Light-dependency of nitrate uptake by phytoplankton over the spring bloom in Auke Bay,Alaska

The effect of light intensity on nitrate uptake by natural populations of phytoplankton was examined by ¹⁵N traceruptake experiments during the spring (March–May 1987) in Auke Bay, Alaska. The data were fit to a rectangular hyperbolic model which included a term for dark uptake. Three types of curves described nitrate uptake as a function of light intensity. The first (Type I) had a low half-saturation light intensity (K _I), low chlorophyll-specific uptakes rates, no dark uptake and occasional photoinhibition. These were observed during a period of biomass decrease, accompanied by low daily light and strong wind, prior to the major bloom. The second type (Type II) had relatively high K _I, high chlorophyll-specific uptake rates, and no dark uptake. Type II curves were observed during most of the period prior to nitrate depletion in the surface waters. Types I and II both appeared prior to nitrate depletion in the water and reflected variations in the light history of the phytoplankton population. The third type (Type III) occurred in nitrate-deplete conditions, when nitrate uptake was less dependent on light intensity (i.e., high rates of dark uptake and lower K _I). Decreased light-dependency during this period was coupled with physiological nitrogen deficiency in the population. Comparing these parameters to those of photosynthetic carbon fixation, K _Ivalues of nitrate uptake were generally higher than those of photosynthesis prior to nitrate depletion, and lower during nutrient-deplete conditions.     

Phosphate uptake behavior of natural phytoplankton during exposure to solar ultraviolet radiation in a shallow coastal lagoon

The effect of solar UV radiation (UVR: 290–400 nm) on the ³²P-phosphate uptake rates of natural phytoplankton from a southern Atlantic Ocean coastal lagoon was studied during two consecutive summers at one station located in the marine-influenced area. Due to the shallowness of this lagoon and also to the generally high UV water transparency in this area, phytoplankton are exposed to high UV irradiances. The ³²P-phosphate uptake rates measured at several phosphate concentrations were inhibited up to 59.2% by UVR, although uptake stimulation was also observed in four of nine experiments (up to 28%). The effect of UVR on the apparent maximum velocity of ³²P-phosphate uptake (V _uptake) ranged from an inhibition of 49% to a stimulation of 31%. Although the highest inhibition values were associated with the maximum registered incident UV irradiance, a significant correlation between these two parameters was not observed. Changes in microalgal community structure were not related to the observed UV effect; however, a significant relationship was found between the inhibition of ³²P-phosphate uptake rates and V _uptake used as a proxy for phosphate deficiency. This relationship suggests that the phytoplankton phosphorus nutritional status modulates their sensitivity to UV exposure. Overall, our results suggest that solar UVR has the potential to affect phosphorus cycling.Communicated by O. Kinne, Oldendorf/Luhe     

Phosphorus metabolism of oceanic dinoflagellates: phosphate uptake,chemical composition and growth of Pyrocystis noctiluca

The phosphorus metabolism of Pyrocystis noctiluca Murray (Schuett) 1886 has characteristics which may enhance its potential for success in orthophosphate impoverished waters. The steady-state phosphate uptake rates were equal in the light and dark, and were directly proportional to both the phosphorus cell quota and the cell division rate. In contrast, nutrient-saturated uptake rates were multiphasic, faster in the light than the dark, 2 to 4 orders of magnitude greater than steady-state rates, and were inversely proportional to both the phosphorus cell quota and the cell division rate. These uptake characteristics suggest that P. noctiluca may take up phosphate coincidently at their typically low ambient concentrations as well as to exploit episodic nutrient events in nature. Cell division rates were a hyperbolic function of the ambient orthophosphate concentration. The shortest doubling time was 8.7 d, the phosphate concentration at half the maximum division rate was 0.15 M and the threshold, concentration for cell division was ca 0.05 M PO ₄ ^3- . Division rates of P. noctiluca in the ocean are much faster than predicted from the measured ambient orthophosphate concentrations. Since this dinoflagellate has high naturally occurring alkaline phosphatase activities, and can utilize organic-P compounds, we suggest that organic-P can be as important as orthophosphate in supporting the observed division rates of P. noctiluca in the sea.     

Uptake and translocation of phosphorus in eelgrass (Zostera marina)

The uptake and translocation of phosphorus in eelgrass (Zostera marina L.) was studied in two-compartment chambers using ³²P and autoradiography. Eelgrass was able to take up phosphorus both with leaves and rootrhizomes. Only a small amount (less than 4%) of the total amount of phosphorus taken up from either source was translocated within the plants during an incubation time of 120 h. Release of translocated phosphorus from the plant tissues to the surrounding water was not detected. The autoradiographs showed that the translocated phosphorus was localized mainly in the actively growing plant tissues, i.e. the stem and young leaves, and nodes of the rhizomes and young roots. The uptake of phosphorus in leaves and the bidirectional translocation in the plants was significantly lower in the dark. The uptake of phosphorus in rootrhizomes was unaffected by light-conditions. The concentration of phosphate in the water of one compartment did not affect the phosphorus uptake by the plant parts in the opposite compartment. However, the translocation was significantly reduced when both compartments were supplied with identical phosphate concentrations. The results of the present investigation indicate that the quantitative significance of eelgrass in the cycling of phosphorus between sediment and water may have been greatly overestimated in earlier studies. The amount of phosphorus taken up by root-rhizomes and subsequently translocated to leaves is probably insignificant during most of the growing season in comparison to the amount taken up by the leaves from the surrounding water. However the uptake of phosphorus by root-rhizomes may be significant in the nutrition of eelgrass during periods with low phosphate levels in the water.     

Uptake and release of phosphorus by phytoplankton in the Chesapeake Bay estuary,USA

The phytoplankton uptake and release rates for inorganic phosphate, dissolved organic phosphate and polyphosphate were estimated during 5 cruises on the Chesapeake Bay over a 9-month period. Phosphorus in all pools turned over in several minutes to 100 h, and each soluble pool appeared to contain fractions which were metabolically useful to the phytoplankton. Maximal uptake rates (V _m ) for orthophosphate ranged from 0.02 to 2.95 μg-at P (1.h)^-1 with half saturation constants (K _s ) between 0.09 and 1.72 μg-at P l^-1. At low soluble reactive phosphorus concentrations, the uptake rate of trace ³²P orthophosphate was initially rapid, but declined after 15 to 60 min incubation. The data suggest that the initial uptake phase was dominated by exchange of ³²PO₄ ^≡ for ³¹PO₄ ^≡ in the membrane transport systems whereas the subsequent phase represented the net incorporation of orthophosphate into phytoplankton cells.     

Relationship between phytoplankton cell size and the rate of orthophosphate uptake: in situ observations of an estuarine population

Orthophosphate uptake by a natural estuarine phytoplankton population was estimated using two methods: (1) ³²P uptake experiments in which filters of different pore sizes were used to separate plankton size-fractions; (2) ³³P autoradiography of phytoplankton cells. Results of the first method showed that plankton cells larger than 5 m were responsible for 2% of the total orthophosphate uptake rate. 98% of the total uptake rate occurred in plankton composed mostly of bacteria, which passed the 5 m screen and were retained by the 0.45 m pore-size filter. There was no orthophosphate absorption by particulates in a biologically inhibited control containing iodoacetic acid. Orthophosphate uptake rates of individual phytoplankton species were obtained using ³³P autoradiography. The sum of these individual rates was very close to the estimated rate of uptake by particulates larger than 5 m in the ³²P labelling experiment. Generally, smaller cells were found to have a faster uptake rate per m³ biomass than larger cells. Although the nannoplankton constituted only about 21% of the total algal biomass, the rate of phosphate uptake by the nannoplankton was 75% of the total phytoplankton uptake rate. Results of the plankton autoradiography showed that the phosphate uptake rate per unit biomass is a power function of the surface: volume ratio of a cell; the relationship is expressed by the equation Y=2x10^-11 X ^1.7, where Y is gP m^-3 h^-1 and X is the surface: volume ratio. These results lend support to the hypothesis that smaller cells have a competitive advantage by having faster nutrient uptake rates.     

Phosphate acquisition in the giant clam-zooxanthellae symbiosis

The effect of phosphate on the giant clam Tridacna gigas and on its symbiotic dinoflagellate Symbiodinium sp. was compared with that on cultured Symbiodinium sp. originally isolated from the same clarn species. Incubation of whole clams in elevated phosphate (10 M) reduced their capacity for phosphate uptake, but the uptake capacity of the clam's zooxanthellae population was not influenced. In addition, there was no change in the zooxanthellae density and the N:P ratio, of these algae., On the other hand, cultured zooxanthellae were influenced by the phosphate regimen of their culture medium. Compared with controls (0 M P), addition of 10 M phosphate to the culture medium caused an increase of 100% in cell density and decreases of 50% in the N:P ratio, and 80% in the phosphate-uptake capacity of the zooxanthellae. Zooxanthellae freshly isolated from the clams exhibited properties similar to those of zooxanthellae cultured in the absence of phosphate. These results demonstrate that the zooxanthellae population of T. gigas have limited access to the inorganic phosphate in sea water and the phosphate reserves within the animal host.     

Succession and growth limitation of phytoplankton in the Gulf of Bothnia (Baltic Sea)

A one year field study of four stations in the Gulf of Bothnia during 1991 showed that the biomass was ca. two times, and primary productivity ca. four times, lower in the north (Bothnian Bay) than in the south (Bothnian Sea) during the summer. Nutrient addition experiments indicated phosphorus limitation of phytoplankton in the Bothanian Bay and the coastal areas in the northern Bothnian Sea, but nitrogen limitation in the open Bothanian Sea. A positive correlation between the phosphate concentration and the production/biomass ratio of phytoplankton was demonstrated, which partly explained the differences in the specific growth rate of the phytoplankton during the summer. Differences in photosynthetic active radiation between the stations also showed a covariation with the primary productivity. The relative importance of nutrient or light limitation for photosynthetic carbon fixation could not, however, the conclusively determined from this study. Marked differences in phytoplankton species composition from north to south were also observed. The number of dominating species was higher in the Bothnian Sea than in the Bothnian Bay. The distribution of some species could be explained as due to nutrient availability (e.g. Nodularia spumigena, Aphanizomenon sp.), while salinity probably limits the distribution of some limnic as well as marine species. The potentially toxic phytoplankton N. spumigena, Dinophysis acuminata and Chrysochromulina spp. were common in the Bothnian Sea but not in the Bothnian Bay. The pico- and nanoplankton biomass during late summer was higher than previously reported due to a revised carbon/volume ratio.     

Dark CO2 uptake by the diatom Chaetoceros simplex in response to nitrogen pulsing

In a continuing investigation of dark CO₂ uptake by nitrogen-limited cultures of the marine diatom Chaetoceros simplex (Bbsm), we expanded on several of our earlier conclusions regarding the potential application of this physiological response for measuring the degree and type of nitrogen limitation in phytoplankton populations. First, the duration over which the maximal enhancement of dark ¹⁴CO₂ uptake was sustained after NH ₄ ⁺ enrichment was a function both of the concentration of added NH ₄ ⁺ and the standing crop of phytoplankton nitrogen — in effect, the total N demand. Second, pulsing with NH ₄ ⁺ for a given degree of N-limitation always produced the same level of enhanced dark CO₂ uptake regardless of whether the cultures were preconditioned with oxidized or reduced nitrogen. In contrast, urea pulsing led to reduced dark CO₂ uptake, but the effect was most pronounced in cells grown on NO ₃ ^– . And third, the assay could be used to distinguish readily between no, moderate, and severe N limitation. The degree of severe N limitation was quantitatively correlated with the degree of enhanced dark CO₂ uptake, but this relationship was not so clear in the region of moderate N limitation. The main advantage of the assay is that it is a relatively simple and effective alternative to more complicated techniques for gauging the degree and form of N limitation in phytoplankton. Further evaluation will be required, both in the laboratory and field, before the assay can be calibrated for quantitative use.Contribution No. 5982 from the Woods Hole Oceanographic Institution     

Time-course of photoadaptation in the photosynthesis-irradiance relationship of a dinoflagellate exhibiting photosynthetic periodicity

Cultures of the marine dinoflagellate Glenodinium sp. were light-shifted and rates of photoadaptation determined by monitoring changes in cell volume, growth rate, pigmentation, parameters of the photosynthesisirradiance (P-I) curves and respiration. To approximate physiological conditions of field populations, cells were cultured on an alternating light-dark cycle of 12hL:12hD, which introduced a daily periodicity of photosynthesis. One result of the present study was to demonstrate how specific parameters of the P-I relationship influenced by periodicity of the light: dark cycle are distinguished from photosynthetic parameters influenced by changes in light level. Under steady-state conditions, rates of both light-saturated (P_max) and light-limited photosynthesis changed in unison over the day; these changes were not related to pigmentation, and displayed their maxima midday. This close relationship between P_max and the slope (a) of the cellular P-I curves in steadystate conditions was quickly adjusted when growth illumination was altered. Rates of light-limited photosynthesis were increased under low light conditions and the periodicity of cellular photosynthesis was maintained. The short-term responses of the P-I relationship to changing light level was different, depending on (1) whether the light shift was from high to low light or vice versa, and (2) whether the high light levels were sufficient to promote maximal photosynthesis rates. Major increases in the photosynthetic carotenoid peridinin, associated with a single type of light-harvesting chromo protein in the chloroplast, was observed immediately upon shifting high light cultures to low light conditions. Following pigment synthesis, significant increases in rates of light-limited photosynthesis were observed in about one-tenth the generation time, while cellular photosynthetic potential was unaffected. it is suggested that general results were consistent with suggested that general results were consistent with earlier reports that the major photoadaptive strategy of Glenodinium sp. is to alter photosynthetic unit (PSU) size. Photoadaptive response times to high light were light-dependent, but appeared to be shower than photoadaptive responses to low light. If light intensities were bright enough to maximize growth rates, photosynthetic response times were on the order of a generation period and pigmentation fell quickly as cells divided at a faster rate. If light-intensities were not sufficient to maximize growth rates, then pigment content did not decline, while rates of light-limited photosynthesis declined quickly. In all cases, photoadaptation was followed best by monitoring fast changes in half saturation constants for photosynthesis, rather than fluctuating changes in pigmentation. Results compared well with time-course phenomena reported for other groups of phytoplankton. Overall, results suggest phytoplankton can bring about photo-induced changes in photosynthesis very quickly and thus accommodate widely fluctuating light regimes over short periods of time.     

Algal chloroplasts in the protoplasm of three species of benthic foraminifera: taxonomic affinity,viability and persistence

The ultrastructure and pigment content of algal chloroplasts (derived from Bacillariophyceae or Chrysophyceae) are described from 3 benthic species of brackish-water foraminiferans.Elphidium williamsoni Haynes contains 4×10⁶ chloroplasts mg^-1, whereas the contents ofNonion germanicum (Ehrenberg) andE. excavatum (Terquem) are about 10% of this value. The two former contain chlorophyllsa andc and fucoxanthin, but these pigments were not detectable in the latter.E. williamsoni andN. germanicum had a net uptake of¹⁴C–HCO ₃ ^- , proportional to their content of chlorophyll and number of chloroplasts, increasing linearly up to approximately 10 Klux. At light saturation the former assimilates 2.3x10^-3 mg C mg^-1 h^-1 and the latter only about 20% of this value. Dark uptake was insignificant in all cases. Uptake could not be demonstrated inE. excavatum. The photosynthesis effected by these species is trivial in terms of the total benthic carbon fixation effected by the microflora. The chloroplasts survived longer in forminiferans kept in the dark than in light/dark adapted individuals. To keep a steady state population of chloroplasts under light/dark conditions,E. williamsoni must eat at least 65 chloroplasts individual^-1 h^-1, whereas the minimum consuption rate inN. germanicum is 20.     

粤北2座饮用水源地水库的富营养化与浮游植物群落动态

粤北地区的水库以山地型水库为主,其中有不少担负着饮用水源的功能。为了解粤北地区水源地水库的富营养化状态与浮游植物种群的动态变化,于2011年的枯水期（2―3月）和丰水期（6―7月）对花山和白水礤2座中型水库进行了采样调查,对水库的营养盐和浮游植物种群进行了分析。结果表明：2座水库均为贫营养型;浮游植物在枯水期和丰水期的种类变化不大,共鉴定出的浮游植物6门37种（属）,以硅藻为主要优势种群,优势种为小环藻（Cyclotella sp.）和颗粒直链藻（Melosira granulata）。同时,枯水期和丰水期2座水库浮游植物的丰度和生物量都比较低,其值分别为0.65×106～1.95×106cells.L-1、0.11 mg.L-1和0.73×106～8.9×106cells.L-1、0.05～0.50 mg.L-1。在浮游植物种群动态中,2座水库浮游植物丰度和生物量的季节变化主要表现为硅藻丰度和生物量的变化,低浓度的氮、磷营养盐限制是影响这2座贫营养水库浮游植物动态变化主要因素。     

Autoradiographic study to detect metabolically active phytoplankton and bacteria in the Rhode river estuary

The rate of utilization of inorganic carbon (C) and phosphate (P) by phytoplankton and bacteria in the Rhode River estuary has been estimated using liquid-emulsion autoradiography during four times of the year. Metabolic activity of phytoplankton was estimated by calculating silver grains above individual species. From these counts, the relative C and P uptake rates of individual species per unit of biomass and per volume of water were estimated. Examination of the autoradiograms showed that the metabolically most active, algae were smaller than 10 m. Both C and P were paken up by these smaller species at a higher rate than their proportion of the total biomass per volume of water would indicate. Uptake of C and P per unit of cell volume varied within a species and among the various phytoplankton at the different seasons of the year. Metabolic activity of planktonic bacteria in safranin-stained autoradiograms was also estimated by counting bacteria with associated grains and cells without grains. The ratio of 33p-labeled to unlabeled bacteria was highest in November. This high metabolic activity of bacteria in November corresponded with high P uptake rates of the phytoplankton at that time. Throughout this study, only 28 to 42% of the total phytoplankton biomass was metabolically active and, 63 to 85% of the bacteria.     

富营养化水体降磷对浮游植物群落结构特征的影响

浮游植物是水生态系统中物质循环和能量流动的基础,作为初级生产者,浮游植物的群落结构直接影响着水生态系统的结构和功能。在水产养殖生产中,如何根据养殖生物对生活环境的需求开展精准培水、定向培水,培养养殖生物所需要的浮游植物,在维持养殖水域生态平衡的同时又能为养殖生物提供一定的饵料资源,这一直是摆在水产科技工作者面前的重要难题和研究热点。已有的资料大都是通过添加磷的方式研究磷改变对浮游植物生长的影响,而有关富营养化水体降磷对浮游植物群落结构影响的研究尚未见报道。为此,试验通过向取自富营养化湖泊的水体中加入磷去除剂,采用Pielou均匀度指数、Mcnaughton优势度指数和Shannon多样性指数,研究自然水体中的磷被降低后水体浮游植物群落结构的变化情况。结果表明,所取富营养化水体中共检出绿藻（Chlorophyta）、硅藻（Bacillariophyta）、蓝藻（Cyanophyta）、裸藻（Euglenophyta）、隐藻（Cryptophyta）、甲藻（Pyrrophyta）6门29种（包括变种和变型）;其中绿藻、蓝藻、硅藻、隐藻、裸藻、甲藻分别有7、4、2、1、1种,分别占总种数的24.13%、13.79%、6.90%、3.45%、3.45%。富营养化水体降磷后,虽然试验组和对照组在浮游植物种类组成上没有差异,但浮游植物群落结构特征发生了很大变化,浮游植物数量明显降低,由13 238.8×104cells·L-1降低至3 997.5×104cells·L-1,下降了69.8%;浮游植物优势种从1门（蓝藻（Cyanophyta））6种增加到3门（绿藻（Chlorophyta）、硅藻（Bacillariophyta）、蓝藻（Cyanophyta））12种,优势度指数从97.29%降低至86.30%,优势种门数和优势种种数远远高于对照组,优势度明显低于对照组;同时,浮游植物多样性指数和均匀度分别从1.85和0.38升高至2.60和0.54,显示出试验组浮游植物多样性和均匀度优于对照组。研究表明富营养化水体降磷对浮游植物群落结构产生了明显影响,使群落结构处于更加复杂、完整和稳定的状态。     

Alkaline phosphatase activity in subtropical Central North Pacific waters using a sensitive fluorometric method

This paper describes a fluorometric method for assaying low levels of the enzyme alkaline phosphatase in seawater. The assay is based on the hydrolysis of the monophosphate ester bond of 3-0-methylfluorescein phosphate. This enzyme is synthesized by many microorganisms when phosphate becomes limiting. Alkaline phosphatase activity was detected in phytoplankton from the nutrient-impoverished surface waters of the subtropical Central North Pacific Ocean. The presence of naturally occurring phosphatase suggests that phosphorus may be limiting to phytoplankton growth in these waters. The phytoplankton in water samples lacking enzyme activity at the time of collection produced phosphatase within 1 to 2 days of incubation at in situ temperatures.     

Tidal variations in the photosynthesis of estuarine phytoplankton isolated in a tank

In 1981 two large (1 200 1) seawater samples from the St. Lawrence Estuary were kept under constant temperature and light conditions for periods of 50 and 68 h, respectively. In both tank experiments, semidiurnal variations in NH₄ were observed that could be related to cyclical NH₄ uptake by the phytoplankton. Semidiurnal cycles in photosynthetic efficiency (^B) and intracellular chlorophyll a in the tank, phased on tides at sea, were also evidenced in both experiments. These results support the hypothesis that variations in phytoplankton photosynthetic activity, which are possibly endogenous, can be phased on semidiurnal variations in vertical tidal mixing (variations of the mean light conditions in the mixed layer). In addition, observed variations in intracellular chlorophyll a suggest the possibility of endogenous cycles of phytoplankton light and shade adaptation.Contribution to the program of GIROQ (Groupe interuniversitaire de recherches océanographiques du Québec)     

Some experiments on phosphate assimilation by coastal marine plankton

A study of phosphate assimilation by coastal marine plankton revealed that both phytoplankton and microheterotrophs incorporated radioactive phosphorus (³³P). Size fractionation of the particulate matter (using 1 m pore diameter Nucleopore^® membrane filters), antibiotic treatment (using garamycin), and independent estimaties of photoautotrophic (¹⁴CO₂ uptake) and heterotrophic (³H-glucose uptake) activities were employed to separate phyto- and bacterioplankton phosphate uptake. Results indicated that phytoplankton ³³P-uptake was best estimated by the fraction of particulate matter retained on the 1 m membrane filters. Usually, less than 10% of the phytoplankton (based on chlorophyll a measurements) passed the 1 m pore-diameter filters, whereas about 90% of the heterotrophic activity passed. At least 50% of the ³³P-uptake was associated with the <1 m fraction. It may be possible to resolve the phytoplankton and bacterial contributions to ³³P-uptake by comparing the percent of total ³³P-uptake with the percent of total ³H-glucose uptake associated with the >1 m fraction.     

Persistent diel rhythms in the chlorophyll fluorescence of marine phytoplankton species

The diel periodicities of in-vivo chlorophyll fluorescence and DCMU-enhanced chlorophyll fluorescence of 47 marine phytoplankton species were examined for 2 d in a 14 h L:10 h D light: dark cycle and then in continous light for another 2 to 3 d. Almost all phytoplankton species exhibit a more rapid increase in in-vivo fluorescence and DCMU-enhanced fluorescence during the light phase than during the dark phase. About one-half of the species examined exhibited persistent diel rhythms in continous light, indicating the operation of a biological clock. No phylogenetic or habitat related trends as to which species exhibited persistent rhythms were apparent. Of the phyla of eukaryotic phytoplankton adequately examined, none lacked biological clocks. Contrary to past hypotheses, some phytoplankton species maintain a persistent diel rhythm in a constant environment while reproducing at a rate greater than one division per day.     

Orthophosphate uptake by phytoplankton and bacterioplankton from the Los Angeles Harbor and Southern California coastal waters

Orthophosphate (P) uptake on a seasonal basis in surface waters and in vertical profiles was directly proportional to the standing stocks of phytoplankton and bacterioplankton in the outer Los Angeles Harbor and in southern California coastal waters during 1978–1979. A phytoplankton-enriched size fraction (PEF) which was retained on a 1 m pore-size filter contained 83% of the total chlorophyll a but only 18% of the total bacteria. A bacterioplankton-enriched size fraction (BEF) which passed the 1 m filter but was retained on a 0.2 m filter contained 82% of the total bacteria but only 17% of the total chlorophyll a. PEF and BEF accounted for 91 and 9% of the microbial carbon, respectively. The differential uptake of 10 radiolabeled substrates more fully characterized PEF and BEF. ³³P uptake occurred in both PEF and BEF, accounting for 47 and 53%, respectively, of the total uptake. ³³P uptake by both size fractions was inhibited by low concentrations of 2,4-dinitrophenol (DNP), N-ethylmaleimide (NEM) and carbonyl cyanide, m-chlorophenylhydrozone (CCCP). Darkness and low levels of 3-(3,4-dichlorophenyl)-1,1-dimethylurea (DCMU) selectively inhibited ³³P uptake by PEF; valinomycin selectively inhibited ³³P uptake by BEF. An experiment measuring ³³P uptake velocity versus P concentration produced sigmoidal saturation kinetics at high levels of exogenous P. Kinetic parameter analyses according to the Hill equation gave a V _max of 7.12 nmol l^–1 h^–1 and aK _t of 0.41 nmol l^–1 for PEF, and a V _max of 5.17 nmol l^–1 h^–1 and aK _t of 112 nmol l^–1 for BEF. Consideration of relative surface areas of phytoplankton and bacterioplankton, their ³³P uptake rates in light and dark, and estimates of the population turnover times emphasizes the potential importance of bacterioplankton in community phosphorus metabolism.     

Effects of nitrite on phosphate uptake in anaerobic-oxic process

An anaerobic-oxic (A/O) biological phosphorus removal reactor was operated to study the effect of nitrite on phosphate uptake. The phosphorus uptake profile was determined under different operating conditions. The results indicated that in addition to oxygen and nitrate (DPB_Na, nitrate denitrifying phosphorus removal), to some extent, nitrite could also serve as an electron acceptor to achieve nitrite denitrifying phosphorus removal (DPB_Ni). The quantity and rate of phosphorus uptake of DPB_Ni, however, were evidently lower than that of DPB_Na. The experiment results revealed that nitrite would bring toxic action to phosphate-accumulating organisms (PAOs) when NO₂ ^?-N ? 93.7 mg/L. The nitrite existing in the anoxic reactor made no difference to the quantity and rate of denitrifying phosphorus removal, but it could reduce the consumption of nitrate. Moreover, the data showed that the aerobic phosphate uptake of DPB_Ni was lower than that of anaerobic phosphorus-released sludge in a traditional A/O process. However, there was not much difference between these two kinds of sludge in terms of the total phosphorus uptake quantity and the effluent quality.