Phytoplankton productivity in turbid waters

Many of the freshwater areas in the world are turbid, due tosuspended inorganic particles. The euphotic depth of the shallowturbid impoundment, Wuras Dam, varies between 0.3–1.3m. This results in a compressed production profile where accuratemeasurements become difficult. Tubes of various lengths havebeen used and usually render higher rates, when compared todiscrete bottle incubations. A tube the depth of the euphoticzone confines the phytoplankton in the light and the rates measuredrepresent the maximal possible under the prevailing conditions.Longer tubes include an aphotic portion and give an idea ofthe magnitude of respiration losses. The depth of the mixinglayer appears to be especially important in turbid systems asthe time spent in the dark, relative to the light is of greatimportance and may be the most important regulating factor insuch waters. ^*This paper is the result of a study made at the Group for AquaticPrimary Productivity (GAP), Second International Workshop heldat the National Oceanographic Institute, Haifa, Israel in April–May1984.     

The contribution of phytoplankton productivity in turbid freshwaters to their trophic status

Certain factors influencing phytoplankton productivity are accentuated in turbid waters. They include mixing, spectral quality shifts, scattering, light fluctuations, and overall light attenuation. Measurements of productivity is influenced by the presence of inorganic turbidity. Together with the above factors high turbidity causes difficulties to assess and model phytoplankton productivity. Estimations of ^B, P_m ^B, I_k and _m only reflect on the physiological condition of the phytoplankton, which differs little between water types of temperate regions. Measurement of integral vertical productivity, efficiency and fractional absorption by the phytoplankton of light energy conversion, however, are greatly influenced by inorganic turbidity. Because of high ratios of mixing to euphotic depth, the critical mixing depth is one of the most important factors influencing overall productivity in turbid waters.     

Diel periodicity in phytoplankton productivity

Daily variation in phytoplankton productivity influences the dynamics and linkages between several large scale processes in aquatic ecosystems. As part of an opening address to the 5th International workshop for the Group for Aquatic Productivity (GAP), the daily patterns of variability in photosynthesis for different algal classes was introduced and accompanied by a discussion of the sources of environmental and endogenous regulation of repeating biological oscillations that occur in phytoplankton on timescales of one day. It is suggested that one way to develop a database that serves to sort and predict phytoplankton variability over the day may be to encourage the creation of a temporal library. Such a library would be comprised of temporally fixed maps of circadian clock-controlled rhythms for individual species, as well as temporally variable maps of diel periodicities that only can be defined for a selected set of environmental conditions.     

Navigation by light polarization in clear and turbid waters

Certain terrestrial animals use sky polarization for navigation. Certain aquatic species have also been shown to orient according to a polarization stimulus, but the correlation between underwater polarization and Sun position and hence the ability to use underwater polarization as a compass for navigation is still under debate. To examine this issue, we use theoretical equations for per cent polarization and electric vector (e-vector) orientation that account for the position of the Sun, refraction at the air-water interface and Rayleigh single scattering. The polarization patterns predicted by these theoretical equations are compared with measurements conducted in clear and semi-turbid coastal sea waters at 2 m and 5 m depth over sea floors of 6 m and 28 m depth. We find that the per cent polarization is correlated with the Sun's elevation only in clear waters. We furthermore find that the maximum value of the e-vector orientation angle equals the angle of refraction only in clear waters, in the horizontal viewing direction, over the deeper sea floor. We conclude that navigation by use of underwater polarization is possible under restricted conditions, i.e. in clear waters, primarily near the horizontal viewing direction, and in locations where the sea floor has limited effects on the light's polarization.     

Temporal and spatial variations in phytoplankton productivity in surface waters of a warm-temperate,monomictic lake in New Zealand

Surface phytoplankton productivity measurements were carried out in morphologically complex Lake Rotoiti with the objective of defining variations between sites and seasons, and the dominant environmental drivers of these variations. Measurements were carried out monthly at two depths at each of three morphologically diverse stations for 1 year throughout the lake. Productivity at the surface of the shallow embayment was significantly higher in most months of the year compared with the surface of the other two stations but there were no significant differences from September to December 2004. There were no relationships between measured environmental variables and primary productivity or specific production. Inorganic nutrient concentrations at the surface of the shallow station were low throughout the whole year but at the other two stations they showed a typical pattern for monomictic lakes of higher levels during winter mixing and declining concentrations during thermal stratification. The high variability between sites found in this study indicates that it is important to account for local differences in productivity in morphologically diverse lakes, and that whole lake productivity estimates may vary greatly depending on the location and depth of productivity measurements.     

Seasonal patterns of phytoplankton productivity and abundance in nearshore oligotrophic waters of the Levant Basin (Mediterranean)

A biweekly sampling program from two stations at the easternLevant Basin was carried out during a 1-year period (1983).The first station (neritic) was located 2 km offshore over theIsraeli continental shelf, while the second (pelagic) was located10 km offshore slightly beyond the continental shelf. It wasfound that during summer the relatively close pelagic watershad chlorophyll a concentrations comparable with the most oligotrophicdeep sea regions of the world's oceans. During winter and spring,profound fluctuations were observed in both phytoplankton standingcrop and primary productivity at the neritic station. This wasin response to weather phenomena, such as heavy rains or storms,which did not affect the pelagic Station to such an extent.The picoplanklon size fraction (<3 µm) dominated atthe neritic station during summer and fall, while the nanoplanktonfraction (3–20 µm) dominated during spring. At thepelagic station the picoplankton fraction dominated almost allyear round, but it is suspected that some portion of it wasphotosynthetically inactive.     

Use of coastal waters as condenser coolant in electric power plants: Impact on phytoplankton and primary productivity

(1) Studies on phytoplankton entrained in cooling system of a power plant revealed a reduction in biomass and gross primary productivity (GPP) at outfall, compared to intake.     

Diel patterns of phytoplankton productivity in Lake Vechten

Summary A review of the literature on phytoplankton primary production studies in lakes indicates that in most cases the daily primary production rates have been derived by multiplying the short-term (usually 3 or 4 hours) production measurement with a light factor. This factor is a ratio between the total irradiance during the day and during the period of incubation. The aim of the present study was to verify this method of calculation. Since the primary production rate is of great importance for the carbon cycle of lakes, this study can be regarded as a fundamental contribution to the integrated research of the ecosystem of lake Vechten (the Netherlands) (BESTet al., 1978).Photosynthetic carbon fixation was determined using the radiocarbon method of STEEMANN NIELSEN (1952). Thein situ measurements were carried out for 2 hours incubation periods starting at 15–30 minutes before sunrise and ending 15–30 minutes after sunset. Also measured were: water temperature, light penetration, oxygen and chlorophyll. Total incident solar radiation data were obtained from the Royal Netherlands Meteorological Institute (K.N.M.I.) at de Bilt (situated at 5 km from lake Vechten). The production during two consecutive 2-hourly periods,e.g. period 1 and period 2, were summed up and using the irradiance data during the 4 hours, daily production was calculated. These calculations were repeated for period 2 and 3, and so on. The sum of all the short-term measurements during a day,i.e. the total daily primary production, was taken for comparison with the production calculated by using the sum of the production during two successive periods and the light factor.Daily production rates obtained by extrapolating from short-term incubation periods both in the morning and in the late afternoon appeared to overestimate the real daily production (Fig. 1) up to 100%. It is likely, that in the morning the lack of nutrient limitation and relatively better physiological state of algae, and in the afternoon increase of phytoplankton biomass during the day can be considered as the factors causing the discrepancy between the calculated and real production. On the other hand, the underestimation of daily production rate based on midday time intervals on sunny days, was about 25%. It is attributed to photoinhibition, especially in the present study where the measurements were limited to the upper water strata (0–4m).Is is concluded that short-termin situ exposures between 10.00 and 14.00 hr appeared to be a good indicator of total primary production, although underestimates up to 25% on sunny days are to be taken into account.     

Light control on phytoplankton production in a shallow and turbid estuarine system

Tagus estuary is one of the largest estuaries of Western Europe. With the aim of unravelling the drivers of primary production in this shallow and turbid nutrient replete estuary, we tested the hypothesis that light availability is a major factor controlling phytoplankton production. Environmental parameters, phytoplankton biomass, community composition, and photosynthetic parameters were monitored at two sites in the estuary during a complete annual cycle. Despite the fact that nutrient concentrations were always above growth-limiting values, Chl a concentrations were relatively low throughout the study period. High water column turbidity, due to riverine inputs, promoted a rapid attenuation of light and created a compressed profile with optimal photosynthetic conditions. Therefore, the phytoplankton community, dominated by small cells, such as diatoms and cryptophycean flagellates, displayed highly photosynthetic efficiency and low light-saturated photosynthetic rates as a photo-acclimation response to low light conditions year-round. Primary production rate was unimodal, peaking in the summer months. In such estuarine system, gross primary production could thus be predicted by an existing robust empirical model based on pigment standing crop (Chl a), surface irradiance (E ₀) and optical depth (Z _eup). Compared to other shallow estuaries, the Tagus can be classified as a low- to moderately productive estuary, being the turbidity-induced low light conditions the principal factor limiting phytoplankton growth.     

14C-labeling of the compounds excreted by phytoplankton for employment as a realistic tracer in secondary productivity measurements

Preparations of the dissolved organic compounds released by photosynthesizing marine phytoplankton have been obtained with¹⁴carbon activities as high as 1.5 × 10⁵ dpm/ml. The radioisotope content of the preparations resides wholly in dissolved organic compounds of low molecular weight (MW<3500), which are uncontaminated by residual¹⁴C-labeled inorganic carbon. The labeled compunds arise through photosynthetic fixation and do not appear to be products of cell lysis during the incubation or to originate from cell damage during the filtration step employed.     

厦门近岸海域大型底栖动物次级生产力

于2013年5月和11月在厦门近岸海域设置67个站位进行大型底栖动物定量调查,运用Brey(1990)经验公式对该海域的次级生产力进行估算。结果表明:该海域大型底栖动物年均总次级生产力P和P/B值分别为4.6±10.1 g AFDW·m-2·a-1和1.0±0.4a-1,软体动物和多毛类为该海域P值的主要贡献类群,秋季的P值略高于春季,同安湾的P值明显高于大嶝海域、九龙江口、厦门外海域和围头湾。相关性分析显示,该海域次级生产力与沉积物有机质含量以及水体底温呈显著相关,底质类型以及采砂、航道清淤、环境污染等人类活动干扰也是影响次级生产力分布的主要因素。     

Fish-mediated zooplankton community structure in shallow turbid waters: a mesocosm study

Wetlands Ecology and Management - Turbidity influences the success of fish feeding, but little is known about the difference in the effects of turbidity as a result of organic and inorganic matter....     

The distribution of phytoplankton in some Central East African waters

Summary Observations of the distribution of phytoplankton were made in Pilkington Bay, Lake Victoria and in Lake Kyoga. For Pilkington Bay, series of samples were taken along an east-west line in the north-west corner of the bay and along a north-south line through the mouth of the bay. For Lake Kyoga, the main series of samples was taken from the north-east arm to the point of inflow of the Victoria Nile.Counts of algae were made by the sedimentation technique and it was found that for Pilkington Bay Melosira was the dominant genus during the period of the investigation. For the north-east arm of Lake Kyoga the dominant alga in mid-August was Lyngbya limnetica.At times, marked changes not only in density of phytoplankton but also in vertical distribution were observed from station to station in Pilkington Bay.During May an increase of Melosira occurred in the north-west corner of Pilkington Bay and this increase is as likely to have been due to water movements as to growth.Water movements have an important effect on phytoplankton distribution and it is possible that surface water movements bring about inoculation of relatively dense concentrations of phytoplankton, especially Melosira, into the Buvuma Channel from Pilkington Bay.The contribution of the north-east arm of Lake Kyoga to the Victoria Nile system was found to be markedly different chemically and biologically from that of Lake Victoria.A number of new records of algae from Lake Kyoga are listed.

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Résumé Des recherches sur la distribution du phytoplancton furent poursuivies dans la baie de Pilkington, dans le lac Victoria et dans le lac Kyoga. A la baie de Pilkington, des séries d'échantillons furent prélevées sur une ligne allant de l'est à l'ouest et située dans la partie nord-ouest de la baie, ainsi que sur une ligne traversant du nord au sud l'entrée de la baie. Au lac Kyoga, la principale série d'échantillons fut prélevée à partir de sa pointe nord-est jusqu'à l'arrivée des eaux de la branche mère du Nil.Le dénombrement des algues fut fait selon le procédé de la sédimentation et les résultats de l'enquête indiquent que, dans la baie de Pilkington, Melosira était le genre le plus répandu pendant la durée des recherches. Quant à la pointe nord-est du lac Kyoga, l'algue la plus répandue, à la mi-août, était Lyngbya limnetica.A certains moments, des variations marquèes, non seulement dans la densité du phytoplancton mais encore dans sa distribution verticale, furent constatées de divers postes d'observation sur la baie de Pilkington.Pendant le mois de mai, il se produisit une augmentation de la quantité de Melosira dans la partie nord-ouest de la baie de Pilkington, augmentation qui semble provenir des mouvements de l'eau ainsi que de la croissance.Le mouvement de l'eau exerce une influence importante sur la distribution du phytoplancton et il est possible que les mouvements de surface de l'eau produisent l'augmentation dans la canal de Buvuma de concentrations assez denses de phytoplancton, de Melosira surtout, provenant de la baie de Pilkington.L'apport de la pointe nord-est du lac Kyoga au réseau de la branche mère du Nil se révéla de composition chimique et biologique sensiblement differente de celle du lac Victoria.Un certain nombre d'observations nouvelles des algues du lac Kyoga ont été notées.

     

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   

Notes on the distribution of phytoplankton in some Kenya waters

The distribution of the major plankton algae in a number of Kenya waters is described. The lakes and dams are shown to fall into ecological groups related to figures for the pH, conductivity and alkalinity of their waters and characterised by the dominance of certain types of alga. The composition of the phytoplankton collected at approximately monthly intervals from Sasumua and Ruiru reservoirs is described. Plankton periodicity is demonstrated for both waters and is shown to be related to rainfall. The periodicity of plankton in Lake Naivasha is noted.     

The seasonal productivity of phytoplankton in a hypertrophic, gravel-pit lake

The seasonal time course of phytoplankton primary productivitywas studied weekly in a hypertrophic, gravel-pit lake closeto Madrid, Spain. Chlorophyll a ranged 22–445 mg m^–2.Gross primary productivity attained 0.28±0.14 g C m^–2h^–1 (range: 0.06–0.60), its yearly value being 900g C m^–2, but the shallow euphotic depths and the highplankton respiration ensured that net productivity was generallylow. Respiration losses amounted to 0.31±0.24 g O₂ m^–2h^–1, with phytoplankton respiration roughly attainingone-half of overall plankton respiration. Areal phytoplanktonproductivity and plankton respiration followed a seasonal trendbut this was not the case for photosynthetic capacity. Surfacephotoinhibition was evenly distributed throughout the study.Quantum yields showed an increasing depth trend, but no seasonaltrend. Both P_max and I_k were both temperature- and irradiance-dependent.As compared with lakes of lesser trophic degree, phytoplanktonprimary production in hypertrophic lakes might be increasednot only by higher nutrient contents but also by low chlorophyll-specificattenuation coefficients and low background, non-algal attenuation,thereby allowing for higher areal chlorophyll contents and hencehigher areal productivity. Our study suggests that physical(irradiance and water column stability) as well as chemicalfeatures (dissolved inorganic carbon and soluble reactive phosphorus)may control seasonality of phytoplankton primary productionin this lake despite recent claims that only physical factorsare of significance in hypertrophic lakes. However, this doesnot explain all the variability observed and so a food web controlis also likely to be operating.     

Spatial distribution of phytoplankton productivity in the Amundsen Sea, Antarctica

To date, no direct measurements of primary production were taken in the Amundsen Sea, which is one of the highest primary productivity regions in the Antarctic. Phytoplankton carbon and nitrogen uptake experiments were conducted at 16 selected stations using a ¹³C–¹⁵N dual isotope tracer technique. We found no statistically significant depletions of major inorganic nutrients (nitrate?+?nitrite, ammonium, and silicate) although the concentrations of these nutrients were markedly reduced in the surface layer of the polynya stations where large celled phytoplankton (>20?μm) predominated (ca. 64?%). The average chl-a concentration was significantly higher at polynya stations than at non-polynya stations (p?<?0.01). Average daily carbon and nitrogen uptake rates by phytoplankton at polynya stations were 2.2?g?C?m^?2?day^?1 (SD?=?±1.4?g?C?m^?2?day^?1) and 0.9?g?N?m^?2?day^?1 (SD?=?±0.2?g?N?m^?2?day^?1), respectively, about 5–10 times higher than those at non-polynya stations. These ranges are as high as those in the Ross Sea, which has the highest productivity among polynyas in the Antarctic Ocean. The unique productivity patterns in the Amundsen Sea are likely due to differences in iron limitation, phytoplankton productivity, the timing of phytoplankton growing season, or a combination of these factors.     

Nitrogen uptake by heterotrophic bacteria and phytoplankton in Arctic surface waters

We estimated rates of heterotrophic bacterial and phytoplanktonuptake of nitrate, ammonium, and urea using ¹⁵N-labelled nitrogenand specific metabolic inhibitors of prokaryote and eukaryotenitrogen metabolism in the surface waters of the North Water(northern Baffin Bay) during autumn that were characterizedby the absence of cyanobacteria (comprising prochlorophytes).The percentage of nitrate + ammonium uptake by heterotrophicbacteria ranged between 44 and 78% of the measured total uptakeand was the highest when the phytoplankton biomass was relativelylow (<2 µg Chlorophyll a L^–1). Phytoplanktonaccounted for a larger fraction (e.g., 58–95%) of ureauptake than heterotrophic bacteria. When our results are combinedwith those from previous studies carried out in diverse temperateand polar areas, it appears that heterotrophic bacteria accountfor 25% (14–40%; median and interquartile range) of thetotal nitrate uptake in surface waters with chlorophyll biomass<2 µg L^–1. Estimates of new production computedfrom phytoplankton carbon uptake and f-ratios may be stronglyoverestimated in regions where nitrate uptake by heterotrophicbacteria is high and the biomass of phytoplankton is low.     

Effects of bottle size in determinations of primary productivity by phytoplankton

Determinations of primary productivity were made by the radiocarbon method at regular intervals over a year in samples, taken from the eutrophic waters of the Menai Strait, North Wales, and contained in bottles of capacities from 135 ml up to 2290 ml. Fixation per unit volume in particulate matter retained by 0 · 45 m pore size membrane filters was independent of bottle size over most of the year. There was a consistent divergence, however, during the period of rapid phytoplankton growth in the spring, when small bottles gave up to three times higher values than large ones. Possible effects of bottle size on primary productivity determinations are discussed but the cause of this particular result is not apparent.