Leptodora kindtii survival in the laboratory

Leptodora kindtii, a pelagic predatory cladoceran, suffers high mortality on transfer to laboratory, which makes the experimental work difficult. We investigated the causes of high mortality, using four variables: water volume, animal density, light intensity, and origin of water for culturing, i.e., water from native or a non-native lake. For the experiments we used Leptodora and water from Lake Loosdrecht and Lake Maarsseveen (The Netherlands). Water was found to be the most important factor; the animals did not necessarily do better in lake water from which they were collected. Water volume and animal density were of limited importance, and light intensity did not affect survival.     

Influence of Temperature, Oxygen, and pH on a Metalimnetic Population of Oscillatoria rubescens

Planktonic Oscillatoria spp. often inhabit depths of thermally stratified lakes in which gradients of physical and chemical factors occur. Measurements of photosynthetic rate or photosynthetic carbon metabolism were used to evaluate the importance of vertical gradients of temperature, oxygen, and pH upon Oscillatoria rubescens in Crooked Lake, Ind. At the low light intensities experienced in situ, neither photosynthetic rate nor relative incorporation of carbon dioxide into low-molecular-weight compounds, polysaccharide, or protein was affected by temperature. At a 10-fold-higher light intensity, the photosynthetic rate increased as temperature increased; most of the additional carbon accumulated as polysaccharide. Polysaccharide which was synthesized at high light intensity and temperature was respired when the organisms were placed in the dark, but was not used for protein biosynthesis. When O. rubescens was shifted from high light to low light, a fraction of the polysaccharide was metabolized into protein. Adaptation to growth at lower temperatures by O. rubescens cultures resulted in a decrease in the maximum photosynthetic rate. Oxygen inhibited photosynthesis by only 10 to 15% at concentrations typically found in the lake. The photosynthetic rates at pH values which occurred in Crooked Lake were all near the maximum. Thus, gradients of temperature, oxygen, or pH are not likely to significantly affect the distribution of O. rubescens in Crooked Lake, given the low light intensity at which O. rubescens grows and the range of values for those factors in the lake.     

Determination of growth-limiting nutrients for red species of Oscillatoria and two ‘oligotrophic’ diatoms

Laboratory batch experiments with dilute phytoplankton communities were carried out to determine growth-limiting nutrients and the degree of growth limitation for Asterionella formosa, Hass., Tabellaria fenestrata (Lyngb.) Kütz. and red species of Oscillatoria under specific temperature and light conditions. Water samples from five Norwegian lakes with average epilimnetic total phosphorus concentrations ranging from 5 to 30 µg P per 1 were investigated. Both enrichment and transplant experiments were carried out. In samples from the most oligotrophic lakes (Lake Randsfjorden and Lake Tyrifjorden) phosphorus was found to be the growth-limiting nutrient. In samples from Lake Mjøsa silicate was also growth-limiting for the diatoms, while nitrogen could be limiting for both asterionella and Oscillatoria from Lake Steinsfjorden. Phosphorus was often the only limiting nutrient determined for Oscillatoria in Lake Gjersjøen (the most eutrophic of the lakes). In samples from this lake, however, Asterionella was also growth-limited directly or indirectly as a result of high (pH > 9). This was also found for Asterionella and Tabellaria from lake Mjøsa by means of transplant experiments. Oscillatoria from Lake Gjersjøen could not grow in filtered water from Lake Mjøsa but obtained maximum growth rate after addition of phosphate and chelated iron in combination.     

Effects of Inorganic Turbidity on the Phytoplankton of an Amazonian Lake Impacted by Bauxite Tailings

The dumping of bauxite tailings into Batata Lake, an Amazonian clear-water lake, generated high levels of turbidity and caused a serious decrease in phytoplankton densities, which could possibly be the result of a photosynthetic limitation due to light attenuation together with an increase in algal sinking due to the adhesion of clay particles. This study aimed to investigate the sinking process through the addition of different suspended clay concentrations in columns containing Batata lake water. Since no effect of the suspended clays on Batata Lake phytoplankton sinking was observed, it was then evaluated, under laboratory conditions, whether the low conductivity of the Batata Lake water could interfere with the algae-clay aggregation process. Cultures of two algal species known to be capable to aggregate to Batata Lake suspended clays in algal culture medium: Staurodesmus convergens and Phormidium amoenum, were added to both the low conductivity Batata Lake water (14 μS cm^?1) and the high conductivity algal culture media (WC – 300 μS cm^?1 and Z8 – 560 μS cm^?1) together with Batata lake suspended clays. In both algal culture media and Batata lake water the two species had their sinking accelerated due to clay adhesion. It is thus suggested that the decrease in phytoplankton densities recorded in Batata Lake may not be related to an increase in phytoplankton loss rates due to algal-clay aggregation, but rather are a consequence of decreasing growth rates because of light attenuation.     

Seasonal changes of phytoplankton and cyanobacteria/cyanotoxin risk in two shallow morphologically altered lakes: Effects of water level manipulation (Wieprz-Krzna Canal System,Eastern Poland)

Seasonal development of phytoplankton was compared over two years in two eutrophic, morphologically altered lakes. During study, the water level in Lake Tomaszne were periodically regulated whereas in Lake Mytycze, the water level manipulation was not performed. We assumed that the supply with fertile waters and subsequent discharge can be reflected in seasonal changes of phytoplankton taxa composition and biomass, especially of toxigenic cyanobacteria. In Lake Tomaszne, the development of toxigenic Nostocales (Aphanizomenon gracile and Dolichospermum planctonicum) was supported by the entrance of water from a canal (due to supply of water containing NH₄⁺-N). After water discharge, the replacement of Nostocales by the toxigenic Planktothrix agardhii was associated with low light conditions and a supply of phosphates from the bottom sediments. In Lake Mytycze, microalgae (Chlorococcales) were predominant throughout the study period. The rapid growth of toxigenic cyanobacteria (A. gracile, Planktolyngbya limnetica and Microcystis spp.) occurred only at extremely low water levels. In Lake Tomaszne, the lake with periodic water level regulation, the high cyanobacteria/cyanotoxin risk and decline of its ecological status were more conspicuous than in Lake Mytycze, the lake with natural water level changes.     

Nitrogen Fixation by the Photosynthetic Sulfur Bacterium Chlorobium phaeobacteroides from Lake Kinneret

N₂ fixation by Chlorobium phaeobacteroides from Lake Kinneret was dependent on ammonia concentration and light intensity. In the thermocline of Lake Kinneret, N₂ fixation and photosynthesis were low. It was concluded that the bacteria do not contribute significantly to the organic nitrogen load of the lake.     

Decomposition Studies in Two Central Ontario Lakes Having Surficial pHs of 4.6 and 6.6

The rates of cellulose breakdown, composition of detrital microflora, and density of bacterial populations were determined in the epilimnetic sediments and water columns of two poorly buffered, oligotrophic, Canadian Shield lakes having mean surficial pHs of 4.6 (Bat Lake) and 6.6 (Harp Lake). The decomposition rate was significantly lower in oxic sediment of the acidified lake than of the circumneutral lake, but water column rates were almost identical in the two lakes. These results are explained in terms of the groups of cellulolytic microorganisms which were observed by phase-contrast microscopy as being active at the different sites: fungi in Bat Lake water and Cytophaga-like bacteria in the water and sediment of Harp Lake. Cytophaga-like bacteria were also the main decomposers in Bat Lake sediment, but their activity was restricted at porewater pHs of <5.0. Acridine orange direct counts of bacteria in the top centimeter of sediment ranged from 3.7 × 10⁸ to 1.0 × 10⁹ per g, and counts in planktonic water samples ranged from 4.9 × 10⁵ to 1.2 × 10⁶ per ml. Bacterial densities at most sites decreased significantly (P < 0.001) from August to late October, but did not show a consistent pattern of differences related to pH.     

The ecology of Biomphalaria sudanica in Lake Ziway, Ethiopia

A longitudinal study was made over a period of 24 months from January 2001 to December 2002 in Lake Ziway, Ethiopia, to elucidate factors influencing changes in the population density of Biomphalaria sudanica and to identify seasons of peak transmission of Schistosoma mansoni. Between January 2001 and December 2002, bimonthly visits were made to the lake to collect data on snail population density and schistosome infection in snails, vegetation and lake water level. Water samples were collected during the dry and rainy seasons and chemical analyses were made for major cations, anions, electrical conductivity, total hardness and pH using standard methods for the examination of water and wastewater. The seasonal fluctuation in the population density of B. sudanica was found to be highly associated with rainfall, water level of the lake and vegetation availability and abundance. Water chemical analysis showed that major cations and anions were all within the range reported for other African freshwaters. Both malacological and meteorological data show that snail population density in Lake Ziway peaks at the end of the long rainy season (June–August), coinciding with a seasonal transmission peak of schistosomiasis.     

Presence and genetic diversity of microcystin-producing cyanobacteria (<Emphasis Type="Italic">Anabaena</Emphasis> and <Emphasis Type="Italic">Microcystis</Emphasis>) in Lake Kotokel (Russia,Lake Baikal Region)

A survey was conducted for the presence of cyanobacteria toxins in Lake Kotokel due to a few cases of Haff disease registered in 2008–2009 caused by consumption of fish from Lake Kotokel, and wildlife mortality including large fish kill. The aims of this study were to determine what cyanotoxins (if any) were present in the lake, to describe phytoplankton composition including morphology, density, and species diversity of cyanobacteria, as well as to evaluate the trophic state of the lake. Samples were collected from both nearshore and central sites in August of 2009. Aphanocapsa holsatica dominated the phytoplankton. The presence of toxigenic genotypes of Microcystis spp. and Anabaena lemmermannii was detected by sequencing of PCR-amplified aminotransferase domain of microcystin synthetase gene. LR, RR, and YR microcystin (MC) variants were detected with liquid chromatography-UV mass spectrometry. The data do not shed light on the etiology of Haff disease in Lake Kotokel region, nevertheless taking into account the recreational importance of the lake and its direct connection to Lake Baikal, a necessity to monitor cyanobacteria in these water bodies is evident. This is the first report on simultaneous detection of MC-producing genotypes and MCs in the Lake Baikal region.     

Differences in the exploitation of bream in three shallow lake systems and their relation to water quality

SUMMARY 1. The development of bream populations, water transparency, chlorophyll‐a concentration, extent of submerged vegetation and densities of the zebra mussel, Dreissena polymorpha, were analysed in three shallow eutrophic lake systems subject to different fish management. 2. In Lake Veluwemeer, the bream population was reduced from c. 100 to 20 kg ha^?1 after 5 years of fishing. The mortality caused by the fishery was estimated at 38% of bream >15 cm in addition to a 13% natural mortality of bream >17 cm. The decline was followed by an expansion of the Chara beds present in the shallow parts, an increase in water transparency in the open‐water zone, an increase in the density of zebra mussels and a decrease in chlorophyll‐a concentrations. 3. The newly created Lake Volkerak showed trends opposite to those in Lake Veluwemeer. Bream colonised the lake in 1988 and reached a biomass of c. 140 kg ha^?1 in 1998. The water transparency decreased from a maximum of 3 m to c. 1 m and the chlorophyll‐a concentration increased from 5 to 45 μg L^?1. Submerged vegetation colonised up to 20% of the total lake area in the first 5 years after creation of the lake in 1987 but decreased to 10% as turbidity increased. 4. Seine fishery in the Frisian lake system did not appear to affect the bream population despite annual catches as high as 40–50 kg ha^?1. The estimated natural mortality of fish >15 cm was 15% and mortality by fishery was 26%. The high loss was apparently compensated by good recruitment and high growth rates resulting from a c. 1 °C higher water temperature during the years when bream were removed by fishing. There was only a slight decrease in chlorophyll‐a concentrations and a slight increase in water transparency. 5. The results of this study suggest that the effects of bream exploitation in eutrophic lakes can vary depending on the efficiency of the fishery, recruitment success and temperature regime. In the absence of fishery, bream dominated the fish community in the study lakes and apparently prevented D. polymorpha and submerged vegetation from establishing because of physical disturbance, enhanced internal P‐loading and resettling of resuspended sediments.     

RETENTION OF DISSOLVED COMPOUNDS BY MEMBRANE FILTERS AS AN ERROR IN THE 14C METHOD OF PRIMARY PRODUCTION MEASUREMENT1

Membrane filters retain ¹⁴C bicarbonate, ¹⁴C glycollate, and other ¹⁴C labeled substances from filtrates of algal cultures and lake water. By refiltering different volumes of the filtrate from algal cultures and from lake water after incubation with ¹⁴C bicarbonate, it was shown that the labeled material retained was not proportional to volume but showed a saturation effect with increasing volume filtered. When the radioactivity retained by a filter is divided by the volume filtered, decreasing values are obtained with increased volume filtered. This radioactivity may represent a significant addition to the radioactivity in particulate material on the filters, resulting in a similar type of curve when different volumes of lake water or cultures are filtered. Values of radioactivity per milliliter were constant using Chlorella in Chu 10 medium. However, the curve could, be obtained by increasing pH and bicarbonate concentrations in the medium and on resuspending the algae in Lake Ontario (winter) filtrate. The values of cpm/ml retained from filtrates were low in Cryptomonas cultures and the curve was not obtained unless population density was reduced, thus increasing the relative contribution to the radioactivity on the filters. The curve was not always obtained in lake water. It was significant in 10 out of 14 experiments in Lake Ontario and in 2 out of 5 experiments in Grenadier Pond. Changes in lake water rather than in experimental techniques were probably responsible. On 2 occasions when values of cpm/ml were constant in Lake Ontario, addition of sodium bicarbonate without a pH change resulted, in a significant curve. Our experiments do not disprove the possibility of cell damage during Millipore filtration, however, it has been shown that ¹⁴C labeled substances retained from solutions can account for the entire range of decreasing values as a function of volume filtered.     

洪湖水体藻类藻相特征及其对生境的响应

藻类是水生态系统的重要成分,它的群落结构、细胞密度变化与水环境相适应,随水环境的变化而改变,因此藻相变化是评价水体质量的一项重要指标。2009—2010年在洪湖水面不同方位布点采样,对水体的浮游藻类藻相(群落结构、密度)和水质状况(水位(water level,H)、水温(water temperature,tw)、透明度(transparency,SD)、总氮(total nitrogen,TN)、总磷(totalphosphorus,TP)、高锰酸盐指数(permanganate index,CODMn)和叶绿素含量(chlorophyll a,Chl-a)等)进行了逐月的调查、监测,采用湖库营养状态指数法对湖泊富营养化评价,并运用多元逐步回归方法建立水体藻类与生境因子的回归方程。结果表明:洪湖水体总体上已达到轻度富营养化状态;藻类以蓝藻门、硅藻门和绿藻门为主,共鉴定出7门65属,藻细胞密度为1.14×106—3.24×107个/L,藻相季节变化特征明显。藻类组成以蓝藻门密度最高(52.93%),硅藻门(25.96%)和绿藻门(16.83%)次之,隐藻门(1.98%)、金藻门(1.64%)、裸藻门(0.42%)和甲藻门(0.25%)相对较低。藻类藻相及优势种在不同季节有所差异,冬春季节(12—5月)以硅藻门的直链藻、小环藻和针杆藻为优势种,夏秋季节(7—11月)以蓝藻门的鱼腥藻和微囊藻为优势种;湖泊藻类细胞密度与tw、CODMn呈正显著相关关系,与H、TN、TP、SD相关关系不显著;藻细胞生长逐步回归方程为y=3.7815+0.0794tw+0.5670CODMn-1.3467SD,藻细胞生长主要受水温和有机污染物等的影响,氮磷不是藻类生长的控制因子;在湖泊不同区域,环境条件存在差异,导致藻类生长过程中起主导作用的环境因子存在一定的差异,蓝藻生长主要受tw、CODMn和SD控制,绿藻生长主要受H、tw和CODMn影响,而硅藻生长决定于水体CODMn。     

Spatiotemporal distribution of bacteriochlorophylls in the meromictic Lake Suigetsu, Japan

The spatiotemporal distribution of chlorophyll pigments (chloropigments) in the water column of a meromictic lake, Lake Suigetsu (Fukui, Japan), was investigated. Water samples were collected from the central basin of Lake Suigetsu bimonthly between May 2008 and March 2010 at appropriate depths, including the oxic surface, oxic–anoxic interface, and anoxic bottom layers. Chlorophyll a, related to cyanobacteria and eukaryotic phytoplankton, was detected throughout the water column during the years of the study, whereas bacteriochlorophyll e, related to brown-colored green sulfur bacteria, was detected in the anoxic layers below the chemocline at a maximum concentration of 825 μg L^?1. The concentration of bacteriochlorophyll e was generally maximal at or just below the chemocline of the lake. The cellular content of bacteriochlorophyll e was estimated to be low in the upper part of the chemocline and tended to increase with increasing water depth. Bacteriochlorophyll a, which was presumably related to purple sulfur bacteria, was only detected at the chemocline during summer and autumn at concentrations of 5.4–16.3 μg L^?1. Our analysis of the chloropigment distribution for the two years of the study suggested that brown-colored green sulfur bacteria are the predominant phototroph in the anoxic layers of Lake Suigetsu, and that these play a significant role in the carbon and sulfur cycling of the lake, especially from spring to summer.     

Ecology of purple sulfur bacteria in the highly stratified meromictic Lake Shunet (Siberia, Khakassia) in 2002–2009

Phototrophic sulfur bacteria form dense accumulations in the chemocline zones of stratified lakes where light reaches the sulfide-containing layers of water. Many works are dedicated to the ecophysiology of these microorganisms in meromictic lakes. However, the role of these microorganisms in the trophic network of these ecosystems, the ways of biomass utilization, and the contribution to the turnover of biogenic elements have so far been insufficiently understood. This work deals with the analysis of many years?? seasonal dynamics of the biomass of purple sulfur bacteria and the physicochemical conditions of their environment in Lake Shunet (Siberia, Khakassia, Russia), unraveling the causes of their anomalous development in the chemocline of this lake, as well as the comparative analysis of such type of ecosystems. Lake Shunet is characterized by markedly pronounced stratification and the high density of purple sulfur bacteria (PSB) in the chemocline, which is comparable to that of Lake Mahoney (Canada) where the number of PSB is the greatest among those known in the world. It was shown that, in the period 2002?C2009, the total amount of bacterio-chlorophyll a in the water column of Lake Shunet increased and did not correlate with the seasonal variations in temperature and illumination in the chemocline. It was established that PSB cells in the purple layer experienced the effect of self-shading. The sedimentation rate of purple sulfur bacteria in Lake Shunet was low due to the pronounced density gradient in the chemocline zone. Thus, the high number of PSB in the chemocline was due to the combination of strong illumination, a high sulfide concentration, and a high water density gradient, which was responsible for stable stratification and contributed to the accumulation of the cells in a narrow layer. The data obtained could be useful for the paleoreconstruction of climatically deter-mined changes in the level of the lake and its periods of meromixis by the presence of carotenoids and bacte-riochlorophylls in the bottom sediments.     

Phosphorus limitation in some tropical African lakes

Two of three Kenyan lakes studied between November 1979 and October 1980 have very short ³³PO₄ turnover times, indicating a high phosphorus (P) demand throughout the year. The P turnover time in Lakes Oloidien and Sonachi is as rapid as in the most P deficient temperate zone lakes. The third lake, Lake Naivasha, has a lower overall P demand and a wide seasonal range, with lowest demand between November 1979 and February 1980 when a P deficiency was unlikely. On an annual basis the Lake Naivasha status is, however, not statistically different from that recorded during the summer in Lake Memphremagog, a generally P-limited temperate zone lake. Lake Naivasha and Lake Oloidien fit well to the line of best fit for the Dillon-Rigler relationship relating total phosphorus (TP) and chlorophyll a derived in temperate zone lakes. Thus, temperate zone models predicting aspects of lake behaviour on the basis of TP may also be applicable to these two tropical lakes. Saline lake Sonachi had not only a short P turnover time but also responded dramatically to the fertilization of enclosures with P. However, it does not fit the TP-chla or the total nitrogen-chla plots from the temperate zone. This suggests that, in this saline lake at least, much of the TP is unavailable to the algae, with some of it in a particulate form that is readily extracted with boiling water. The epilimnetic N:P ratios also characterize lakes Oloidien and Sonachi lakes as highly P deficient and lake Naivasha as more moderately P limited. A single set of measurements in Winam Gulf (Lake Victoria) also showed a rapid P turnover time and thus P limitation, but as in lake Sonachi much of the TP was in a non-algal particulate form. Occasional measurements in three other hypertrophic and saline lakes suggest them to be primarily light limited on the basis of their very high photosynthetic cover. These findings support the hypothesis of a primary P limitation for those lakes not light limited, and contradicts literature suggestions that nitrogen is the primary limiting element in tropical lakes.     

Seasonal Distribution of Cyprinid Herpesvirus 3 in Lake Biwa,Japan

The seasonal distribution of the cyprinid herpesvirus 3 (CyHV-3) in Lake Biwa, Japan, was investigated. CyHV-3 was distributed all over the lake 5 years after the first outbreak. The mean concentration of CyHV-3 in water showed annual oscillation, with a peak in the summer and a trough in winter. Our results suggested that CyHV-3 is present at high density in reductive environments, such as reed zones and turbid or eutrophic water.A novel fatal disease of fish caused by cyprinid herpesvirus 3 (CyHV-3), also known as koi herpesvirus or carp interstitial nephritis and gill necrosis virus, which infects the common carp (Cyprinus carpio carpio) and ornamental koi (Cyprinus carpio koi) was reported at the end of the 1990s, and it has spread rapidly worldwide (13). In 2003, the first mass mortality in Japan was observed in Lake Kasumigaura, Ibaraki Prefecture (17), and the disease immediately spread all over the country.Lake Biwa is the largest and oldest freshwater lake in Japan. It occupies 670 km², and the total length of the coastline is 241 km. The first and relatively small-scale mortality caused by CyHV-3 was observed in the autumn of 2003 in Lake Biwa, and mass mortality occurred in the following spring, in which more than 100,000 carp died (10). Thus, the disease is a great threat not only to the cultivation industry and koi collectors but also to the natural carp population. Carp is regarded as an ecological engineer that has an impact on freshwater ecosystems, and therefore, mass mortality will affect the entire lake ecosystem (10).The pathogenesis and diagnosis of the disease have been studied intensively, but the dynamics of CyHV-3 has not been clarified. Recently, the major portal of CyHV-3 entry was reported to be fish skin (2), which means that infection via water is possible. Thus, to determine the method by which the virus spreads and to evaluate the infectious risk in the environment, one must clarify the CyHV-3 dynamics in the natural environment. In the present study, we surveyed the seasonal distribution pattern of CyHV-3 in Lake Biwa, Japan, using a quantitative method.     

Picoplankton photosynthesis and diurnal variations in photosynthesis-irradiance relationship in a eutrophic and meso-oligotrophic lake

The abundance and relative importance of autotrophic picoplankton were investigated in two lakes of different trophic status. In the eutrophic lake, measurements of primary production were performed on water samples in situ and in a light incubator three times during the day whereas for the oligotrophic lake, only one measurement of primary production was performed on water samples in the incubator. Dark-carbon losses of phytoplankton from Lake Loosdrecht were investigated in time series. Cell numbers of autotrophic picoplankton in eutrophic Lake Loosdrecht (3.2 × 10⁴ cells ml^–1) were lower than in meso-oligotrophic Lake Maarsseveen (9.8 and 11.4 × 10⁴ cells ml^–1 at the surface and bottom respectively). In the phytoplankton of both lakes the ratio of picoplankton production increased with decreasing light intensity. In Lake Loosdrecht depth-integrated contribution of picoplankton to total photosynthesis was less than 4%. The P-I-relationship showed diurnal variations in light saturated photosynthesis, while light limited carbon uptake remained constant during the day. Dark carbon losses from short-term labelled phytoplankton during the first 12 hours of the night period accounted for 10–25% of material fixed during the preceeding light period.     

Interaction of water quantity with water quality: the Lake Chapala example

Water quality may be significantly determined by water quantity. Lake Chapala, México is a large lake beset with numerous water quality problems. The decline in water volume over the past 20 years, a serious problem itself, is associated with causing or enhancing several problems of quality. Five such problems are explored herein. These are: extensive infestations of water hyacinth (Eichhornia crassipes), a declining native fishery, light limitation of phytoplankton production at the base of the food chain, shallow-water algal blooms resulting in water supply treatment problems, and the presence of toxic metals in the harvested and sold fishes.     

Measurement of Proteolysis in Natural Waters

Microbiological proteolysis in Lake Champlain water was measured in situ and in vitro by the spectrophotometric measurement of the rate of release of soluble color from an insoluble azure dye derivative of hide powder. Water samples sterilized by microfiltration were never proteolytic. In situ proteolysis was found to be very dependent upon water temperature (1 to 23°C). No measurable activity was observed below 4°C. The in vitro proteolysis rate at 20°C was found to be 2.3 times the rate at 15°C and 6 times the rate at 10°C. Water taken from beneath the ice-covered lake throughout the winter and tested in the laboratory at 20°C was found to show an increasing proteolytic potential during the winter months. The highest activity was obtained as the ice broke up in early spring. Microbiological proteolysis in water from Burlington Harbor was often four times that found in center lake water. In most experiments proteolysis was inhibited completely by 2 μg of Cu²⁺ and inhibited 67% by 0.75 μg/ml. Proteolysis was markedly stimulated by 20 to 40 μg of Casitone or Casamino Acids per ml. The predominant bacteria growing in the proteolysis flasks were species of Pseudomonas and Flavobacterium. Pure cultures of Pseudomonas required traces of Casitone, Casamino Acids, or yeast extract for proteolysis of hide powder azure, whereas those of Flavobacterium did not. The requirement could not be met by a mixture of 21 amino acids and eight vitamins.     

Size-dependent growth of Microcystis colonies in a shallow,hypertrophic lake: use of the RNA-to-total organic carbon ratio

Microcystis was cultured under standard conditions in BG-11 and M-11 media. Using results of an analysis of RNA and total organic carbon (TOC) content, a significant logarithmic relationship between Microcystis growth rate and the RNA/TOC ratio was described to measure the growth rate. Colonial Microcystis samples collected in a shallow, hypertrophic lake (Lake Taihu, China) during May–November 2012 were divided into six size classes (<75, 75–100, 100–150, 150–300, 300–500, and >500 μm), and the RNA/TOC ratio of each class was analyzed to evaluate differences in growth. The growth rate of colonies in the 150–300-μm size class was highest from May to August, but the growth rate increased along with the increase in colony size from September to November. Our results also indicated that water temperature did not change the relationship between growth rate and colony size, but the growth rate of larger colonies was higher than the growth rate of smaller colonies at conditions of low total nitrogen, low total dissolved phosphorus concentration, and high light intensity. Taken together, these results suggest that large colonial Microcystis possess an advantage that is a consequence of this faster growth at lower nutrient concentrations and high light intensities.