The impact of NO inf3 sup− loading on the freshwater macrophyte Littorella uniflora: N utilization strategy in a slow-growing species from oligotrophic habitats

The decline and disappearance of Littorella uniflora from oligotrophic waters which have become eutrophic has been associated with shading or reduced CO₂ supply. However NO _inf3 ^sup– concentrations can reach very high levels (100–2000 mmol m^–3 compared with <1–3 in oligotrophic habitats). To investigate the impact of NO _inf3 ^sup– loading alone, plants were grown under three NO _inf3 ^sup– regimes (very low, near-natural and high). The interactive effects of NO _inf3 ^sup– and photon flux density (low and high regimes) on N assimilation and accumulation, CO₂ concentrating mechanisms, C₃ photosynthesis and growth were also examined. The results were unexpected. Increased NO _inf3 ^sup– supply had very little effect on photosynthetic capacity, crassulacean acid metabolism (CAM) or lacunal CO₂ concentrations ([CO₂]_i), although there was considerable plasticity with respect to light regime. In contrast, increased NO _inf3 ^sup– supply resulted in a marked accumulation of NO _inf3 ^sup– , free amino acids and soluble protein in shoots and roots (up to 25 mol m^–3, 30 mol m^–3 and 9 mg g^–1 fresh weight respectively in roots), while fresh weight and relative growth rate were reduced. Total N content even under the very low NO _inf3 ^sup– regime (1.6–2.3%) was mid-range for aquatic and terrestrial species (and 3.1–4.3% under the high NO _inf3 ^sup– regime). These findings, together with field data, suggest that L. uniflora is not growth limited by low NO _inf3 ^sup– supply in natural oligotophic habitats, due not to an efficient photosynthetic nitrogen use but to a slow growth rate, a low N requirement and to the use of storage to avoid N stress. However the increased NO _inf3 ^sup– concentrations in eutrophic environments seem likely have detrimental effects on the long-term survival of L. uniflora, possibly as a consequence of N accumulation.     

Ammonium uptake in alpine streams in the High Tatra Mountains (Slovakia)

Uptake of NH _inf4 ^sup+ -N by streambed biota of mountain brooks was studied in the alpine zone of the High Tatra Mountains. Experiments were performed involving in situ dosing of ammonium directly to the acidified stream and incubations of ammonium and streambed bryophytes in enclosures within a range of pH from 4.45 to 8.10.NH _inf4 ^sup+ -N uptake length decreased with decreasing stream discharge, while comparable values of discharge-normalized uptake lengths were found during two in situ experiments.Maximum uptake rates of NH _inf4 ^sup+ -N obtained during the incubation of bryophytes (6 to 11 mg m^–2 h^–1) were comparable with results of two in situ experiments (8 and 12 mg m^–2 h^–1). The average NH _inf4 ^sup+ -N uptake rates observed during incubations lasting 3 to 5 hours (4.3 mg m^–2 h^–1) were not related to the pH of stream water. Nitrification of about 50% of the NH _inf4 ^sup+ -N added was observed in non-acidified streams, but was negligible in acidified streams. Significant photoinhibition of nitrification was observed in non-acidified streams during enclosure experiments.     

Biological denitrification of water in a two-chambered immobilized-cell bioreactor

Summary A double-chambered bioreactor based on a composite immobilized-cell gel layer/microporous membrane structure was applied to the continuous denitrification of high-nitrate water. Immobilized denitrifying bacteria (Pseudomonas denitrificans) were provided with separate flows of nitrate and carbon (C) nutrient, with no contamination of the treated water by cell leakage from the gel. Using acetate (7.5 mm) as a C source and a C/N ratio of 3 (mol/mol), specific denitrification rates ranging from 15 to 25 g NO _inf3 ^sup– · h^–1 · – cm^–2 membrane surface (50–85 g NO _inf3 ^sup– · h^–1 · cm^–3 gel) were obtained. The denitrifying activity remained stable for several months. At the flow rate used (10 cm³ · h^–1), the effluents contained noticeable amounts of NO _inf2 ^sup– ions but the treated water remained uncontaminated by the carbon nutrient. Most NO _inf2 ^sup– ions disappeared from the treated water in a second reactor connected in series. When fed with an unchlorinated sludge supernatant as C nutrient, immobilized bacteria performed efficient denitrification of water for only 3 weeks. Diffusion experiments showed that acetate ions diffused much less rapidly than NO _inf3 ^sup– or NO _inf2 ^sup– ions through the composite structure. Further developments of the system are considered.     

Water chemistry and periphyton in an alpine wetland

Remote high elevation sites are thought to be good sites to monitor global change and anthropogenic effects on ecosystems. This study was conducted during 1987–1990 in a high elevation wetland (3593 m) located in the Green Lakes Valley, Front Range, Colorado (USA). Salix spp. was the dominant riparian species in this 2 ha. wetland. Small shallow pools (<0.5 m depth) constituted a water area of 236 m³. The major source of water during the study period was snowmelt. The wetland had a well defined outlet and inlet, although an undetermined amount of water entered as groundwater from the snow patch above. Outlet discharge was 424–460 m³ during the month of July and declined thereafter as water input from the snowpatch declined. Inlet discharge was 67% of outlet discharge. Water temperatures in the outlet were always less than 6.8°C, pH 6.0–6.3, and mean conductivity 30.8 µS cm^–1. Both NO _inf3 ^sup– and SO _inf4 ^sup–2 were higher in the inlet thanin the outlet. Dominant cations in the inlet and outlet waters were Ca⁺² Mg⁺² > K⁺ + Na⁺; dominant anions were SO _inf4 ^sup–2 HCO _inf3 ^sup– > NO _inf3 ^sup– Cl^–. Nutrient limitation by P was demonstrated once using nutrient diffusing substrata. No limitation could be shown for NO _inf3 ^sup– , HCO _inf3 ^sup– , or Fe+EDTA. Slow colonization rates of periphyton on tiles were attributed to low temperatures and/or ultraviolet radiation. However, interannual differences in biomass on tiles were as much as 300% after 35 days. A minimum of 16–54 samples would be needed to detect a significant interannual change in biomass on tiles after 35 days assuming that the extreme case for periphyton patchiness. Global climate change is likely to affect discharge and water temperature in this wetland which hill have direct and indirect affects on population dynamics and ecosystem function.     

The acquisition of inorganic carbon by four red macroalgae

Photosynthesis was studied in four species of red marine macroalgae: Palmaria palmata, Laurencia pinnatifida, Lomentaria articulata and Delesseria sanguinea. The rate of O₂ evolution for submersed photosynthesis was measured as a function of incident photon flux density at normal pH and inorganic carbon concentration (pH 8.0, 2 mol m^–3), and as a function of inorganic carbon concentration at pH 8.0 at saturating and at limiting photon flux density. The rate of CO₂ uptake was measured for emersed photosynthesis as a function of CO₂ partial pressure at saturating photon flux density. Previous pH-drift results suggest that Palmaria and Laurencia are able to use HCO _inf3 ^sup– as well as CO₂ whereas Lomentaria and Delesseria are restricted to CO₂. None of the algae are saturated by 2 mol m^–3 inorganic carbon at high light (400 mol m^–2 s^–1) but are saturated at low light (35 mol m^–2 s^–1). The inorganic C concentration at which half the light-saturated rate of O₂ evolution is achieved is higher for Palmaria and Laurencia (1.51 and 1.85 mol m^–3) than for Lomentaria and Delesseria (0.772 and 0.841 mol m^–3). The lower values for the latter two species could reflect their putative restriction to CO₂. If expressed in terms of CO₂, the half-saturation values yield 7.2 and 7.8 mmol m^–3 respectively, which are very similar to values obtained previously during pH-drift experiments but at lower concentrations of HCO _inf3 ^sup– , consistent with restriction to CO₂. The photosynthetic conductance (m s^–1), calculated from the initial slope for photosynthesis at low concentrations of inorganic carbon, correlates with the suggested ability to extract inorganic carbon based on pH-drift results. Calculations made assuming that CO₂ is the only species diffusing across the boundary layer are consistent with boundary layer thicknesses of 20 and 19 m for Lomentaria and Delesseria respectively, which is feasible given the rapid water movement in the experiments. For Laurencia however, an unreasonably small boundary layer thickness of 6 m is necessary to explain the flux, which indicates co-diffusion by HCO _inf3 ^sup– . In the apparent absence of external carbonic anhydrase, direct uptake of HCO _inf3 ^sup– , rather than external conversion to CO₂ is indicated in this species. In air, the CO₂ concentration at which photosynthesis is half-maximal increases in the same order as the ability to raise pH in drift experiments. At 21 kPa the CO₂ compensation partial pressures for Palmaria and Laurencia at 0.56 and 1.3 Pa are low enough to suggest a carbon-concentrating mechanism is operating, while those of Lomentaria at 1.8 Pa and particularly that of Delesseria at 4.5 Pa could be explained without a carbon-concentrating mechanism. The algae tested (all except Delesseria) showed more O₂ evolution than could be accounted for with a photosynthetic quotient of 1.0 and uncatalysed conversion of HCO _inf3 ^sup– to CO₂ outside the cell in high light at pH 8.0 when high algal fresh weight per unit medium was used. These results are concordant with other data suggesting use of HCO _inf3 ^sup– by Palmaria and Laurencia, but discordant with the rest of the available information in indicating use of HCO _inf3 ^sup– by Lomentaria. The reason for this is unclear. The lightsaturated rate of O₂ evolution on an algal area basis and the photon flux density needed to saturate photosynthesis were related partly to the habitat from which the seaweeds were collected, but more strongly to the ability to use HCO _inf3 ^sup– . Values for the two users of HCO _inf3 ^sup– , Palmaria (population used was intertidal; also occurs subtidally) and Laurencia (intertidal/shaded intertidal), were greater than for Lomentaria (shaded intertidal), which was greater than Delesseria (subtidal), both of which are believed to be restricted to CO₂. In accordance with earlier ¹³C data and, for Delesseria, estimates of the achieved growth rates in situ, carbon is likely to be saturating and use of HCO _inf3 ^sup– is unlikely to occur in the normal low-light habitats of Lomentaria and Delesseria. Analysis of N-use efficiencies show that they are closer to the low-CO₂-affinity Laminariales than the high-CO₂-affinity Fucaceae.     

Nitrogen cycling in lake sediments bioturbated by Chironomus plumosus larvae, under different degrees of oxygenation

Sediment cores containing different densities of Chironomus plumosus, ranging from 0 to 12 000 ind. m^–2, were incubated in the laboratory, with 100 and 39% O₂ saturation in the overlying water. Rates of O₂ uptake, and fluxes of the various inorganic N species were measured after addition of ¹⁵NO _inf3 ^su– to the overlying water. The animals enhanced O₂ and NO _inf3 ^su– uptake, due to irrigation. Denitrification of NO _inf3 ^su– coming from the overlying water (Dw) and dissimilatory NO _inf3 ^su– reduction to NH _inf4 ^sup+ (DNRA) represented 20–30 and 4–10% of the NO _inf3 ^su– uptake, respectively. Only 20–40% of the measured NH _inf4 ^sup+ effluxes corresponded to DNRA, the rest was probably due to animal excretion. Nitrite production, mostly from dissimilatory NO _inf3 ^sup– reduction, was detected at both 39 and 100% oxygen saturation. Higher rates of NO _inf2 ^su– production at the lower oxygen concentrations, were probably due to a thinner oxic layer, compared to fully oxygenated waters. The presence of Chironomus plumosus increased nitrification rates, relative to non-inhabited microcosms. However, nitrification rates were low compared to Dw, probably due to low numbers of nitrifiers in the sediment. At 39% oxygen saturation, rates of nitrification and denitrification of NO _inf3 ^su– generated within the sediment were not measurable.     

Ulva rigida (Ulvales,Chlorophyta) tank culture as biofilters for dissolved inorganic nitrogen from fishpond effluents

Ulva rigida was cultivated in 7501 tanks at different densities with direct and continuous inflow (at 2, 4, 8 and 12 volumes d^–1) of the effluents from a commercial marine fishpond (40 metric tonnes, Tm, of Sparus aurata, water exchange rate of 16 m³ Tm^–1) in order to assess the maximum and optimum dissolved inorganic nitrogen (DIN) uptake rate and the annual stability of the Ulva tank biofiltering system. Maximum yields (40 g DW m^–2 d^–1) were obtained at a density of 2.5 g FW 1^–1 and at a DIN inflow rate of 1.7 g DIN m^–2 d^–1. Maximum DIN uptake rates were obtained during summer (2.2 g DIN M^–2 d^–1), and minimum in winter (1.1 g DIN m^–2 d^–1) with a yearly average DIN uptake rate of 1.77 g DIN m^–2 d^–1 At yearly average DIN removal efficiency (2.0 g DIN m^–2 d^–1, if winter period is excluded), 153 m² of Ulva tank surface would be needed to recover 100% of the DIN produced by 1 Tm of fish.Abbreviations DIN= dissolved inorganic nitrogen (NH _inf4 ^sup+ + NO _inf3 ^sup– + NO _inf2 ^sup– ); - FW= fresh weight; - DW= dry weight; - PFD= photon flux density; - V= DIN uptake rate     

Electrogenic Cl− absorption byAmphiuma small intestine: Dependence on serosal Na+ from tracer and Cl− microelectrode studies

Summary The Na⁺ requirement for active, electrogenic Cl^– absorption byAmphiuma small intestine was studied by tracer techniques and double-barreled Cl^–-sensitive microelectrodes. Addition of Cl^– to a Cl^–-free medium bathingin vitro intestinal segments produced a saturable (K _m =5.4mm) increase in shortcircuit current (I _sc) which was inhibitable by 1mm SITS. The selectivity sequence for the anion-evoked current was Cl^–=Br^–>SCN^–>NO ₃ ^– >F^–=I^–. Current evoked by Cl^– reached a maximum with increasing medium Na concentration (K _m =12.4mm). Addition of Na⁺, as Na gluconate (10mm), to mucosal and serosal Na⁺-free media stimulated the Cl^– current and simultaneously increased the absorptive Cl^– flux (J _ms ^Cl ) and net flux (J _net ^Cl ) without changing the secretory Cl^– flux (J _sm ^Cl ). Addition of Na⁺ only to the serosal fluid stimulatedJ _ms ^Cl much more than Na⁺ addition only to the mucosal fluid in paired tissues. Serosal DIDS (1mm) blocked the stimulation. Serosal 10mm Tris gluconate or choline gluconate failed to stimulateJ _ms ^Cl . Intracellular Cl^– activity (a _Cl ⁱ ) in villus epithelial cells was above electrochemical equilibrium indicating active Cl^– uptake. Ouabain (1mm) eliminated Cl^– accumulation and reduced the mucosal membrane potential _m over 2 to 3 hr. In contrast, SITS had no effect on Cl^– accumulation and hyperpolarized the mucosal membrane. Replacement of serosal Na⁺ with choline eliminated Cl^– accumulation while replacement of mucosal Na⁺ had no effect. In conclusion by two independent methods active electrogenic Cl^– absorption depends on serosal rather than mucosal Na⁺. It is concluded that Cl^– enters the cell via a primary (rheogenic) transport mechanism. At the serosal membrane the Na⁺ gradient most likely energizes H⁺ export and regulates mucosal Cl^– accumulation perhaps by influencing cell pH or HCO ₃ ^– concentration.     

Sels minéraux et cycles de marées dans un estuaire de Bretagne nord (Dourduff,France)

Short-term variations in nutrient concentrations of water-masses have been studied in a Brittany estuary over several tidal cycles, during winter and summer. NH _inf4 ^sup+ , NO _inf2 ^su– , NO _inf3 ^sup– , SiO₂ and PO _inf4 ^su3– have been measured at a fixed station. The Dourduff estuary is characterized by a very low river discharge (80 l · s^–1 during the minimum water runoff and 1 000 l · s^–1 during the maximum) and an important tidal range (9 m at spring tides). SiO₂ and NO _inf3 ^sup+ concentrations are directly related to freshwater flow whereas PO _inf4 ^su3– is partially adsorbed by seston in the turbid ebb waters. NH _inf4 ^sup+ concentration seems to be, in part, dependent upon sediment resuspension: late ebb and onset of flood periods liberate NH _inf4 ^sup+ into the overlying water column. Nutrient concentrations are also related to seasons. Nutrient fluxes are insignificant or negative during summer periods, so the estuary imports nutrients for its own regulation whereas during winter periods it exports NO _inf3 ^sup– and SiO₂ (ca 50 kg NO _inf3 ^sup– and ca 200 g SiO₂ during a single spring tide). The NO₃: PO₄ ratio is always above 15:1 and can reach 300:1; moreover this ratio fluctuates during the tidal cycle. This imbalance originates in terrestrial discharges of nitrogen compounds.

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Sels minéraux et cycles de marées dans un estuaire de Bretagne nord (Dourduff, France)

     

Effect of nutrient deficiency on accumulation and relative molecular weight of poly-β-hydroxybutyric acid by methylotrophic bacterium,Pseudomonas 135

Summary Pseudomonas 135, a facultative methylotroph, was cultivated on methanol as a sole carbon and energy source for the accumulation of poly--hydroxybutyric acid (PHB). The cells grew fairly well on minimal synthetic medium containing 0.5% (v/v) of methanol at pH 7.0 and 30° C. The maximum specific growth rate was determined to be 0.26–0.28 h^–1 with a growth yield of 0.38 in the optimized growth medium. For stimulation of PHB accumulation in the cells, deficiency of nutrients such as NH _inf4 ^sup+ , Mg²⁺ and PO _inf4 ^sup3– was crucial even though cell growth was significantly suppressed. The PHB content of a 40-h culture was determined to be 37% of the total cell mass in NH _inf4 ^sup+ -limited medium, 42.5% on Mg²⁺-deficient medium, and 34.5% on PO _inf4 ^sup3– -deficient medium. The maximum content of PHB in the cells could reach 55% in NH _inf4 ^sup+ -limited fed-batch culture. The average relative molecular eight determined by gel permeation chromatography was 3.7 × 10⁵ in NH _inf4 ^sup+ -limited culture, 2.5 × 10⁵ in Mg²⁺-deficientmedium, and 3.1 × 10⁵ in PO _inf4 ^sup3– -deficient medium. Polydispersity determined in each culture was relatively high (about 10–11). The solid PHB had a melting temperature of 173° C. Correspondence to: J. M. Lebeault     

A method for removal of toxic chromium using dialysis-sac cultures of a chromate-reducing strain of Enterobacter cloacae

Summary A method for removal of toxic hexavalent chromium (chlomate: CrO _inf4 ^sup2– ) was developed by use of dialysis-sac cultures of a chromate-reducing strain of Enterobacter cloacae (HO1). E. cloacae strain HO1 cells were put in dialysis (semipermeable membrane) sacs, and the sacs were submerged in water containing toxic CrO _inf4 ^sup2– . The dialysis sacs allowed CrO _inf4 ^sup2– to diffuse into the culture, and CrO _inf4 ^sup2– was reduced anaerobically in the dialysis sacs by the E. cloacae cells. Because reduced chromium readily formed insoluble chromium hydroxides in the dialysis sacs, the greater part of reduced chromium was unable to diffuse out through the semipermeable membrane. Thus the dialysis culture of E. cloacae strain HO1 could successfully remove toxic chromium from the surrounding water. If the initial concentration of CrO _inf4 ^sup2– was less than 4mM (208 ppm as chromium), about 90% of the total chromium could be removed from water by the described method. Offprint requests to: H. Ohtake     

Ontogeny of the Na+−H+ exchanger in rat ileal brush-border membrane vesicles

Summary The developmental maturation of Na⁺–H⁺ antiporter was determined using a well-validated brush-border membrane vesicles (BBMV's) technique. Na⁺ uptake represented transport into an osmotically sensitive intravesicular space as evidenced by an osmolality study at equilibrium. An outwardly directed pH gradient (pH inside/pH outside=5.2/7.5) significantly stimulated Na⁺ uptake compared with no pH gradient conditions at all age groups; however, the magnitude of stimulation was significantly different between the age groups. Moreover, the imposition of greater pH gradient across the vesicles resulted in marked stimulation of Na⁺ uptake which increased with advancing age. Na⁺ uptake represented an electroneutral process.The amiloride sensitivity of the pH-stimulated Na⁺ uptake was investigated using [amiloride] 10^–2–10^–5 m. At 10^–3 m amiloride concentration, Na⁺ uptake under pH gradient conditions was inhibited 80, 45, and 20% in BBMV's of adolescent, weanling and suckling rats, respectively. Kinetic studies revealed aK _m for amiloride-sensitive Na⁺ uptake of 21.8±6.4, 24.9±10.9 and 11.8±4.17mm andV _max of 8.76±1.21, 5.38±1.16 and 1.99±0.28 nmol/mg protein/5 sec in adolescent, weanling and suckling rats, respectively. The rate of pH dissipation, as determined by the fluorescence quenching of acridine orange, was similar across membrane preparation of all age groups studied. These findings suggest for the first time the presence of an ileal brush-border membrane Na⁺–H⁺ antiporter system in all ages studied. This system exhibits changes in regard to amiloride sensitivity and kinetic parameters.     

Nitrogen and phosphorus uptake by the Brazilian kelp Laminaria abyssalis (Phaeophyta) in culture

The uptake of ammonium, nitrate and phosphate by laboratory-grown young sporophytes of Laminaria abyssalis was measured in a perturbed system (batch mode) at 18 °C and 35 ± 5 µE m^–2 s^–1 photon flux density. Uptake of all appeared to follow saturation-type nutrient uptake kinetics. The NO _inf3 ^sup– (K _s = 14.0 µM, V _max = 5.0 µmol h^–1 g^–1 dry wt) and NH _inf4 ^sup+ (K _s = 4.6 µM, V _max= 2.0 µmol h^–1 g^–1 dry wt) were taken up simultaneously, although NH _inf4 ^sup+ was taken up more rapidly. Values of K ₃ and V _max for phosphate were, respectively, 2.21 µM and 0.83 µmol h^–1 g^–1 dry wt. Nitrate and phosphate were both consumed in similar rates (V _max /Ks 0.37) at low concentrations. NH _inf4 ^sup+ , thus, might be a more efficient form of N fertilizer if artificial enrichment of seawater is used.     

Sodium transport through the amiloride-sensitive Na-Mg pathway of hamster red cells

Previous work showed that in hamster red cells the amiloride-sensitive (AS) Na⁺ influx of 0.8 mmol/liter cells/hr is not mediated by Na-H exchange as in other red cells, but depends upon intracellular Mg²⁺ and can be increased by 40-fold by loading cells with Mg²⁺ to 10 mm. The purpose of this study was to verify the connection of AS Na⁺ influx with Na-dependent, amiloride-sensitive Mg²⁺ efflux and to utilize AS Na⁺ influx to explore that pathway.Determination of unidirectional influx of Na⁺ and net loss of Mg²⁺ in parallel sets of cells showed that activation by extracellular [Na⁺] follows a simple Michaelis-Menten relationship for both processes with a K _m of 105–107 mm and that activation of both processes is sigmoidally dependent upon cytoplasmic [Mg²⁺] with a [Mg²⁺]_0.5 of 2.1–2.3 mm and a Hill coefficient of 1.8. Comparison of V_max for both sets of experiments indicated a stoichiometry of 2 Na: l Mg. Amiloride inhibits Na⁺ influx and Mg²⁺ extrusion in parallel (K _i = 0.3 mm). Like Mg²⁺ extrusion, amiloride-sensitive Na⁺ influx shows an absolute requirement for cytoplasmic ATP and is increased by cell swelling. Hence, amiloride-sensitive Na⁺ influx in hamster red cells appears to be through the Na-Mg exchange pathway.There was no amiloride-sensitive Na⁺ efflux in hamster red cells loaded with Na⁺ and incubated with high [Mg²⁺] in the medium with or without external Na⁺, nor with ATP depletion. Hence, this is not a simple Na-Mg exchange carrier.     

Zooplankton induced decrease in inorganic phosphorus uptake by plankton in an oligotrophic lake

Experiments conducted on samples collected from a large oligotrophic lake revealed the following: (1) excretion rates of PO _inf4 ^sup3– by single Daphnia thorata were below detection (5 pmol animal^–1 min^–1) in 20 ml of oligotrophic lake water over a period of 10 min, (2) experimental addition of D. thorata to 20 ml aliquots of lake water decreased community-wide microbial uptake of PO _inf4 ^sup3– on two occasions (as measured by ³²PO _inf4 ^sup3– incorporation), and (3) the presence of D. thorata increased uptake by organisms smaller than 1µm, and decreased uptake by large phytoplankton. The specific mechanism for these responses remains unclear, but the results imply that when phytoplankton larger than 1µm encounter cm scale patches of water recently occupied by Daphnia they may experience decreased PO _inf4 ^sup3– availability rather than elevated concentrations of PO _inf4 ^sup3– caused by excretion. We show that ³²P uptake experiments using natural plankton assemblages can be influenced by the presence or absence of large zooplankton, and that neither grazing, turbulence, nor PO _inf4 ^sup3– excretion can account for this influence.     

The ability of several high arctic plant species to utilize nitrate nitrogen under field conditions

The ability to utilize NO _inf3 ^sup– in seven high arctic plant species from Truelove Lowland, Devon Island, Canada was investigated, using an in vivo assay of maximum potential nitrate reductase (NR) activity and applications of ¹⁵N. Plant species were selected on the basis of being characteristic of nutrient-poor and nutrient-rich habitats. In all species leaves were the dominant site of NR activity. Root NR activity was negligible in all species except Saxifraga cernua. NO _inf3 ^sup– availability per se did not appear to limit NR activity of the species typically found on nutrient-poor sites (Dryas integrifolia, Saxifraga oppositifolia, and Salix arctica), or in Cerastium alpinum, as leaf NR activities remained low, even after NO _inf3 ^sup– addition. ¹⁵NO _inf3 ^sup– uptake was limited in D. integrifolia and Salix arctica. However, the lack of field induction of NR activity in C. alpinum and Saxifraga oppositifolia was not due to restricted nitrate uptake, as ¹⁵NO _inf3 ^sup– labelled NO _inf3 ^sup– entered the roots and shoots of both species. Leaf NR activity rates were low in three of the species typical of nutrient-rich habitats (O. digyna, P. radicatum and Saxifraga cernua), sampled from a site containing low soil NO _inf3 ^sup– . Additions of NO _inf3 ^sup– significantly increased leaf NR activity in these latter species, suggesting that potential NR activity was limited by the availability of NO _inf3 ^sup– . ¹⁵N labelled NO _inf3 ^sup– was taken up by O. digyna. P. radicatum and Saxifraga cernua. Although two species (D. integrifolia and Salix arctica) showed little utilization of NO _inf3 ^sup– , we concluded that five of the seven selected high arctic plant species (C. alpinum, O. digyna, P. radicatum, Saxifraga cernua and Saxifraga oppositifolia) do have the potential to utilize NO _inf3 ^sup– as a nitrogen source under field conditions, with the highest potential to utilize NO _inf3 ^sup– occurring in three of the species typically found on fertile habitats.     

Kinetic studies on the stimulation of Na+−H+ exchange activity in renal brush border membranes isolated from thyroid hormone-treated rats

Summary Na⁺–H⁺ exchange activity in renal brush border membrane vesicles isolated from hyperthyroid rats was increased. When examined as a function of [Na⁺], treatment altered the initial rate of Na⁺ uptake by increasingV _m (hyperthyroid, 18.9±1.1 nmol Na⁺ · mg^–1 · 2 sec^–1; normal, 8.9±0.3 nmol Na⁺ · mg^–1 · 2 sec^–1), and not the apparent affinityK _Na ⁺ (hyperthyroid, 7.3±1.7mm; normal, 6.5±0.9mm). When examined as a function of [H⁺] and at a subsaturating [Na⁺] (1mm), hyperthyroidism resulted in the proportional increase in Na⁺ uptake at every intravesicular pH measured. A positive cooperative effect on Na⁺ uptake was found with increased intravesicular acidity in vesicles from both normal and hyperthyroid rats. When the data were analyzed by the Hill equation, it was found that hyperthyroidism did not change then (hyperthyroid, 1.2±0.06; normal, 1.2±0.07) or the [H⁺]_0.5 (hyperthyroid, 0.39±0.08 m; normal, 0.44±0.07 m) but increased the apparentV _m (hyperthyroid, 1.68±0.14 nmol Na⁺ · mg^–1 · 2 sec^–1; normal 0.96±0.10 nmol Na⁺ · mg^–1 · 2 sec^–1). The uptake of Na⁺ in exchange for H⁺ in membrane vesicles from normal and hyperthyroid animals was not influenced by membrane potential. H⁺ translocation or debinding was rate limiting for Na⁺–H⁺ exchange since Na⁺–Na⁺ exchange activity was greater than Na⁺–H⁺ exchange activity. Hyperthyroidism caused a proportional increase and hypothyroidism caused a proportional decrease in Na⁺–Na⁺ and Na⁺–H⁺ exchange. We conclude that hyperthyroidism leads to either an increase in the number of functional exchangers in the membrane or exactly proportional increases in the rate-limiting steps for Na⁺–Na⁺ and Na⁺–H⁺ exchange activity.     

Diurnal variation in physical-chemical properties and primary production in the interconnected marine,mangrove and freshwater biotopes of Kakinada coast,Andhra Pradesh,India

Diurnal variation in hydrological variables and dissolved inorganic nutrients such as PO _inf4 ^sup3– -P, N O _inf2 ^sup– -N, NO _inf3 ^sup– -N and NH _inf4 ^sup+ -N were studied in three interconnected biotopes including freshwater, marine and mangrove brackish water of the Kakinada coastal zone, Andhra Pradesh. Samples were collected at intervals of 3 hours, for a period of 24 hours. In the marine environment salinity varied from 26 to 32 whereas in the mangrove waters it fluctuated from 12 to 20 and in both biotopes salinity showed bimodal type of oscillation. Dissolved oxygen content was high in the mangrove waters during day time but decreased rapidly during the night hours. In the marine environment PO_f4 ^p3–-P concentration varied from 0.345 to 1.195 g at l^–1, NO _inf3 ^sup– -N from 1.03 to 6.62 g at l^–1 and NO _inf2 ^sup– -N from 0.086 to 0.506 g at l^–1. The highest and the lowest concentrations of PO _inf4 ^sup3– -P, NO _inf3 ^sup– -N, NO _inf2 ^sup– -N recorded in the mangrove waters were 0.790 and 0.325 g at l^–1, 7.10 and 1.60 g at l^–1 and 0.278 and 0.060 g at l^–1, respectively. The concentration of PO _inf4 ^sup3– -P, NO _inf3 ^sup– -N and NO _inf2 ^sup– -N were high in the freshwater canal, the maximum and minimum values being 1.110 and 0.730 g at l^–1, 26.40 and 9.98 g at l^–1 and 0.520 and 0.252 g at l^–1 respectively. The concentration of ammonia was relatively high in the mangrove water. Gross and net primary production in the mangrove water was 4 times higher than in the marine biotope. There was no export of dissolved nutrients from the mangrove environment to the adjacent marine waters.     

Dissociation of cellular K+ accumulation from net Na+ transport by toad urinary bladder

Summary A number of published data suggest a variable stoichiometry between the rates of cellular potassium uptake and net sodium transport (J _Na) across the urinary bladder of the toad. This problem was examined by simultaneously studying the intracellular chemical activity of potassium (a _K) with open-tip K⁺-selective microelectrodes and micropipets, and monitoringJ _Na by measuring the short-circuit current (SCC). When bathed in the short-circuited state with solutions containing ana _K of 2.7mm, the mean ±sem values for intracellulara _K were 43±0.6mm.Ouabain, at a concentration of 10^–2 m, reduced intracellulara _K by 56–67% and SCC by 96–100%. At 5×10^–4 m, ouabain reversibly reduced intracellulara _K by 40–55%, and SCC by 63–68%; the inhibition of SCC was only partly reversible during the period of observation.Removal of external potassium reduced intracellulara _K by 69–80% and SCC by 51–76%. Restoration of external potassium entirely returned intracellulara _K to its control value, but only partially reversed the inhibition of SCC during the period of study. Furthermore, recovery ofa _K began 19–43 min before that of SCC; recovery ofa _K was 90–97% complete before any increase in SCC could be measured. Although other interpretations are possible, the simplest interpretation of the data is that the processes responsible for potassium accumulation and transepithelial sodium transport are not identical. We propose the existence of a separate transfer mechanism at the basolateral cell membrane, responsible for accumulating intracellular potassium, and not directly coupled to active sodium transport.     

Single-file diffusion through the Ca2+-activated K+ channel of human red cells

Summary We have examined the effect of internal and external pH on Na⁺ transport across toad bladder membrane vesicles. Vesicles prepared and assayed with a recently modified procedure (Garty & Asher, 1985) exhibit large, rheogenic, amiloridesensitive fluxes. Of the total²²Na uptake measured 0.5–2.0 min after introducing tracer, 80±4% (mean±se,n=9) is blocked by the diuretic with aK ₁ of 2×10^–8 m. Thus, this amiloridesensitive flux is mediated by the apical sodium-selective channels. Varying the internal (cytosolic) pH over the physiologic range 7.0–8.0 had no effect on sodium transport; this result suggests that variation of intracellular pHin vivo has no direct apical effect on modulating sodium uptake. On the other hand,²²Na was directly and monotonically dependent on external pH. External acidification also reduced the amiloride-sensitive efflux across the walls of the vesicles. This inhibition of²²Na efflux was noted at external Na⁺ concentrations of both 0.2 m and 53mm.These results are different from those reported with whole toad bladder. A number of possible bases for these differences are considered and discussed. We suggest that the natriferic response induced by mucosal acidification of whole toad urinary bladder appears to operate indirectly through one or more factors, presumably cytosolic, present in whole cells and absent from the vesicles.