Planktonic indices in the evaluation of the ecological status and the trophic state of the longest lake in Poland

Due to the intensive mixing polymictic lakes should be homogenous. However, morphometric diversity and high water dynamics contribute to the differentiation of many parameters in various areas of the lakes. This study analyzes both phytoplankton and zooplankton to assess differences in water quality along the north–south axis of the longest lake in Poland. New phytoplankton indicators were applied for determining the lake's ecological status: the Q index based on functional groups and the PMPL (Phytoplankton Metric for Polish Lakes) index based on phytoplankton biomass. TSI_ROT index (Rotifer Trophic State Index), which comprises the percentage of species indicating a high trophic state in the indicatory group and the percentage of bacteriovorus in the Rotifera population, was used for zooplankton analysis.TP content was different at different sites – we observed its gradual increase from the south to the north. Spatial variation of phosphorus did not considerably affect plankton diversity. The phytoplankton was dominated by Oscillatoriales, typical of shallow, well-mixed eutrophic lakes. The ecological status of the lake based on the EQR (Ecological Quality Ratio) was poor or moderate. The zooplankton was dominated by rotifers (at almost all sites), which indicates a eutrophic state of the lake. The values of phytoplankton indices at the studied sites did not differ considerably; the differences resulted more from local conditions such as the contaminant inflow and the macrophyte development than water dynamics.We have demonstrated that in the lake dominated by filamentous Cyanobacteria the ecological status should be determined according to the PMPL index or other indices dependent on the dominant Cyanobacteria species. Since the Q index does not include the functional group S1, the results can lead to the false conclusion that water quality improves with an increased amount of phytoplankton. The high abundance of Cyanobacteria in the lake may have contributed to the poor growth of rotifers.     

Distribution of mitochondrial DNA variation in lake sturgeon (Adpenser fulvescens) from the Moose River basin, Ontario, Canada

We analysed mitochondrial DNA (mtDNA) variation of lake sturgeon ( Adpenser fulvescens ) from the Moose River basin. Our objective was to address various proximate and ultimate factors which may influence the distribution of lake sturgeon mtDNA haplotype lineages in this watershed. The lake sturgeon sampled were characterized by only two mtDNA hapiotypes based on a restriction fragment length polymorphism analysis with 40 restriction endonucleases and direct sequencing of 275 nucleotides in the mtDNA control region. We detected no heterogeneity in the mtDNA haplotype frequencies of lake sturgeon captured from different sites within rivers including those separated by major hydroelectric installations. However, lake sturgeon from one tributary had significantly different haplotype frequencies than those from other tributaries suggesting that they composed a discrete genetic stock. These results suggest that gene flow among most sites is significant and is an important factor affecting the distribution of mtDNA variation in this species. The genetic structuring and diversity are discussed in relation to lake sturgeon management and conservation.     

An ecological study of the macrophytic vegetation of the Doodhadhari Lake,Raipur, M. P., India 1. Distribution and seasonal change in aquatic plants

Summary The distribution of aquatic plants in Doodhadhari lake, Raipur, M.P., India was studied by establishing eight stations. Permanent belt transects were run from all these eight stations every month for a year to assess the seasonal change in vegetational composition. Each transect was taken from the shore to the maximum depth. A contour survey was made and the total area during different seasons were determined. The fluctuation of water level was marked almost every fortnight for a year. The percentage frequency and percentage cover of different species were found to exhibit significant changes during different seasons. Except a few submerged aquatic plant species which are perennial all other species appear and disappear as the seasons progress. The perennial species which are not much affected by the seasonal change are heavily eaten by cattles. The pattern of succession has been outlined after evaluating the changes.     

Further discussion about the features of Lake Puma Yum Co, South Tibet, China

Further discussion about the limnological features of Lake Puma Yum Co, South Tibet, China, is provided based on the results of several investigations. By using depth data from all over the lake, the whole submarine topography has been compiled. Horizontal analysis of the water's physicochemical features indicates that compared with the relatively uniform water features at other lake areas, apparent spatial heterogeneity exists in the water of the subaquatic alluvial fan induced by the Jiaqu River, the biggest inflow. Vertical analysis of water characteristics using two-factor analysis of variance with no re-experiment indicates that temperature, dissolved oxygen, and pH of the water vary with water depth rhythmically, whereas other parameters demonstrate no evident vertical variation, which shows that chemical stratification is not obvious. But this does not exclude slightly higher concentrations of Ca²⁺ induced by lower pH at the bottom of deep lake water. The hydrochemistry difference between inflow water and lake water reveals the loss of Ca²⁺ in lake water, which indicates calcite deposition may be an important characteristic of lake sediment.     

Patterns of β‐diversity in a Mexican tropical dry forest

Abstract. Patterns of β‐diversity in a highly diverse tropical dry forest tree community are described; the contribution of environmental heterogeneity and distance to β‐diversity was assessed. Significant differences in elevation, insolation, slope and soil water holding capacity (p < 0.01), variables related to water availability, were found among 830 m × 100 m transects laid along contrasting slopes of a system of three parallel microbasins. A gradient in elevation and insolation was found within north‐facing transects, among 10 m × 10 m sites; south‐facing transects showed an elevation gradient while crest transects showed a gradient in water holding capacity. In total 119 species were registered, with 27 to 64 species per transect, and 4 to 16 species per site. A large β‐diversity was found among and within transects; two indices of β‐diversity consistently showed a higher β‐diversity within transects than among them. Among transects, 64% of the variance in species composition could be attributed to the environmental variables; an additional 22% to the spatial distribution of sites. Within transects, 42% of the deviance in β‐diversity values was explained by insolation, and 19% by distance. β‐diversity increased with distance and with difference in insolation among sites; north‐facing transects, those with most contrasting insolation conditions, had the steepest increase in β‐diversity with distance. Such increase was clearly associated with changes in species composition, not with changes in species richness.     

三峡水库运行期间原生动物群落的时空异质性

于2010年10月—2011年6月三峡水库正常运行周期内对库区干流原生动物进行调查,研究其空间分布及水库周期排蓄期间的变化。共检测到原生动物99种,蓄水后纤毛虫有增多的趋势。水库运行的不同阶段优势种不同,大致演变为:砂壳纤毛虫(蓄水期)—非砂壳类纤毛虫(高位运行期间)—有壳肉足虫(低位运行期间)。不同水域优势种也存在差异,从上游到下游特征指示种变化为:有壳肉足虫(变动回水区)—纤毛虫(湖泊区)。结果表明,三峡水库原生动物的分布具有明显的时空异质性(P0.05),影响原生动物时空分布的主要因素有透明度、温度、电导率和叶绿素a。原生动物平均密度为952.19个/L,平均生物量为8.14μg/L。蓄水期上游现存量高于下游,低位运行期间则低于下游。原生动物Marglef和Shannonn-Weiver多样性指数平均值分别为3.78和2.18,1月份最低,6月份最高。蓄水175 m后上游变动回水区原生动物具有较高的丰度。水库冬蓄夏排的运行模式模糊了河流本身的季节变化,使原生动物的种类和现存量更多的受水库水动力学的影响,使水体理化因子和水文特征呈现明显的时空差异,最终形成原生动物种群的时空异质性分布。     

Aggression Level in Different Water Velocities Depends on Population Origin in Grayling, Thymallus thymallus

Phenotypic plasticity is recognized as an important mechanism of adaptation. However, because of its potential costs and limits, it has been hypothesized to be reduced and ultimately become lost when there is no selection for its maintenance. Heterogeneous environments in particular are expected to favour and thus maintain plastic phenotypes. Lakes and rivers differ in their flow regimes. In addition to higher average water velocity, rivers are characterized by distinct spatial and temporal variation in water flow, whereas lakes can be regarded as quite uniform in this respect. We studied whether behaviour, which is generally considered to be highly plastic, shows differences in the degree of plasticity between lake and river populations of the European grayling, Thymallus thymallus, fry in response to different water velocities. Given that aggressive behaviour in fish has been shown to relate to ambient flow regime, we compared aggressiveness of hatchery‐reared grayling originating from hatchery stocks of two lake and two river populations in still and flowing water. River fish showed higher aggressiveness in flowing water compared with still water, whereas aggressiveness of lake fish did not appear to vary according to water velocity. The higher plasticity of aggressiveness evoked in river fish by different water velocities may thus represent an adaptation to more variable flow and presumably related feeding conditions in their natural environment.     

Comparative limnology of a deep-discharge reservoir and a surface-discharge lake on the Madison River, Montana

SUMMARY. Phytoplankton standing crop, primary production, light penetration, temperature, and various chemical concentrations were measured in a man-made, deep-discharge, reservoir and in a natural, surface-discharge, lake in order to relate limnological conditions in the two bodies of water to their depth of outflow. The quantity and depth distribution of heat stored during the summer varied markedly. The reservoir functioned as a heat trap, whereas heat was readily dissipated from the lake. Salinity increased more in the lower layer of the lake. Throughout the summer, nutrient-rich water was discharged from the reservoir whereas nutrient-poor water was discharged from the lake. Phytoplankton standing crops were greater in the lake and were dominated by flagellates and diatoms. In the reservoir, blue-green algae were predominant. Rates of primary production and respiration were higher in the lake, but estimated algal turnover times were faster in the reservoir. It was concluded that depth of outflow has a direct and predictable effect on certain physical and chemical conditions within these two bodies of water; but effects of discharge depth on phytoplankton were secondary and thus difficult to ascertain.     

Environmental variation,vegetation distribution,carbon dynamics and water/energy exchange at high latitudes

Abstract. The responses of high latitude ecosystems to global change involve complex interactions among environmental variables, vegetation distribution, carbon dynamics, and water and energy exchange. These responses may have important consequences for the earth system. In this study, we evaluated how vegetation distribution, carbon stocks and turnover, and water and energy exchange are related to environmental variation spanned by the network of the IGBP high latitude transects. While the most notable feature of the high latitude transects is that they generally span temperature gradients from southern to northern latitudes, there are substantial differences in temperature among the transects. Also, along each transect temperature co‐varies with precipitation and photosynthetically active radiation, which are also variable among the transects. Both climate and disturbance interact to influence latitudinal patterns of vegetation and soil carbon storage among the transects, and vegetation distribution appears to interact with climate to determine exchanges of heat and moisture in high latitudes. Despite limitations imposed by the data we assembled, the analyses in this study have taken an important step toward clarifying the complexity of interactions among environmental variables, vegetation distribution, carbon stocks and turnover, and water and energy exchange in high latitude regions. This study reveals the need to conduct coordinated global change studies in high latitudes to further elucidate how interactions among climate, disturbance, and vegetation distribution influence carbon dynamics and water and energy exchange in high latitudes.     

Molecular genetic examination of the polymorphic Arctic charr Salvelinus alpinus of Thingvallavatn, Iceland

Thingvallavatn, Iceland contains two sympatric morphotypes (benthic and limnetic) of Arctic charr Salvelinus alpinus. Each morphotype is composed of two morphs and these differ markedly in ecology, behaviour and life history. We used molecular genetic approaches to test whether (i) genetic heterogeneity exists among morphs and (ii) if morphs arose in allopatry and came into secondary contact or arose sympatrically within the lake through genetic segregation and/or phenotypic plasticity. Direct sequencing of 275 bp of the mitochondrial DNA (mtDNA) control region, mtDNA restriction fragment length polymorphisms and single locus minisatellite analyses detected insufficient variation to test our hypotheses. Analysis of multilocus minisatellite band sharing detected no significant differences between morphs within the same morphotype. However, significant differences among morphs belonging to different morphotypes suggest some genetic heterogeneity in Thingvallavatn charr. Limnetic charr from Thingvallavatn were more similar to sympatric benthic charr than to allopatric limnetics from two other Icelandic lakes. This suggests that the Thingvallavatn morphs arose sympatrically within the lake rather than in allopatry followed by secondary contact.     

普者黑岩溶湖泊湿地湖滨带景观格局演变对水质的影响

湖滨带作为湖泊与陆地之间的过渡带,是健康湖泊生态系统的重要组成部分。湖滨带景观格局的演变会对湿地水质产生重要影响,因此探究影响岩溶湿地水质变化的湖滨带关键景观因子,对深入了解景观格局对岩溶湿地水质的影响过程与机制具有重要意义。选择普者黑岩溶湖泊湿地为研究对象,以2005、2007、2009、2011年共4年的Landsat遥感影像及水质监测数据为基础,通过划定湖泊湿地湖滨带缓冲区域,运用秩相关分析和冗余分析研究湖滨带景观格局对普者黑岩溶湖泊湿地水质的影响。结果表明,湖滨带不同缓冲区内景观结构类型比例差异较大;枯水期水质与土地利用类型和景观格局指数的影响大于丰水期;景观格局在不同缓冲区尺度对岩溶湿地的水质具有不同的效应;随着监测点缓冲距离的增加,个别景观指数可较好的揭示湖滨带景观格局演变对岩溶湿地水质的影响,其中,蔓延度指数(CONTAG)、斑块结合度指数(COHSION)、均匀度指数(SHEI)对水质参数的影响较大,边界密度(ED)、聚集度(AI)对水质参数的影响随缓冲距离的增加逐渐减弱,其他景观指数对水质影响差异并不明显,最大斑块指数(LPI)在缓冲距离≤300m的区域内与水质的关系较密切,面积加权平均斑块分维数(AWMPFD)与水质参数有显著负相关性,多样性指数(SHDI)对水质的影响具有不确定性;另外,大部分水质参数与土地利用面积比例有较好的相关性,且湿地面积比例是表征岩溶湖泊湿地水环境质量的主要指标。     

Delineation of vegetation shaded ox-bow lakes in Ganges flood plain,India

Floating vegetation cover over the ox-bow lake withstands against its sharp delineation. A good many spectral indices are successfully used for water body delineation. But how far these are applicable in vegetation-shaded ox-bow lakes is a research question. The study also aimed that if the existing indices are not satisfactory and how a new index could be endorsed for resolving the problem. The study additionally monitored the ox-bow lake and vegetation cover area from 1991 to 2021 based on Landsat satellite images.Normalized differences water index (NDWI), Modified NDWI (MNDWI), Re-modified NDWI (RmNDWI), and Normalized Difference Vegetation Index (NDVI) spectral indices were used for delineating ox-bow lakes and multiple accuracy test measures revealed that these are not highly satisfactory. Vegetation inclusive aggregated water index (ViAWI) was built by coupling mentioned spectral indices with the vegetation index and the ensemble map was found more accurate.Monitoring the ox-bow lake area clearly showed that these declined in the last 30 years irrespective of the historical drainage modification legacy of the major rivers to which the ox-bow lakes belonged. Aquatic vegetation cover within ox-bow lakes changed dynamically.The endorsed ViAWI would be a good approach for resolving wetland delineation shaded with floating vegetation and it could be used in other regional units worldwide. Quantitative information regarding ox-bow lake and vegetation cover within ox-bow lakes would be valuable data support for adopting ox-bow lake conservation and restoration planning.     

Habitat diversity and ostracod distribution patterns in Belarus

Ostracod diversity and abundance was studied in 10 different types of water bodies of Belarus (bogs, brooks, canals, oxbows, ponds, reservoirs, rivers, springs, shoal of lake and temporary pools). Hydrochemical variables, sediment, and vegetation were analyzed. In total 156 different localities were investigated. Habitat diversity was based mainly upon the closely correlated hydrochemical variables of mineralization (hardness total and carbonate, conductivity, total value of dissolved substances), although bottom, vegetation characteristics and other factors (pH, dissolved oxygen, nutrients) were also significant. The ostracods found included 62 species in 27 genera comprising 8 cosmopolitan, 17 Holarctic, 13 Palearctic species; 21 of these species are known from central and southern Europe and adjacent areas, while 3 are characteristic for eastern Europe. The distribution of freshwater ostracod assemblages reflected the habitat and depended on water body type. Heterogeneous oxbows and temporary pools supported 37 species, while other types of pool maintained only 27–14 species. The population density of different species varied from 0.5 to more than 10 000 ind./m². Indices of local alpha diversity were significantly correlated with the number of species and temperature and were maximal in heterogeneous habitats. The variation of population density was not connected with habitat patterns but appeared to be regulated by the biotic interactions in the community. Habitat diversity, verified by the beta-diversity indices, enabled us to find localities with a similar heterogeneity level and species richness. Beta-diversity values were independent of species number as well as abundance but a significant positive correlation (p < 0.05) was found with temperature, pH and dissolved oxygen. This index probably reflected the general patterns of different localities.     

Variation in spatial and temporal gradients in zooplankton spring development: the effect of climatic factors

1. We examined the temporal and spatial heterogeneity of zooplankton in lake surface waters during the spring of 3 years in Lake Washington, U.S.A., a large lake with a high production of sockeye salmon fry. 2. We show large within‐season and among‐year variation in the horizontal distribution of temperature, chlorophyll a concentration, and zooplankton in the lake. The main pattern, a delay in zooplankton population increase from the north‐ to the south‐end of the lake, recurred in each year and was persistent within each spring. 3. The delay is primarily caused by the development of a temperature gradient during spring warming, as cold mountain water enters the south end of the lake, while warm water enters the north end via a river draining a nearby lake. Climate factors, such as air temperature and precipitation during winter and spring, appear to influence the extent of the delay of zooplankton increase. 4. If the climate continues to warm, the temporal disconnection in zooplankton development between lake areas immediately influenced by cold river inflow and areas that are influenced by spring warming may increase in magnitude. Thus, the different areas of the lake may not contribute equally to fish production.     

The Characteristics of Foliar δ 13C Values of Plants and Plant Water Use Efficiency Indicated by δ13C Values in Two Fragmented Rainforests in Xishuangbanna,Yunnan

The foliar δ13 C values of 226 plant species sampled from 7 transects belonging to 2 rainforests (named Chengzi and Bubeng, respectively) in Xishuangbanna of Yunnan Province, China were analyzed. The characteristics of foliar δ13 C values and water use efficiency (WUE) of plants indicated by δ13 C values in this region were studied. In the mean time, the average foliar δ13 C values of plants in different transects and with different growth forms (i.e., tree, shrub, herb and liana) were compared. The results showed that: 1. the foliarδ13 C value in Xishuangbanna, ranging from -3.865%--2.760%, was similar to those of other typical rainforests in the world (Amazon and Puerto Rico, for instance), which indicated that the rainforests in this region had the typical characteristics of rainforests of the world; 2. there were significant differences between Chengzi and Bubeng in average foliarδ13 C values, with the latter being lower than that of the former; significant differences also existed between different transects in the same forest, which indicated that water conditions and orientation of transects might have resulted in these differences; 3. the average foliarδ13 C value of evergreen plants was significantly lower than that of deciduous plants, and there also existed significant differences between different growth forms, implying that the WUE of these plant species was also quite different.      

GENETIC STRUCTURE OF GEOGRAPHICALLY MARGINAL POPULATIONS OF PONDEROSA PINE

Eleven populations of ponderosa pine (Pinus ponderosa) located on an east-west transect of the Palmer Divide of Central Colorado were studied. Within each population transects of approximately 20 × 250 m were established. In seven populations the transects represented contrasting ecological conditions such as north and south facing slopes. Within each transect 200–250 trees greater than 10 cm in height were tagged, their locations mapped, their ages determined and their diameters and heights measured. Electrophoretic analyses of mature needle tissue indicated that while most of the allozyme variation resided within transects, significant genetic heterogeneity could be found between populations and transects. Among populations consistent patterns of genetic variation were observed at only two loci. Five of the 13 loci had consistent but very small differences between transects within populations. Considerable genetic heterogeneity occurred among 20 m sections of the transects and among age classes within transects. The genetic structure of these populations can be explained by mosaic patterns of seedling recruitment characteristic of these ponderosa pine stands. Only a few maternal trees contribute to each patch of seedlings, and this localized founder effect produces the genetic structure observed in these populations.     

Spatial variation in vegetation structure coupled to plant available water determined by two-dimensional soil resistivity profiling in a Brazilian savanna

Tropical savannas commonly exhibit large spatial heterogeneity in vegetation structure. Fine-scale patterns of soil moisture, particularly in the deeper soil layers, have not been well investigated as factors possibly influencing vegetation patterns in savannas. Here we investigate the role of soil water availability and heterogeneity related to vegetation structure in an area of the Brazilian savanna (Cerrado). Our objective was to determine whether horizontal spatial variations of soil water are coupled with patterns of vegetation structure across tens of meters. We applied a novel methodological approach to convert soil electrical resistivity measurements along three 275-m transects to volumetric water content and then to estimates of plant available water (PAW). Structural attributes of the woody vegetation, including plant position, height, basal circumference, crown dimensions, and leaf area index, were surveyed within twenty-two 100-m² plots along the same transects, where no obvious vegetation gradients had been apparent. Spatial heterogeneity was evaluated through measurements of spatial autocorrelation in both PAW and vegetation structure. Comparisons with null models suggest that plants were randomly distributed over the transect with the greatest mean PAW and lowest PAW heterogeneity, and clustered in the driest and most heterogeneous transect. Plant density was positively related with PAW in the top 4 m of soil. The density-dependent vegetation attributes that are related to plot biomass, such as sum of tree heights per plot, exhibited spatial variation patterns that were remarkably similar to spatial variation of PAW in the top 4 m of soil. For PAW below 4 m depth, mean vegetation attributes, such as mean height, were negatively correlated with PAW, suggesting greater water uptake from the deep soil by plants of larger stature. These results are consistent with PAW heterogeneity being an important structuring factor in the plant distribution at the scale of tens of meters in this ecosystem.     

Seasonal variation of the planktonic population in lake yunoko,as followed by the assay of chlorophyll,protein, RNA and DNA in the total harvested planktonic samples

Seasonal variation of the biomass of plankton in Lake Yunoko, a eutrophic lake in Japan at an altitude of 1478 in, was followed by measuring simultaneously the quantities of chlorophyll, protein, RNA and DNA in water samples harvested from different depths at a definite site in different seasons of a year. The contents of the four cellular constituents and the sum of them in a given water column showed characteristic seasonal changes during the year. Various ratios derived from the four contents were grouped into two distinct types; one is the winter-spring type and the other the summer-autumn type. It was found that the sum of the four contents and the ratio of the protein-content to the RNA-content were quantitatively related to the chlorophyll-content of the water. Based on the assumption that a certain water sample contained only photosynthetic plankton, analyses were made to estimate the proportions of photosynthetic and non-photosynthetic plankton to the total planktonic mass, the growth rates of these plankton, and the net productivity of the lake.     

过水性湖泊自净能力的动态变化

通过对过水性湖泊骆马湖1991—2003年出、入湖口附近主要水质指标监测资料的分析,研究了湖泊湿地自净能力的变化情况。结果表明:1991—2003年,各采样点水质指标无显著变化,但出、入湖口水质差异显著,表明骆马湖目前尚有较强的自净能力;各采样点间主要水质指标的变异系数逐渐减小,表明湖泊对水体总氮、溶解氧、挥发酚、非离子氨、砷等主要富营养化物质和污染物的净化能力不断减小,湿地生态系统的自净能力显著下降。总氮、溶解氧及部分外源污染物指标在不同采样点间的变异系数可作为湿地生态系统自净能力与健康状况的重要参考指标。     

Formation,Transport and Retention of Aggregates in a River‐Lake System (Spree,Germany)

The formation, particle size distribution, structure and retention of aggregates were studied in a river‐lake system of the lowland River Spree and factors influencing these processes were evaluated. Samples were taken from the inflow and outflow of a flushed lake, as well as along the adjacent flowing reach of the River Spree, between April 2001 and May 2002. The aim was to record the influence of the seasons and different turbulence intensities on the size, shape, composition, abundance and transport properties of the particles. As additional parameters, the phytoplankton biomass, the concentration of suspended particulate matter, the concentrations of nutrients and the discharge were measured. The abundance of the particles showed a strong seasonality in the investigated period, which closely correlated with the concentrations of suspended particulate matter and particulate organic matter in the water column. The organic carbon content of the suspended matter varied between 37% (dry weight) in summer and about 14% in winter. The concentration of particles ranged between 500 and 2500 particles/ml. The number of particles was significantly lower upstream from the lake than at the downstream transects. The majority of the aggregates in the River Spree were smaller than 500 µm, most of the particles even showing a diameter less than 50 µm. Many particles, above all algae, were washed out of the lake Neuendorfer See into the adjacent flowing reach of the River Spree. Algae influenced the abundance of the particles and contributed to the formation of aggregates with their stickiness. In the river flowing section large particles were formed by turbulence structures, whilst simultaneously the number of smaller particles decreased in the water column caused by aggregation processes. In general, an increasing flow velocity and discharge rate resulted in a larger amount of aggregates in the water column. On the other hand, particle abundance was reduced in the flow direction when the flow velocity was low. Under these conditions particles were retained by sedimentation and benthic filter‐feeding. (© 2005 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)