Seasonal dynamics of picophytoplankton in Lake Kinneret, Israel

1. Picophytoplankton (picocyanobacteria and picoeukaryotes) communities in Lake Kinneret were studied from 1988 to 1992. No prochlorophytes were observed in the lake. 2. Picocyanobacteria were a prominent and ubiquitous component of the phytoplankton, being present at all depths throughout the year, with concentrations ranging from 2 ± 10–8 ± 10⁵ cells ml^?1. Low cell numbers in winter and spring were followed at the end of the annual dinoflagellate bloom by maximal abundances in summer-autumn in the epilimnion. High cell numbers (> 10⁴ cells ml^?1) were sometimes also found in the anaerobic hypolimnion. Net growth rates for picocyanobacteria ranged from 0.29 to 0.60 divisions day^?1. 3. Picoeukaryotes were a very minor constituent of the picoplankton, mostly present in winter and spring, and sometimes at the end of autumn, with concentrations ranging from 44 to 5700 cells ml^?1. Higher cell numbers tended to occur in the near surface water layers. In August-September, picoeukaryotes were found only in the hypolimnion. In December, the occurrence of picoeukaryotes in the deep water layers probably resulted from advection with cold water currents from the Jordan river. Net growth rates for picoeukaryotes ranged from 0.26 to 0.43 divisions day^?1. 4. Overall, the contribution of picophytoplankton to the phytoplankton standing crop in Lake Kinneret was limited; picocyanobacteria and picoeukaryotes accounted for no more than 7.0 and 0.1% of total algal biomass (semiannual average), respectively. 5. Picophytoplankton cell numbers in pelagic waters were usually similar to those in shallower lake stations. 6. Picocyanobacteria appear to be an autochthonous population, whereas picoeukaryotes are probably brought annually by the Jordan River and do not maintain themselves in the lake.     

The Seasonal Dynamics and Composition of Photosynthetic Picoplankton Communities in Temperate Lakes in Ontario,Canada

The seasonal abundance and composition of photosynthetic picoplankton (0.2-2 μm) was compared among five oligotrophic to mesotrophic lakes in Ontario. Epilimnetic picocyanobacteria abundance followed a similar pattern in all lakes; maximum abundance (2-4 × 10⁵ cells · ml⁻¹) occurred in late summer following a period of rapid, often exponential increase after epilimnetic temperatures reached 20 °C. In half of the lakes picocyanobacteria abundance was significantly correlated with temperature, while in other lakes the presence of a small spring peak resulted in a poor correlation with temperature. In all lakes there was a significant correlation between epilimnetic abundance and day of the year. Correlations with water chemistry parameters (soluble reactive phosphorus, total phosphorus, particulate C: P and C: N) were generally weaker or insignificant. However, in the three lakes with the highest spring nitrate concentrations, a significant negative correlation with nitrate was observed. During summer stratification, picocyanobacteria abundance reached a maximum within the metalimnion and at or above the euphotic zone (1% of incident light) in all lakes. These peaks were not related to nutrient gradients. The average total phytoplankton biomass ranged from 0.5 g m⁻³ (wet weight) in the most oligotrophic lake to 1.4 g m⁻³ for the most mesotrophic with picoplankton biomass ranging from 0.01 g m⁻³ to 0.3 g m⁻³. Picocyanobacteria biomass comprised 1 to 9 % of total phytoplankton biomass in late summer, but in one year for one lake represented a maximum of 56%. Other photosynthetic picoplankton (unidentified eukaryotes, Chlorella spp. Nannochloris spp.), although less abundant (10³ cells · ml⁻¹) than picocyanobacteria, represented biomass equal or greater than that of the picocyanobacteria in spring and early summer. On average, half of the photosynthetic picoplankton biomass was eukaryotic in the more coloured lakes, while in the clear lakes less than 20% was eukaryotic. Among the lakes there was a significant positive correlation between the average light extinction coefficient and the proportion of eukaryotic biomass of the picoplankton. In mesotrophic Jack's Lake, the contribution of picoplankton to the maximum photosynthetic rate ranged from 10 to 47% with the highest values in the spring (47%) and late summer (33%), as a result of eukaryotic picoplankton and picocyanobacteria respectively. Picocyanobacteria cell specific growth rates were high during July (0.6-0.8 day⁻¹) and losses were close to 80% of the growth rate. Thus, despite low biomass, photosynthetic picoplankton populations appeared to turn over rapidly and potentially contributed significantly to planktonic food webs in early spring and late summer.     

Grazing impact on the cyanobacterium Microcystis aeruginosa by the heterotrophic flagellate Collodictyon triciliatum in an experimental pond

We estimated the grazing impact of the heterotrophic flagellate Collodictyon triciliatum on the harmful, bloom-forming cyanobacterium Microcystis aeruginosa in an experimental pond during a Microcystis bloom from summer to winter in 2010. For these experiments, we calculated the grazing rates from the digestion rate of C. triciliatum and its food vacuole contents. During the study period, M. aeruginosa exhibited one bloom event with a maximum density of 1.1 × 10⁵ cells ml^?1. The cell density of C. triciliatum fluctuated from below the detection limit to 291 cells ml^?1. The number of M. aeruginosa cells ingested by C. triciliatum food vacuoles ranged between 0.4 and 10.8 cells flagellate^?1, and the digestion rate of C. triciliatum at 25 °C was 0.73 % cell contents min^?1. The grazing rate of C. triciliatum on the M. aeruginosa prey was 0.2–6.9 cells flagellate^?1 h^?1, and its grazing impact was 0.0–25.3 % standing stock day^?1. The functional response of C. triciliatum to the M. aeruginosa prey followed the Michaelis–Menten model of significance (r ² = 0.873, p < 0.001) in our experimental systems, in which the prey concentration varied from 1.0 × 10⁴ to 2.1 × 10⁶ cells ml^?1. The maximum grazing rate was 6.2 prey cells grazer^?1 h^?1, and the half-saturation constant was 1.2 × 10⁵ cells ml^?1. We present evidence that C. triciliatum grazing explained the remarkable decrease in M. aeruginosa cell density in the pond. The present study is the first demonstration of the high potential of protistan grazing on M. aeruginosa to reduce cyanobacterial blooms.     

Quantified distribution of diatoms during the stratified [2pt] period of Boadella reservoir

We collected data and samples, from June to November of 1999 and 2000, to in situ quantify the abundance of phytoplankton in Boadella reservoir. Samples were taken at different stations along the reservoir and diatoms were persistent in the epilimnion and were the main phytoplankton component, with a peak of abundance up to 5 10⁵ particles ml^–1. The diatom growth during the initiation of the summer bloom was high in the reservoir upstream concurrent with maximum Chlorophyll a concentrations. A delay in the onset of the diatom bloom, together with lower values of the volume concentration, was found in 1999 compared to the results in 2000 and was attributed to the different stratification of the reservoir as a result of meteorological conditions. The diatom population sank from the epilimnion by sedimentation and formed aggregates that accumulated at the bottom of the epilimnion. Sedimentation to the hypolimnion occurred at the end of the bloom, where peaks of Chlorophyll a were found.     

Possible food chain relationships between bacterioplankton,protozoans, and cladocerans in a reservoir

Ingestion of fluorescent particles by natural protozoan assemblage was studied in the Řimov Reservoir (Southern Bohemia) from April to October, 1987. Attached and free-living bacterial abundance, proportion of active bacteria, density of suspended particles and biomass of cladocerans were also monitored. Heterotrophic nanoflagellates (HNF; 5–12.8 10²ml⁻¹) were the dominant bacterial micrograzers during the spring period and consumed 3 to 9% of the total bacteria per day. After the spring phytoplankton bloom maximum densities of suspended particles and attached bacteria (up to 28% of the total counts) were found. Development of cladocerans in May sharply decreased the proportion of attached bacteria and kept them below 5% of the total counts. All the studied components of plankton except Cladocera decreased during the clearwater phase. The most significant drop was observed in the numbers of protozoans, and they were negligible for bacterial elimination. Bacterial losses during that time apparently were due to cladoceran grazing. During the summer period, ciliates (15–142 ml⁻¹) were mostly dominant micrograzers, and protozoan community grazing increased up to 21% of bacterial standing stock per day. The proportion of active bacteria was strongly correlated with protozoan grazing (r=0.83).     

Autotrophic Picoplankton: Community Composition,Abundance and Distribution across a Gradient of Oligotrophic British Columbia and Yukon Territory Lakes

Autotrophic picoplankton communities were examined in eleven oligotrophic lakes from a broad geographic region of western Canada, representing a variety of physico-chemical and biological conditions. During our study, several of the lakes were treated with additions of inorganic nitrogen and phosphorus fertilizers. Picoplankton communities in most lakes were dominated (>70%) by unicellular or colonial coccoid cyanobacteria, provisionally identified by morphological and autofluorescence properties as Synechococcus. Also common in some lakes were red-fluorescing cyanobacteria and Chlorella-like eucaryotes. Autotrophic picoplankters contributed from 36-63% to total chlorophyll, from >2-26% to total phytoplankton carbon, and from 29–53% to total photosynthesis. Average populations ranged from >5-10,000 cells·ml⁻¹ in winter and early spring to 65-75,000 cells · ml⁻¹ in summer and fall. Peak densities in most lakes occurred in August-September and most populations were within the epilimnion or metalimnion/hypolimnion boundary. Subsurface peaks were prevalent only in untreated, strongly stratified lakes. Eucaryotic picoplankters became dominant in acidic (pH < 6.2), humic lakes. Colonial picoplankters were more common in more productive interior lakes in August, and though present, were uncommon in coastal systems. Picoplankton populations exhibited large increases under ice in a Yukon lake, and their abundance and seasonal distribution showed little relation to temperature or to light. Fertilization of lakes resulted in picoplankton population increases (>2x) and the elimination of subsurface peaks. Nutrients were considered to be one of the major factors controlling population abundance in these oligotrophic lakes with average pH < 6.5.     

Picoplankton in Lake Maggiore,Italy

In 1992 we examined the morphological characteristics and space-time distribution of picoplankton cells in Lake Maggiore, a subalpine lake in which oligotrophication is in progress. We measured by image analyser the biovolume of autotrophic (APP), eukaryotic and prokaryotic. and heterotrophic (HPP) picoplankton. Among the APP < 2μm the yellow fluoresceing are the dominating cells in the euphoric zone. The red cells, mainly eukaryotic, on average are only 11% of the total abundance of cells < 5μm. The APP cell numbers range from 9.5 × 10³ cells ml⁻¹ to 1.3 × 10⁵ cells ml⁻¹ (average: 5 × 10⁴ cells ml⁻¹). Their mean biovolume shows a minimum value of 7.8mm³ m⁻³ in March and a maximum of 186.3mm³ m-³ in September. The contribution of biovolume of yellow cells to total phytoplankton biovolume varies between 0.3% and 27%. suggesting that picocyanobacteria, at this stage of lake recovery, are not yet a dominant component. The HPP cell density is two order of magnitude higher than the APP with a mean value of 2.6 × 10⁶ cells ml⁻¹. APP mean cell size fluctuates from a minimum of 0.5 μm to a maximum of 1.4urn (0.26–1.69μm³ volume), while HPP range from 0.4 to 0.7 um (0.07–0.57 μm³ volume), making it easier to distinguish them on a dimensional basis for most of the year. During the period of thermal stratification, a peak in abundance was noted in the central part of the metalimnion at depths receiving less than 10% of surface irradiance. The total picoplanktonic carbon fraction (APP and HPP) varied from 38 to 384 μgC 1⁻¹ with a mean value of 133μgC 1⁻¹ which represents 42% of POC collected on GF/C filters. Most of the picoplankton carbon is made up of HPP cells (34% of the total POC).     

Determination of Eubacterial and Cyanobacterial Size and Number in Lake Baikal Using Epifluorescence

Chroococcoid cyanobacteria, (mean size = 0.79 μm, likely Synchetocystis limnetica Popovsk) and total eubacteria (mean size = 0.33 μm), from Lake Baikal, USSR, were enumerated using epifluorescence microscopy and sized with image analysis. Bacterial densities ranged from 0.44 · 10⁶ cells ml⁻¹ at 250 m to 2.3 · 10⁶ cells ml⁻¹ at the surface. Mean eubacterial abundance was 1.3 · 10⁶ cells ml⁻¹. Cyanobacterial densities were more variable, ranging from 0.42 · 10⁴ cells ml⁻¹ at 250 m to 9.8 · 10⁴ cells ml⁻¹ at the surface, with a mean abundance of 2.7 · 10⁴ cells ml⁻¹. The cyanobacteria, in particular, occurred in clusters resembling “marine snow”. Our results indicate that Lake Baikal picoplankton size and density are similar to other large lakes but may have a more diverse community structure than in other large oligotrophic lakes.     

Yellow water in La Jolla Bay,California, July 1980. I. A bloom of the dinoflagellate, Gymnodinium flavum Kofoid & Swezy

During the latter half of July, 1980, a bloom of Gymnodinium flavum Kofoid & Swezy caused water discoloration in La Jolla Bay, California. This naked dinoflagellate dominated the phytoplankton, numeri- cally and by volume, and was found in concentrations as high as 6.15 × 10³ cells · ml^?1. It was most abundant near the surface above a shallow (5–10 m), sharp thermocline and a nitracline at 10 m. Near the end of July, the depth of maximum phytoplankton abundance descended and water discoloration was no longer visible at the surface even though areal concentrations of G. flavum did not decrease. Concurrent with changes in the vertical distribution of the phytoplankton, warm, nutrient-depleted water moved into the area and nitrate availability in the upper 20 m of the water column was drastically reduced. Measure- ments of the chemical composition of the phytoplankton do not, however, indicate progressive nutrient stress during the period of environmental change. We conclude that shoaling of the thermocline and nitracline associated with apparent upwelling were conducive to development of the bloom and that advection of warmer water from offshore led to disappearance of yellow surface water from the bay.     

GRAZING AND GROWTH OF THE MIXOTROPHIC CHRYSOMONAD POTERIOOCHROMONAS MALHAMENSIS (CHRYSOPHYCEAE) FEEDING ON ALGAE

The growth and grazing characteristics of Poterioochromonas malhamensis (Pringsheim) Peterfi (= Ochromonas malhamensis Pringsheim) (ca. 8 μm) feeding on phytoplankton, including the cyanobacteria Synechococcus sp. (ca. 2 μm) and Microcystis viridis (A. Brown) Lemmermann (ca. 6 μm) and the green alga Chlorella pyrenoidosa Chick (ca. 13 μm), were investigated in laboratory experiments involving the following treatments: (1) light without added algal prey (autotrophy), (2) light with added algal prey (mixotrophy), and (3) dark with added algal prey (phagotrophy). There were significantly higher cell numbers under mixotrophic and phagotrophic growth than under autotrophic growth. With phytoplankton as food, growth rates under both mixotrophy and phagotrophy were about two or three times higher than those under autotrophy, indicating that the algal diets were readily able to support the population growth of P. malhamensis. There were no significant differences in growth rate between mixotrophic and phagotrophic cultures during exponential growth. The ingestion rate of P. malhamensis with algal prey was also similar under both continuous light and dark. Poterioochromonas malhamensis ingested on average 0.27 M. viridis cells·flagellate^{− 1} ·h^{− 1} and 0.18 C. pyrenoidosa cells·flagellate^{− 1} ·h^{− 1} in continuous light and 0.25 M. viridis cells·flagellate^{− 1} ·h^{− 1} and 0.18 C. pyrenoidosa cells·flagellate^{− 1} ·h^{− 1} in continuous dark during exponential growth. The results showed that light had no effect on the growth and ingestion rates of P. malhamensis for phagotrophy during exponential growth. However, phagotrophic populations of P. malhamensis were incapable of growth in continuous darkness for longer than 5 days. Populations of P. malhamensis showed no increase when prey was added again after 4 days in continuous darkness, indicating that light is necessary for sustained phagotrophic growth of P. malhamensis. The study suggests that P. malhamensis, which has strong tolerance for light, is light dependent for phagotrophy.     

The microbial food web structure of a hypertrophic warm-temperate shallow lake, as affected by contrasting zooplankton assemblages

The composition of zooplankton is known to affect the structure of the microbial trophic web. The zooplankton of the hypertrophic Laguna Chascomús (Argentina) is generally dominated by rotifers and cyclopoids copepods. An unusual dominance by small-cladocerans was observed after a massive winter fish kill in 2007. We hypothesized that small-cladocerans would increase the grazing pressure on heterotrophic flagellates (HF), reducing the degree of coupling between HF and picoplankton. The aim of this study was to investigate the microbial food web structure under two contrasting zooplankton assemblages. The lake was sampled every other week between 2007 and 2009. The abundances of heterotrophic bacteria (HB) and picocyanobacteria (Pcy) laid among the highest values reported for aquatic systems (>10⁸ and 10⁷ cells ml^?1, respectively). Pcy averaged 53% of total picoplanktonic biomass. When small-cladocerans dominated zooplankton HF reached the higher abundance (>10⁵ cells ml^?1) and picoplankton showed the opposite pattern, while the proportion of grazing resistant morphologies (i.e. microaggregates of Pcy) was higher. In contrast, when rotifers dominated, HF abundance decreased and picoplankton increased. Our data suggest that the degree of HF–HB coupling was affected by changes in zooplankton dominance. In contrast to our initial hypothesis, the present results suggest that large numbers of rotifers (>5,000 ind. l^?1) are more efficient than small-cladocerans at controlling HF populations.     

The use of glucose to regulate pH values of culture media and increase the production of baculovirus (BmNPV) and foreign protein (HBsAg)

When BmN-4 and M-BmN cells were grown in shake flasks, the pH initially dropped and later increased. The increase in pH signaled a ‘metabolic switch’ that was used here as an indicator for initiating a supplemental glucose and glutamine feed. Using the pH-based fed-batch culture method described, the maximum cell densities of BmN-4 cells and M-BmN cells were increased from 30×10⁵ cells ml⁻¹ to 43×10⁵ and 52×10⁵ cells ml⁻¹, respectively. Correspondingly, the production of polyhedra (4·5×10⁵ OBs ml⁻¹) and HBsAg (574 ng ml⁻¹), from the infection of BmN-4 and M-BmN by wild-type and recombinant BmNPV viruses, respectively, were both significantly enhanced 50% and 100%, respectively. This feeding strategy was implemented with no advanced instrumentation yet facilitated significantly increased yield in shake flasks. The technique should benefit those in research laboratories employing the baculovirus expression system as a rapid and efficient production system.     

Carbohydrate metabolism in Manduca sexta during late larval development

The carbohydrate metabolism in Manduca sexta underwent significant changes during late larval development. Approximately 10% of fat body glycogen phosphorylase was active during the feeding period of the 5th instar, pharate-pupal development and after the pupal moult; it is concluded that glycogen synthesis prevailed. During the last larval and the pupal moult, as well as the wandering stage the percentage of active phosphorylase was significantly increased indicating that fat body glycogen stores were broken down to supply substrates to meet the demands of carbohydrate metabolism. In the course of the last larval moult and the wandering stage the fat body glycogen content decreased significantly from about 300 to about 200 μg mg⁻¹ dry mass substantiating that carbohydrates were released from the fat body. Prior to phosphorylase activation, the concentrations of total haemolymph sugars decreased significantly from about 12 to about 6 mg trehalose equivalents ml⁻¹ (last larval moult) and from about 18 to about 12 mg ml⁻¹ (wandering stage), and increased again slightly when phosphorylase was activated. The haemolymph glucose concentration decreased significantly from about 1.1 to 0.3 mg ml⁻¹ (last larval moult) and in the course of the 5th-instar feeding period from about 1.1 to 0.2 mg ml⁻¹, and remained at this level until the beginning of adult development. The amount of chitosan present in the cuticle increased steadily during the feeding period of the 5th instar from about 10 to 110 mg. It appears that fat body glycogen might be broken down during the last larval moult and the wandering period to provide substrates for chitin synthesis. A dramatic decrease in the amount of chitosan was observed prior to the pupal moult.     

Sedimentation of Nodularia spumigena and distribution of nodularin in the food web during transport of a cyanobacterial bloom from the Baltic Sea to the Kattegat

Nodularia spumigena is a toxic cyanobacteria that blooms in the Baltic Sea every year. In the brackish water of the Baltic Sea, its toxin, nodularin, mainly affects the biota in the surface water due to the natural buoyancy of this species. However, the fate of the toxin is unknown, once the cyanobacteria bloom enters the more saline waters of the Kattegat. In order to investigate this knowledge gap, a bloom of N. spumigena was followed during its passage, carried by surface currents, from the Baltic Sea into the Kattegat area, through the Öresund strait. N. spumigena cells showed an increased cell concentration through the water column during the passage of the bloom (up to 130 10³ cells ml⁻¹), and cells (4.2 10³ cells ml⁻¹) could be found down to 20 m depth, below a pycnocline. Sedimentation trap samples from below the pycnocline (10–12 m depth) also showed an increased sedimentation of N. spumigena filaments during the passage of the bloom. The toxin nodularin was detected both in water samples (0.3–6.0 μg l⁻¹), samples of sedimenting material (a toxin accumulation rate of 20 μg m^-2 day⁻¹), zooplankton (up to 0.1 ng ind.⁻¹ in copepods), blue mussels (70–230 μg kg⁻¹ DW), pelagic and benthic fish (herring (1.0–3.4 μg kg⁻¹ DW in herring muscle or liver) and flounder (1.3-6.2 μg kg⁻¹ DW in muscle, and 11.7-26.3 μg kg⁻¹ DW in liver). A laboratory experiment showed that N. spumigena filaments developed a decreased buoyancy at increased salinities and that they were even sinking with a rate of up to 1,7 m day⁻¹ at the highest salinity (32 PSU). This has implications for the fate of brackish water cyanobacterial blooms, when these reach more saline waters. It can be speculated that a significant part of the blooms content of nodularin will reach benthic organisms in this situation, compared to blooms decaying in brackish water, where most of the bloom is considered to be decomposed in the surface waters.     

In vitro assays on the susceptibility of four species of nematophagous fungi to anthelmintics and chemical fungicides/antifungal drug

Using nematophagous fungi for the biological control of animal parasitic nematodes will become one of the most promising strategies in the search for alternative chemical drugs. The purpose of this study was to check the in vitro activity of four anthelmintics, four chemical fungicides and two antifungal drugs on the spore germination of nematophagous fungi: Duddingtonia flagrans (SF170), Arthrobotrys oligospora (447), Arthrobotrys superba (435) and Arthrobotrys sp. (PS011). A modified 24-well cell culture plate assay was conducted to evaluate the susceptibility of nematophagous fungi against drugs tested by calculating the effective middle concentrations (EC₅₀) of each tested drug to inhibit the germination of fungal spores. EC₅₀ ranged between 0·7 and 47·2 μg ml⁻¹ for fenbendazole, thiabendazole and ivermectin, except levamisole (546·5–4057·8 μg ml⁻¹). EC₅₀ of tested fungicides was 0·6–2·3 μg ml⁻¹ for carbendazim, 55·9–247·4 μg ml⁻¹ for metalaxyl, 24·4–45·2 μg ml⁻¹ for difenoconazole, and 555·9–1438·3 μg ml⁻¹ for pentachloronitrobenzene (PCNB). EC₅₀ of two antifungal drugs was 0·03–3·4 μg ml⁻¹ for amphotericin B and 0·3–10·9 μg ml⁻¹ for ketoconazole. The results showed that 10 tested drugs, except for levamisole and PCNB, had in vitro inhibitory effects on nematophagous fungi. The chlamydospores of D. flagrans had the highest sensitivity to nine tested drugs, except for ketoconazole.     

Autotrophic picoplankton community dynamics in a pre-alpine lake in British Columbia,Canada

Autotrophic picoplankton (APP) were studied in Chilko Lake, a large, deep ultra-oligotrophic pre-alpine lake (elevation: 1172 m) in the south central coast mountains of British Columbia. Data from 1985 (untreated) and 1990 (treated) were used to compare and contrast APP community response to a whole-lake fertilization experiment. The APP communities of Chilko Lake were dominated by the coccoid cyanobacteria Synechococcus and its colonial morph which comprised about 99% of the APP community of Chilko Lake. Chlorella-like eukaryotic picoplankters and small cyanobacteria were rare, comprising < 1 % of the APP community. In 1990 autotrophic picoplankters contributed an average of 73% to total chlorophyll, and 54% to total photosynthesis. Average APP abundance ranged from lows of 4,000–5,000 cells ml^-1 in winter and spring to highs of 50000–150000 cells ml^-1 in early August with no apparent autumnal increase. APP populations were uniformly distributed in the epilimnion, but during calm periods in August often formed a peak near the metalimnion/hypolimnion boundary. Seasonal and vertical distribution patterns of APP showed little relation to temperature or to light. When nutrients were added to the lake in 1990, APP populations doubled within 3 wk of addition and average abundance (6.16 × 10⁴ cells · ml^-1) was twice 1985 APP numbers. Bottom-up control by scarce nutrient supplies is considered the primary factor regulating community composition and abundance during the initial population growth phase (June, July) with top-down control by grazing during nutrient colimitation periods when the epilimnion is deplete of both nitrogen and phosphorus (August, September).     

Feeding Rate of Brachionus plicatilis O. F. Müller on Two Types of Food Depending on Ambient Temperature and Salinity

Feeding rates of Brachionus plicatilis were studied for two types of food — algae Monochrysis lutheri and baker's yeast Saccharomyces cerevisae. The main regularities of changes in filtration rate and ration were studied in small culture volumes (1 ml) for adult amictic females depending on food concentration (1, 2, 4, 8 and 16 · 10⁶ cells · ml⁻¹), ambient temperature (16 and 26 °C), and salinity (5, 10, 15, 20, 25 and 30 ppt). B. plicatilis ration did not depend on the salinity, but was largely determined by temperature and food concentration. It was found that at 16 and 26 °C the dependence of the ingestion rate (ration) on food concentration differed greatly. A hypothesis was suggested to explain this phenomenon. A critical concentration of both types of food at which the increase in the rotifer ration ceased is 4 · 10⁶ cells · ml^−1. This is the minimum “background” food concentration for B. plicatilis mass cultivation. The average rations measured at the concentration of M. lutheri and S. cerevisae of 4 · 10⁶ cells · ml⁻¹ where 1.3 ± 0.1 and 4.8 ± 1.3 μg dry weight. · ind⁻¹ · day⁻¹ at 26 °C and 0.54 ± 0.1 and 1.9 μg d. w. · ind⁻¹ · day⁻¹ at 16 °C, respectively. The rations obtained in the laboratory were corrected for the conditions of rotifer commercial production in the open field in summer time. The correct values were 0.86 and 0.72 μg d. w. · ind⁻¹ · day⁻¹ for algae and yeast, respectively.     

Influence of Eutrophication on Bacteria in Two Fjords of the Western Baltic

Longitudinal transects in the Schlei Fjord (Kiel Bight) revealed strong increases of microbiological parameters from the entrance towards the landlocked end of the fjord. In the inner part up to 14 × 10⁶ bacteria ml⁻¹ (microscopical count), 77 × 10⁻¹ saprophytic bacteria ml⁻¹ (plate count) and a thymidine incorporation rate of 0.436 nmol 1⁻¹ h⁻¹ were observed. The data were compared with earlier results from the same system and those from the nearby located Kiel Fjord. The observations indicate a very high degree of eutrophication in the Schlei Fjord and a lesser one in the Kiel Fjord. The significance of total bacterial numbers and numbers of saprophytic bacteria as indicators for eutrophication and contamination is discussed.     

Production and purification of 2-phenylethanol by Saccharomyces cerevisiae using tobacco waste extract as a substrate

2-phenylethanol (2-PE), which is extracted naturally from plant or biotechnology processing, is widely used in the food and cosmetics industries. Due to the high cost of 2-PE production, the valorization of waste carbon to produce 2-PE has gained increasing attention. Here, 2-PE was produced by Saccharomyces cerevisiae using tobacco waste extract (TWE) as the substrate. Considering the toxicity of nicotine and its inhibition of 2-PE, the tolerance of S. cerevisiae was first evaluated. The results suggested that the production of 2-PE by S. cerevisiae in TWEs could be carried out at 2·0 mg ml⁻¹ nicotine concentrations and may be inhibited by 1·0 mg ml⁻¹ 2-PE. Thus, the compounds in the TWEs prepared at different temperatures were detected, and the results revealed that the TWEs prepared at 140°C contained 2·18 mg ml⁻¹ of nicotine, had total sugar concentrations of 26·8 mg ml⁻¹ and were suitable for 2-PE production. Due to feedback regulation, the 2-PE production was only 1·11 mg ml⁻¹, and the remaining glucose concentration remained at 13·78 mg ml⁻¹, which indicated insufficient glucose utilization. Then, in situ product recovery was further implemented to remove this inhibition; the glucose utilization (the remaining concentration decreased to 3·64 mg ml⁻¹) increased, and the 2-PE production increased to 1·65 mg ml⁻¹. The 2-PE produced in the fermentation broth was first isolated by elution from the resin with 75% ethanol and then by removing the impurities with 2·5% activated charcoal, and pure 2-PE was identified by gas chromatography mass spectrometry. The results of this study suggest that TWE could be an alternative carbon source for 2-PE production. This could provide an outlet tobacco waste as well as reducing the price of natural 2-PE, although more strategies need to be explored to improve the production yield of 2-PE by using TWE.     

Alteration of plankton communities and biogeochemical cycles by harmful Cochlodinium polykrikoides (Dinophyceae) blooms

Cochlodinium polykrikoides is a globally distributed, ichthyotoxic, bloom-forming dinoflagellate. Blooms of C. polykrikoides manifest themselves as large (many km²) and distinct patches with cell densities exceeding 10³ ml⁻¹ while water adjacent to these patches can have low cell densities (<100 cells ml⁻¹). While the effect of these blooms on fish and shellfish is well-known, their impacts on microbial communities and biogeochemical cycles are poorly understood. Here, we investigated plankton communities and the cycling of carbon, nitrogen, and B-vitamins within blooms of C. polykrikoides and compared them to areas in close proximity (<100 m) with low C. polykrikoides densities. Within blooms, C. polykrikoides represented more than 90% of microplankton (>20 μm) cells, and there were significantly more heterotrophic bacteria and picoeukaryotic phytoplankton but fewer Synechococcus. Terminal restriction fragment length polymorphism analysis of 16S and 18S rRNA genes revealed significant differences in community composition between bloom and non-bloom samples. Inside the bloom patches, concentrations of vitamin B₁₂ were significantly lower while concentrations of dissolved oxygen were significantly higher. Carbon fixation and nitrogen uptake rates were up to ten times higher within C. polykrikoides bloom patches. Ammonium was a more important source of nitrogen, relative to nitrate and urea, for microplankton within bloom patches compared to non-bloom communities. While uptake rates of vitamin B₁ were similar in bloom and non-bloom samples, vitamin B₁₂ was taken up at rates five-fold higher (>100 pmol⁻¹ L⁻¹ d⁻¹) in bloom samples, resulting in turn-over times of hours during blooms. This high vitamin demand likely led to the vitamin B₁₂ limitation of C. polykrikoides observed during nutrient amendment experiments conducted with bloom water. Collectively, this study revealed that C. polykrikoides blooms fundamentally change microbial communities and accelerate the cycling of carbon, some nutrients, and vitamin B₁₂.