INTRASPECIFIC COMPARISONS OF NITRATE UPTAKE IN THREE MARINE DIATOMS1

Short-term (within 5 min) and long-term (≤2 h) rates of nitrate uptake were determined for the marine diatoms, Nitschiella longissima (Cleve), Skeletonema costatum (Greville) Cleve and Asterionella japonica (Cleve). Pigment levels, cell carbon, nitrogen and cell volume were also determined for cells in the logarithmic and stationary phases of growth. For each species, one clone isolated from oligotrophic coastal water and one clone isolated from eutrophic coastal water were compared. Long-term NO₃^? uptake typically followed saturation kinetics describable by the Michaelis-Menten expression. Under experimental conditions, half-saturation constants ranged from 0.6 to 2.2 μM NO₃^?. Generally, the oligotrophic clones had lower Ks and V_max (on a per cell basis) than their eutrophic counterparts, though this was only statistically significant in one pair of clones. Eutrophic and oligotrophic clones also differed in their short-term response to nutrient addition; oligotrophic clones showed greatest rate of uptake at the lowest nitrate addition while uptake by eutrophic clones increased with increasing nitrate concentration. However, all clones had very similar V_max values expressed on a dry weight basis. Under N-starvation, cellular C and pigment levels (and N to a lesser extent) generally declined more in eutrophic than in oligotrophic clones. While the differences between inshore and offshore clones were not great, the results are consistent with the hypothesis that eutrophic waters support algae which grow faster and are less conservative biochemically than cells in oligotrophic waters.     

Rates of photosynthesis of two lichens and of their isolated algal components

Abstract

The rate of photosynthesis of two lichen species (Peltigera leucophlebia and Ramalina farinacea) was found to be 30 to 40% that of spinach leaf dises and 20% that of the free-living alga Chlorella when the results were expressed on a per mg chlorophyll basis. When the algae were isolated from the thalli, the rate of photosynthesis per mg chlorophyll increased for Ramalina farinacea and decreased for Peltigera leucophlebia. Product analysis indicated that the products of photosynthesis depended on the association of the alga with the fungus: algae isolated from the thalli showed a «shift» in products from sugars and sugar alcohols. to compounds such as organic acids. The results suggest that a symbiotic relationship with a fungus alters both the rate and products of algal photosynthesis.     

Observations in guanotrophic environments

Summary Examples are given of initial guanotrophy in acid oligotrophic environment and of stabilized guanotrophy of long standing, both in acid oligotrophic and eutrophic environment.Characteristic of a guanotrophic environment is the accumulation of phosphate. In hard waters phosphate is accompanied by large amounts of saline nitrogen compounds. In soft waters the saline nitrogen production seems to be inhibited through low bacteriological activity. In eutrophic guanotrophic environments oxygen production and biochemical oxygen demand are both high. In oligotrophic guanotrophic environments the oxygen content as a rule does not reach saturation and biochemical oxygen demand is fairly low. The amounts of chloride and calcium do not change significantly by the addition of excrements of birds.Diatoms, blue green algae and desmids are very scarce in guanotrophic environments. In hard waters mesosaprobic forms are present in the plankton community. In soft waters no strong saprobic tendencies could be found.During the initial stage of guanotrophy in an acid oligotrophic environment, the desmids disappear together with other sensitive species as Dinobryon pediforme and Bosmina obtusirostris. Unicellular flagellates as Chlamydomonas appear in increasing numbers. Several factors in the environment respond to the changes by increasing fluctuations of the values recorded.There was evidence of transport and introduction of microorganisms by waterfowl.     

Nitrogen as a Factor Affecting Algal Growth Potential of an Oligotrophic Coastal Environment of Eastern Mediterranean Sea

Potential nitrogen limitation to chl a production in surface waters of Saronicos Gulf, Aegean Sea was assayed using the alga Pavlova lutheri as the test organism. The oligotrophic and eutrophic water types of this area were compared by in situ and in vitro chl a production estimations. Additions of ammonium alone as well as in combination with complete nutrient enrichment were made to the oligotrophic waters and the algal growth yield was determined and compared with the corresponding yield in unenriched water cultures. The results from routine nutrient analysis and bioassay experimentation support the view that nitrogen has a priority among the factors limiting phytoplankton growth in the Eastern Mediterranean Sea.     

Photosynthesis,photooxidation of chlorophyll and fluorescence of normal and manganese-deficient Chlorella with and without hydrogenase

Summary Growth, chlorophyll content, chloroplast structure, photosynthesis, photooxidation of chlorophyll and fluorescence were studied in normal and manganese-deficient, closely related Chlorella strains with hydrogenase (Chlorella vulgaris f. tertia 211-8k) and without hydrogenase (Chlorella vulgaris 211-8m).Under Mn-deficient conditions, algae with hydrogenase grow slowly for several weeks without becoming chlorotic and without any major change in thylakoid structure, whereas those without hydrogenase show a rapid loss of most of their chlorophyll, followed by a breakdown of thylakoid structure. In algae without hydrogenase, the inhibition of photosynthesis by Mn deficiency is much less pronounced when photosynthesis is determined on a chlorophyll rather than on a cell-volume or dry-weight basis. Thus the little remaining chlorophyll of these algae is photosynthetically much more active than the chlorophyll of the Mn-deficient, non-chlorotic algae with hydrogenase.Photooxidation of chlorophyll under pure O₂ in very strong light is always accelerated by Mn deficiency.Only in algae containing hydrogenase is there under aerobic conditions a pronounced peak of fluorescence at the beginning of illumination. This is indicative of a high degree of reduction of Q, the primary electron acceptor of System II of photosynthesis. The fluorescence peak can be eliminated by either 1 min preillumination with far red (=717 nm) or by treatment in the dark for 1 hr with pure O₂. In algae without hydrogenase, in contrast, fluorescence intensity at the onset of illumination is lower than the steady-state level, indicating an oxidized state of Q. In these algae a high start of fluorescence can only be produced by prolonged anaerobic incubation. These results indicate that even under aerobic conditions algal hydrogenase, or a biochemical system very closely associated with it, has some residual activity which enables it to feed electrons into System II of photosynthesis, thereby keeping Q in a reduced state with correspondingly high fluorescence at the beginning of illumination. In organisms without hydrogenase, in contrast, this can only be achieved by prolonged anaerobiosis. In addition, the presence of hydrogenase seems to protect the chlorophyll against photooxidative destruction when the cells are under Mn deficiency.This paper is dedicated to Professor A. Pirson on the occasion of his 60th birthday.     

CHARACTERIZATION OF TWO CHLORELLA VULGARIS (CHLOROPHYCEAE) STRAINS ISOLATED FROM WASTEWATER OXIDATION PONDS1

We report here on the characterization and isolation of two ecotypes of Chlorella vulgaris Beyerinck that coexist in wastewater reservoirs. One ecotype (C1) contains high amounts of chlorophyll b, is capable of autotrophic growth, and can utilize only a few organic solutes for growth. The second ecotype (C2) contains low amounts of chlorophyll b, requires vitamin B₁₂, and can support its growth with a broad range of organic compounds. Of the two ecotypes, the latter showed slower growth rates when light was the sole source of energy. Cells of C2-type Chlorella attained higher photosynthetic activities than C1-type cells at saturating irradiances. However, their low chlorophyll b content and lower light utilization efficiency suggest that C2-type Chlorella contains relatively low amounts of light-harvesting antennae, a disadvantage in severely light-limited ecosystems like wastewater reservoirs. We hypothesize that the two Chlorella types coexist by adopting different lifestyles: C1-type cells rely largely on their photosynthetic potential for energy conservation and growth, whereas C2-type cells may exploit their heterotrophic properties for this purpose.     

Comparison of anaerobic mineralization processes in sediments between littoral reed and offshore sites in a shallow hypertrophic lake

During three complete annual cycles, chlorophyll a concentrations and primary production rates of algae epiphytic on Phragmites australis in eutrophic Lake Belau were determined. Primary production rates reached a peak during spring due to the growth of diatoms and filamentous green algae. The chlorophyll-specific rates of photosynthesis were significantly higher during periods of stratification and increased exponentially with an increase in water temperature. No photoinhibition was observed, even at high irradiances. I _k values were higher in summer than during periods of circulation.     

Phytoplankton biomass and distribution in a shallow eutrophic lake (Lake George,Uganda)

Summary Lake George, a shallow lake in western Uganda, supports a permanent and dense crop of phytoplankton, and may be regarded as eutrophic although the ambient concentrations of inorganic nitrogen and phosphorus are low. The figures for the annual nutrient loadings (Viner and Smith, 1973) would suggest, however, a eutrophic lake when analysed on the scheme of eutrophication proposed by Vollenweider (1968).The horizontal distribution of chlorophyll a shows a concentric pattern, with the maximum values occurring towards the center. This horizontal variation is thought to reflect water movements, and a general pattern of water flow is proposed.The majority of the species show no seasonal variation but populations of both Anabaena and Melosira show annual variations. These two species also have a horizontal distribution pattern which is the reverse of other species. This pattern is used to support the proposed movements of water.Phytoplankton generation times are discussed in relation to the diurnal cycle occurring in Lake George.     

Phototrophic Picoplankton in Temperate Lakes: Seasonal Abundance and Importance along a Trophic Gradient

The seasonal development of autotrophic picoplankton was investigated in seven Danish lakes representing a eutrophication gradient. Highest cell abundance between 1.5 to 6 × 10⁵ cells ml⁻¹ were found in mid-summer. Minor peaks were observed in spring. In winter, densities were below 10³ ml⁻¹. The highest relative picoplankton contribution to total autotrophic biomass also occurred in mid-summer. In the eutrophic lakes and one humic lake the average seasonal contribution of picoplankton to total chlorophyll was below 1% increasing to 5-8% in the meso- and oligotrophic clear water lakes. During short periods the proportion of picoplankton did reach 25%. The higher relative importance of picoplankton in less productive lakes was not due to higher actual chlorophyll concentrations, but due to a much more pronounced response by larger algae at higher nutrient loading. Both cyanobacteria and eukaryote organisms were present as picoplankton. Only eukaryotes were found in one eutrophic lake and an acidic, humic lake. In the eutrophic lakes eukaryote picoplankton was dominant; both with respect to cell densities and biovolume, whereas cyanobacteria dominated the two meso-oligotrophic lakes. Autotrophic picoplankton were present in all lake types, however their importance seemed to be less in most eutrophic lakes than in less productive, meso-oligotrophic lakes.     

Brackish Eutrophic Water Treatment by Iris pseudacorus L.-Planted Microcosms: Physiological Responses of Iris pseudacorus L. to Salinity

Iris pseudacorus L. has been widely used in aquatic ecosystem to remove nutrient and has achieved positive effects. However, little is known regarding the nutrient-removal performance and physiological responses of I. pseudacorus for brackish eutrophic water treatment due to high nutrients combined with certain salinity levels. In this study, I. pseudacorus-planted microcosms were established to evaluate the capacity of I. pseudacorus to remove excessive nutrients from fresh (salinity 0.05%) and brackish (salinity 0.5%) eutrophic waters. The degradation of total nitrogen and ammonia nitrogen were not affected by 0.5% salinity; 0.5% salinity promoted the degradation of nitrate nitrogen while severely inhibited the degradation of total phosphorus. Additionally, 0.5% salinity was found to induce stress responses quantified by measuring six physiological indexes. Compared to 0.05% salinity, 0.5% salinity resulted in significant decreases in the chlorophyll a, b and total chlorophyll contents of I. pseudacorus which closely related to photosynthesis (p < 0.05). Furthermore, the higher proline, malondialdehyde contents and antioxidant enzyme activities were detected in I. pseudacorus exposed to 0.5% salinity, which provided protection against reactive oxygen species. The results highlight that the cellular stress assays are efficient for monitoring the health of I. pseudacorus in salinity shock-associated constructed wetlands.     

Phytoplankton ecology of the larger Scottish lochs

Summary

Lake phytoplankton biomass and species composition of 15 of Scotland's larger lochs are viewed here as major responses to the interplay between eutrophication pressures from the catchment, and to a suite of physical, chemical and biotic attributes of the waters. Pressures varied considerably: from Morar to Lubnaig in terms of catchment-to-loch area ratio; from Awe, Katrine, Morar and Ness to Leven on the basis of losses of phosphorus from the catchments; and from St Mary's down to Shiel on the basis of altitude. Values for factors determining the impact of the pressures also range over an order-of-magnitude: loch mean depth from the shallowest (Leven and Menteith) to the deepest (Ness and Morar); predicted annual mean total phosphorus levels (highest in Leven and lowest in Morar, Shiel and Katrine); theoretical hydraulic flushing rate (lowest in Katrine and highest in Veyatie). Rankings based on these features predicted tolerably well the relative standings of the lochs in terms of overall phytoplankton biomass — with mean annual chlorophyll concentrations from c. 0.5 μg l^-1 in Morar to 100 μg 1 ^-1 in Leven — although the algal crops in Leven depend very much on Daphnia population densities. The relative likelihood of eutrophic or oligotrophic species predominating was also reasonably well anticipated. A comparison of these rankings with those based on the amounts of chlorophyll observed per unit loading of the major limiting nutrient (P) showed that Leven and Menteith are the most efficient at converting the nutrient resources into biomass (respectively, up to 100, and c. 60 mg chlorophyll_a m^-3 g^-1 P m ^-2 y^-1), with the clear waters Katrine and Morar, and the humic-stained Tay belying their otherwise oligotrophic or dystrophic character. These contrast with values of 0.6–2.5 mg chlorophyll_a m ^-3 g^-1 P m^-2 y^-1 obtained for Ness. Reference to algae recorded at the turn of the century show that Leven has been markedly enriched. However, shifts are also indicated for Earn and Lubnaig which are susceptible to enhanced inputs of bio-available P from fish-farms, and for Katrine.     

Diversity of parasitic fungi associated with phytoplankton in Hawaiian waters

Parasitic fungi infect large phytoplankton species in freshwater, playing a fundamental role in their host's health and habitat range. However, those associated with the marine phytoplankton community remain largely unknown. This study investigated the infectivity and biodiversity of phytoplanktonic parasitic fungi in three ecosystems of Hawaiian waters, with contrasting trophic statuses – oligotrophic (Waikiki Beach), mesotrophic (Kaneohe Bay) and eutrophic (Ala Wai Canal). The occurrence of fungal parasites (e.g. attached spores) was primarily associated with diatom cells (i.e. the most vulnerable populations) as well as various pelagic fungal forms (i.e. zoosporic, yeast and mycelial), suggesting the coexistence of different fungal lifestyles. Phylogenetic analysis categorized our retrieved fungal sequences from six clone libraries into five taxonomic orders that belonged to the phyla of Ascomycota and Basidiomycota, along with culturable fungal endophytes and pathogens from diverse host resources. The great majority of these sequences (～93%) were associated with three taxonomic orders of Ascomycota (Pleosporales, Hypocreales and Saccharomycetales). There was greater infectivity and diversity of fungal species in eutrophic (Ala Wai) waters compared with oligotrophic (Waikiki Beach) waters, and both factors were significantly (P?相似文献   

Oligotrophic waters of the Northwest Atlantic support taxonomically diverse diatom communities that are distinct from coastal waters

Diatoms are important components of the marine food web and one of the most species-rich groups of phytoplankton. The diversity and composition of diatoms in eutrophic nearshore habitats have been well documented due to the outsized influence of diatoms on coastal ecosystem functioning. In contrast, patterns of both diatom diversity and community composition in offshore oligotrophic regions where diatom biomass is low have been poorly resolved. To compare the diatom diversity and community composition in oligotrophic and eutrophic waters, diatom communities were sampled along a 1,250 km transect from the oligotrophic Sargasso Sea to the coastal waters of the northeast US shelf. Diatom community composition was determined by amplifying and sequencing the 18S rDNA V4 region. Of the 301 amplicon sequence variants (ASVs) identified along the transect, the majority (70%) were sampled exclusively from oligotrophic waters of the Gulf Stream and Sargasso Sea and included the genera Bacteriastrum, Haslea, Hemiaulus, Pseudo-nitzschia, and Nitzschia. Diatom ASV richness did not vary along the transect, indicating that the oligotrophic Sargasso Sea and Gulf Stream are occupied by a diverse diatom community. Although ASV richness was similar between oligotrophic and coastal waters, diatom community composition in these regions differed significantly and was correlated with temperature and phosphate, two environmental variables known to influence diatom metabolism and geographic distribution. In sum, oligotrophic waters of the western North Atlantic harbor diverse diatom assemblages that are distinct from coastal regions, and these open ocean diatoms warrant additional study, as they may play critical roles in oligotrophic ecosystems.     

Nutrient-limited productivity of calcareous versus fleshy macroalgae in a eutrophic,carbonate-rich tropical marine environment

The results of a study of nutrient enrichment with nitrogen (N) and phosphorus (P) on productivity and calcification of fleshy and calcareous algae are reported in this study. Plants were collected from a nearshore eutrophic site in the Florida Keys (USA) and experimentally pulsed during the night with combinations of N and P. After several days of pulsing (7–10 days), net productivity, calcification, and alkaline phosphatase activity (APA), were measured. Productivity of fleshy algae were frequently enhanced by N, P, and N+P, during both summer and winter. Phosphorus limited the productivity of Hydroclathrus clathratus during winter and Ulva spp. during summer, whereas nitrogen limited the productivity of Laurencia intricata during both seasons. During summer, Dictyota cervicornis productivity was not enhanced by any nutrient enrichment. Nitrogen limited the productivity of the three calcareous species Penicillus capitatus, Penicillus dumetosus and Halimeda opuntia during winter and that of H. opuntia during summer. Neither N nor P enrichment increased calcification of calcareous species, and P enrichment greatly inhibited calcification of P. dumetosus during winter. Nutrient enrichment enhanced the productivity of the fleshy species to a greater extent than that of calcareous algae. The seawater DIN:SRP molar ratio was low at our eutrophic study site (molar ratio average of 3:1 during winter and 9:1 during summer) compared to more oligotrophic sites in the Florida Keys, suggesting that in carbonate-rich environments, eutrophication shifts nutrient regulation of productivity from P to N. APA activities of fleshy macroalage were higher than calcareous algae, and rates of all macro algae were 2- to 7-fold higher in summer compared to winter. Productivity was also about 3-fold higher in fleshy compared to calcareous species and about 2-fold higher in summer compared to winter. These results suggest that nutrient enrichment enhances productivity of fleshy algae to a greater extent than that of calcareous algae. Thus, overgrowth of calcareous algae by more opportunistic fleshy forms could reduce carbonate accretion in tropical coastlines experiencing increased eutrophication.     

Comparing microscopic counts and pigment analyses in 46 phytoplankton communities from lakes of different trophic state

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Evidence of coprophagy in freshwater zooplankton

1. Vertical transport of nutrients in sedimenting faecal material is greatly reduced by coprophageous organisms. Unfortunately, nearly all work on faecal production, sedimentation and coprophagy has dealt with copepods in marine ecosystems. Here, we report the first evidence of coprophagy in freshwater zooplankton from oligotrophic and eutrophic lakes. We used ¹⁴C‐labelled algae and faecal material to estimate the rates of algal clearance and coprophagy. 2. Measured feeding rates per individual on faecal material were similar (Daphnia pulex, D. rosea, Leptodiaptomus tyrelli) or even higher (D. lumholtzi) than filtering rates on phytoplankton. This finding does not necessarily implicate active selection of faeces over algae because: (i) we did not use the same food concentrations for faeces and algae, and (ii) grazers of slightly different sizes were used in each test. 3. Weight‐specific clearance rates of L. tyrelli and Holopedium gibberum on faecal matter (0.084–0.089 mL μg^?1 h^?1) were higher than in the daphniids (0.026 mL μg^?1 h^?1). 4. The data indicate that coprophagy in freshwater ecosystems is an important mechanism of nutrient recycling, and this process should be taken into account when studying nutrient fluxes within lakes and reservoirs.     

Restoration of eutrophied shallow softwater lakes based upon carbon and phosphorus limitation

Plant communities from oligotrophic, poorly buffered waters are seriously threatened by both, acidification and eutrophication/alkalinization. Acidification is mainly caused by atmospheric deposition of acidifying substances while eutrophication is often the result of inlet of nutrient enriched, calcareous brook- or groundwater. The plant production in very soft waters is often limited by low levels of inorganic carbon, nitrogen and/or phosphorus. This paper deals with the possibilities for restoration of formerly oligotrophic but now eutrophied and alkalinized softwater systems. Restoration based upon nitrogen limitation is not likely to be successful as the atmospheric deposition of nitrogen in The Netherlands is very high. Phosphorus limitation can also be a problem. One can stop the input of phosphorus and remove the mud layer, but the problem remains that also the deeper mineral sandy sediments are saturated with phosphate. A possible remedy, however, is a combination of carbon- and phosphorus limitation. Many plants from eutrophic environments never occur in very soft waters, probably as a result of carbon limitation. In addition, mobilisation of phosphate is much lower in waters with very low bicarbonate levels. Restoration of a former oligotrophic softwater lake by reducing the inlet of calcareous surface water, in combination with removal of the organic sediment layer, appeared to be very successful. Many endangered plant species such asIsoetes echinospora, Luronium natans, Deschampsia setacea andEchinodorus repens developed spontaneously from the still viable seedbank.     

Seasonality of Melosira-plankton of the great northern lakes

The paper discusses the seasonality of Melosira-plankton in Ladoga and Onega Lakes and its comparison with that in other large northern lakes. The periodicity of Melosira in dimictic temperate lakes is mainly connected with periods of turbulence of the lake water in spring and autumn. The role of Melosira in the primary productivity of great northern lakes is important both for the oligotrophic phase and in the case of eutrophication. In very advanced states of eutrophication the spring crop of Melosira-plankton may be the cause of oxygen depletion in the hypolimnion.     

The pelagic system in the photic zone of the tropical Atlantic

Summary A multidisciplinary study of the carbon budget in the upper 300 meter of permanently stratified waters was started by two NECTAR-expeditions (North Equatorial Current Trans Atlantic Research) with HMS TYDEMAN in 1977 and 1978 (BAARS, ZIJLSTRA and TIJSSEN, 1979). In 1979 additional measurements were performed during the Gulf of Guinea-expedition with MS TYRO.Primary production in the nutrient depleted mixed layer of the North Equatorial Current estimated from the diurnal cycle in the O₂ concentration (TIJSSEN, 1979) and in POC (POSTMA and ROMMETS, 1979) revealed values 4–10 times higher than the data from the¹⁴C method in the literature: 800–2000 against ca. 200 mg C/m²/day. Moreover,¹⁴C incubations performed in bottle volumes of 4 liter and over 2 hour periods, instead of the recommended 12 hours for oligotrophic waters, gave 5–15 times higher values as incubations in the commonly used 300 ml (or smaller) bottles (GIESKES, KRAAY and BAARS, 1979). In the latter bottles a dramatic decrease of chlorophyll concentrations was observed, suggesting either heavy damage to fragile microflagellates by glasswall contacts and/or insufficient nutrient recycling by the lack of zooplankton in small samples. This then could account for the phenomena of low production and decreasing algal stock in long incubations with small bottles. These results suggest that today's picture of the primary production in the world's oceans (DE VOOIJS, 1979) needs probably a thorough reexamination. On the other hand, experiments in the North Sea and in the Gulf of Guinea did not indicate an effect of bottle size on¹⁴C incorporation and the¹⁴C method gave comparable estimates of primary production as the high precision oxygen method (photometric endpoint detection in the Winkler titration,cf. TIJSSEN, 1979). However, in these waters nutrient concentrations are always clearly above detection levels so that all previous data from somewhat richer areas may have been correct. In relation to the large oligotrophic parts of the oceans a question remains about the fate of the probably high primary production. Is it consumed by the algae themselves by night (POSTMA, 1980), are bacteria and microzooplankton more important consumers than formerly thought, or is the daily ration of zooplankters much higher as expected from extrapolation of filtration experiments in more eutrophic waters? We hope to clarify this topic during the coming NECTAR'82 expedition.Another main objective of the programme concerns the character of the deep chlorophyll maximum in permanently stratified waters. This layer is in the North Equatorial Current located at the depth of the nitratocline and at ca. 1% of the incident light at the surface (SPITZER and WERNAND, 1981). Primary production in the layer seems to be negligible while detailed vertical profiles of zooplankton, obtained with a Longhurst-Hardy Plankton Recorder, revealed no obvious concentrations in the layer. Chlorophyll analysis by thin-layer-chromatography (GIESKES, KRAAY and TIJSSEN, 1978) demonstrated that more than half of the chlorophyll a in the layer consists of an isomer which bleaches rapidly when transferred to higher light levels. The hypothesis was formulated that the chlorophyll maximum layer, at least in this region of the Atlantic, is an accumulation of chlorophyll breakdown products with a quite long turnover time at low light levels. In contrast to these findings, chlorophyll maxima near West-Africa and in the Gulf of Guinea were located at 5–10% light and contained more living algal cells (most of them as small as 1–3 m) than the nutrientpoor mixed layer above it. Primary production profiles had therefore a bimodal shape, with peaks at 30–50% light and at the chlorophyll maximum. Chlorophyll isomers, now analysed with High Pressure Liquid Chromatography, were also in these waters present at nearly all stations and comprised 30–70% of total chlorophyll comparable to the situation in the North Equatorial Current (GIESKES and KRAAY, 1981). It could be shown that these isomers are not involved in primary production, so that well established relationships between chlorophyll, light and primary production, found in oceanographic literature, have to be reconsidered.     

Responses of a eutrophic pond community to separate and combined effects of N:P supply and planktivorous fish: a mesocosm experiment

We conducted an outdoor mesocosm experiment of factorial design consisting of three levels of nutrient supply (no nutrient addition and additions of nitrogen and phosphorus in ratios of 10:1 and 45:1) cross-classified with two levels of bluegill (Lepomis macrochirus) (presence and absence). Nutrient supply significantly affected total phosphorus (TP), total nitrogen (TN), TN: TP ratio, turbidity, Secchi depth, phytoplankton chlorophyll, filamentous blue-green algae, periphyton chlorophyll, Asplanchna and non-predatory rotifers. The presence of bluegill significantly increased TP, turbidity, diatoms, unicellular green algae, colonial blue-green algae, filamentous blue-green algae, periphyton chlorophyll, Asplanchna and non-predatory rotifers, and decreased Secchi depth, cladocerans, cyclopoid copepodids, copepod nauplii and chironomid tube densities. Nutrient supply and fish effects were not independent of each other as shown by significant nutrient × fish interaction effects for TP, Secchi depth, filamentous blue-green algae, periphyton chlorophyll, Asplanchna and non-predatory rotifers.