Photosynthetic o(2) exchange kinetics in isolated soybean cells

Light-dependent O₂ exchange was measured in intact, isolated soybean (Glycine max. var. Williams) cells using isotopically labeled O₂ and a mass spectrometer. The dependence of O₂ exchange on O₂ and CO₂ was investigated at high light in coupled and uncoupled cells. With coupled cells at high O₂, O₂ evolution followed similar kinetics at high and low CO₂. Steady-state rates of O₂ uptake were insignificant at high CO₂, but progressively increased with decreasing CO₂. At low CO₂, steady-state rates of O₂ uptake were 50% to 70% of the maximum CO₂-supported rates of O₂ evolution. These high rates of O₂ uptake exceeded the maximum rate of O₂ reduction determined in uncoupled cells, suggesting the occurrence of another light-induced O₂-uptake process (i.e. photorespiration).

Rates of O₂ exchange in uncoupled cells were half-saturated at 7% to 8% O₂. Initial rates (during induction) of O₂ exchange in uninhibited cells were also half-saturated at 7% to 8% O₂. In contrast, steady-state rates of O₂ evolution and O₂ uptake (at low CO₂) were half-saturated at 18% to 20% O₂. O₂ uptake was significantly suppressed in the presence of nitrate, suggesting that nitrate and/or nitrite can compete with O₂ for photoreductant.

These results suggest that two mechanisms (O₂ reduction and photorespiration) are responsible for the light-dependent O₂ uptake observed in uninhibited cells under CO₂-limiting conditions. The relative contribution of each process to the rate of O₂ uptake appears to be dependent on the O₂ level. At high O₂ concentrations (≥40%), photorespiration is the major O₂-consuming process. At lower (ambient) O₂ concentrations (≤20%), O₂ reduction accounts for a significant portion of the total light-dependent O₂ uptake.

     

Changes in alkaline phosphatase activity and phosphate uptake in P-limited phytoplankton,induced by light intensity and spectral quality

Alkaline phosphatase activity and P uptake were determined in P-limited Dunaliella tertiolecta, Thalassiosira pseudonana, Phaeodactylum tricornumtum, and Prymnesium parvum grown under different light intensities and colors. Both intracellular and extracellular enzyme activities varied with the intensity and quality of light in a species-specific manner. The spectral composition of the light also affected P uptake kinetics. No correlation was found between enzyme activity and V_max both within a species and for pooled data for all four species, indicating that the change in uptake kinetics and enzyme activity was not related to P limitation, but induced by the light conditions. Changes in the optimum N:P ratio induced by light were also not related to P uptake kinetics or enzyme activity. These data suggest that light conditions may in themselves have profound effects on species competition for limiting nutrients. Furthermore, since both alkaline phosphatase activity and P uptake were influenced by the prevailing light conditions we suggest that these parameters be used cautiously when determining the P nutritional status of phytoplankton in nature.Address for reprint requests     

VARIABILITY IN NITRATE UPTAKE KINETICS IN THALASSIOSIRA PSEUDONANA (BACILLARIOPHYCEAE)1

Short-term (1–9 min) nitrate uptake kinetics were measured in Thalassiosira pseudonana (Hust.) Hasle & Heimdal grown in nitrate-limited, ammonium-limited, and nitrate-sufficient continuous cultures. For all cultures, maximal nitrate uptake rates did not develop until approximately 3 min after nitrate addition; thereafter, nitrate uptake rates remained constant or declined slightly. The K_s and V_max for the nitrate-limited cultures were higher at any growth rate than those for the ammonium-limited or nitrate-sufficient cultures. Thus, much higher nitrate concentrations would be required to saturate nitrate uptake in nitrate-limited Thalassiosira pseudonana than is usually considered necessary. The lack of data for other species grown under a range of environmental conditions makes it difficult to generalize about the effect of preconditioning on nitrate uptake kinetics.     

Urea uptake by the scleractinian coral Stylophora pistillata

Urea can be one of the major sources of nitrogen for phytoplankton, but little is known about its importance for corals. Experiments were therefore designed to assess the uptake rates of urea by the scleractinian coral Stylophora pistillata; ¹⁵N-urea was used to follow the incorporation of nitrogen into the zooxanthellae and animal tissue. The uptake kinetics of urea in the tissue of S. pistillata showed that there is a concentration-dependent uptake of urea. The transport of urea was composed of a linear component (diffusion) at concentrations higher than 6 μmol N-urea l^− 1 and an active carrier-mediated component, at lower concentrations. The value of the carrier affinity (K_m = 1.05 μmol urea l^− 1) indicates a good adaptation of the corals to low levels of urea in seawater. At the in situ concentration of ca. 0.2 μmol N-urea l^− 1, the uptake rate was equal to 0.1 nmol N h^− 1 cm^− 2. Urea uptake was at least four times higher in the animal than in the algal fraction, and five times higher when corals were incubated in the light than in the dark. These results could be explained by the involvement of urea in the calcification process, which is also enhanced by light. Comparison of urea uptake rates with nitrate or ammonium uptake rates for the same S. pistillata species, at in situ concentrations, showed that urea is preferred to nitrate and may therefore be an important source of nitrogen for scleractinian corals.     

The Kinetics of Chlorate Uptake by XD Tobacco Cells

The uptake of [³⁶Cl]chlorate by the 14U variant of the XD cell line of Nicotiana tobaccum L. cv Xanthi was investigated to examine the use of chlorate as a nitrate analog in transport studies. The kinetics of chlorate uptake against concentration was complex. Evidence was obtained, e.g., by means of nitrate competition, that these kinetics could be resolved into two components indicating the existence of two influx mechanisms: a saturable high affinity transport system (HATS) and a low affinity transport system (LATS) that showed first order kinetics. HATS has an apparent K_m for chlorate of 0.3 millimolar, and a marked pH dependence. The V_max dropped about fivefold as the pH was changed from the optimum pH (5.5-6.5), while the K_m remained virtually unchanged. The activity of HATS was completely inhibited by 15 millimolar nitrate and was less sensitive to chloride. LATS was inhibited by chloride and showed some inhibition by nitrate. It was concluded that [³⁶Cl]chlorate can be used as an analog for nitrate uptake studies only in a limited low concentration range where HATS is the main route for chlorate influx.     

Oxygen exchange in leaves in the light

Photosynthetic O₂ production and photorespiratory O₂ uptake were measured using isotopic techniques, in the C₃ species Hirschfeldia incana Lowe., Helianthus annuus L., and Phaseolus vulgaris L. At high CO₂ and normal O₂, O₂ production increased linearly with light intensity. At low O₂ or low CO₂, O₂ production was suppressed, indicating that increased concentrations of both O₂ and CO₂ can stimulate O₂ production. At the CO₂ compensation point, O₂ uptake equaled O₂ production over a wide range of O₂ concentrations. O₂ uptake increased with light intensity and O₂ concentration. At low light intensities, O₂ uptake was suppressed by increased CO₂ concentrations so that O₂ uptake at 1,000 microliters per liter CO₂ was 28 to 35% of the uptake at the CO₂ compensation point. At high light intensities, O₂ uptake was stimulated by low concentrations of CO₂ and suppressed by higher concentrations of CO₂. O₂ uptake at high light intensity and 1000 microliters per liter CO₂ was 75% or more of the rate of O₂ uptake at the compensation point. The response of O₂ uptake to light intensity extrapolated to zero in darkness, suggesting that O₂ uptake via dark respiration may be suppressed in the light. The response of O₂ uptake to O₂ concentration saturated at about 30% O₂ in high light and at a lower O₂ concentration in low light. O₂ uptake was also observed with the C₄ plant Amaranthus edulis; the rate of uptake at the CO₂ compensation point was 20% of that observed at the same light intensity with the C₃ species, and this rate was not influenced by the CO₂ concentration. The results are discussed and interpreted in terms of the ribulose-1,5-bisphosphate oxygenase reaction, the associated metabolism of the photorespiratory pathway, and direct photosynthetic reduction of O₂.     

Nitrate Utilization by the Diatom Skeletonema costatum: II. Regulation of Nitrate Uptake

Nitrate utilization has been characterized in nitrogen-deficient cells of the marine diatom Skeletonema costatum. In order to separate nitrate uptake from nitrate reduction, nitrate reductase activity was suppressed with tungstate. Neither nitrite nor the presence of amino acids in the external medium or darkness affects nitrate uptake kinetics. Ammonium strongly inhibits carrier-mediated nitrate uptake, without affecting diffusion transfer. A model is proposed for the uptake and assimilation of nitrate in S. costatum and their regulation by ammonium ions.     

Hydrogen sulfide-producing kinetics of Shewanella oneidensis in sulfite and thiosulfate respiration

Shewanella oneidensis is a model species for aquatic ecosystems and plays an important role in bioremediation, biofuel cell manufacturing and biogeochemical cycling. S. oneidensis MR-1 is able to generate hydrogen sulfide from various sulfur species; however, its catalytic kinetics have not been determined. In this study, five in-frame deletion mutants of S. oneidensis were constructed and their H₂S-producing activities were analyzed. SirA and PsrA were the two major contributors to H₂S generation under anoxic cultivation, and the optimum SO₃²⁻ concentration for sulfite respiration was approximately 0.8 mM, while the optimum S₂O₃²⁻ concentration for thiosulfate respiration was approximately 0.4 mM. Sulfite and thiosulfate were observed to interfere with each other during respiration, and a high concentration of sulfite or thiosulfate chelated extracellular free-iron but did not repress the expression of sirA or psrA. Nitrite and nitrate were two preferred electron acceptors during anaerobic respiration; however, under energy-insufficient conditions, S. oneidensis could utilize multiple electron acceptors simultaneously. Elucidiating the stoichiometry of H₂S production in S. oneidensis would be helpful for the application of this species in bioremediation and biofuel cell manufacturing, and would help to characterize the ecophysiology of sulfur cycling.     

Nitrogen uptake kinetics of Prymnesium parvum (Haptophyte)

The uptake rates of different nitrogen (N) forms (NO₃⁻, urea, and the amino acids glycine and glutamic acid) by N-deficient, laboratory-grown cells of the mixotrophic haptophyte, Prymnesium parvum, were measured and the preference by the cells for the different forms determined. Cellular N uptake rates (ρ_cell, fmol N cell⁻¹ h⁻¹) were measured using ¹⁵N-labeled N substrates. P. parvum showed high preference for the tested amino acids, in particular glutamic acid, over urea and NO₃⁻ under the culture nutrient conditions. However, extrapolating these rates to Baltic Seawater summer conditions, P. parvum would be expected to show higher uptake rates of NO₃⁻ and the amino acids relative to urea because of the difference in average concentrations of these substrates. A high uptake rate of glutamic acid at low substrate concentrations suggests that this substrate is likely used through extracellular enzymes. Nitrate, urea and glycine, on the other hand, showed a non-saturating uptake over the tested substrate concentration (1–40 μM-N for NO₃⁻ and urea, 0.5–10 μM-N for glycine), indicating slower membrane-transport rates for these substrates.     

Distinctive Light and CO(2)-Fixation Requirements of Nitrate and Ammonium Utilization by the Cyanobacterium Anacystis nidulans

The effect of light intensity on the rates of ammonium and nitrate uptake and of CO₂ fixation has been determined in intact Anacystis nidulans cells. Ammonium uptake became saturated at photon flux values of about 60 microeinsteins per square meter per second, whereas both nitrate uptake and CO₂ fixation reached saturation at about 250 microeinsteins per square meter per second, the rates of the two latter processes being tightly correlated at any light intensity assayed. Inhibition of ammonium assimilation resulted in the loss of correlation between CO₂ fixation and nitrate uptake, the latter process exhibiting then a reduced light requirement. The results establish a clear distinction between ammonium utilization and nitrate utilization with regard to their light requirement and to the nature of their dependence upon CO₂ fixation.     

Uptake kinetics of 99Tc in common duckweed

The uptake of the nuclear waste product technetium-99 was studied in common duckweed (Lemna minor). In addition to measurements, a model involving two compartments in duckweed with different chemical forms of technetium was derived. The model was tested by chemical speciation, i.e. differentiating between reduced Tc-compounds and Tc(VII)O(4)(-). The TcO(4)(-) concentrations measured were in good agreement with those predicted by the model. Two processes determine technetium uptake: (1) transport of Tc(VII)O(4)(-) across the cell membrane, and (2) reduction of Tc(VII). The TcO(4)(-) concentration in duckweed reaches a steady state within 2 h while reduced Tc-compounds are stored, as a result of absence of release or re-oxidation processes. Bioaccumulation kinetic properties were derived by varying 99Tc concentration, temperature, nutrient concentrations, and light intensity. The reduction of technetium in duckweed was highly correlated with light intensity and temperature. At 25 degrees C the maximum reduction rate was observed at light intensities above 200 μmol m(-2) s(-1) while half of the maximum transformation rate was reached at 41 μmol m(-2) s(-1). Transport of TcO(4)(-) over the cell membrane requires about 9.4 kJ mol(-1), indicating an active transport mechanism. However, this mechanism behaved as first-order kinetics instead of Michaelis-Menten kinetics between 1x10(-14) and 2.5x10(-5) mol l(-1) TcO(4)(-). Tc uptake could not be inhibited by 10(-3) mol l(-1) nitrate, phosphate, sulphate or chloride.     

Ammonium uptake kinetics in root and leaf cells of Zostera marina L.

Ammonium uptake rates and the mechanism for ammonium transport into the cells have been analysed in Zostera marina L. In the cells of this species, a proton pump is present in the plasmalemma, which maintains the membrane potential. However, this seagrass shows a high-affinity transport mechanism both for nitrate and phosphate which is dependent on sodium and is unique among angiosperms. We have then analysed if the transport of another N form, ammonium, is also dependent of sodium. First, we have studied ammonium transport at the cellular level by measurements of membrane potentials, both in epidermal root cells and mesophyll cells. And second, we have monitored uptake rates in whole leaves and roots by depletion experiments. The results showed that ammonium is taken up by a high-affinity transport system both in root and leaf cells, although two different of kinetics could be discerned in mesophyll cells (with affinity constants of 2.2 ± 1.1 μM NH₄⁺, in the range 0.01-10 μM NH₄⁺, and 23.2 ± 7.1 μM NH₄⁺, at concentrations between 10 and 500 μM NH₄⁺). However, only one kinetic could be observed in epidermal root cells, which showed a K_m = 11.2 ± 1.0 μM NH₄⁺, considering the whole ammonium concentration range assayed (0.01-500 μM NH₄⁺). The higher affinity of leaf cells for ammonium was consistent with the higher uptake rates observed in leaves, with respect to roots, in depletion experiments at 10 μM NH₄⁺ initial concentration. However, when an initial concentration of 100 μM was assayed, the difference between uptake rates was reduced, but still being higher in leaves. Variations in proton or sodium-electrochemical gradient did not affect ammonium uptake, suggesting that the transport of this nutrient is not driven by these ions and that the ammonium transport mechanism could be different to the transport of nitrate and phosphate in this species.     

Oxygen uptake kinetics in chronic heart failure: clinical and physiological aspects

One of the hallmark symptoms of patients with chronic heart failure (CHF) is exercise intolerance. Therefore, exercise testing has become an important tool for the evaluation and monitoring of heart failure. Whereas the maximal aerobic capacity (peak VO₂) is a reliable indicator of the severity and prognosis of heart failure, submaximal exercise parameters may be more closely related to the ability to perform daily activities. As such, oxygen (O₂) uptake kinetics, describing the rate change of O₂ uptake during onset or recovery of submaximal constant-load exercise (O₂ onset and recovery kinetics, respectively), have been shown to be useful parameters for objectively evaluating the functional capacity of CHF patients. However, their evaluation in this population is not a routine part of daily clinical practice. Possible reasons for this include a lack of standardisation of the assessment methodology and a limited number of studies evaluating the clinical use of O₂ uptake kinetics in CHF patients. In addition, the pathophysiological mechanisms underlying the delay in O₂ uptake kinetics in these patients are not completely understood. This review discusses the current literature on the clinical potency and physiological determinants of O₂ uptake kinetics in CHF patients and provides directions for future research. (Neth Heart J 2009;17:238–44.)     

Continuous ammonium enrichment of a woodland stream: uptake kinetics, leaf decomposition, and nitrification

• 1 In order to test for nitrogen limitation and examine ammonium uptake by stream sediments, ammonium hydroxide was added continuously at concentrations averaging 100 μg1^-1 for 70 days to a second- order reach of Walker Branch, an undisturbed woodland stream in Tennessee.
• 2 Ammonium uptake during the first 4h of addition corresponded to adsorption kinetics rather than to first-order uptake or to Michaelis- Menten kinetics. However, the calculated adsorption partition coefficient was two to four orders of magnitude greater than values reported for physical adsorption of ammonium, suggesting that the uptake was largely biotic.
• 3 Mass balance indicated that the uptake of ammonium from the water could be accounted for by increased nitrogen content in benthic organic detritus. Nitrification, inferred from longitudinal gradients in NO₃, began soon after enrichment and increased dramatically near the end of the experiment.
• 4 Both ammonium and nitrate concentrations dropped quickly to near background levels when input ceased, indicating little desorption or nitrification of excess nitrogen stored in the reach.
• 5 There was no evidence of nitrogen limitation as measured by weight loss, oxygen consumption, phosphorus content, and macroinvertebrate density of red oak leaf packs, or by chlorophyll content and aufwuchs biomass on plexiglass slides. A continuous phosphorus enrichment 1 year earlier had demonstrated phosphorus limitation in Walker Branch.

     

The Kok Effect in Chlamydomonas reinhardi

A Haxo-Blinks rate-measuring oxygen electrode together with a modulated light source gave an average current signal (change in net O₂ exchange) and a modulated current signal (photosynthetic O₂ evolution). Using this apparatus, net O₂ exchange and photosynthetic O₂ evolution at low intensities have been studied in the green alga, Chlamydomonas reinhardi. At both 645 nm and 695 nm, the curves of net O₂ exchange as a function of light intensity were steeper at lowest intensities than about compensation, indicative of the Kok effect. The effect was greater at 695 nm than at 645 nm. The corresponding curves of photosynthetic O₂ evolution, on the other hand, showed no Kok effect; here, the slope was lowest at lowest intensity. The absence of the Kok effect in O₂ evolution, together with its sensitivity to monofluoroacetic acid, show that it is due to an interaction of photosynthesis and respiration. The effect was exaggerated by 3-(3,4-dichlorophenyl)-1,1-dimethylurea. In the presence of concentrations of this inhibitor sufficient to inhibit O₂ evolution completely, a light-induced change in net O₂ exchange remained. This was interpreted as a system I dependent depression of respiratory O₂ uptake. The Kok effect remained undiminished in concentrations of carbonyl cyanide m-chlorophenylhydrazone and 2,4-dinitrophenol which partially uncoupled either oxidative phosphorylation alone or both oxidative and photosynthetic phosphorylations. The above results can be explained within a model of the Kok effect in which O₂ uptake is depressed by diversion of reductant away from respiratory electron transport and into photosystem I. The same photodepression of O₂ uptake also appears to account for a transient in net O₂ exchange seen in several algae upon turning off the light.     

Changes in Net O(2) Exchange Induced by Inorganic Nitrogen in the Blue-Green Alga Anacystis nidulans

The response of net O₂ exchange to light intensity by intact Anacystis nidulans cells in the presence of saturating NaHCO₃ concentrations followed a curve with an inflection near the light-compensation point. Addition of either KNO₃ or NH₄Cl stimulated O₂ uptake in the dark and at light intensities below the light-compensation point. This resulted in steeper slopes of the curve calculated below and above the light-compensation point. At O₂ concentrations limiting dark respiration, addition of inorganic nitrogen had no effect on either dark respiration or O₂ exchange in the light. The apparent changes in photosynthetic yield observed under normal O₂ concentration disappeared when respiration was limited by O₂ availability, indicating that the effects of inorganic nitrogen on O₂ exchange at low light intensities are due to stimulation of respiration rather than to increases in photosynthetic yield.     

The impact of slow stomatal kinetics on photosynthesis and water use efficiency under fluctuating light

Dynamic light conditions require continuous adjustments of stomatal aperture. The kinetics of stomatal conductance (g_s) is hypothesized to be key to plant productivity and water use efficiency (WUE). Using step-changes in light intensity, we studied the diversity of light-induced g_s kinetics in relation to stomatal anatomy in five banana genotypes (Musa spp.) and modeled the impact of both diffusional and biochemical limitations on photosynthesis (A). The dominant A limiting factor was the diffusional limitation associated with g_s kinetics. All genotypes exhibited a strong limitation of A by g_s, indicating a priority for water saving. Moreover, significant genotypic differences in g_s kinetics and g_s limitations of A were observed. For two contrasting genotypes, the impact of differential g_s kinetics was further investigated under realistic diurnally fluctuating light conditions and at the whole-plant level. Genotype-specific stomatal kinetics observed at the leaf level was corroborated at whole-plant level by transpiration dynamics, validating that genotype-specific responses are still maintained despite differences in g_s control at different locations in the leaf and across leaves. However, under diurnally fluctuating light conditions the impact of g_s speediness on A and intrinsic (_iWUE) depended on time of day. During the afternoon there was a setback in kinetics: absolute g_s and g_s responses to light were damped, strongly limiting A and impacting diurnal _iWUE. We conclude the impact of differential g_s kinetics depended on target light intensity, magnitude of change, g_s prior to the change in light intensity, and particularly time of day.     

Regulation of Nitrate Uptake in Penicillium chrysogenum by Ammonium Ion

A nitrate uptake system is induced (along with nitrate reductase) when NH₄⁺-grown Penicillium chrysogenum is incubated with inorganic nitrate in synthetic medium in the absence of NH₄⁺. Nitrate uptake and nitrate reduction are probably in steady state in fully induced mycelium, but the ratios of the two activities are not constant during the induction period. Substrate concentrations of ammonium cause a rapid decay of nitrate uptake and nitrate reductase activity. The two activities are differentially inactivated (the uptake activity being more sensitive). Glutamine and asparagine are as effective as NH₄⁺ in suppressing nitrate uptake activity. Glutamate and alanine were about half as effective as NH₄⁺. Cycloheximide interferes with the NH₄⁺-induced decay of nitrate uptake activity. The ammonium transport system is almost maximally deinhibited (or derepressed) in nitrate-grown mycelium.     

Nitrate and phosphate uptake kinetics of the harmful diatom Coscinodiscus wailesii,a causative organism in the bleaching of aquacultured Porphyra thalli

The large diatom Coscinodiscus wailesii is one of the problematic species which indirectly cause bleaching damage to “Nori” (Porphyra thalli) cultivation through competitive utilization of nutrients during its bloom. In the present study, we experimentally investigated the nitrate (N) and phosphate (P) uptake kinetics of C. wailesii, Harima-Nada strain. Maximum uptake rates (ρ_max), obtained by short-term experiments, were 58.3 and 95.5 pmol cell⁻¹ h⁻¹ for nitrate and 41.9 and 59.1 pmol cell⁻¹ h⁻¹ for phosphate at 9 and 20 °C, respectively. The half saturation constants for uptake (K_s) were 2.91 and 5.08 μM N and 5.62 and 6.67 μM P at 9 and 20 °C, respectively. The ρ_max values of C. wailesii, much higher than those of other marine phytoplankton species, suggest that C. wailesii is able to take up large amounts of nutrients from the water column. On the other hand, V_max/K_s (V_max; V_max = ρ_max/Q₀, Q₀; minimum cell quota) values of C. wailesii, which is a better measure to evaluate the competitive ability for nutrient uptake, were low in dominant diatom species. This parameter indicates that C. wailesii is disadvantaged compared to other diatom species in competing for nutrients, and the decreasing nutrient concentrations from winter to spring is an important factor limiting C. wailesii blooming in early spring.     

Nitrate uptake and storage in the seaweed Ulva rigida C. Agardh in relation to nitrate availability and thallus nitrate content in a eutrophic coastal lagoon (Sacca di Goro, Po River Delta, Italy)

The seasonal cycle of biomass and tissue composition of Ulva rigida C. Agardh, in relation to nitrogen availability in the water column, was studied in 1991-1992 in the Sacca di Goro, a highly eutrophic lagoon in the Po River Delta (Italy). Nitrate uptake rates and storage capacity were also determined in laboratory experiments. The seasonal growth of U. rigida was related to the seasonal trend of nitrogen concentration in the water column. U. rigida biomass increased exponentially during spring and attained peaks of about 300-400 g dry mass (DM) m⁻² in June. As biomass increased, U. rigida depleted nitrate in the water column. Thallus nitrate reserves also declined from 100 μmol N (g DM)⁻¹ to almost undetectable levels, and total thallus nitrogen declined from 4% to 2.5% DM and 1.25% DM in 1991 and 1992, respectively. During summer, U. rigida decomposition increased, and organic nitrogen concentrations in the water column increased. The uptake experiments demonstrated an inverse relationship between thallus nitrate content and nitrate uptake rates. A modified Michaelis-Menten equation that accounts for thallus nitrate fit the uptake data well. U. rigida can accumulate up to about 400-500 μmol nitrate (g DM)⁻¹ in cellular reserves. U. rigida in the Sacca di Goro has higher K_m and lower V_max/K_m ratios for nitrate uptake than other chlorophycean species, indicating a low efficiency of uptake at low nitrate concentrations. This low uptake efficiency, and the ability to exploit N availability by storing cellular nitrate pools in excess of immediate growth needs, may represent a physiological response to an eutrophic environment where nitrate is in large supply for most of the year.