Validation of the use of the lipophilic thiocyanate anion for the determination of membrane potential in Ehrlich ascites tumor cells

Summary The utility of the lipophilic anion thiocyanate (SCN⁺) as a probe for the indirect estimation of the cell membrane potential (V _m ) in Ehrlich ascites tumor cells has been evaluated by comparison to direct electrophysiological measurements. SCN accumulation is consisten with first-order uptake into a single kinetically-identifiable cellular compartement, achieving steadystate distribution in 20–30 min at 22°C. The steady-state distribution ratio ([SCN^–] _c /[SCN^–] _e ) in physiological saline is 0.44±0.02. Treatment of the cells with proparanolol (0.13 mM), an activator of Ca²⁺ dependent K⁺ channels, reduces the steady-state distribution ratio to 0.19±0.02. Conversely, treatmetn with BACl₂ (10 mM), an antagonist of the pathway, increases the SCN^– distribution ratio to 0.62±0.01. The equilibrium potentials (V _SCN ) calculated under these conditions are virtually identical to direct electrophysiological measurements of theV _m made under the same conditions. The effect of varing extracellular [K⁺]([K⁺] _e ) in the presence of constant [Na⁺] _e =100 mM has also been tested. In control cells, elevation of [K⁺] _e from 6 to 60 mM reducesV _SCN from –20.6±1.0 to –13.2±1.2 mV. Again, microelectrode measurements give excellent quantitative agreement. Propranolol increases the sensitivity of the cells to varying [K⁺] _e , so that a 10-fold elevation reducesV _SCN by approximately 31 mV. BaCl₂ greatly reduces this reponse: a 10-fold elevation in [K⁺] _e yielding only a 4-mV rediction inV _SCN . It is concluded that the membrane potential of Ehrlich cells can be estimated accurately from SCN^– distribution measurements.     

Na+ and K+ fluxes stimulated by Na+-coupled glucose transport: Evidence for a Ba2+-insensitive K+ efflux pathway in rabbit proximal tubules

Summary Addition of glucose or the nonmetabolizable analogue -methyl-d-glucoside to rabbit proximal tubules suspended in a glucoseand alanine-free buffer caused a sustained increase in intracellular Na⁺ content (+43±7 nmol · (mg protein)^–1) and a concomitant but larger decrease in K⁺ content (–72±11 nmol· (mg protein)^–1). A component of the net K⁺ efflux was Ba²⁺ insensitive, and was inhibited by high (1mm) but not low (10 m) concentrations of the diuretics, furosemide and bumetanide. The increase in intracellular Na⁺ content is consistent with the view that the increased rates of Na⁺ and water transport seen in the proximal tubule in the presence of glucose can be attributed (at least in part) to a stimulation of basolateral pump activity by an increased [Na⁺] _i .     

New solution method for equations of reaction and mass transfer in biocatalyst particles

Summary For numerical solution of the reaction-mass transfer equations for immobilised biocatalysts it may be better to start integration at the particle surface and proceed inwards: calculations are targetted on the region to which practically interesting changes are often confined (because concentrations are effectively zero in the interior); and during iterative solution wrong initial estimates may be rejected after detecting anomalies early in the integration.Symbols C_b substrate concentration in bulk (mol m^–3) - c dimensionless substrate concentration (C/C_b) (-) - D_e effective diffusion coefficient (m²s^–1) - Da Damkohler number (V.r_o ²/D_e.K_s) (-) - K_s substrate concentration kinetic coefficient (mol m^–3) - k_e external mass transfer coefficient (ms^–1) - r_o bead radius (m) - Sh Sherwood number (k_e.r_o/D_e) (-) - V maximum rate per unit volume in beads (mol m^–3s^–1) - x dimensionless distance from bead centre (r/r_o) (-) - dimensionless kinetic coefficient (K_s/C_b) (-) - _o effectiveness factor (-)     

Changing suspended sediment and particulate phosphorus loads and pathways in underdrained lowland agricultural catchments; Herefordshire and Worcestershire,U.K.

Data obtained from a small (150 ha) experimental catchment, Hereford U.K., have shown that land drains contributed >50% of the total catchment suspended sediment (SS) yield over a two year period. In one of the monitored drains, annual sediment yields were 964 and 978 kg ha^–1. Particulate phosphorus (PP) contributed >60% of total phosphorus lost through the drains and at least 73% of the total drain load came from topsoil. A major question that was not answered by the monitoring programme was whether SS and PP loads had increased since the drains had been installed between the 1960s and 1980s. To address this problem, a sediment yield record was reconstructed from the Kyre Pool catchment in Worcestershire that has a similar drainage history and soil types. Reservoir sediments were dated using the ²¹⁰Pb crs method and results suggest a fourfold increase in SS yield (300–1170 kg ha^–1 yr^–1) and PP loads (0.19–0.79 kg ha^–1 yr^–1) since the 1960s. The most recent SS and PP loads are comparable to those obtained from catchment monitoring. The high lake sediment ¹³⁷Cs inventory suggests a significant influx of eroded topsoil and ¹³⁷Cs activities in the most recent lake sediments are comparable to those of monitored land drains, supporting the hypothesis that land drainage has had a major impact on SS and PP yields and pathways.     

Recycling ofd-glucose in collagenous cuticle: A means of nutrient conservation?

Summary Transport by an epithelium, possessing an accumulating, saturable transport system in the apical membrane as well as a finite Fick permeability to the transported solute, was considered in the steady state in the case of zerocis concentration, and in the presence of a peripheral diffusion resistance in a layer apposing thecis face of the tissue (unstirred solution or structural coating). Under suitable conditions, the combination of peripheral diffusion resistance and accumulating epithelial transport may lead to recycling of solute at thecis face of the epithelium. This causes a decrease of the effective permeability to diffusionaltrans-cis flow across the tissue. The phenomenon is discussed in terms of epidermald-glucose transport by the integument of aquatic animals with a collagenous cuticle, such as the seawater-acclimated polychaete wormNereis diversicolor. The recycling phenomenon may be of significance to other epithelia with the function of maintaining large concentration gradients of permeating substances.List of Symbols and Fixed Parameter Values C _m Bulk medium solute concentration,cis face of epidermisC _m=0 mol cm^–3 - C _i Concentration of solute at interface between cuticle and unstirred medium (mol cm^–3) - C _s Concentration of solute atcis face of apical epidermal membrane (mol cm^–3) - C _e Concentration of solute in extracellular fluid,trans-side of epidermisC _e=1.0×10^–6 mol cm^–3 - D _m Diffusion coefficient of solute in outside mediumD _m=6.7×10^–6 cm² sec^–1 - D _c Diffusion coefficient of solute in cuticleD _c=7.4×10^–9 cm² sec^–1 - _m Operative thickness of unstirred medium layer - _c Thickness of cuticle - J Steady-state net flux of solute through cuticle or unstirred layer (flux is positive indirectioncis-trans) (mol cm^–2 sec^–1) - J _i ^max Maximal influx through saturable transport system in apical membraneJ _i ^max =2.0×10^–12 mol cm^–2 sec^–1 - K _t Transport constant, saturable systemK _t=1.0×10^–7 mol cm^–3 - P Epithelial permeability (cm sec^–1)     

The effect of water depth on bacterial numbers,thymidine incorporation rates and C:N ratios in northeast Atlantic surficial sediments

The effect of water depth on bacterial biomass and their ability to synthesise DNA, by measuring their rate of [³H]-thymidine incorporation, was investigated in the northeast Atlantic at three sites of varying water depth (1100–3580 m) and sediment characteristics. Thymidine incorporation rates (y) in surficial sediments varied between 0.028 and 1.44 pmol h^–1 g^–1 and showed an exponential relationship with depth (x) according to the equation y= 2.05e^–0.0011x (r=0.9830 for n=7, P<0.001). However, this relationship failed when a layer of phytodetritus was found overlying the surface sediment and [³H]-thymidine incorporation rates increased by 80–339%. In contrast, bacterial numbers varied between 1.09 and 11.96 × 10⁸ cells g^–1 (dry weight) and showed no significant relationships with water depth or sediment POC/TN content. Significant exponential relationships were also found between water depth (x) and the POC (y ₁) and total nitrogen (TN, y ₂) content of surficial sediments according to the following equations: where y ₁ = 719e^–0.0003x (r=0.8700 for n=9, P<0.01) and y ₂ = 76e^–0.0002x(r=0.7582 for n=9 P<0.02). These relationships were irrespective of the presence or absence of an overlying layer of phytodetritus. This suggests that the POC and TN content of these surficial deep sea sediments is directly related to the flux of material through the water column, which significantly impacts bacterial production.     

Thiol-dependent passive K+Cl− transport in sheep red blood cells: VI. Functional heterogeneity and immunologic identity with volume-stimulated K+(Rb+) fluxes

Summary Ouabain-resistant (OR), volume-or N-ethylmaleimide (NEM)-stimulated K⁺(Rb⁺)Cl^– fluxes were measured in low-K⁺ sheep red cells and found to be functionally separate but immunologically similar. In anisosmotic solutions both K⁺ effluxes and Rb⁺ influxes of NEM-treated and control cells were additive. In contrast to the NEM-stimulated K⁺Cl^– flux, metabolic depletion did not reduce K⁺Cl^– flux of normal or swollen cells. The anion preference of OR K⁺ efflux in NEM-treated cells was Br^–>Cl^–>HCO ₃ ^– =F^–I^–=NO ₃ ^– =CNS^–, and hence consistent with a reported Br^–>Cl^–>NO ₃ ^– sequence of the volume-dependent K⁺Cl^– transport. Alloimmune anti-L_l antibodies known to decrease passive K⁺ fluxes in low K⁺ cells reduced by 51% both volume-and NEM-stimulated, furosemidesensitive Rb⁺Cl^– fluxes suggesting their immunologic identity, a conclusion also supported by anti-L₁ absorption studies. Since pretreatment with anti-L₁ prevented the activation of Rb⁺ influx by NEM, and the impermeant glutathionmaleimide-I did not stimulate Rb⁺Cl^– influx, the NEM reactive SH groups must be located apart from the L₁ antigen either within the membrane or on its cytoplasmic face. A model is proposed consisting of a K⁺Cl^– transport path(s) regulated by a protein with two functional subunits or domains; a chemically (C _s) and a volume (V _s)-stimulated domain, both interfacing with the L₁ surface antigen. Attachment of alloanti-L₁ from the outside reduces K⁺Cl^– transport stimulated throughC _s by NEM orV _s by cell swelling.     

Studies on (NA + K)-activated ATPase XLV. Magnesium induces two low-affinity non-phosphorylating nucleotide binding sites per molecule

ATP and adenylylimidodiphosphate (AdoPP[NH]P) bind to (Na⁺ + K⁺)-ATPase in the absence of Mg²⁺ (EDTA present) with a homogeneous but 15-fold different affinity, the K_d values being 0.13 μM and 1.9 μM, respectively. The binding capacities of the two nucleotides are nearly equal and amount to 3.9 and 4 nmol/mg protein or 1.7 and 1.8 mol/mol (Na⁺ + K⁺)-ATPase, respectively. The K_d value for ATP is equal to the K_m for phosphorylation by ATP (0.05–0.25 μM) and the binding capacity is equivalent to the phosphorylation capacity of 1.8 mol/mol (Na⁺ + K⁺)-ATPase. Hence, the enzyme contains two high-affinity nucleotide binding and phosphorylating sites per molecule, or one per α-subunit. Additional low-affinity nucleotide binding sites are elicited in the presence of Mg²⁺, as shown by binding studies with the non-phosphorylating (AdoPP[NH]P). The K_d and binding capacity for AdoPP[NH]P at these sites is dependent on the Mg²⁺ concentration. The K_d increases from 0.06 mM at 0.5 mM Mg²⁺ to a maximum of 0.26 mM at 2 mM Mg²⁺ and the binding capacity from 1.5 nmol/mg protein at 0.5 mM Mg²⁺ to 3.3 nmol/mg protein at 4 mM Mg²⁺. Extrapolation of a double reciprocal plot of binding capacity vs. total Mg²⁺ concentration yields a maximal binding capacity at infinite Mg²⁺ concentration of 3.8 nmol/mg protein or 1.7 mol/mol (Na⁺ + K⁺)-ATPase. The K_d for Mg²⁺ at the sites, where it exerts this effect, is 0.8 mM. The K_d for the high-affinity sites increases from 1.5–1.9 μM in the absence of Mg²⁺ to a maximum of 4.2 μM at 2 mM Mg²⁺ concentration. The binding capacity of these sites (1.8 mol/mol enzyme) is independent of the Mg²⁺ concentration. Hence, Mg²⁺ induces two low-affinity non-phosphorylating nucleotide binding sites per molecule (Na⁺ + K⁺)-ATPase in addition to the two high-affinity, phosphorylating nucleotide binding sites.     

Fed-batch production of baker's yeast using millet (Pennisetum typhoides) flour hydrolysate as the carbon source

A fermentation medium based on millet (Pennisetum typhoides) flour hydrolysate and a four-phase feeding strategy for fed-batch production of baker's yeast,Saccharomyces cerevisiae, are presented. Millet flour was prepared by dry-milling and sieving of whole grain. A 25% (w/v) flour mash was liquefied with a thermostable 1,4--d-glucanohydrolase (EC 3.2.1.1) in the presence of 100 ppm Ca²⁺, at 80°C, pH 6.1–6.3, for 1 h. The liquefied mash was saccharified with 1,4--d-glucan glucohydrolase (EC 3.2.1.3) at 55°C, pH 5.5, for 2 h. An average of 75% of the flour was hydrolysed and about 82% of the hydrolysate was glucose. The feeding profile, which was based on a model with desired specific growth rate range of 0.18–0.23 h^–1, biomass yield coefficient of 0.5 g g^–1 and feed substrate concentration of 200 g L^–1, was implemented manually using the millet flour hydrolysate in test experiments and glucose feed in control experiments. The fermentation off-gas was analyzed on-line by mass spectrometry for the calculation of carbon dioxide production rate, oxygen up-take rate and the respiratory quotient. Off-line determination of biomass, ethanol and glucose were done, respectively, by dry weight, gas chromatography and spectrophotometry. Cell mass concentrations of 49.9–51.9 g L^–1 were achieved in all experiments within 27 h of which the last 15 h were in the fedbatch mode. The average biomass yields for the millet flour and glucose media were 0.48 and 0.49 g g^–1, respectively. No significant differences were observed between the dough-leavening activities of the products of the test and the control media and a commercial preparation of instant active dry yeast. Millet flour hydrolysate was established to be a satisfactory low cost replacement for glucose in the production of baking quality yeast.Nomenclature C _ox Dissolved oxygen concentration (mg L^–1) - CPR Carbon dioxide production rate (mmol h^–1) - C _s0 Glucose concentration in the feed (g L^–1) - C _s Substrate concentration in the fermenter (g L^–1) - C _s.crit Critical substrate concentration (g L^–1) - E Ethanol concentration (g L^–1) - F _s Substrate flow rate (g h^–1) - i Sample number (–) - K _e Constant in Equation 6 (g L^–1) - K _o Constant in Equation 7 (mg L^–1) - K _s Constant in Equation 5 (g L^–1) - m Specific maintenance term (h^–1) - OUR Oxygen up-take rate (mmol h^–1) - q _ox Specific oxygen up-take rate (h^–1) - q _ox.max Maximum specific oxygen up-take rate (h^–1) - q _p Specific product formation rate (h^–1) - q _s Specific substrate up-take rate (g g^–1 h^–1) - q _s.max Maximum specific substrate up-take rate (g g^–1 h^–1) - RQ Respiratory quotient (–) - S Total substrate in the fermenter at timet (g) - S ₀ Substrate mass fraction in the feed (g g^–1) - t Fermentation time (h) - V Instantaneous volume of the broth in the fermenter (L) - V ₀ Starting volume in the fermenter (L) - V _si Volume of samplei (L) - x Biomass concentration in the fermenter (g L^–1) - X ₀ Total amount of initial biomass (g) - X _t Total amount of biomass at timet (g) - Y _p/s Product yield coefficient on substrate (–) - Y _x/e Biomass yield coefficient on ethanol (–) - Y _x/s Biomass yield coefficient on substrate (–) Greek letters Moles of carbon per mole of yeast (–) - Moles of hydrogen atom per mole of yeast (–) - Moles of oxygen atom per mole of yeast (–) - Moles of nitrogen atom per mole of yeast (–) - Specific growth rate (h^–1) - _crit Critical specific growth rate (h^–1) - _E Specific ethanol up-take rate (h^–1) - _max.E Maximum specific ethanol up-take rate (h^–1)     

Inhibition of N2 fixation by white clover (Trifolium repens L.) at low concentrations of NO inf3 sup− in flowing solution culture

The impact of sustained low external concentrations of NO ₃ ^– (0, 10, 100 and 1000 mmol m^–3) on plant growth and the relative acquisition of N through N₂ fixation and NO ₃ ^– uptake by established, nodulated white clover (Trifolium repens L. cv. Blanca) was studied over 28 days in flowing solution culture. Nitrogen fixation was measured by N difference and ¹⁵N dilution methods. Plants supplied with NO ₃ ^– achieved higher relative growth rates (% MathType!MTEF!2!1!+-% feaafiart1ev1aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn% hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr% 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq-Jc9% vqaqpepm0xbba9pwe9Q8fs0-yqaqpepae9pg0FirpepeKkFr0xfr-x% fr-xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGabmiEayaara% aaaa!3702!\[\bar x\]=0.091 d^–1) compared with control plants dependent on N₂ fixation (0.073 d^–1). Nitrate plants showed progressive increases in shoot: root d.w. ratios from 4 to 6.5–7.6 between days 0–28, compared with 5.1 on day 28 for control plants. Increases in both nodule d.w. and numbers per plant were inhibited after day seven at all concentrations of NO ₃ ^– . The severity of inhibition of N₂ fixation increased with increasing NO ₃ ^– concentration and with time. The total amounts of N₂ fixed per plant between days 0–7 after supplying 10, 100 and 1000 mmol m^–3 NO ₃ ^– , respectively, were 37–39, 28–30 and 0–13%, of the total N acquired. Between days 7–28 the proportional contributions of N₂ fixation to total N acquisition declined to 3, 0.5 and 0%, respectively, in these treatments. The corresponding mean specific rates of N₂ fixation between days 0–7 were, respectively, 5.4, 3.2, and 2.0 mmol N d^–1 g^–1 nodule d.w., compared with 7.9 mmol N d^–1 g^–1 nodule d.w. for zero NO ₃ ^– plants. There was no evidence of a transitory increase in N₂ fixation following the addition of NO ₃ ^– , even at the lowest supply concentration.     

Freshwater to seawater acclimation of juvenile bull sharks (<Emphasis Type="Italic">Carcharhinus leucas</Emphasis>): plasma osmolytes and Na<Superscript>+</Superscript>/K<Superscript>+</Superscript>-ATPase activity in gill,rectal gland,kidney and intestine

This study examined the osmoregulatory status of the euryhaline elasmobranch Carcharhinus leucas acclimated to freshwater (FW) and seawater (SW). Juvenile C. leucas captured in FW (3 mOsm l^–1 kg^–1) were acclimated to SW (980–1,000 mOsm l^–1 kg^–1) over 16 days. A FW group was maintained in captivity over a similar time period. In FW, bull sharks were hyper-osmotic regulators, having a plasma osmolarity of 595 mOsm l^–1 kg^–1. In SW, bull sharks had significantly higher plasma osmolarities (940 mOsm l^–1 kg^–1) than FW-acclimated animals and were slightly hypo-osmotic to the environment. Plasma Na⁺, Cl^–, K⁺, Mg²⁺, Ca²⁺, urea and trimethylamine oxide (TMAO) concentrations were all significantly higher in bull sharks acclimated to SW, with urea and TMAO showing the greatest increase. Gill, rectal gland, kidney and intestinal tissue were taken from animals acclimated to FW and SW and analysed for maximal Na⁺/K⁺-ATPase activity. Na⁺/K⁺-ATPase activity in the gills and intestine was less than 1 mmol Pi mg^–1 protein h^–1 and there was no difference in activity between FW- and SW-acclimated animals. In contrast Na⁺/K⁺-ATPase activity in the rectal gland and kidney were significantly higher than gill and intestine and showed significant differences between the FW- and SW-acclimated groups. In FW and SW, rectal gland Na⁺/K⁺-ATPase activity was 5.6±0.8 and 9.2±0.6 mmol Pi mg^–1 protein h^–1, respectively. Na⁺/K⁺-ATPase activity in the kidney of FW and SW acclimated animals was 8.4±1.1 and 3.3±1.1 Pi mg^–1 protein h^–1, respectively. Thus juvenile bull sharks have the osmoregulatory plasticity to acclimate to SW; their preference for the upper reaches of rivers where salinity is low is therefore likely to be for predator avoidance and/or increased food abundance rather than because of a physiological constraint.     

Action potentials inAcetabularia: Measurement and simulation of voltage-gated fluxes

Summary Amounts and temporal changes of the release of the tracer ions K⁺ (⁸⁶Rb⁺),²²Na⁺, and³⁶Cl^– as well as of H⁺ in the course of action potentials inAcetabularia have been recorded. New results and model calculations confirm in quantitative terms the involvement of three major ion transport systemsX in the plasmalemma: Cl^– pumps, K⁺ channels, and Cl^– channels (which are marked in the following by the prefixes,P, K andC) with their equilibrium voltages _X V _e and voltage/time-dependent conductances, which can be described by the following, first approximation. Let the maximum (ohmic) conductance of each of the three populations of transporter species be about the same (_P L, _KL,_C L=1) but voltage gating be different: the pump ( _{p V e} about –200 mV) being inactivated (open,oclosed,c) at positive going transmembrane voltages,V _m; the K⁺ channels (_K V _e about –100 mV) are inactivated at negative goingV _m; and the Cl^– channels (_C V _e: around 0 mV), which are normally closed (c) at a restingV _m (near_PV_e) go through an intermediate open (o) state at more positiveV _m before they enter a third shut state (s) in series. Model calculations, in which voltage sensitivities are expressed by the factorf=exp(V _mF/(2RT)), simulate, the action potential fairly well with the following parameters (_PK_co10/f ks^–1,_PK_oc1000·f ks^–1,_KK_co200·f ks^–1,_Kk_oc2/f ks^–1,_cK_co500·f ks^–1,_CK_oc5/f ks^–1,_CK_so0.1/f ks^–1,_Ck_os20·f ks^–1). It is also shown that the charge balance for the huge transient Cl^– efflux, which frequently occurs during an action potential, can be accounted for by the observation of a corresponding release of Na⁺.     

Rhizosphere priming effects on the decomposition of soil organic matter in C4 and C3 grassland soils

Using a natural abundance ¹³C method, soil organic matter (SOM) decomposition was studied in a C₃ plant – `C<sub>4</sub> soil' (C<sub>3</sub> plant grown in a soil obtained from a grassland dominated by C<sub>4</sub> grasses) system and a C<sub>4</sub> plant – `C₃ soil' (C₄ plant grown in a soil taken from a pasture dominated by C₃ grasses) system. In C₃ plant – `C<sub>4</sub> soil' system, cumulative soil-derived CO<sub>2</sub>–C were higher in the soils planted with soybean (5499 mg pot<sup>–1</sup>) and sunflower (4484 mg pot<sup>–1</sup>) than that in `C₄ soil' control (3237 mg pot^–1) without plants. In other words, the decomposition of SOM in soils planted with soybean and sunflower were 69.9% and 38.5% faster than `C<sub>4</sub> soil' control. In C<sub>4</sub> plant – `C₃ soil' system, there was an overall negative priming effect of live roots on the decomposition of SOM. The cumulative soil-derived CO₂–C were lower in the soils planted with sorghum (2308 mg pot^–1) and amaranthus (2413 mg pot^–1) than that in `C<sub>3</sub> soil' control (2541 mg pot<sup>–1</sup>). The decomposition of SOM in soils planted with sorghum and amaranthus were 9.2% and 5.1% slower than `C₃ soil' control. Our results also showed that rhizosphere priming effects on SOM decomposition were positive at all developmental stages in C₃ plant – `C<sub>4</sub> soil' system, but the direction of the rhizosphere priming effect changed at different developmental stages in the C<sub>4</sub> plant – `C₃ soil' system. Implications of rhizosphere priming effects on SOM decomposition were discussed.     

Regulation of respiration and energy transduction in cytochrome c oxidase isozymes by allosteric effectors

The binding of TNP-ATP (2 or 3-O-(2,4,6-trinitrophenyl)-ATP) to cytochrome c oxidase (COX) from bovine heart and liver and to the two-subunit COX of Paracoccus denitrificans was measured by its change of fluorescence. Three binding sites, two with high (dissociation constant K_d = 0.2 µM) and one with lower affinity (K_d = 0.9 µM), were found at COX from bovine heart and liver, while the Paracoccus enzyme showed only one binding site (K_d = 3.6 µM). The binding of [³⁵S]ATPaS was measured by equilibrium dialysis and revealed seven binding sites at the heart enzyme (K_d = 7.5 µM) and six at the liver enzyme (K_d = 12 µM). The Paracoccus enzyme had only one binding site (K_d = 16 µM). The effect of variable intraliposomal ATP/ADP ratios, but at constant total concentration of [ATP + ADP] = 5 mM, on the H⁺/e^- stoichiometry of reconstituted COX from bovine heart and liver were studied. Above 98% ATP the H⁺/e^- stoichiometry of the heart enzyme decreased to about half of the value measured at 100% ATP. In contrast, the H⁺/e^- stoichiometry of the liver enzyme was not influenced by the ATP/ADP ratio. It is suggested that high intramitochondrial ATP/ADP ratios, corresponding to low cellular work load, will decrease the efficiency of energy transduction and result in elevated thermogenesis for the maintenance of body temperature. (Mol Cell Biochem 174: 131–135, 1997)     

Rabit distal colon epithelium: II. Characterization of (Na+, K+, Cl−)-cotransport and [3H]-bumetanide binding

Summary Loop diuretic-sensitive (Na⁺,K⁺,Cl^–)-cotransport activity was found to be present in basolateral membrane vesicles of surface and crypt cells of rabbit distal colon epithelium. The presence of grandients of all three ions was essential for optimal transport activity (Na⁺,K⁺) gradien-driven³⁶Cl fluxes weree half-maximally inhibited by 0.14 m bumetanide and 44 m furosimide. While⁸⁶Rb uptake rates showed hyperbolic dependencies on Na⁺ and K⁺ concentrations with Hill coefficients of 0.8 and 0.9, respectively, uptakes were sigmoidally related to the Cl^– concentration, Hill coefficient 1.8, indicating a 1 Na⁺: 1 K⁺:2 Cl^– stoichiometry of ion transport.The interaction of putative (Na⁺, K⁺, Cl^–)-cotransport proteins with loop diuretics was studied from equilibrium-binding experiments using [³H]-bumetanide. The requirement for the simulataneous presence of Na⁺,K⁺, and Cl^–, saturability, reversibility, and specificity for diuretics suggest specific binding to the (Na⁺, K⁺, Cl^–)-cotransporter. [³H]-bumetanide recognizes a minimum of two classes of diuretic receptors sites. high-affinity (K _D1=0.13 m;B _max1 =6.4 pmol/mg of protein) and low-affinity (K _D2=34 m;B _max2=153 pmol/mg of protein) sites. The specific binding to the high-affinity receptor was found to be linearly competitive with Cl^– (K ₁=60mm), whereas low-affinity sites seem to be unaffected by Cl^–. We have shown that only high-affinity [³H]-bumetanide binding correlates with transport inhibition raising questions on the physiological significance of diuretic receptor site heterogeneity observed in rabbit distal colon epithelium.     

Nitrogen fixation in subarctic streams influenced by beaver (Castor canadensis)

Nitrogen fixation was measured in four subarctic streams substantially modified by beaver (Castor canadensis) in Quebec. Acetylene-ethylene (C₂H₂ C₂H₄) reduction techniques were used during the 1982 ice-free period (May–October) to estimate nitrogen fixation by microorganisms colonizing wood and sediment. Mean seasonal fixation rates were low and patchy, ranging from zero to 2.3 × 10^–3 µmol C₂H₄ · cm^–2 · h^–1 for wood, and from zero to 7.0 × 10^–3 µmol C₂H₄ · g AFDM^–1 · h^–1 for sediment; 77% of all wood and 63% of all sediment measurements showed no C₂H₂ reduction. Nonparametric statistical tests were unable to show a significant difference (p > 0.05) in C₂H₂ reduction rates between or within sites for wood species or by sediment depth.Nitrogen contributed by microorganisms colonizing wood in riffles of beaver influenced watersheds was small (e.g., 0.207 g N · m^–2 · y^–1) but greater than that for wood in beaver ponds (e.g., 0.008 g N · m^–2 · y^–1) or for streams without beaver (e.g., 0.003 g N · m^–2 · y^–1). Although mass specific nitrogen fixation rates did not change significantly as beaver transform riffles into ponds, the nitrogen fixed by organisms colonizing sediment in pond areas (e.g., 5.1 g N · m^–2 · y^–1) was greater than that in riffles (e.g., 0.42 g N · m^–2 · y^–1). The annual nitrogen contribution is proportional to the amount of sediment available for microbial colonization. We estimate that total nitrogen accumulation in sediment, per unit area, is enhanced 9 to 44 fold by beaver damming a section of stream.     

Nitrification, denitrification, and nitrate ammonification in sediments of two coastal lagoons in Southern France

Summary Seasonal and diurnal variations in sediment-water fluxes of O₂, NO ₃ ^– , and NH ₄ ⁺ as well as rates of nitrification, denitrification, and nitrate ammonification were determined in two different coastal lagoons of southern France: The seagrass (Zostera noltii) dominated tidal Bassin d'Arcachon and the dystrophic Etang du Prévost. Overall, denitrification rates in both Bassin d'Arcachon (<0.4 mmol m^–2 d^–1) and Etang du Prévost (<1 mmol m^–2 d^–1) were low. This was mainly caused by a combination of low NO ₃ ^– concentrations in the water column and a low nitrification activity within the sediment. In both Bassin d'Arcachon and Etang du Prévost, rates of nitrate ammonification were quantitatively as important as denitrification.Denitrification played a minor role as a nitrogen sink in both systems. In the tidal influenced Bassin d'Arcachon, Z. noltii was quantitatively more important than denitrification as a nitrogen sink due to the high assimilation rates of the plants. Throughout the year, Z. noltii stabilized the mudflats of the bay by its well- developed root matrix and controlled the nitrogen cycle due to its high uptake rates. In contrast, the lack of rooted macrophytes, and dominance of floating macroalgae, made nitrogen cycling in Etang du Prévost more unstable and unpredictable. Inhibition of nitrification and denitrification during the dystrophic crisis in the summer time increased the inorganic nitrogen flux from the sediment to the water column and thus increased the degree of benthic-pelagic coupling within this bay. During winter, however, benthic microalgae colonizing the sediment surface changed the sediment in the lagoon from being a nitrogen source to the over lying water to being a sink due to their high assimilation rates. It is likely, however, that this assimilated nitrogen is liberated to the water column at the onset of summer thereby fueling the extensive growth of the floating macroalgae, Ulva sp. The combination of a high nitrogen coupling between sediment and water column, little water exchange and low denitrification rates resulted in an unstable system with fast growing algal species such as phytoplankton and floating algae.     

Losses of inorganic carbon and nitrous oxide from a temperate freshwater wetland in relation to nitrate loading

We studied the export of inorganic carbon and nitrous oxide (N₂O) from a Danish freshwater wetland. The wetland is situated in an agricultural catchment area and is recharged by groundwater enriched with nitrate (NO₃ ^–) (1000 M). NO₃ ^– in recharging groundwater was reduced (57.5 mol NO₃ ^– m^–2 yr^–) within a narrow zone of the wetland. Congruently, the annual efflux of carbon dioxide (CO₂) from the sediment was 19.1 mol C m^–2 when estimated from monthly in situ measurements. In comparison the CO₂ efflux was 4.8 mol C m^–2 yr^–1 further out in the wetland, where no NO₃ ^– reduction occurred. Annual exports of inorganic carbon in groundwater and surface water was 78.4 mol C m^–2 and 6.1 mol C m^–2 at the two sites, respectively. N₂O efflux from the sedimenst was detectable on five out of twelve sampling dates and was significantly (P < 0.0001) higher in the NO₃ ^– reduction zone (0.35–9.40 mol m^–2 h^–1, range of monthly means) than in the zone without NO₃ ^– reduction (0.21–0.41 mol m^–2 h^–1). No loss of dissolved N₂O could be measured. Total annual export of N₂O was not estimated. The reduction of oxygen (O₂) in groundwater was minor throughout the wetland and did not exceed 0.2 mol 0₂ m^–2yr^–1. Sulfate (SO₄ ^––) was reduced in groundwater (2.1 mol SO₄ ^–– m^–2 yr^–1) in the zone without NO₃ ^– reduction. Although the NO₃ ^– in our wetland can be reduced along several pathways our results strongly suggest that NO₃ ^– loading of freshwater wetlands disturb the carbon balance of such areas, resulting in an accelerated loss of inorganic carbon in gaseous and dissolved forms.     

Potassium transport in red blood cells of frog Rana temporaria: demonstration of a K−Cl cotransport

Pathways of K⁺ movement across the erythrocyte membrane of frog Rana temporaria were studied using ⁸⁶Rb as a tracer. The K⁺ influx was significantly blocked by 0.1 mmol·l^-1 ouabain (by 30%) and 1 mmol·l^-1 furosemide (by 56%) in the red cells incubated in saline at physiological K⁺ concentration (2.7 mmol·l^-1). Ouabain and furosemide had an additive effect on K⁺ transport in frog red cells. The ouabain-sensitive and furosemide-sensitive components of K⁺ influx saturated as f(K⁺)_e with apparent K _m values for external K _e ⁺ concentration of 0.96±0.11 and 4.6±0.5 mmol·l^-1 and V _max of 0.89±0.04 and 2.8±0.4 mmol·l cells^-1·h^-1, respectively. The residual ouabain-furosemide-resistant component was also a saturable function of K _e ⁺ medium concentration. Total K⁺ influx was significantly reduced when frog erythrocytes were incubated in NO _- ³ medium. Furosemide did not affect K⁺ transport in frog red cells in NO ₃ ^- media. At the same K _e ⁺ concentration the ouabain-furosemide-insensitive K⁺ influx in Cl^- medium was significantly greater than that in NO _- ³ medium. We found no inhibitory effect of 1 mmol·l^-1 furosemide on Na⁺ influx in frog red cells in Cl^- medium. K⁺ loss from the frog erythrocytes in a K⁺-free medium was significantly reduced (mean 58%) after replacement of Cl^- with NO _- ³ . Furosemide (0.5 mmol·l^-1) did not produce any significant reduction in the K⁺ loss in both media. The Cl^--dependent component of K⁺ loss from frog red cells was 5.7±1.2 mmol·l^-1·h^-1. These results indicate that about two-thirds of the total K⁺ influx in frog erythrocytes is mediated by a K–Cl cotransport which is only partially blocked by furosemide.Abbreviations DMSO dimethyl sulphoxide - K _e ⁺ external concentration of K⁺ - K _m apparent Michaelis constant for external - K⁺ K _e ⁺ at V _max/2 - RBC red blood cell(s) - V _max maximal velocity of the unidirectional K⁺ influx - TRIS tris(hydroxymethyl)aminomethane     

Effects of antidiuretic hormone on cellular conductive pathways in mouse medullary thick ascending limbs of Henle: I. ADH increases transcellular conductance pathways

Summary This paper reports experiments designed to assess the relations between net salt absorption and transcellular routes for ion conductance in single mouse medullary thick ascending limbs of Henle microperfusedin vitro. The experimental data indicate that ADH significantly increased the transepithelial electrical conductance, and that this conductance increase could be rationalized in terms of transcellular conductance changes. A minimal estimate (G _c ^min ) of the transcellular conductance, estimated from Ba⁺⁺ blockade of apical membrane K⁺ channels, indicated thatG _c ^min was approximately 30–40% of the measured transepithelial conductance. In apical membranes, K⁺ was the major conductive species; and ADH increased the magnitude of a Ba⁺⁺-sensitive K⁺ conductance under conditions where net Cl^– absorption was nearly abolished. In basolateral membranes, ADH increased the magnitude of a Cl^– conductance; this ADH-dependent increase in basal Cl^– conductance depended on a simultaneous hormone-dependent increase in the rate of net Cl^– absorption. Cl^– removal from luminal solutions had no detectable effect onG _e , and net Cl^– absorption was reduced at luminal K⁺ concentrations less than 5mm; thus apical Cl^– entry may have been a Na⁺,K⁺,2Cl^– cotransport process having a negligible conductance. The net rate of K⁺ secretion was approximately 10% of the net rate of Cl^– absorption, while the chemical rate of net Cl^– absorption was virtually equal to the equivalent short-circuit current. Thus net Cl^– absorption was rheogenic; and approximately half of net Na⁺ absorption could be rationalized in terms of dissipative flux through the paracellular pathway. These findings, coupled with the observation that K⁺ was the principal conductive species in apical plasma membranes, support the view that the majority of K⁺ efflux from cell to lumen through the Ba⁺⁺-sensitive apical K⁺ conductance pathway was recycled into cells by Na⁺,K⁺,2Cl^– cotransport.