Decomposition of protein compounds in an eutrophic lake: spatial and temporal distribution of exopeptidase and endopeptidase activities in various size fractions

Activities of exopeptidases and endopeptidases in various size fractions and the possible regulation of these enzymes in response to the changes in substrate concentrations were studied. The endopeptidase activities were determined using a protein substrate labelled with a fluorochrome. Among the enzyme activities studied only leucine aminopeptidase and endopeptidase activities were recorded. The protein compounds did not seem to cleave by synergistic endo and exoenzyme mechanisms. The inhibitory effect of ethylenediamine tetraacetate (EDTA) and phenylmethylsulfonile fluoride (PMSF) suggested a high proportion of metallo-proteases and serine-proteases. The inhibitory profile at 1 and 5 m indicated that planktonic organisms probably produced the same type of proteases, whereas enzymes present in the 0–1.2 and 1.2–100 μm fractions were not similar. The mean percentages of aminopeptidase activity at 1, 5 and 14 m in the dissolved fraction were 12.5, 12.7 and 18.4%. This enzyme activity was low in the 0.2–1.2 μm fraction (12.1% at 1 m, 13.3% at 5 m and 19.1%, at 14 m) compared to that measured in the 1.2–100 μm fraction, whereas the average percentages of endopeptidase activities in this fraction were 50.9% at 1 m, 50.1% at 5 m and 53.5% at 14 m. The bacteria attached to particles had a higher specific activity than free-living bacteria. It was 11.7 times higher than the enzyme activity associated with larger free-living bacteria and 112.3 times higher than the activity of small free-living bacteria. In this study, the specific activity of the aminopeptidase (activity in the fraction 0.2–100 μm per number of bacteria) was correlated with Chl a at 1 m (r = 0.65, P <0.01), 5 m (r = 0.78, P <0.001) and 14 m (r = 0.96, P <0.001). The production of protein compounds by the phytoplankton could therefore regulate aminopeptidase activity. This revised version was published online in July 2006 with corrections to the Cover Date.     

Dynamic of phytoplankton size-class and photosynthetic activity in a tropical hypereutrophic lake: the Yaounde municipal lake (Cameroon)

This study carried out within the framework of a multi-disciplinary project, aimed at highlighting the fundamental processes governing the functioning of the hypertrophic Yaoundé Municipal Lake. It was based on the hypothesis that, even within a small range of lake trophic status, important variations can occur in the species composition, biomass and photosynthetic activity of the phytoplankton size-fractions. For this purpose, samples were taken at weekly intervals from November 1996 to December 1997 at a fixed set of depths in the water column. Spatial-temporal fluctuations of some physical–chemical variables, associated with biological variables such as phytoplankton size-class species composition, phytoplankton size-class biomass, phytoplankton primary production and chlorophyll-a were analysed. The water transparency was low and rarely exceeded 100 cm. Conductivity values relatively higher increased generally from the top to the lake bottom. The oxygen deficiency, and sometimes anoxia, recorded from 2.5 m depth resulted in high quantities of ammonium nitrogen. Total phosphorus and total Kjeldahl nitrogen concentrations were characteristics of hypertrophic lakes. The fertility of this biotope favoured the development of a high phytoplanktonic community with remarkable physiological adaptations to the variations of the nutritive potentials of the lake, characterized by the size-structure of these organisms. Cells of small size (<12 μm) contributed up to 11.42% of the total phytoplanktonic biomass. Species with average size (12–45 μm), dominated by Chlamydomonas spp., represented a more significant contribution reaching up to 69.85%, whereas the cells of big size (>45 μm), mainly Euglenophyta, maintained the relatively most important biomass, accounting for up to 89.85% of the total phytoplanktonic biomass. Chlorophyll-a concentrations are among the highest reported for both fresh water and sea water, being a consequence of high proportions of Chlorophyta and Euglenophyta. This led to intense phytoplanktonic photosynthetic activity which continued throughout the year, even though it was confined to the upmost first meter of the water column. Analyses pointed out the allogenic nature of the functioning of this urban lake ecosystem, due to a poor waste management on the surrounding landscape. Handling editor: J. Padisak     

Decay of proteinase and peptidase activities of human and rabbit erythrocytes during cellular aging

Variations in activity of the membrane-bound and cytosolic proteinases and peptidases were analyzed in human and rabbit erythrocytes at various stages of their life-span. The patterns observed with human erythrocytes were the following. (a) The acidic endopeptidase activity associated with the membranes undergoes a substantial decline during cellular aging, with an estimated half-life of 65 days. Concomitantly it appears to become progressively more latent. (b) All cytosolic proteinase and peptidase activities described previously (Pontremoli, S., Melloni, E., Salamino, F., Sparatore, B., Michetti, M., Benatti, U., Morelli, A. and De Flora, A. (1980) Eur. J. Biochem. 110, 421–430) decline exponentially throughout the erythrocyte life-span, with the exception of dipeptidyl aminopeptidase III. The calculated half-lives were: 60 days for the neutral endopeptidase; 87 days for the total acidic endopeptidase activity which is accounted for by three distinct enzymes; 49 days for aminopeptidase B and 133 days for a second aminopeptidase with broad substrate specificity; 84 days for dipeptidyl aminopeptidase II. The results obtained with the rabbit erythrocytes were: (a) no significant decline of leucine aminopeptidase, dipeptidyl aminopeptidase II and III activities in the transition from reticulocytes to mature erythrocytes; (b) very limited decline of aminopeptidase B activity; (c) a pronounced age-dependent decay, in increasing order, of neutral endopeptidase, aminopeptidase A, carboxypeptidase and acidic endopeptidase activities.     

Seasonal variations of microphytoplankton assemblages and environmental variables in the coastal zone of Bozcaada Island in the Aegean Sea (NE Mediterranean Sea)

Seasonal changes in the microphytoplankton assemblages were examined in the coastal zone of Bozcaada Island with regard to some major physical and chemical variables. Samples were collected from May 2000 to December 2001 at four stations. A total of 108 dinoflagellates, 102 diatoms, 1 chrysophycean, 3 dictyochophycean, and 1 prasinophycean species were identified and quantified during the study period. Diatoms and dinoflagellates were the most important in terms of species number and abundance. The maximum values of total microphytoplankton were observed at 0.5 m depth (46.2 × 10³ cells l⁻¹ at st. 3) in May as this was the month when the diatom Pseudo-nitzschia pungens bloomed. Chlorophyll (chl) a concentration ranged between 0.08 (August) and 0.78 μg l⁻¹ (February). May was another important month in which chlorophyll a increased (0.41–0.47 μg l⁻¹). Species diversity values (H′_log2) ranged from 1.66 bits (June, 20 m) to 4.11 bits (November, 0.5 m). The increase was attributed to a more balanced distribution of abundance among species. The amounts of nitrate + nitrite (0.6−3.7 μg-at N l⁻¹), phosphate (0.2−0.6 μg-at P l⁻¹) and silicate (0.7−2.5 μg-at Si l⁻¹) were recorded on each sampling occasion. Nutrient concentrations and chl a values of the research area were found to be poorer than those of the many other coastal areas in the northeastern Mediterranean. The mean atomic ratio of nitrogen to phosphorus varied from 1.3 (June) to 12.9 (February). This ratio was lower than the Redfield ratio of 16 for ocean phytoplankton, and phytoplankton was potentially limited by nitrogen for most of the months. The result of this study confirms and emphasizes the oligotrophic nature of the eastern Mediterranean.     

Presence or absence of picophytoplankton in the western Ross Sea during spring 1994: a matter of size definition?

The occurrence of picophytoplankton in the Ross Sea was investigated during the cruise ROSSMIZE leg 1 (November/December 1994) using epifluorescence microscopy. This study was focused on the methodological aspects dealing with size definition of picophytoplankton. The results showed that a small difference (1 μm) in the definition of the upper size limit of picophytoplankton (2.0 vs 3.0 μm) may have significant implications for the relative importance of this component in the Ross Sea ecosystem. Moreover, the lack of correlation between autotrophs 0.2–2 μm in size and larger autotrophic cells (2–3 μm) in the marginal ice zone and in the closed pack-ice zone suggests that these two components have different ecological roles that are emphasized in these environmental conditions. Received: 25 August 1997 / Accepted: 5 January 1998     

Experimental evidence for interactions between bacterial peptidase and alkaline phosphatase activity in the Baltic Sea

From the observed pattern of aminopeptidase and alkaline phosphatase activities in the Baltic Sea, the question arose whether there is an interaction between the activities of both enzymes. In experiments with 0.8 m filtered seawater, the effects of commercial alkaline phosphatase on bacterial aminopeptidase, the effects of commercial peptidase on bacterial alkaline phosphatase activity (APA), and the effects of proteins, carbohydrates and inorganic nutrients on the activities of both enzymes were investigated.Addition of commercial alkaline phosphatase stimulated bacterial aminopeptidase activity and, similarly, the addition of commercial peptidase increased the APA in bacteria. The proteins, albumin and casein, stimulated aminopeptidase activity and APA simultaneously. Experiments using ammonium and glucose suggested that stimulation of APA by peptidase could be mediated by nitrogen and carbon availability. There were also some indications that stimulation of aminopeptidase activity by alkaline phosphatase functioned by catalysing phosphate release from organic phosphorus compounds.     

Influence of Region-Specific Alterations of Neuropeptidase Content on the Catabolic Fates of Neuropeptides in Alzheimer's Disease

Abstract: We established the cartography of 11 exo- and endopeptidases in the frontal and parietal cortices and in the cerebellum of brains of patients diagnosed with a senile dementia of the Alzheimer's type (SDAT). Comparison with those of four subjects who had died without known neurologic or psychiatric illness indicated that there existed a region-specific alteration of the peptidase contents in the disease. In the frontal area of SDAT brains, postproline dipeptidyl aminopeptidase and aminopeptidase M activities were significantly reduced. In the parietal cortex of SDAT brain, activities of three additional endopeptidases—angiotensin-converting enzyme, proline endopeptidase, and endopeptidase 24.15—were also drastically reduced. In contrast, the cerebellum displayed a set of proteolytic activities that remained unaffected in SDAT brain. The putative influence of the disease on the catabolic fates of neurotensin, neuropeptide Y, and somatostatin(1–14) was investigated. Neurotensin was catabolized at identical rates in the frontal and parietal cortices in nondemented and SDAT brains. In contrast, neuropeptide Y metabolism was slowed down in SDAT brains in the frontal but not in the parietal cortex. Finally, the degradation velocities of somatostatin(1–14) were lowered in both cortical areas of SDAT brains. It is interesting that, by means of specific peptidase inhibitors, we demonstrated that endopeptidase 24.15 participated in somatostatin(1–14) inactivation in the parietal but not in the frontal cortex. It is suggested that the lowering of the rate of somatostatin(1–14) inactivation in the parietal cortex of SDAT brains likely results from the depletion of endopeptidase 24.15 in this brain region.     

Localization of angiotensin-converting enzyme,prolyl endopeptidase and other peptidases in cultured neuronal or glial cells

To determine the cellular localization of nervous tissue peptidases, 7 peptidases and 2 lysosomal marker enzyme activities were measured in cultured mouse and rat cells. Neuronal cells of both species exhibited higher activities of angiotensin-converting enzyme (ACE) and prolyl endopeptidase (Pro-EP) than glial cells did. In contrast, arginyl endopeptidase and lysosomal enzymes (acid phosphatase, β-glucuronidase) in the neuronal cell lines were lower than those in the glial cell lines. Other peptidases (alanyl aminopeptidase, arginyl aminopeptidase, leucyl aminopeptidase, dipeptidyl aminopeptidase) activities were not specifically localized in either cell lines. The effects of cellular differentiation on these peptidase activities in the PC 12h cell line and rat glioblasts were also examined using nerve growth factor (NGF) and glia maturation factor (GMF), respectively. Neuron specific peptidase (ACE and Pro-EP) activities were decreased in PC12h cells cultured with NGF, and Pro-EP activity was increased in the glioblast cells cultured with GMF. These results support the idea that some of the peptidases are differentially localized in neuronal or glial cells, and play physiological roles in central or peripheral neural tissues.     

A comparison of phytoplankton size-fractions in Mondsee,an alpine lake in Austria: distribution,pigment composition and primary production rates

Production rates, abundance, chlorophyll a (Chl a) concentrations and pigment composition were measured for three size classes (<2 μm, 2–11 μm and >11 μm) of phytoplankton from May to December 2000 in deep, mesotrophic, alpine lake Mondsee in Austria. The study focuses on differences among phytoplankton size fractions characterised by their surface area to volume ratio ([mm² l⁻¹: mm³l⁻¹]), pigment distribution patterns and photosynthetic rates. Particular attention was paid to autotrophic picophytoplankton (APP, fraction <2 μm) since this size fraction differed significantly from the two larger size fractions. Among the three fractions, APP showed the highest surface area to volume ratios and a high persistence in the pattern of lipophilic pigments between temporarily and spatially successive samples (about 80% similarity of pigment composition between samples over seasons and depths). The epilimnetic abundance of APP varied seasonally with an annual maximum of 180 × 10³ cells ml⁻¹ in June (at 4–9 m). The minimum (October at 12 m) was more than an order of magnitude lower (4.9 × 10³ ml⁻¹). APP peaked during autumn and contributed between 24% and 42% to the total area-integrated Chl a (10–23 mg m⁻²) and between 16% and 58% to total area-integrated production (5–64 mg m⁻²  h⁻¹) throughout seasons.     

Temporal and spatial distributions of dissolved organic carbon and nitrogen in two small lakes on the Southwestern China Plateau

Temporal and spatial distributions of dissolved organic carbon (DOC), dissolved organic nitrogen (DON), chlorophyll-a and inorganic nitrogen were investigated in two small mountainous lakes (Lake Hongfeng and Baihua), on the Southwestern China Plateau, based on almost 2 years’ field observation. DOC concentrations ranged from 163 μM to 248 μM in Lake Hongfeng and from 143 μM to 308 μM in Lake Baihua, respectively, during the study period. DON concentrations ranged from 7 μM to 26 μM in Lake Hongfeng and from 14 μM to 47 μM in Lake Baihua. DOC showed vertical heterogeneity with higher concentrations in the epilimnion than in the hypolimnion during the stratification period. The DON concentration profiles appeared to be more variable than the DOC profiles. Apparent DON maxima occurred in the upper layer of water. In Lake Hongfeng, DOC concentration in the surface water was highest at the end of spring and early summer. DON concentration was 2–5 μM higher in May 2003 and in June 2004 than in adjacent months. DOC and chlorophyll-a concentrations were significantly correlated (r = 0.79, P < 0.05). The period of highest concentrations of DOC in Lake Hongfeng was also the season of concentrated rainfall. Algae activity and allochthonous input might result in an increase of DOC and DON concentrations together. In Lake Baihua, the maximum concentrations of DOC and DON in the surface water occurred simultaneously in May 2003 and February 2004. DOC concentrations were significantly correlated with DON (r = 0.90, P < 0.01), indicating the common sources. Allochthonous input, biological processes, stratification and mixing were the most important factors controlling the distributions and cycling of dissolved organic matter (DOM) and inorganic nitrogen in these two lakes. Inference from the corresponding vertical distributions of DOM and inorganic nitrogen indicated that DOM played potential roles in the internal loading of nitrogen and metabolism in the water body in these small lakes. The carbon/nitrogen (C/N) ratio showed a potential significance for tracing the source and biogeochemical processes of DOM in the lakes. These results are of significance in the further understanding of biogeochemical cycling and environmental effects of DOM and nitrogen in lake ecosystems.     

Genetic Diversity of Eukaryotic Plankton Assemblages in Eastern Tibetan Lakes Differing by their Salinity and Altitude

Eukaryotic plankton assemblages in 11 high-mountain lakes located at altitudes of 2,817 to 5,134 m and over a total area of ca. one million square kilometers on the Eastern Tibet Plateau, spanning a salinity gradient from 0.2 (freshwater) to 187.1 g l⁻¹ (hypersaline), were investigated by cultivation independent methods. Two 18S rRNA gene-based fingerprint approaches, i.e., the terminal restriction fragment length polymorphism and denaturing gradient gel electrophoresis (DGGE) with subsequent band sequencing were applied. Samples of the same lake type (e.g., freshwater) generally shared more of the same bands or T-RFs than samples of different types (e.g., freshwater versus saline). However, a certain number of bands or T-RFs among the samples within each lake were distinct, indicating the potential presence of significant genetic diversity within each lake. PCA indicated that the most significant environmental gradient among the investigated lakes was salinity. The observed molecular profiles could be further explained (17–24%) by ion percentage of chloride, carbonate and bicarbonate, and sulfate, which were also covaried with change of altitude and latitude. Sequence analysis of selected major DGGE bands revealed many sequences (largely protist) that are not related to any known cultures but to uncultured eukaryotic picoplankton and unidentified eukaryotes. One fourth of the retrieved sequences showed ≤97% similarity to the closest sequences in the GenBank. Sequences related to well-known heterotrophic nanoflagellates were not retrieved from the DGGE gels. Several groups of eukaryotic plankton, which were found worldwide and detected in low land lakes, were also detected in habitats located above 4,400 m, suggesting a cosmopolitan distribution of these phylotypes. Collectively, our study suggests that there was a high beta-diversity of eukaryotic plankton assemblages in the investigated Tibetan lakes shaped by multiple geographic and environmental factors.     

Simulation of water colors in a shallow acidified lake, Lake Onneto, Japan, using colorimetric analysis and bio-optical modeling

Lake Onneto has unusually brilliant water colors, such as blue-green, green, and greenish yellow. We investigated the coloration mechanism in this lake by measuring the radiometric water color and inherent optical properties (IOPs), such as attenuation, absorption, and scattering coefficients of color-producing agents (CPAs) in the lake. The hue of the water body was determined using colorimetric analysis. In addition, the radiometric water color of the lake was simulated using bio-optical modeling. Results showed that the hues of the water body were different between two sampling stations (blue-green and green at 3.1 and 5.5 m of bottom depth, respectively). However, the total suspended solids (TSS) concentrations were almost identical between the two stations (0.47 and 0.42 mg l⁻¹, respectively). In addition, the attenuation and absorption coefficients showed that the CPAs in the water body were only inorganic suspended solids (ISS) more than 0.7 μm in diameter, and specific CPAs, such as dissolved mineral ions and aqueous colloids, were not observed in the lake. Simulation of the radiometric water color showed that the radiation around 600 nm of wavelength (yellow region) steeply increased with decreasing bottom depth, indicating that the water colors of Lake Onneto are strongly governed by the light reflection from yellowish bottom sediments.     

The seasonal abundance and vertical distribution of the <3-μm phytoplakton in the north basin of Lake Biwa

The seasonal changes in the size-fractionated chlorophylla concentrations (<3 μm, 3 to 25 μm, and >25 μm) were investigated at a pelagic site of the north basin of Lake Biwa during June to December 1985. Autofluorescing plankton cells in the <3-μm fractions were also examined using the fluorescein isothiocyanate staining epifluorescence microscopic technique. The <3-μm phytoplankton (usually dominated by chroococcoid cyanobacteria except for a few cases dominated by small eukaryotes) showed a clearly different pattern of seasonal change compared with the larger fractions. That is, from August to early September, chlorophylla of the larger fractions declined considerably, while the <3-μm chlorophylla did not decrease significantly. Moreover, cyanobacterial cell density in the <3-μm fraction showed a maximum value (2–3.5×10⁵ cells·ml⁻¹) during this period. The relative contribution of the <3-μm chlorophylla to the total chlorophylla increased from <5% to 45% during the course of this change. No clear vertical trend in the distribution and composition of the <3-μm phytoplankton was found, except that relatively large cyanobacteria (>4 μm³) appeared at a depth of 15m but not at 0,5 and 10 m from late July to August. These large cells were also found in November and December. The drastic seasonal change of phytoplankton size structure occurring in this basin was discussed in relation to grazing, nutrient depletion and sinking. Contribution from Otsu Hydrobiological Station, Kyoto Univeristy (No. 308, foreign language series).     

Simultaneous extraction and purification of a cell wall-associated peptidase and β-casein specific proteas fromStreptococcus cremoris AC1

Summary A cell wall-associated, β-casein specific protease and a peptidase were purified simulta-neously fromStreptococcus cremoris AC1. The molecular weights are 145,000 daltons for the pro-tease and 36,000 for the peptidase. The protease has a pH optimum at 5.5-6 and a temperature optimum at 40° C. It is activated by 1 mM of Ca⁺⁺ but severely inhibited by higher Ca⁺⁺ concentrations. Further inhibitor studies indicate that the protease is probably a serin protease. The peptidase shows aminopeptidase activity and most effectively hydrolyses L-lysyl-p-nitroanilide, and to a lesser extent IMeucyl-, L-alanyl- and L-alanyl-L-alanyl-p-nitroanilide. No endopeptidase activity could be detected. The peptidase is irreversibly inhibited by EDTA.     

Precipitation patterns, dissolved organic matter and changes in the plankton assemblage in Lake Escondido (Patagonia, Argentina)

Global warming affects the hydrological cycle by increasing the frequency and intensity of extreme rainfall events and dry spells. These changes potentially affect the quantity and quality of dissolved organic matter (DOM) input into lakes. In this study, we investigated if changes in precipitation over a 3-year period correspond to changes in DOM and whether these changes affect light attenuation and plankton community composition. We sampled Lake Escondido, a shallow, oligotrophic Andean lake, nine times, analyzing coloured DOM and plankton community composition. During the study period, we observed that variations in the precipitation regime correlated with DOM parameters (water colour and molecular weight), and this, in turn, affected the plankton composition. Chlorophyll a concentrations of both phytoplanktonic fractions (less than and greater than 2 μm) were related to water colour and TDP. We observed in the small fraction (<2 μm) an increase in phycocyanin-rich cells during periods of high water colour. Larger phytoplanktonic cells (>2 μm) presented two biomass peaks corresponding to increases of the cyanophyte Chroococcus planctonicus and of the haptophyte Chrysochromulina parva. As precipitation decreased, the lake became more transparent, favouring C. planctonicus and mixotrophic oligotrich ciliates with endosymbiotic Chlorella. In the context of global climate change, our results highlight the potential impact of changes in precipitation patterns and, consequently, in DOM quality on the plankton community.     

Specific inhibition of endopeptidase 24.16 by dipeptides.

The inhibitory effect of various dipeptides on the neurotensin-degrading metallopeptidase, endopeptidase 24.16, was examined. These dipeptides mimick the Pro10-Tyr11 bond of neurotensin that is hydrolyzed by endopeptidase 24.16. Among a series of Pro-Xaa dipeptides, the most potent inhibitory effect was elicited by Pro-Ile (Ki approximately 90 microM) with Pro-Ile greater than Pro-Met greater than Pro-Phe. All the Xaa-Tyr dipeptides were unable to inhibit endopeptidase 24.16. The effect of Pro-Ile on several purified peptidases was assessed by means of fluorigenic assays and HPLC analysis. A 5 mM concentration of Pro-Ile does not inhibit endopeptidase 24.11, endopeptidase 24.15, angiotensin-converting enzyme, proline endopeptidase, trypsin, leucine aminopeptidase, pyroglutamyl aminopeptidase I and carboxypeptidase B. The only enzyme that was affected by Pro-Ile was carboxypeptidase A, although it was with a 50-fold lower potency (Ki approximately 5 mM) than for endopeptidase 24.16. By means of fluorimetric substrates with a series of hydrolysing activities, we demonstrate that Pro-Ile can be used as a specific inhibitor of endopeptidase 24.16, even in a complex mixture of peptidase activities such as found in whole rat brain homogenate.     

Dipeptidyl peptidase IV. Purification for use in peptide sequencing

Isolation and purification of dipeptidyl peptidase IV from pig kidney are described. The specific activity of the enzyme is 24.9 U/mg protein. Chromatography on Gly-Pro-AH-Sepharose is the most important procedure for the separation from other enzyme activities. The enzyme preparation is free of aminopeptidase, dipeptidase and prolyl endopeptidase activity; it can be used for peptide-sequence analysis.     

A five-year study of autotrophic winter picoplankton in Lake Balaton,Hungary

Picoeukaryotes dominate the phytoplankton of Lake Balaton—the largest shallow lake in Central Europe—in the winter period. We examined the annual dynamics of picoplankton abundance and composition in the lake in order to establish if the picoeukaryotes merely survive the harsher winter conditions or they are able to grow in the ice-covered lake when the entire phytoplankton is limited by low light and temperature. Lake Balaton has an annual temperature range of 1–29°C, and it is usually frozen between December and February for 30–60 days. In the spring-autumn period phycocyanin and phycoerythrin rich Cyanobacteria are the dominant picoplankters, and picoeukaryotes are negligible. Our five-year study shows the presence of three types of picophytoplankton assemblages in Lake Balaton: (1) Phycoerythrin-rich Cyanobacteria—the dominant summer picoplankters in the mesotrophic lake area; (2) Phycocyanin-rich Cyanobacteria—the most abundant summer picoplankters in the eutrophic lake area and; (3) Picoeukaryotes—the dominant winter picoplankters in the whole lake. The observed winter abundance of picoeukaryotes was high (up to 3 × 10⁵ cells ml⁻¹), their highest biomass (520 μg l⁻¹) exceeded the maximum summer biomass of picocyanobacteria (500 μg l⁻¹). Our results indicate that the winter predominance of picoeukaryotes is a regular phenomenon in Lake Balaton, irrespective of the absence or presence of the ice cover. Picoeukaryotes are able to grow at as low as 1–2°C water temperature, while the total phytoplankton biomass show the lowest annual values in the winter period. In agreement with earlier findings, the contribution of picocyanobacteria to the total phytoplankton biomass in Lake Balaton is inversely related to the total phytoplankton biomass, whereas no such relationship was observable in the case of picoeukaryotes.     

Investigation of bathymetry and water quality of Lake Nam Co, the largest lake on the central Tibetan Plateau, China

Comprehensive field investigations have been conducted four times on Nam Co, central Tibet, from September 2005 to September 2008. Here, we present the preliminary results focusing on the bathymetric survey and water quality measurements. The isobathic map shows that Nam Co is a high-altitude, deep lake where a flat and large basin lies in the central part with a water depth of more than 90 m. Water depth data from the northwestern bank areas of Nam Co provide unquestionable evidence of rising water levels in the last 3 decades because of the formation of two small islands that were still peninsulas in the 1970s. Water quality measurements taken at 19 stations during three summer field campaigns (2006, 2007 and 2008) covering almost all of the lake areas showed that the temperature, pH, dissolved oxygen and electric conductivity of surface water are on average 11.43°C, 9.21, 8.90 mg l⁻¹ and 1,851 μS cm⁻¹, respectively. The surface water shows no obvious spatial variability among all the stations. Vertical fluctuations of profiles, however, display some differences in thermocline and related parameters, such as pH and dissolved oxygen. According to the vertical variations of water quality parameters, the water column in relatively deep lake areas of Nam Co could be divided into three layers with distinctly various features: the epilimnion is from the surface to about 18–20 m depth in which the parameters are homogeneous with higher temperature and abundant sunlight; the metalimnion ranged from 20–60 m where a thermocline develops; the deepest layer forms a cold and dark hypolimnion.