The relationship between nutrient status and chemical composition of Peridinium cinctum during the bloom in Lake Kinneret

Changes in water chemistry and the major chemical and elementalconstituents of Peridinium cinctum have been followed duringthe 1976 growth season (February-June) in Lake Kinneret. Thedecline of the bloom was not associated with changes in anysingle physical or chemical parameter of the lake water, althoughthe ambient N:P ratio was higher before the peak of Peridinium.Carbon, nitrogen and chlorophyll in the cells were almost constantover the growth season, averaging 48, 4 and 0.9% dry weight,respectively. There was an initial drop in cell phosphorus from0.7% to 0.2% dry weight which then remained stable after April.During the bloom period the carbohydrate and lipid content ofPeridinium decreased, nucleic acid increased, whereas proteinshowed no definite trend. The results suggest that (a) Peridiniumis not severely nutrient limited during most of the growth season;and (b) criteria based upon cellular composition used to definenutrient status in other groups of algae, may not be directlyapplicable to armoured dinoflagellates.     

Encystment of Peridinium gatunense: occurrence, favourable environmental conditions and its role in the dinoflagellate life cycle in a subtropical lake

1. The abundance of cysts of the bloom‐forming dinoflagellate Peridinium gatunense in the sediments of Lake Kinneret and the effects of environmental conditions on encystment were studied in relation to bloom dynamics. Peak cyst formation coincided with the highest growth rate of the population, prior to bloom peak. 2. Peridinium cysts were counted in water and sediment corer samples from 2000 to 2003 and in archived sediment trap samples collected during 1993–94. The cyst data were examined in relation to ambient temperature and nutrient records, and revealed no direct correlation. 3. In laboratory encystment experiments with Peridinium cells collected from the lake, 0.2–3% of the vegetative cells encysted. Temperature, light and cell density had no significant effect on the percentage of encystment. 4. Cysts were always present in the lake sediments but their abundance in ‘non Peridinium’ years was much lower than after a massive bloom. Vegetative cells were always present in the water column after the collapse of the annual dinoflagellate bloom, potentially serving as the inoculum for the next bloom. We propose that the hardy cysts serve as an emergency ‘gene bank’ to initiate population build up following catastrophic die outs.     

The structure and dynamics of the phytoplankton assemblages in Lake Kinneret, Israel

The phytoplankton of Lake Kinneret, a warm monomictic lake,is dominated by a Pyrrhophyta-Chlorophyta assemblage. Four stagesof succession of planktonic algae occur in the lake, startingwith thermal and chemical destratification and ending with stratification. The index of diversity of the phytoplankton communities is highduring the destratification and mixed periods. The index reachesminimal values during late summer, when the ecosystem is subjectto strong physical, chemical and biological stresses. The diversityin Lake Kinneret increases with the increase in nutrients andnot with the increase in temperature. During most of the year, the nanoplanktonic forms are in greaternumbers than the netplankton species. This fact is correlatedwith the amounts of available nutrients in the lake. The annual averages of the wet autotrophic biomass in Lake Kinneretare very high in comparison with other warm lakes. The contributionof the nanoplanktonic species to the total algal biomass isvery small during the Peridinium bloom, but represents approximatelyhalf of the total algal biomass during the rest of the year. The concentration of nutrients in the water, together with theadverse competitive effect of Peridinium on other algae, areto a large extent responsible for the composition, successionand abundance of the phytoplankton assemblages in Lake Kinneret.     

SUPEROXIDE DISMUTASE ACTIVITY IN PERIDINIUM GATUNENSE IN LAKE KINNERET: EFFECT OF LIGHT REGIME AND CARBON DIOXIDE CONCENTRATION1

The activity of superoxide dismutase (EC 1.15.1.1, superoxide: superoxide oxidoreductase) (SOD) was determined in Peridinium gatunense Lemm. under natural and controlled conditions. SOD activity increased toward the end of the spring algal bloom in Lake Kinneret simultaneously with maximal photosynthetic activity and conditions of elevated ambient stress such as high irradiance. Activity staining of native polyacrylamide gel electrophoresis gels of bloom samples showed a similar pattern to the spectrophotometrically measured SOD. Both Mn SOD and CuZn SOD were present, however no Fe SOD was found in Peridinium. One of three isoenzymes of Mn SOD showed marked differential regulation of activity under stress. An increase in the quantity of the 32-kDa Mn SOD polypeptide during the bloom was found to be unrelated to senescence; it was assumed that this polypeptide was induced by stress. Thus, SOD in Peridinium undergoes physiological and molecular acclimation to seasonal environmental changes. When Peridinium was exposed to various O₂ and CO₂ concentrations in culture, CuZn SOD significantly increased under high C0₂ concentrations and normoxic conditions (20% O₂). However, at high irradiances, Peridinium cultures exposed to low and high CO₂ concentrations also had similar CuZn SOD activity. It was concluded that stressful irradiance is the overriding cause of increased SOD activity in both lake samples and in cultures of Peridinium.     

HOT WATER EXTRACTABLE PHOSPHORUS—AN INDICATOR OF NUTRITIONAL STATUS OF PERIDINIUM CINCTUM (DINOPHYCEAE) FROM LAKE KINNERET (ISRAEL)?1

The intracellular levels of hot water extractable and total phosphorus were determined in the dinoflagellate Peridinium cinctum. f. westii (Lemm.) Lef. for natural samples from the bloom in Lake Kinneret and from laboratory cultures. Amounts of phosphorus (P) in the hot water fraction, relative to total cellular phosphorus, were similar in lake Peridinium and in cells grown in high ambient orthophosphate (P_i) media (3–6 mg P · l^?1). The absolute amounts of hot water extractable P in natural cell and those cultured at lower P_i concentrations (0.02–0.05 mg P · 1^?1) were similar, although average P_i in lake water were 4 μg · l^?1. Under most growth conditions the hot water extract contained approximately equal amounts of molybdate reactive phosphorus (MRP) and non-MRP. Short chain (6–9 units) polyphosphates (mol wt 630–950) probably constituted the bulk of the non-MRP pool, which was hydrolysable by alkaline phosphatase and may serve as a precursor for a more permanent P store. Intracellular P levels and distribution were not directly dependent on external P_i concentrations but may be determined by the N:P atomic ratio or overall external ionic milieu. Peridinium grown in low ambient P_i released significant amounts of non-MRP compounds. In Lake Kinneret, for at least most of the bloom period, Peridinium does not appear to be limited by P supply.     

Differences in nitrate and ammonia uptake among components of a phytoplankton population

We examined the NO₃^– and NH₄⁺ uptake capabilities of thedinoflagellate Peridinium cinctum and of the accompanying nanoplanktonduring the spring P. cinctum bloom in Lake Kin-neret. Throughoutthe Peridinium season, the smaller algae had greater affinitiesand faster specific uptake rates for both NO₃^–and NH₄⁺It appears that P. cinctum cannot directly compete with nanoplanktonfor nitrogen nutrients. Other factors such as the ability ofdinoflagellates to swim freely in the water column and low grazingpressures may explain their dominance in the lake.     

Sulphate reduction in the hypolimnion and sediments of Lake Kinneret, Israel

1. Lake Kinneret is a warm (13–30°C) monomictic lake. Between January and June a heavy annual bloom of the dinoflagellate Peridinium gatunense dominates phytoplankton biomass (250 g m^?2). At the beginning of the summer, degradation and decomposition of the Peridinium biomass occurs, serving as a trigger for intense sulphate reduction in the hypolimnion and sediments. 2. The rates of sulphate reduction in the sediments varied seasonally from 12 to 1700 nmol SO₄.^?2 reduced cm^?3 day^?1 in December and July, respectively. The availability of organic matter and sulphate is high in June after the crash of the Peridinium bloom and the beginning of stratification and is lowest in December before overturn. 3. Sulphate concentrations in the hypolimnion range between 0.52 mM and 0.20 mM during mixing (January-April) and before overturn (December), respectively. The depletion in sulphate in the hypolimnion is stoichiometrically correlated to the increase in sulphide. The lake is not depleted of sulphate at any time, so the sulphate reduction process in Lake Kinneret is not limited by sulphate concentrations except in the sediments just before overturn.     

Meteorological factors affecting the bloom of Anabaenopsis raciborskii Wolosz. (Cyanophyta:Hormogonales) in the shallow Lake Balaton, Hungary

There was a heavy bloom of a nitrogen-fixing blue-green algaAnabaenopsis raciborskii Wolosz. in Lake Balaton in September-October1982. The authors studied the dynamics of the phyto- and bacterio-plankton of the lake by daily and weekly samplings. Some meteorologicalfactors were also considered. It could be concluded that thecauses of the bloom were accumulating nutrients being enrichedjust before the bloom-period suddenly washed into the lake byheavy rains, followed by windless warm days (water temperatures26–29°C). An expressed correlation between bacterio-and phytoplankton indicates their close trophic relationship.     

The role of phosphatases in the metabolism of Peridinium cinctum,from Lake Kinneret

The annual algal bloom (February–June) in Lake Kinneret consists almost entirely of the dinoflagellatePeridinium cinctum f.westii (Dinophyceae). To clarify the role of phosphatases in the alga, experiments were carried out using cells from culture or from the lake. In culture, as the external ambient orthophosphate (Pi) concentration decreased, alkaline phosphatase activity increased (and to some extent acid phosphatase activity, as well). Hot water extractable P decreased, although molybdate reactive phosphorus (MRP) appeared to be utilized in preference to the non-MRP component of this pool. Alkaline phosphatase inPeridinium collected from the lake as well as cells grown in culture under a high (3–6 mg l^–1) ambient Pi concentration in both continuous light and a 12:12 light-dark cycle, showed a diurnal fluctuation in activity. These results, together with previous observations suggest that the phosphatases inPeridinium are controlled by changes in intracellular phosphorus levels (other than the hot water extractable pool) and/or by other metabolic processes not directly involved in P nutrition.     

Aphanizomenon ovalisporum (Forti) in Lake Kinneret, Israel

The filamentous cyanobacterium Aphanizomenon ovalisporum wasobserved for the first time in Lake Kinneret in August 1994and formed a prominent bloom from September through October.Aphanizomenon ovalisporum reappeared in diminished amounts inthe summer and fall of 1995. These events are the first recordof significant quantities of a potentially toxic nitrogen-fixingcyanobacterium in this lake. No definite provenance of inoculumhas been identified, although A.ovalisporum was also observedin a newly reflooded area (Lake Agmon) in the catchment. Unusuallyhigh water temperatures and low wind inputs were observed priorto and during the A.ovalisporum bloom period. These, togetherwith possibly enhanced availability of phosphorus or other growthfactors, may have contributed to the cyanobacterium growth in1994. Phosphorus limi tation, as indicated by high cellularalkaline phosphatase activity, the onset of stormy conditionsand a fall in water temperatures led to the demise of the 1994bloom. Although the A. ovalisporum bloom in 1994 had no seriousdirect impact on water quality, the continued presence of apotentially toxic cyanobacterium in Lake Kinneret, a major nationalwater supply source, is a cause for serious concern.     

Seasonal and environmental influences on antioxidative protection inPeridinium gatunense in Lake Kinneret

As the only freshwater lake in Israel, Lake Kinneret serves a number of important functions which directly rely upon the viability of the water. The annual outbreak of a dinoflagellate bloom strictly governs the nature of the macro and micro food web and ultimately determines water quality.The freshwater dinoflagellatePeridinium gatunense is subject to a wide range of environmental stresses throughout the spring bloom period. It was confirmed that SOD played an important antioxidative maintainance role throughout the bloom, especially during periods of relatively high photosynthetic activity (820 mg C m^–2 day^–1), when activity reached 500 Units SOD mg protein^–1. In addition, high light stress (>300 mol photons m^–2 s^–1) induced SOD activity, despite the low dissolved inorganic carbon (DIC) concentrations at the end of the bloom (1.3 mM). Catalase activity was only significant at the end of the bloom, peaking at 120 mol O₂ mg protein^–1 min^–1, when induced by photorespiratory activity.A series of experiments withPeridinium cultures showed that 2 × 10^–4 M ascorbate inhibited catalase activity >50% within 15 min incubation, bothin vivo andin vitro. It is suggested that the high concentrations of ascorbate, found previously inPeridinium during early and mid-bloom (0.2–1.6 mM), not only eliminate H₂O₂ build-up, but also prevent (directly or indirectly) the induction of catalase.     

PHOSPHORUS,NITROGEN AND THE GROWTH OF ALGAE IN LAKE KINNERET1

The intracellular concentrations of carbon, nitrogen, phosphorus and chlorophyll a of phytoplankton and zooplankton in Lake Kinneret were determined from 1969 to 1973. The ratios C:P, C:N, chlorophyll a:P, chlorophyll a:N of the algae showed fluctuations which could be related to the nutrient conditions that influence the annual pattern of phytoplankton development, especially in respect to the dinoflagellate bloom of Peridinium cinctum (OFM) Ehr. f. westii (Lemm.) Lef. Relatively high intracellurar P values at the start of the bloom indicated adequate availability of this nutrient and luxury consumption over a short period of time. Later, Peridinium continued to grow despite unusually high C:P ratios (> 300:1). In most years, phosphorus may have eventually limited growth, however, in 1970, the bloom censed despite comparatively high intracellular P concentrations. These observations, together with supplementary evidence from nutrient addition experiments and determinations of specific alkaline phosphatase levels, indicated that, for most of the growth phase of the bloom, Peridinium cells were not directly limited by P. The decline of the bloom usually, but not always (e.g., in 1970), was marked by very high C:P ratios. Thus, a shortage of P may often be a contributory factor to the cessation of the Peridinium bloom and may be limiting phytoplankton growth in the fall. Over the years 1969–73, possibly due to an overall drop in salinity, there appears to be a trend to lower levels of biologically bound phosphorus in Lake Kinneret, without a concomitant decrease in carbon biomass.     

Effect of temperature on growth of the cyanobacterium Aphanizomenon flos-aquae in Lake Biwa and Lake Yogo

The water bloom‐forming cyanobacterium Aphanizomenon flos‐aquae Ralfs ex Bornet et Flahault (Nos‐tocales, Cyanophyceae) appeared in Lake Biwa and Lake Yogo in 1999 for the first time. The morphological characteristics were described using natural samples. In contrast to the other water bloom‐forming cyanobacteria such as Microcystis and Anabaena in Lake Biwa and Lake Yogo, the small summer population of A. flos‐aquae is apt to grow in winter, suggesting the low temperature preference or tolerance of this species. In order to clarify the effect of temperature on the growth, culture experiments were conducted using an axenic strain isolated from Lake Biwa. The strain could grow at above 8°C with an optimum temperature ranging from 23 to 29°C, and survived even at 5°C for at least 25days under low light conditions. Although these results confirmed the ability of the bloom formation during late autumn and winter, it is still unclear why the Aphanizomenon bloom occurred at temperatures of ca 10°C in December and not immediately after the disappearance of Microcystis and/or Anabaena bloom during autumn.     

Lake Kinneret phytoplankton: Response to N and P enrichments in experiments and in nature

A series of water samples from Lake Kinneret was supplemented with 100 µM N (as NH₄ or as NO₃ and/or 10 µM orthophosphate-P. The yield of phytoplankton both as chlorophyll and in cell numbers of major species was determined after a two-week incubation. During these experiments, some of the algae present initially never multiplied (e.g. Peridinium and Peridiniopsis spp. Cryptomonas spp., Rhodomonas spp. and Crysochromulina parva); others e.g. Anomoeoneis exilis, Synedra sp., Chlamydomonas sp., Elakatothrix gelatinosa), undetected in the original sample, grew out during the incubation. Chlorophyte species (the majority of commonly observed forms in the lake) responded most readily to added nutrients.The results of these enrichment experiments were related to the long-term record of phytoplankton populations observed in the lake and suggest that through summer and fall, when ambient levels of both P and N are minimal, P was generally, but not always, the most limiting nutrient for algal growth. In the spring, after the decline of the Peridinium bloom, P appeared to be limiting the growth of Chlorophyta. Although most algal species grew equally well on NH₄ or NO₃, some species appeared to respond preferentially either to the former (Coelastrum, Chodatella) or to the latter (Chroococcus, Anomoeoneis) source of N.     

Some observations on the green planktonic alga, Botryococcus braunii and its bloom form

The cells and colonies of Botryococcus braunii laboratory cultureswere examined by interference and scanning electron microcopyand compared with cells isolated from a bloom in Lake Kinneret,Israel. The green cells were located in cups representing theparental cell wall; the cell walls of successive daughter cellsappeared to be fused to the parent and daughter cells wherethey were contiguous. The arrangement of green cells in laboratorycultures was consistent; groups of 2 or 4 cells formed a unitand these units appeared joined together at their bases to formclusters. Green cells from the lake bloom appeared in irregularclusters of units of 2, 3 or more cells. Red bloom cells appearedto be dead with each cup compressed and empty with a hole showingat the cell surface. A hypothesis describing the role of senescenceand nitrogen depletion, based on cytological, ecological, andchemical data, is invoked to explain the change of the bloomcells from green relatively low lipid to orange (or red) highlipid cells.     

The IJsselmeer and its phytoplankton--with special attention to the suitability of the lake as a habitat for Oscillatoria agardhii Gom

The IJsselmeer (surface area 1200 km², mean depth 4.5 m, residencetime 0.4 year, phosphorus load 7 g m^–2 year^–1) isa very important conservation area. Regular summer bloomingof Oscillatoria spp. can depreciate this value, so the boundsof possibility of this kind of blooming have been investigated.Therefore samples were taken along the shore and in the openwater from 1974 to 1982, continuous temperature profile measurementswere made in the same period in the middle of the lake and insitu primary production was measured in 1976 and 1977. The phytoplanktonconsists of green algae throughout the year, diatoms in spring,and blooms of Microcystis aeruginosa in summer. Blooming ofOscillatoria agardhii Gom occurs regularly in summer along theFrisian shore. In 1976, however, a heavy bloom of this algaoccurred in the whole lake. Comparing the IJsselmeer with shallowerOscillatoria-lakes in the Netherlands distinct differences arepresent concerning biomass, chlorophyll a content, relativevolume of the euphotic zone and light-dark cycle. Not only thelarger depth and extensiveness of the IJsselmeer are unfavourablefactors for Oscillatoria, but also the separation by land reclamationof many of the shallow littoral regions from the main body ofthe lake. High temperature and microstratification are neededto develop a bloom in the whole lake.     

The spatial distribution of temperature, oxygen, plankton and fish determined simultaneously in Lake Kinneret, Israel

Temperature and concentrations of oxygen, phytoplankton, zooplanktonand fish were measured simultaneously on the night of 28 February-1March 1991, in Lake Kinneret, Israel. High concentrations ofoxygen, up to 19.9 mg l^–1 (207% saturation), were recorded.The phytoplankton was dominated by the dinoflagellate Peridiniwngatunense, which was horizontally and vertically unevenly distributed.We hypothesize that the oxygen supersaturation was the resultof a high standing stock of Peridinium, combined with high irradianceinput and mild wind-generated turbulence. The relationship betweenthe concentration of oxygen and Peridinium density was highlysignificant, both above the thermocline (negative correlation)and below the thermocline (positive correlation). Zooplanktonbiomass was dominated by cladocerans and cyclopoid copepods.The spatial distribution of these groups was not correlatedwith other measured parameters. Rotifers and calanoid copepodswere highly abundant in the northern part of the lake, and significantlyrelated to oxygen concentrations. It is suggested that the distributionsof rotifers and calanoid copepods are affected by the JordanRiver inflow. fish abundance was not correlated with limnologicalparameters or other biological components. We conclude thatthe distribution of the dominant fish species was governed byfactors other than those measured in this study.     

The ascorbate system and lipid peroxidation in stored potato (Solanum tuberosum L.) tubers

The changes in the components of the ascorbateglutathione systemduring the storage of potato (Solanum tuberosum L. cv. Spunta)tubers for 40 weeks at both 3C and 9C were studied in relationto lipid peroxidation. The level of malondialdehyde was foundto be higher at 3C than at 9C throughout storage. Thus, lipidperoxidation, which is the main cause of membrane deterioration,was accelerated at the lower temperature. Catalase activityincreased throughout storage independently of temperature. Theascorbate content of tubers decreased during storage both at3C and at 9C, as in other ageing processes. However, ascorbateperoxidase activity reached a maximum after about 8 weeks ofstorage, then declined at 9C, but held a higher level at 3C.The dehydroascorbic content also reached a maximum after about8 weeks and was significantly higher in tubers stored at 3C.These findings indicate a greater utilization of ascorbate byascorbate peroxidase at the lower temperature. Ascorbate freeradical reductase, dehydroascorbate reductase and glutathionereductase, the enzymes involved in the regeneration of ascorbate,were not affected by temperature and remained quite unchangedthroughout storage. It can be concluded that the ascorbate systemis involved in the scavenging of the free-radicals responsiblefor lipid peroxidation in stored potato tubers, at least atlow temperatures and in the first period of storage. Key words: Ascorbate, lipid peroxidation, potato tubers, Solanum tuberosum L     

In situ and experimental evidence of the influence of turbulence on cell division processes of Peridinium cinctum forma westii (Lemm.) Lefèvre

Comparison of the diel variations of the wind intensity and the division rate (DR) of Peridinium cinctum forma westii (Lemm.) Lefèvre in situ reveals that the intensity of the wind blowing throughout the whole day does not affect the DR. On the other hand, a strong inhibitory effect is noticed when the wind episodes occur during the time period 18.00–02.00 h. Systematic hourly sampling and staining of Peridinium cells showed that nuclear division takes place between 23.00 and 02.00 h and is completed before cytokinesis begins. Thus the time period 18.00–02.00 h corresponds to the premitotic and mitotic phases of cell division, and the turbulence generated by the wind affects the process of nuclear division.

The relationship between water turbulence and the DR of Peridinium which was observed in Lake Kinneret (Israel) has been checked under experimental conditions. Peridinium was grown without shaking, with continuous rotary shaking and with intermittent shaking at 100 r min^-1. The specific growth rate (k), generation time (G) and mortality rate were followed and compared. The results obtained confirm the facts observed in situ and clarify some aspects. Intermittent shaking of 2 h day^-1 during the dark phase reveals the inhibitory effect of agitation on nuclear division. Continuous shaking causes a high rate of cell mortality. Shaking during the light period does not affect the division process.

The effect of turbulence on the DR of Peridinium explains why the timing of the bloom in Lake Kinneret is a function of the duration and intensity of the mixing period in the lake.     

Effects of thermal effluents from the Bergum power station on the phytoplankton in the Bergumermeer

Summary The Bergum power station (600 MW) of the Friesian Provincial Electricity Board is situated at the northern shore of the Lake Bergum. The lake has a mean depth of 1.3 m and a surface area of 4.4 km². Its northern half is separated by a break-water into an intake area in the north-west and a discharge area in the north-east.The Lake Bergum is connected with other water bodies in the northern provinces of the Netherlands by four canals. The whole yaer various amounts of water enter Lake Bergum mainly from the western canal (Prinses Margrietkanaal) and to a lesser extent from the southern canal (De Lits). In wet seasons lake water flows off, mainly after passing the power station, to the northern canal (De Zwemmer); then the heated water (22 m³.sec_–1) does not enter the discharge area of the lake. When evapo-transpiration exceeds precipitation lake water flows off mainly to the eastern canal (Kolonelsdiep). In these relatively dry periods most of the heated water returns to the lake in the discharge area.We found that the mean increase in water temperature effected by the condensors of the power station was ca. 5°C; the maximum increase was 7.5°C. On average about 25% of the whole lake had a noticable higher (1°C) temperature than the intake water, only 6.5% was about 2°C above ambient temperatures.For about 3.5 years (1974–Sept. 1978) water samples for analysis of the chlorophyll concentrations of the different areas within the lake and the surrounding canals were taken every week during the growing season, and fortnightly during the winter period. The chlorophyll concentrations of the intake water were about 5% higher than those of the discharge water leaving the power station. Near the mouth of the northern canal in the discharge area still small, but significant lower chlorophyll concentrations were found. The southern half of the lake, in which practically no elevated water temperatures were found, had significant higher chlorophyll concentrations (10–15%) than the intake area. Water entering the lake from the western canal had significant (10–15%) lower chlorophyll concentrations than the intake area of the lake. Probably, relatively chlorophyll-poor canal water and chlorophyll-rich water from the southern lake area mix in the intake area. While the water passes the power station the chlorophyll concentrations decrease. In the discharge area of the lake the chlorophyll concentrations of the discharge water gradually increase again to values equal to those of the intake area.During the last 2 years of the research period oxygen production and consumption experiments were conducted almost every month. In each experiment light and dark botties containing intake and discharge water were suspended in water with both water temperatures. The light intensities during the incubation periods (2–3 hours) were chosen according to maximum production values. The incubations were started within one hour and/or one day after sampling. Directly after sampling gross productivity of the intake water incubated at discharge temperatures was about 1.5 times as high as at intake temperatures. The gross productivity of the discharge water was always somewhat lower than the gross productivity of the intake water incubated at corresponding temperatures. After one day this inhibiting effect of passage through the power station had increased, even when the discharge water had been cooled down to intake temperatures immediately after sampling.The oxygen consumption of the discharge water incubated at discharge temperatures as well as at intake temperatures was about 1.3 times the oxygen consumption of the intake water at intake temperatures. After one day the discharge water, which had stayed at discharge temperatures, consumed 1.6–1.7 times as much as the intake water incubated at intake temperatures. The oxygen consumption of the discharge water which had been cooled down to intake temperatures directly after sampling, was after one day still 1.3 times the oxygen consumption of the intake water at intake temperatures.This research was financially supported by the Ministerie van Volksgezondheld en Millieuhygiëne (Ministry of Public Health and the Environment). An extensive report (in Dutch) will be published this year.