectivity enhanced. The Chla exhibited contrast variations with nutrient variables along the temporal hydrological connectivity gradient and generally depended on WT, DO, EC and TP, for the entire study period. Nevertheless, the relative roles of nutrient and non-nutrient variables in phytoplankton growth varied with different degrees of hydrological connectivity as confirmed by the LME models. In the low hydrological connectivity phase, the Chla dynamics were controlled only by water temperature with sufficient nutrients available. In the high hydrological connectivity phase, the synergistic influences of both nutrient and physical variables jointly limited the Chla dynamics. In addition, a significant increasing trend was observed for Chla variations from 2008 to 2018 in the HHC phase, which could largely be attributed to the elevated nutrient concentrations. This study confirmed the strong influences of hydrological connectivity on the nutrient and non-nutrient limitation of phytoplankton growth in floodplain lakes. The present study could provide new insights on the driving mechanisms underlying phytoplankton growth in floodplain lakes.

Phytoplankton community composition, carbon sequestration, and associated regulatory mechanisms in a floodplain lake system.

Phytoplankton contribute approximately 50% to the global photosynthetic carbon (C) fixation. However, our understanding of the corresponding C sequestration capacity and driving mechanisms associated with each individual phytoplankton taxonomic group is limited. Particularly in the hydrologically dynamic system with highly complex surface hydrological processes (floodplain lake systems). Through investigating seasonal monitoring data in a typical floodplain lake system and estimation of primary productivity of each phytoplankton taxonomic group individually using novel equations, this study proposed a phytoplankton C fixation model. Results showed that dominant phytoplankton communities had a higher gross carbon sequestration potential (CSP) (9.50 ± 5.06 Gg C each stage) and gross primary productivity (GPP) (65.46 ± 25.32 mg C m-2 d-1), but a lower net CSP (-1.04 ± 0.79 Gg C each stage) and net primary productivity (NPP) (-5.62 ± 4.93 mg C m-3 d-1) than rare phytoplankton communities in a floodplain lake system. Phytoplanktonic GPP was high (317.94 ± 73.28 mg C m-2 d-1) during the rainy season and low (63.02 ± 9.65 mg C m-2 d-1) during the dry season. However, their NPP reached the highest during the rising-water stage and the lowest during the receding-water stage. Findings also revealed that during the rainy season, high water levels (p = 0.56**) and temperatures (p = 0.37*) as well as strong solar radiation (p = 0.36*) will increase photosynthesis and accelerate metabolism and respiration of dominant phytoplankton communities, then affect primary productivity and CSP. Additionally, water level fluctuations drive changes in nutrients (p = -0.57*) and metals (p = -0.68*) concentrations, resulting in excessive nutrients and metals slowing down phytoplankton growth and reducing GPP. Compared with the static water lake system, the floodplain lake system with a lower net CSP became a heterotrophic C source.

Refining the concept of hydrological connectivity for large floodplain systems: Framework and implications for eco-environmental assessments.

Recent years, the hydrological connectivity has gained popularity in various research fields, however, its definition and threshold effects at a system scale have not received adequate attention. The current research proposes a promising framework to refine the concept of surface hydrological connectivity by combining hydrodynamic modeling experiments, threshold effects and geostatistical connectivity analysis, exemplified by the flood-pulse-influenced Poyang Lake floodplain system (China). To enhance the inherent linkage between hydrological connectivity and eco-environments, total connectivity (TC), general connectivity (GC), and effective connectivity (EC) were proposed to refine the metrics of hydrological connectivity. The results show that substantial differences between the three connectivity metrics are observed for all target directions, demonstrating that the joint role of water depth and flow velocity may produce more dynamic and complex influences on EC than the other two metrics of TC and GC. Topographically, the connectivity objects/areas within the flood pulse system reveal that the floodplain is a more sensitive area than the lake's main flow channels under different connectivity conditions. The modelling experimental studies show that variations in water depth thresholds are more likely to have a strong effect on connectivity for the dry, rising, and falling limbs, rather than the flooding period, while the flow velocity may exert an opposite threshold effect. The lake-floodplain system is characterized by a dynamic threshold behavior, with seasonally varying water depth and velocity thresholds. This study highlights the importance of redefined connectivity concept for facilitating scientific communication by combining hydrodynamic thresholds and offering recommendations for future connectivity assessments using our proposed metrics of TC, GC, and EC.

Hydrodynamic and water quality modeling of a large floodplain lake (Poyang Lake) in China.

Floodplain lakes are valuable to humans because of their various functions and are characterized by dramatic hydrological condition variations. In this study, a two-dimensional coupled hydrodynamic and water quality model was applied in a large floodplain lake (i.e., Poyang Lake), to investigate spatial and temporal water quality variations. The model was established based on detailed data such as lake terrain, hydrological, and water quality. Observed lake water level and discharge and water quality parameters (TN, TP, CODMn, and NH4-N) were used to assess model performance. The hydrodynamic model results showed satisfactory results with R2 and MRE values ranging between 0.96 and 0.99 and between 2.45 and 6.14%, respectively, for lake water level simulations. The water quality model basically captured the temporal variations in water quality parameters with R2 of TN, TP, CODMn, and NH4-N simulation ranges of 0.56-0.91, 0.44-0.66, 0.64-0.67, and 0.44-0.57, respectively, with TP of Xingzi Station and CODMn of Duchang Station excluded, which may be further optimized with supplementation of sewage and industrial discharge data. The modeled average TN, TP, CODMn, and NH4-N concentrations across the lake were 1.36, 0.05, 1.99, and 0.48 mg/L, respectively. The modeled spatial variations of the lake showed that the main channel of the lake acted as a main pollutant passageway, and the east part of the lake suffered high level of pollution. In addition, consistent with previous water quality evaluations based on field investigations, water quality was the highest (average TN = 1.35 mg/L) during high water level periods and the poorest (average TN = 1.96 mg/L) during low water level periods. Scenario analysis showed that by decreasing discharge of upstream flow by 20% could result in the increase of TN and TP concentrations by 25.6% and 23.2% respectively. In summary, the model successfully reproduced the complex water and pollutant exchange processes in the systems involving upstream rivers, the Poyang Lake, and the Yangtze River. The model is beneficial for future modeling of the impact of different load reduction and other hydrological regime changes on water quality variation and provides a relevant example for floodplain lake management.

Plastic pollution in freshwater ecosystems: macro-, meso-, and microplastic debris in a floodplain lake.

Plastic pollution is considered an important environmental problem by the United Nations Environment Programme, and it is identified, alongside climate change, as an emerging issue that might affect biological diversity and human health. However, despite research efforts investigating plastics in oceans, relatively little studies have focused on freshwater systems. The aim of this study was to estimate the spatial distribution, types, and characteristics of macro-, meso-, and microplastic fragments in shoreline sediments of a freshwater lake. Food wrappers (mainly polypropylene and polystyrene), bags (high- and low-density polyethylene), bottles (polyethylene terephthalate), and disposable Styrofoam food containers (expanded polystyrene) were the dominant macroplastics recorded in this study. Contrary to other studies, herein macroplastic item surveys would not serve as surrogates for microplastic items. This is disadvantageous since macroplastic surveys are relatively easier to conduct. Otherwise, an average of 25 mesoplastics (mainly expanded polystyrene) and 704 microplastic particles (diverse resins) were recorded per square meter in sandy sediments. Comparisons with other studies from freshwater and marine beaches indicated similar relevance of plastic contamination, demonstrating for the first time that plastic pollution is a serious problem in the Paraná floodplain lakes. This study is also valuable from a social/educational point of view, since plastic waste has been ignored in the Paraná catchment as a pollutant problem, and therefore, the outcome of the current study is a relevant contribution for decision makers.

Sediment cores as archives of historical changes in floodplain lake hydrology.

Anthropogenic activities are contributing to the changing hydrology of rivers, often resulting in their degradation. Understanding the drivers and nature of these changes is critical for the design and implementation of effective mitigation strategies for these systems. However, this can be hindered by gaps in historical measured flow data. This study therefore aims to use sediment cores to identify historical hydrological changes within a river catchment. Sediment cores from two floodplain lakes (billabongs) in the urbanised Yarra River catchment (Melbourne, South-East Australia) were collected and high resolution images, trends in magnetic susceptibility and trends in elemental composition through the sedimentary records were obtained. These were used to infer historical changes in river hydrology to determine both average trends in hydrology (i.e., coarse temporal resolution) as well as discrete flood layers in the sediment cores (i.e., fine temporal resolution). Through the 20th century, both billabongs became increasingly disconnected from the river, as demonstrated by the decreasing trends in magnetic susceptibility, particle size and inorganic matter in the cores. Additionally the number of discrete flood layers decreased up the cores. These reconstructed trends correlate with measured flow records of the river through the 20th century, which validates the methodology that has been used in this study. Not only does this study provide evidence on how natural catchments can be affected by land-use intensification and urbanisation, but it also introduces a general analytical framework that could be applied to other river systems to assist in the design of hydrological management strategies.

Seasonal variatoon in the distribution and isotpic composition of phytoplanktoon in an amazon floodplain lake, Brazil / Variación estacional de la distribución y composición isotópica del fitoplancton en un lago de inundación en la Amazonia, Brasil

To evaluate the seasonal variation and isotopic composition of phytoplankton, water samples were collected monthly between October 2007 and November 2008 in Lake Catalão, a floodplain lake at the confluence between rivers Negro and Amazon. Analyses of total chlorophyll concentration and ð13C and ð15N 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 ð13C values were relatively constant during the study (-25.1 % ∼ -34.0 %), whereas the ð15N 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.

Con el propósito de evaluar la variación estacional de la abundancia isotópica (ð13C e ð15N) del fitoplancton, muestreos mensuales fueron realizados entre octubre de 2007 y noviembre de 2008 en el lago Catalão, un lago de inundación en la zona de confluencia de los ríos Negro y Solimãµes, ubicado frente a la ciudad de Manaus (AM, Brasil). Análisis de la clorofila total y evaluaciones de la abundancia natural de ð13C y ð15N fueron realizados en las fracciones partículadas de 30-60, 10-30 y < 10 µm en las zonas litoral, pelágica y de macrófitas acuáticas. La concentración de clorofila presentó una relación inversa con la profundidad del lago, siendo relevantes las altas concentraciones encontradas dentro del tapete de macrófitas acuáticas. La fracción < 10µm fue la que presentó la mayor concentración de clorofila, representando más del 40% del material particulado. Los valores de ð13C fueron relativamente constantes durante el período de estudio (-25,1 % ∼ - 34 %), mientras que la abundancia natural de ð15N presentó una amplia variación (15,6 % ∼ – 2,4 %), que fue atribuida al proceso de resuspensión de los sedimentos en los procesos de mezcla de la columna de agua. En este contexto, el fenómeno de la mezcla asociada con la friaje durante el período de aguas altas, fue un evento importante en la dinámica trófica e isotópica del lago. En general las variaciones de la concentración de clorofila fueron asociadas al proceso de dilución, en el cual la concentración es inversa y la abundancia es directamente relacionada con el nivel del agua.

Structure of the testate amoebae community in different habitats in a neotropical floodplain / Estrutura da comunidade de amebas testáceas em diferentes hábitats em uma planície de inundação neotropical

This study evaluated the differences in composition, abundance and morphology of testate amoebae among different habitats of the same aquatic environment (plankton, aquatic macrophyte and sediment) in the Upper Paraná River floodplain. Triplicate samplings were undertaken monthly at each habitat from April 2007 to March 2008. The structure of the community of testate amoebae was different among the habitats. The species typical for each habitat, according to Indval, were classified by their shell morphology. Arcella species together with Difflugia gramen and Difflugia pseudogramem were more abundant for plankton. Trinema and Phryganella stood out by their abundance and frequency in aquatic macrophytes. Centropyxis was an indicator of sediment. The results indicated a higher frequency of hemispherical and spherical shells in plankton and spherical and elongated shells in aquatic macrophytes. In the sediment, there was a high frequency of elongated species. Our results support the hypothesis that the community of testate amoebae has different structures among the habitats, refuting the idea that the organization of this community in plankton is guided by random events like the resuspension of organisms from the sediment and their displacement from marginal vegetation.

Este estudo avaliou as diferenças na composição, abundância e morfologia das amebas testáceas entre diferentes hábitats de um mesmo ambiente aquático (plâncton, macrófitas aquáticas e sedimento) da planície de inundação do alto rio Paraná. As amostras foram coletadas mensalmente no período de abril de 2007 a março de 2008. A estrutura da comunidade de amebas testáceas foi diferente entre os hábitats. As espécies típicas para cada hábitat, de acordo com o Indval, foram classificadas pela morfologia da teca. Espécies de Arcella, Difflugia gramen e Difflugia pseudogramem foram mais abundantes para o plâncton. Trinema e Phryganella destacaram-se pela alta abundância e frequência nas macrófitas aquáticas. Centropyxis foi considerado indicador do sedimento. Os resultados indicaram uma alta frequência de tecas esféricas e hemisféricas no plâncton e de tecas alongadas nas macrófitas aquáticas. No sedimento foi registrada uma maior frequência de espécies alongadas. Nossos resultados suportam a hipótese que a comunidade de amebas testáceas possui estrutura diferente entre os hábitats, refutando a ideia que a comunidade presente no plâncton é guiada por processos estocásticos como a ressuspensão dos organismos do sedimento e simples carreamento da vegetação marginal.

Impoundment effects in the population of Auchenipterus osteomystax (Siluriformes: Auchenipteridae): a Neotropical reservoir case

New impoundments provide opportunities to check whether species that present enough feeding flexibility in natural conditions may take advantage of this situation and, without reproductive restriction, can occupy the most conspicuous habitat in a large reservoir (open areas) and present higher success in the colonization of the new environment. We examined variations in the abundance and feeding of A. osteomystax in two environments, one natural (Sinha Mariana floodplain lake) and one dammed (Manso Reservoir), during two periods: the first year after the filling phase and three years later. Our goal was to evaluate the occupation of the new hábitat (Manso Reservoir), by this species, as well as to test the hypothesis that in the reservoir, unlike the natural environment, there are remarkable changes in diet between the periods. Fish were sampled monthly in the floodplain lake and in the reservoir during two annual periods using gillnets. To evaluate the differences in abundance of A. osteomystax we employed the Kruskal -Wallis test, and the diet analysis was carried out using frequency of occurrence and volumetric methods. Temporal differences in the diet were tested by Kruskal-Wallis test using the scores from a detrended correspondence analysis. A. osteomystax was significantly more abundant in the floodplain lake, where the captures were higher than in the reservoir in almost all months analyzed, and significant variations in abundance between the two periods were not recorded in either the reservoir or the floodplain lake. The diet variation between the two periods, which had a time lag of three years between them, was much less pronounced in the natural environment, where the resource availability is essentially regulated by seasonality. Thus, our hypothesis was accepted; that is, the interannual variations in the diet of A. osteomystax are more relevant in an artificial environment than in a natural one. Rev. Biol. Trop. 60 (2): 699-708. Epub 2012 June 01.

Los embalses nuevos ofrecen la oportunidad de comprobar si especies que presentan suficiente flexibilidad en la alimentación en condiciones naturales pueden aprovechar esta situación y, sin restricciones de reproducción, ocupar la mayor parte del hábitat visible en un gran embalse (espacios abiertos), además, presentar un alto éxito en la colonización del nuevo entorno. Asimismo, examinamos variaciones en la abundancia y alimentación de A. osteomystax, en dos ambientes, uno natural (Sinha Mariana floodplain lake) y otro alterado (Embalse Manso), durante dos periodos: el primer ano después de la fase de llenado y tres años más tarde. Nuestro objetivo fue evaluar la ocupación del nuevo hábitat (Embalse Manso) por esta especie, así como probar la hipótesis de que en el embalse, a diferencia del ambiente natural, se producen cambios notables en la dieta entre los periodos. Los peces fueron muestreados mensualmente en el lago de la planicie de inundación y en el embalse durante dos periodos anuales con redes de enmalle. Para evaluar las diferencias en la abundancia de A. osteomystax empleamos la prueba de Kruskal-Wallis, y el análisis de la dieta se llevo a cabo con el uso de la frecuencia de ocurrencia y métodos volumétricos. Las diferencias temporales en la dieta fueron probadas con Kruskal-Wallis, se usaron los resultados a partir de un análisis de correspondencia sin tendencia. A. osteomystax fue significativamente más abundante en el lago de la llanura de inundación, donde las capturas fueron más altas, que en el embalse en casi todos los meses analizados, y no se registraron variaciones significativas en la abundancia entre los dos periodos tanto en el embalse como en el lago de inundación. La variación en la dieta entre los dos periodos, en los cuales habia un desfase de tres anos entre ellos, fue mucho menos pronunciada en el entorno natural, donde la disponibilidad de recursos es esencialmente regulada por la estacionalidad. Por lo tanto, nuestra hipótesis fue aceptada, es decir, las variaciones interanuales en la dieta de A. osteomystax son más relevantes en un ambiente artificial que en uno natural.

Relationship between the structure of zooplankton community and the water level in a floodplain lake from the Pantanal, Mato Grosso State, Brazil / Relação entre a estrutura da comunidade zooplanctônica e o nível da água em uma lagoa de inundação do Pantanal de Mato Grosso, Brasil

The hydrological condition of floodplain systems alters the structure and dynamic of aquatic communities. We suggest that the structure of zooplankton community changes according to the flood phases and connectivity. This study was carried out in a floodplain lake located in the Northern Pantanal (Brazil). Zooplankton density varied considerably over time, although the sampling stations presented similar densities. The densities ranged from 2,000 ind. m-3 in the high water phase to more than 2,300,000 ind. m-3 during the low water phase when the lake remains isolated. The densities of the groups also presented a temporal variation. Rotifers described the community mainly in the low water phase and microcrustaceans during the high water phase. Variations in the total zooplankton and groups densities were significantly correlated to the PCA 1 axis (negatively composed by water depth and positively by turbidity) and to the food availability (phytoplankton).

A condição hidrológica de sistemas inundáveis altera a estrutura e a dinâmica das comunidades aquáticas. Com isso, sugerimos que a estrutura da comunidade zooplanctônica se altera de acordo com as fases da inundação e conectividade. Este estudo foi realizado em uma lagoa de inundação da parte norte do Pantanal (Brasil). A densidade zooplanctônica variou consideravelmente ao longo do tempo, embora as estações amostrais apresentarem densidades similares. As densidades variaram de 2.000 ind. m-3 na fase de águas altas para mais de 2.300.000 ind. m-3 durante a fase de águas baixas quando a lagoa esteve isolada. As densidades dos grupos também apresentaram variação temporal. Os rotíferos foram relativamente mais importantes durante as águas baixas e os microcrustáceos durante a fase de águas altas. Variações na densidade do zooplâncton e grupos foram significativamente correlacionados com o eixo 1 da PCA (composta negativamente pela profundidade da água e positivamente com a turbidez) e a disponibilidade alimentar (fitoplâncton).

Química de elementos-traço nos sedimentos do Lago do Parú (Manacapuru - Amazonas), sob influência do pulso de inundação do baixo Rio Solimões / Trace elements chemical in Lago do Parú (Manacapuru - Amazonas) sediments, under Lower Solimões River flood pulse influence

O objetivo deste estudo foi determinar as concentrações totais e em frações geoquímicas de Fe, Mn, Co, Cu e Zn em sedimentos, coletados nos períodos de seca (2005) e cheia (2006) do Lago do Parú. Nas partículas de sedimento seco ao ar (SSA) < 45 µm foi feita uma extração seqüencial pelo método de Tessier et al. (1979) que separa os elementos nas frações geoquímicas trocável, carbonácea, oxídica, orgânica e residual. As amostras de extrato diluídas foram lidas em cada fração, por espectrometria de absorção atômica de chama, sendo que o Fe apresentou a maior concentração total e uma forte associação com óxidos. O Mn alcançou a maior fração trocável dentre os elementos, em ambas as estações analisadas. O Zn obteve uma fração trocável constante entre os dois períodos analisados. O Cu se caracterizou por apresentar forte ligação pela fração orgânica, não variando de uma estação para outra nesta fração. O Co apresentou comportamento similar ao do Cu, exceto pela fração orgânica que apresentou diferença de concentração entre os períodos, sendo maior na cheia. As análises multivariadas confirmaram que os metais foram movimentados entre as frações geoquímicas do período seco para o de cheia.

The aim of this work was to determine whole and geochemical fractions of Fe, Mn, Co, Cu and Zn concentrations from sediments collected at low (2005) and high (2006) water seasons in Lago do Parú. From < 45 µm air dried sediment particles was made a Tessier et al. (1979) method to sequential extraction, which separates elements in exchangeable, bound to carbonates, bound to iron and manganese oxides, bound to organic matter and residual geochemical fractions. Diluted samples were read in each fraction, by flame atomic absorption spectrometry, where Fe showed the highest whole concentration and strong association with oxides. Mn reached the biggest exchangeable fraction among elements in both analyzed periods. Cu showed strong association by organic fraction and don't presented difference of concentration between periods. Co presented similar behavior of Cu, except for organic fraction, in which showed difference between periods, where was bigger in high water level period. Multivariate statistical analyses confirmed that metals were displaced in sediments geochemical fractions at low and high water seasons.

Composição do Zooplâncton em diferentes ambientes do lago Camaleão, na ilha da Marchantaria, Amazonas, Brasil

This study aims to verify occurrence and distribution of the major zooplankton groups in three different sub-habitats at Lago Camaleão: channel, aquatic macrophytes and flooded forest, during the high water period (August, 1996). Cladocera, Copepoda and Rotifera occurred with different relative abundances within the three studied environments. In the channel, Cladocera occurred with a high number of species and individuals, Bosminopsis deitersi being the dominant species (89%). Cladocera and Copepoda were equally dominant in the flooded forest, even thought only copepods, nauplius and copepodites immature forms were found. On the macrophytes, Rotifera was the group with the largest occurrence, with the dominance of Lecane quadridentata, Keratella Americana and Brachionus patulus followed by copepods (immature forms) and cladoceres, the latter mostly of the Chydoridae family (21.4%).

Este trabalho teve o objetivo de verificar a ocorrência e a distribuição dos principais grupos de zooplâncton em três diferentes sub-habitats do lago Camaleão: canal, macrófitas aquáticas e floresta alagada, no período de cheia (agosto de 1996). Nos três ambientes estudados, Cladocera, Copepoda e Rotifera ocorreram com abundância relativa diferentes. No canal, Cladocera ocorreu com maior número de espécies e de indivíduos, sendo dominante a espécie Bosminopsis deitersi (89%). Na floresta alagada Cladocera e Copepoda foram igualmente dominantes, ressaltando-se que somente ocorreram as formas imaturas de copépodes, náuplios e copepoditos. Nas macrófitas, o grupo de maior ocorrência foi Rotifera, com a dominância de Lecane quadrídentata, Keratella americana e Brachionus patulus seguido de copépodes (formas imaturas) e de cladóceros, estes na maioria da família Chydoridae (21.4%).

Consumo de pescado e outros alimentos pela população ribeirinha do lago grande de monte alegre, pa - brasil

The present study shows the results on the fish consumption and other food itens by the riparian population from Monte Alegre Lake, Lower Amazon, in Pará State, Brazil. The data were colected monthly during two years jointly with 35 families from 17 fishery communities that practice the fishery with a subsistence or commercial goal, as well as families that not fish. The mean fish consumption was of 369 g/capita/day complemented with 6.1 g/capita/ day of fish flouer, called locally "piracuí". The species preferred were curimatá (Prochilodus nigricans) and acarí-bodó (Liposarcus pardalis). Manioc flouer consumption was higher than in other regions. Families consume fish each 6 days a week. Extrapoling for all population of Lago Grande de Monte Alegre, the fish consumption is more than 3 t/day and about 1,114 t/year.

O presente artigo apresenta resultados sobre o consumo de pescado e outros alimentos pela população ribeirinha do Lago Grande de Monte Alegre, no Estado do Pará, Brasil. Os dados foram coletados mensalmente, por um período de dois anos juntos a 35 famílias de 17 comunidades, que praticam a pesca com fins comerciais e de subsistência, bem como as famílias que nào pescam. O consumo médio de pescado foi de 369 g/capita/dia, complementado com 6,lg/capita/dia de farinha de peixe (piracuí). As espécies mais consumidas foram: curimatá (Prochilodus nigricans) e acarí-bodó (Liposarcus partialis). Em média, as famílias tiveram alguma refeição constituída de pescado em 6 dias de cada semana. Extrapolando para toda a população do Lago, o consumo diário de pescado é pouco mais de 3 t, chegando a 1.114 t/ano.