Notes on a Mesodinium rubrum red tide in San Francisco Bay (California, USA)

Discrete red patches of water were observed in South San FranciscoBay (USA) on 30 April 1993, and examination of live samplesshowed that this red tide was caused by surface accumulationsof the pigmented ciliate Mesodinium rubrum. Vertical profilesshowed strong salinity and temperature stratification in theupper 5 m, peak chlorophyll fluorescence in the upper meter,and differences in the small-scale density structure and fluorescencedistribution among red patches. Events preceding this Mesodiniumred tide included: (i) heavy precipitation and run-off, allowingfor strong salinity stratification; (ii) a spring diatom bloomwhere the chlorophyll a concentration reached 50 mg m^–3;(ii) depletions of dissolved inorganic N and Si in the photiczone; and (iv) several days of rapid warming and stabilizationof the upper surface layer. These conditions may be generalprerequisites for M.rubrum blooms in temperate estuaries. ¹Present address: Station Marine d'Endoume, Centre d'Oceanologiede Marseille, rue Batterie des Lions, 13007 Marseille, France     

The seasonal abundance of the phototrophic ciliate Mesodinium rubrum in Southampton Water, England

The abundance of the marine phototrophic planktonic ciliateMesodinium rubrum was monitored throughout an annual cycle attwo stations in the Southampton Water estuary. Seasonal changesin the concentration of nitrate, ammonia and phosphate weremonitored both at the inner estuary station (NW Netley) andouter estuary station (Calshot). Nutrient levels in the winterwere similar at both stations, and were diminished during sequentialdiatom blooms dominated initially by Sketetonema costatum andthen by Rhizosolenia dclicatula. Nitrate was reduced to a seasonalminimum in the outer estuary following these spring diatom blooms,but in the inner estuary was sustained >500 µg I^–1until the onset of the M.rubrum bloom. During the developmentof a visible red tide of M.rubrum in June/July at NW Netley,nutrient concentrations were considerably reduced. Cell numbersof M.rubrum varied between 2 and 3 cells ml^– during winterto >400 cells ml^–1 during the bloom at NW Netley, whereasat Calshot cell abundance did not increase above 25 cells ml^–1at any time of the year. At NW Netley, dense accumulations ofthe ciliate occurred over restricted depth intervals duringthe bloom and possible factors influencing the observed verticaldistribution of cells are considered. ¹Present address: Biology Department, Faculty of Science, AddisAbaba University, PO Box 1176, Addis Ababa, Ethiopia     

Blooms of Mesodinium rubrum in Southampton Water--do they shape mesozooplankton distribution?

Blooms of the red-tide ciliate Mesodinium rubrum occur everyyear in Southampton Water from late May to August, peaking inabundance in July. During blooms, M.rubrum concentrates in subsurfacelayers during the day and and also undergoes diurnal verticalmigration; this results in supersaturation in the near-surfacewater and significant deoxygenation at lower depths. Duringthe period of M.rubrum bloom, the mesozooplankton communityof Southampton Water is typically dominated by nauplius larvaeand calanoid copepods. The true nature of M.rubrum's impacton mesozooplankton and fish communities is equivocal, with contrastingreports of either bloom-associated avoidance or mortality byzooplankton or fish, or both, or alternatively grazing by micro-and mesoplankton on M.rubrum. A temporal sequence of zooplanktonhauls conducted between mid-May and early August indicated thatvertical profiles of mesozooplankton composition and abundancetypically exhibited lower near-surface densities, with numbersincreasing significantly below 3 m. During blooms, this patternoccurred both inside and outside patches, and therefore thereduced near-surface zooplankton numbers are considered to becaused primarily by turbulent mixing rather than by the associatedoxygen supersaturation induced by M.rubrum. Equally, no clearpattern of mesozooplankton density differences was observedat lower depths, associated with the low concentrations of oxygencaused by M.rubrum respiration. The results of the samplingprogramme undertaken show that M.rubrum does not significantlyexclude zooplankton from the vicinity of patches, nor is thereany associated substantial increase in zooplankton numbers.It is concluded that M.rubrum blooms have no immediate significantimpact on the broad structure of the mesozooplankton communitywithin Southampton Water.     

Uptake of 13C and 15N (ammonium, nitrate and urea) by Microcystis in Lake Kasumigaura

The uptake rate of carbon and nitrogen (ammonium, nitrate andurea) by the Microcystis predominating among phytoplankton wasinvestigated in the summer of 1984 in Takahamaira Bay of LakeKasumigaura. The V_max values of Microcystis for nitrate (0.025–0.046h^–1) and ammonium (0.15–0.17 h^–1) were considerablyhigher than other natural phytoplankton. The ammonium, nitrateand urea uptake by Microcystis was light dependent and was notinhibited with nigh light intensity. The K₁ values were farlower than the I_k values. The carbon uptake was not influencedby nitrogen enrichment. Microcystis accelerated the uptake rateby changing V_max/K _s value when nitrogen versus carbon contentin cells declined. Nitrate was scarcely existent in TakahamairiBay during the summer, when Microcystis usually used ammoniumas the nitrogen source. However, the standing stock of ammoniumin the water was far lower than the daily ammonium uptake rates.Therefore, the ammonium in this water had to be supplied becauseof its rapid turn-over time (–0.7–2.6 h).     

Discrete, subsurface layers of the autotrophic ciliate Mesodinium rubrum off Brazil

Highly constrained, subsurface layers of Mesodinium rubrum (Lohmann)were observed and sampled on the continental shelf off the northerncoast of São Paulo State, Brazil in calm, sunny weather.The layers of this autotrophic ciliate occurred as visible lenticularbillows of red water lying 1.5—2 m below the sea surface.Upper and lower limits of the discolored layers, as seen bydivers, were defined by sharp visual discontinuities. Maximumvertical thickness of the layers was     

Planktonic nitrogen transformations during a declining cyanobacteria bloom in the Baltic Sea

The uptake of ¹⁵N-labelled nitrogen nutrients (ammonium, urea,nitrate) was studied during the decline of a bloom of nitrogen-fixingcyanobacteria in the Baltic Sea. This was done by sampling anorth-south transect of stations, representing different stagesof the bloom. Comparison with nitrogen fixation data showedthat this process was of minor importance, and that the nitrogenuptake was dominated by regenerated nitrogen, mainly ammonium.From time series incubations for studying nutrient uptake, itappears that the regeneration of ammonium was substantial, butthat the production of urea or nitrate was slow. The integrateddaily uptake was calculated for the 0–15 m interval atfour stations and values ranged between 6 and 21 mmol N m^–2day^–1, of which the regenerated nutrients, ammonium andurea, constituted 71–93%. Nitrate was of minor importanceand the highest nitrate uptake rates were found close to thethermocline (at 15 m) and in the southern part of the Baltic.Comparison with carbon fixation data reported from simultaneousmeasurements at two stations gave C/N uptake ratios of 4.9 and2.1 for integrated daily uptake. Contrary to earlier findings,the concentration of DON increased with increasing salinity(from 15 to 17 µmol l^–1). This was correlated withthe declination of the bloom and is suggested to be a resultof a gradual release of less easily utilized DON from the degradationof cyanobacteria. The C/N ratio of DOM was high, 21–23.     

Photosynthetic pigments in the ciliate Laboea strobila from Long Island Sound, USA

Laboea sirobila Lohmann, a marine oligotrich ciliate, was presentin Long Island Sound, USA, from March through June 1984. Peakabundance occurred in mid-June, when it was estimated that 10.2x 10⁶ individuals m^–2 were present in the 37-m deep watercolumn. When preserved specimens were examined with epifluorescencemicroscopy, the photosynthetic pigments chlorophyll and phycoerythrinwere observed within chloroplasts inside the ciliate. Thesepigments were also present in Myrionecta (formerly Mesodinium)rubrum Jankowski, a photosynthetic ciliate which co-occurredwith L. strobila during the present study. Vertical profilesshowed both ciliates to be most abundant in the upper few metersof the water column, especially during periods of strong thermalstratification.     

Nitrate Uptake and Reduction of Aseptically Cultivated Spruce Seedlings, Picea abies (L.) Karst

Spruce (Picea abies (L.) Karst.) seedlings were asepticallycultivated and the effects of different N-nutrition on net uptakeand reduction of nitrate were investigated. The characteristicsof nitrate uptake were calculated, K_s as 0?2 mol m^–3 andV_max as 18 µmol g^–1 d^–1. Low pH, and Al³⁺ in the medium caused adecrease in nitrate uptake rate. An in vivo assay was set upwhich allowed the measurement of NRA in both roots and needlesof spruce seedlings. The in vivo nitrate reductase activitywas repressed by ammonium and stimulated by nitrate. Nitratereduction was similar to nitrate uptake, negatively affectedby low pH and ammonium. Therefore, a limited N-supply to spruceseemed to occur when pH was low in the rhizosphere combinedwith the presence of Al³⁺ and . Key words: Spruce, nitrate uptake, nitrate reduction     

Rapid, Reversible Inhibition of Nitrate Influx in Barley by Ammonium

The rate of influx of nitrate into the roots of intact barleyplants was measured over a period of 3–5 min from externalnitrate concentrations of 1–150 mmol m^–3, using¹³N-labelled nitrate as tracer. Ammonium at external concentrationsof 0.005–50 mol m^–3 inhibited nitrate influx ina manner which did not conform to a simple kinetic model butincreased approximately as the logarithm of the ammonium concentration.At any particular ammonium concentration, inhibition of nitrateinflux reached its full extent within 3 min of the ammoniumbeing supplied and was not made more severe by up to 17 minpre-treatment with ammonium. On removing the external ammonium,nitrate influx returned to its original rate within about 3min. Potassium at 0.005–50 mol m^–3 did not reproducethe rapid effect of ammonium on nitrate influx. Net uptake of nitrate also decreased when ammonium was supplied,over a similar timescale and to a similar extent as nitrateinflux. The decrease in nitrate influx caused by ammonium wassufficient to account for the observed reduction in net uptake,without necessitating any acceleration of nitrate efflux. Key words: Hordeum vulgare, roots, ion transport, short-lived isotopes, ¹³N     

Influence of Root and Content on the Temperature Response of Net and Uptake in Chilling Sensitive and Chilling Resistant Lycopersicon Taxa

We studied the influence of internal ammonium and nitrate contenton the temperature response of ammonium and nitrate uptake inboth chilling sensitive and chilling resistant tomatoes. Threetaxa were examined: Lycopersicon esculentum Mill. cv. T-5, achilling sensitive cultivar, Lycopersicon hirsutum Humb. andBompl. LA 1264, a wild, chilling sensitive accession from thelowlands of Ecuador, and Lycopersicon hirsutum LA1778, a chillingresistant accession from the highlands of Peru. Short exposures(4 h) of L. esculentum cv. T-5 to chilling temperatures irreversiblyinhibited ammonium absorption for at least 6 h. Nitrate absorptionin this taxon and ammonium and nitrate absorption in the L.hirsutum accessions recovered fully and immediately from suchexposures. The chilling resistant accession, L. hirsutum LA1778,showed a lower Q₁₀ for ammonium absorption (1?54?0?10, mean?s.e.)than its chilling sensitive relatives, L. hirsutum LA1264 (2?37?0?35)and L. esculentum cv. T-5 (1?92?0?11). The temperature responseof nitrate absorption depended on internal nitrate status; plantsgrown at high levels of ammonium and nitrate (200 mmol m^–3)showed higher Q₁₀'s for nitrate uptake (2?29?0?10) than thosedepleted of internal (1?86?0?12). Key words: Lycopersicon, ammonium, nitrate, temperature response, chilling     

Nitrogenous nutrient uptake by phytoplankton and ammonium regeneration by microbial assemblage in Lake Biwa

In situ rates of nitrate, ammoniwn and urea uptake by the phytoplanktonassemblage, and the regeneration rate of ammonium by the microbialassemblage, in Lake Biwa were measured using the nitrogen 15tracer method from 1985 to 1987. The rate of total nitrogen(sum of ammonium, nitrate and urea) uptake was in the rangeof 62–594 ng N^–1 r^–1 h^–1. The percentagecontribution of ammonium uptake was 41–92%, that of urea4–58% and that of nitrate <1–28% of total uptake.The annual mean new production which was supported by nitrateuptake was 18% of the total production in 1986. The phytoplanktonassemblage in Lake Biwa preferentially utilized regeneratednitrogen, such as ammonium and urea, whose concentration wasmuch lower than that of nitrate throughout the observation penodwithout in summer. The in situ nitrogen uptake rate was almostsufficient to meet the nitrogen requirement of the phytoplanktonassemblage, except in midsummer when the nitrate concentrationwas below the detection limit of 0.3 µg N r^–1. Inthe trophogemc layer, the rate of ammonium regeneration was66–272 ng N 1^–1 h^–1 Although the ambient ammoniumconcentration in the trophogenic layer was maintained at aroundthe half-saturation constant for ammonium uptake kinetics, theammomum uptake rates were always highly correlated with ammoniumregeneration rates. From the size fractionation experimentsand estimates from the literature, it was suggested that themicrobial assemblage <1 µm may have been the most importantagent responsible for the ammonium regeneration processes inthe trophogenic layer.     

Potential Nitrification as an Indicator of Preferential Uptake of Ammonium or Nitrate by Plants in an Oak Woodland Understorey

The preferences of some woodland understorey species for ammoniumand nitrate were investigated by measuring the potential nitrification(conversion of ammonium to nitrate) in the rhizosphere comparedwith the bulk soil. Less acid-tolerant species, which usuallyprefer nitrate or a mixture of ammonium and nitrate in hydroponicculture, should have a higher potential nitrification in therhizosphere compared to the bulk soil due to a low uptake ofammonium (since ammonium is relatively immobile). Acid-tolerantspecies should have a high uptake of ammonium and thereby loweror equal potential nitrification in the rhizosphere comparedto the bulk soil. The hypothesis was tested in a field investigationof five understorey herb species, Deschampsia flexuosa, Convallariamajalis, Poa nemoralis, Geum urbanum andAegopodium podagrariaperformed in oak forests in southern Sweden. Overall, the twoless acid-tolerant species, Geum urbanum and Aegopodium podagraria,had high potential nitrification in the rhizosphere comparedto the bulk soil (indicating a relatively low uptake of ammonium),whilst the acid tolerant species, Deschampsia flexuosa andConvallariamajalis , had approximately equal potential nitrification inthe rhizosphere compared to the bulk soil (indicating a relativelyhigh uptake of ammonium). In the case of Poa nemoralis, a specieswhich grows in both acid and less acid soils, we found the potentialnitrification in the rhizosphere and in the bulk soil to besimilar at low inorganic nitrogen concentrations, but the difference(rhizosphere > bulk) increased when nitrification in thebulk soil was enhanced (i.e. when the nitrogen availabilityincreased). The potential nitrification in the bulk soil variedbetween 0 and 16 nmol g^-1h^-1and was positively correlated withpH. When species occurred at the same site, the potential nitrificationin the bulk soil tended to be lower for the acid tolerant species.Despite a large variation in potential nitrification, the methodoffers a possibility of measuring the preference of plants forammonium/nitrate in a soil system, under natural conditions.Copyright 2000 Annals of Botany Company Ammonium uptake, nitrate uptake, nitrogen preference, potential nitrification, rhizosphere, Deschampsia flexuosa, Convallaria majalis, Poa nemoralis, Geum urbanum, Aegopodium podagraria     

Trichlorfon-Induced Inhibition of Nitrate and Ammonium Uptake in Cyanobacteria

The possibility that the primary effect of the toxic insecticidetrichlorfon is an inhibition of nitrate uptake in cyanobactenahas been investigated. A drastic reduction in the rate of uptakeis detected 3 h after the addition of the insecticide to batchcultures of nabaena PCC 7119. The dose-response curves indicatea relationship between the degree of inhibition of nitrate uptakeand the reduction of chlorophyll content and growth. Nitratereductase (ferredoxin : nitrate reductase, EC 1.7.99.4 [EC] ) activityis also lowered as a result of insecticide action. When AnabaenaPCC 7119 cells are grown with ammonium as a source of combinednitrogen, trichlorfon reduces the rate of ammonium uptake. Therate of uptake of both nitrate and ammonium is restored uponwashing the cells. Ultrastructural analysis of Anabaena nitrate-growncells shows that trichlorfon does not damage thylakoid membranes,but brings about the accumulation of enlarged cyanophycin granulesand the increase of carboxysome number. Nitrate uptake rateand chlorophyll and phycobiliprotein contents are also reducedby insecticide treatment in the cyanobacteria SynechococcusUAM 211, GloeothecePCC 6501, Plectonema calothricoides, NostocUAM 205 and Chlorogloeopsis PCC 6912. These results are consistentwith the inhibition of nitrate uptake due to weak adsorptionof trichlorfon to the plasmalemma being the main effect of theinsecticide on cyanobacterial metabolism. Key words: Nitrate uptake, cyanobacteria, Anabaena, ammonium uptake, trichlorfon     

Control of Net Uptake of Nutrients by Regulation of Influx in Barley Plants Recovering from Nutrient Deficiency

Rates of influx and net uptake of nitrate, phosphate and sulphatewere measured in intact barley plants, and concurrent effluxwas obtained by difference. Net uptake of these anions variedwidely depending on the nutrient status of the plants, and thedifferences in net uptake could be accounted for almost entirelyby changes in influx. Efflux played only a minor role in regulatingnet uptake of nitrate, phosphate or sulphate during recoveryfrom N-, P-, or S-deficiency. Nitrate influx and short-term ammonium absorption by N-deficientbarley plants were closely correlated, and varied in parallelwith rates of net uptake of nitrate or ammonium by similar plants.Again, it would seem that net uptake of ammonium is controlledpredominantly by changes in the rate of influx.Copyright 1993,1999 Academic Press Hordeum vulgare, barley, nutrient absorption, influx, nitrate, phosphate, sulphate, ammonium     

Effects of Root Temperature and Form of Nitrogen Nutrition on Nitrate Reductase Activity in Oilseed Rape (Brassica napus L.)

The effect of root temperature and form of inorganic nitrogensupply on in vitro nitrate reductase activity (NRA) was studiedin oilseed rape (Brassica napus L. cv. bien venu). Plants weregrown initially in flowing nutrient solution containing 10 µMNH₄NO₃ and then supplied with either nitrate or ammonium for15 d at root temperatures of 3, 7, 11 or 17 °C. Shoot temperatureregime was similar for all plants; 20/15 °C, day/night.Root NRA was highest when roots were grown at 3 and 7 °C.In laminae and petioles NRA was highest when roots were 11 or17 °C. The plants supplied with ammonium had much lowerlevels of NRA in roots after 5 d than the plants supplied onlywith nitrate. NRA in the laminae of plants supplied with ammoniumwas low relative to that in plants supplied with nitrate onlywhen root temperature was 11 or 17 °C. Values of the apparent activation energy (E_a) of NR, calculatedfrom the Arrhenius equation, in laminae and petioles were differentfrom roots suggesting difference in enzyme conformation. Evidencethat the temperature at which roots were growing affected E_awas equivocal. Oilseed rape, Brassica napus L., activation energy, ammonium, Arrhenius equation, nitrate, root temperature, nitrate reductase     

Nitrogen-13 Studies of Nitrate Fluxes in Barley Roots: II. EFFECT OF PLANT N-STATUS ON THE KINETIC PARAMETERS OF NITRATE INFLUX

Influx of nitrate into the roots of intact barley plants wasfollowed over periods of 1–15 min using nitrogen-13 asa tracer. Based on measurements taken over 15 min from a rangeof external nitrate concentrations (0·2–250 mmolm^–3), the kinetic parameters of influx, I_max and K_m, werecalculated. Compared with plants grown in the presence of nitrate throughout,plants that had been starved of N for 3 d showed a significantlygreater value ofI_max for ¹³N-nitrate influx (by a factor of1·4–1·8), but a similar value of K_m (12–14mmol m^–3). Pre-treating N-starved plants with nitratefor about 5 h further increased the subsequent rate of ¹³N-nitrateinflux, but had little effect in the unstarved controls. Allowingfor this induction of additional nitrate transport, the differencein rates of nitrate influx in control and N-starved plants wassufficient to account for the previously-observed differencein net uptake by the two groups of plants. In barley plants grown without any exposure to nitrate, butwith ammonium as N-source, both I_max and K_m for subsequent ¹³N-nitrateinflux were significantly decreased (by about one-half) comparedwith the corresponding nitrate-grown controls. The importance of changes in the rate of influx in the regulationof net uptake of nitrate is discussed. Key words: Ion transport, nitrate, influx, kinetic parameters, N-deficiency     

Effect of temperature and irradiance on the uptake of ammonium and nitrate by <Emphasis Type="Italic">Laurencia brongniartii</Emphasis> (Rhodophyta,Ceramiales)

The effects of temperature (20, 24 and 28 °C) and irradiance (15 and 40 μmol photon m⁻² s⁻¹) on the nitrate and ammonium uptake rates of the subtropical red alga, Laurencia brongniartii, were investigated to prepare for tank cultivation. Nitrate uptake followed saturation kinetics and was faster at higher irradiances and temperatures. In contrast, ammonium uptake was linear over the experimental range and was not affected by an increase in temperature. A parameter, β, was calculated to compare substrate uptake rates of nitrate along the linear portion of the uptake curve with that of ammonium. For nitrate, β was lower at low irradiance and higher at high irradiance (β = 0.007 ± 0.003 and 0.030 ± 0.002 [μmol N L⁻¹ (μmol N g_ww⁻¹ d⁻)⁻¹], respectively). However, β was 0.023 ± 0.002 and 0.034 ± 0.002 [μmol N L⁻¹ (μmol N g_ww⁻¹ d⁻¹)⁻¹] for ammonium, suggesting a preference for ammonium over nitrate.     

The Apparent Induction of Nitrate Uptake by Chara corallina Cells following Pretreatment with or without Nitrate and Chlorate

Nitrate provision has been found to regulate the capacity forChara corallina cells to take up nitrate. When nitrate was suppliedto N sufficient cells maximum nitrate uptake was reached after8 h. Prolonged treatment of the cells in the absence of N alsoresulted in the apparent ability of these cells to take up nitrate.Chlorate was found to substitute partially for nitrate in the‘induction’ step. The effects on nitrate reductionwere separated from those on nitrate uptake by experiments usingtungstate. Tungstate pretreatment had no effect on NO^–₃uptake ‘induced’ by N starvation, but inhibitedNO^–₃ uptake associated with NO^–₃ pretreatment. Chloridepretreatment similarly had no effect on NO^–₃ uptake ‘induced’by N deprivation, but inhibited NO^–₃ uptake followingNO^–₃ pretreatment. The data suggest that there are atleast two mechanisms responsible for the ‘induction’of nitrate uptake by Chara cells, one associated with NO^–₃reduction and ‘induced’ by CIO^–₃ or NO^–₃and one associated with N deprivation. Key words: Nitrate, Chlorate, Chara corallina, Induction     

Seasonal Variations of Dissolved Nitrogen and DOC:DON Ratios in an Intermittent Mediterranean Stream

Seasonal variations of dissolved inorganic nitrogen (DIN) (NO₃–N and NH₄–N) and dissolved organic nitrogen (DON) were determined in Fuirosos, an intermittent stream draining an unpolluted Mediterranean forested catchment (10.5 km²) in Catalonia (Spain). The influence of flow on streamwater concentrations and seasonal differences in quality and origin of dissolved organic matter, inferred from dissolved organic carbon to nitrogen ratios (DOC:DON ratios), were examined. During baseflow conditions, nitrate and ammonium had opposite behaviour, probably controlled by biological processes such as vegetation uptake and mineralization activity. DON concentrations did not have a seasonal trend. During storms, nitrate and DON increased by several times but discharge was not a good predictor of nutrient concentrations. DOC:DON ratios in streamwater were around 26, except during the months following drought when DOC:DON ratios ranged between 42 and 20 during baseflow and stormflow conditions, respectively. Annual N export during 2000–2001 was 70 kg km⁻¹ year⁻¹, of which 75% was delivered during stormflow. The relative contribution of nitrogen forms to the total annual export was 57, 35 and 8% as NO₃–N, DON and NH₄–N, respectively.     

Ammonium Triggers Uptake of NO-3 by Chenopodium rubrum Suspension Culture Cells and Remobilization of their Vacuolar Nitrate Pool

Photoautotrophic cell suspension cultures of Chenopodium rubrumrequire high concentrations of nitrate and ammonium. Duringthe growth phase total NH₄⁺ and the greater portion of NH₃^–were consumed. During the stationary phase nitrate uptake continuedbut at a substantially smaller rate than during the growth phase.During growth the bulk of the absorbed N was incorporated intoprotein, the amount of which was then maintained constant untilsenescence. NH₃^– was accumulated upon transition betweenthe growth and the stationary phase. NH₃^–, like the freeamino acids, was deposited in the vacuole but, unlike thesecompounds, could not be remobilized upon transfer of the cellsinto N-free medium. Readdition of NH₄⁺ to the medium, however,resulted in a mobilization of the vacuolar NH₃^–-pool.Reutilization of both vacuolar N-storage pools must have beenaccomplished by recycling from the vacuole to the cytoplasmbecause N-metabolizing enzymes could not be detected in isolatedvacuoles. Transfer of the cells of the stationary phase intomedium containing NH₃^– and NH₄⁺ resulted in an inductionof nitrate uptake by the cells, but only after a lag phase of4–5 days. It is conceivable that NH₄⁺ induces NH₃^–-translocatingsystems in the plasmalemma and in the tonoplast. (Received December 19, 1988; Accepted March 2, 1989)