Effect of chemical modifiers of amino acid residues on proton conduction by the H+-ATPase of mitochondria

The effect of chemical modifiers of amino acid residues on the proton conductivity of H⁺-ATPase in inside out submitochondrial particles has been studied. Treatment of submitochondrial particles prepared in the presence of EDTA (ESMP) with the arginine modifiers, phenylglyoxal or butanedione, or the tyrosine modifier, tetranitromethane, caused inhibition of the ATPase activity. Phenylglyoxal and tetranitromethane also caused inhibition of the anaerobic release of respiratory H⁺ in ESMP as well as in particles deprived of F₁ (USMP). Butanedione treatment caused, on the contrary, acceleration of anaerobic proton release in both particles. The inhibition of proton release caused by phenylglyoxal and tetranitromethane exhibited in USMP a sigmoidal titration curve. The same inhibitory pattern was observed with oligomycin and withN,N-dicyclohexylcarbodiimide. In ESMP, relaxation of H⁺ exhibited two first-order phases, both an expression of the H⁺ conductivity of the ATPase complex. The rapid phase results from transient enhancement of H⁺ conduction caused by respiratory H⁺ itself. Oligomycin,N,N-dicyclohexylcarbodiimide, and tetranitromethane inhibited both phases of H⁺ release, and butanedione accelerated both. Phenylglyoxal inhibited principally the slow phase of H⁺ conduction. In USMP, H⁺ release followed simple first-order kinetics. Oligomycin depressed H⁺ release, enhanced respiratory H⁺, and restored the biphasicity of H⁺ release. Phenylglyoxal and tetranitromethane inhibited H⁺ release in USMP without modifying its first-order kinetics. Butanedione treatment caused biphasicity of H⁺ release from USMP, introducing a very rapid phase of H⁺ release. Addition of soluble F₁ to USMP also restored biphasicity of H⁺ release. A mechanism of proton conduction by F _o is discussed based on involvement of tyrosine or other hydroxyl residues, in series with the DCCD-reactive acid residue. There are apparently two functionally different species of arginine or other basic residues: those modified by phenylglyoxal, which facilitate H⁺ conduction, and those modified by butanedione, which retard H⁺ diffusion.     

Intracellular sites of the synthesis of sweet potato mitochondrial F1ATPase subunits

Summary Five subunits (-, -, -, - and -subunits) of the six -and -subunits) in the F₁ portion (F₁ATPase) of sweet potato (Ipomoea batatas) mitochondrial adenosine triphosphatase were isolated by an electrophoretic method. The - and -subunits were not distinguishable immunologically but showed completely different tryptic peptide maps, indicating that they were different molecular species. In vitro protein synthesis with isolated sweet potato root mitochondria produced only the -subunit when analyzed with anti-sweet potato F₁ATPase antibody reacting with all the subunits except the -subunit. Sweet potato root poly(A)⁺RNA directed the synthesis of six polypeptides which were immunoprecipitated by the antibody: two of them immunologically related to the -subunit and the others to the - and -subunits. We conclude that the -subunit of the F₁ATPase is synthesized only in the mitochondria and the -, - and -subunits are in the cytoplasm.     

Structure and function of H+-ATPase

(1) Extensive studies on proton-translocating ATPase (H⁺-ATPase) revealed that H⁺-ATPase is an energy transforming device universally distributed in membranes of almost all kinds of cells. (2) Crystallization of the catalytic portion (F₁) of H⁺-ATPase showed that F₁ is a hexagonal molecule with a central hole. The diameter of F₁ is about 90 Å and its molecular weight is about 380,000. (3) Use of thermophilic F₁ permits the complete reconstitution of F₁ from its five subunits (, , , , and ) and demonstration of the gate function of the -complex, the catalytic function of (supported by and ), and the H⁺-translocating functions of all five subunits. (4) Studies using purified thermostable F₀ showed that F₀ is an H⁺-channel portion of H⁺-ATPase. The direct measurement of H⁺-flux through F₀, sequencing of DCCD-binding protein, and isolation of F₁-binding protein are described. (5) The subunit stoichiometry of F₁ may be ₃₃. (6) Reconstitution of stable H⁺-ATPase-liposomes revealed that ATP is directly synthesized by the flow of H⁺ driven by an electrochemical potential gradient and that H⁺ is translocated by ATP hydrolysis. This rules out functions for all the hypothetical components that do not belong to H⁺-ATPase in H⁺-driven ATP synthesis. The roles of conformation change and other phenomena in ATP synthesis are also discussed.     

Proton/electron stoichiometry of mitochondrialbc 1 complex. Influence of pH and transmembrane δpH

The effect of pH and transmembrane pH on the efficiency of the proton pump of the mitochondrialbc ₁ complex bothin situ and in the reconstituted state was studied. In both cases the H⁺/e ^– ratio for vectorial proton translocation by thebc ₁ complex respiring at the steady state, under conditions in which the transmembrane pH difference (pH) represents the only component of the proton motive force (p), was significantly lower than that measured under level flow conditions. The latter amounts, at neutral pH, to 1 (2 including the scalar H⁺ release). In the reconstituted system steady-state pH was modulated by changing the intravesicular buffer as well as the intra/extra-liposomal pH. Under these conditions the H⁺/e^– ratio varied inversely with the pH. The data presented show that pH exerts a critical control on the proton pump of thebc ₁ complex. Increasing the external pH above neutrality caused a decrease of the level flowH ⁺/e ^– ratio. This effect is explained in terms of proton/electron linkage inb cytochromes.     

Keeling plots for hummingbirds: a method to estimate carbon isotope ratios of respired CO<Subscript>2</Subscript> in small vertebrates

The carbon isotope composition of an animals breath reveals the composition of the nutrients that it catabolizes for energy. Here we describe the use of Keeling plots, a method widely applied in ecosystem ecology, to measure the ¹³C of respired CO₂ of small vertebrates. We measured the ¹³C of Rufous Hummingbirds (Selasphorus rufus) in the laboratory and of Mourning (Zenaida macroura) and White-winged (Z. asiatica) Doves in the field. In the laboratory, when hummingbirds were fed a sucrose based C3 diet, the ¹³C of respired CO₂ was not significantly different from that of their diet (¹³C_{C3 diet}). The ¹³C of respired CO₂ for C3 fasted birds was slightly, albeit significantly, depleted in ¹³C relative to ¹³C_{C3 diet}. Six hours after birds were shifted to a sucrose based C4 diet, the isotopic composition of their breath revealed that birds were catabolizing a mixture of nutrients derived from both the C3 and the C4 diet. In the field, the ¹³C of respired CO₂ from Mourning and White-winged Doves reflected that of their diets: the CAM saguaro cactus (Carnegeia gigantea) and C3 seeds, respectively. Keeling plots are an easy, effective and inexpensive method to measure ¹³C of respired CO₂ in the lab and the field.     

TROSY experiment for refinement of backbone psi and phi by simultaneous measurements of cross-correlated relaxation rates and 3,4J(H alpha HN) coupling constants

The TROSY principle has been introduced into a HNCA experiment, which is designed for measurements of the intraresidual and sequential H-C/H^N-N dipole/dipole and H-C/N dipole/CSA cross-correlated relaxation rates. In addition, the new experiment provides values of the ^3,4 J _{H HN} coupling constants measured in an E.COSY manner. The conformational restraints for the and angles are obtained through the use of the cross-correlated relaxation rates together with the Karplus-type dependencies of the coupling constants. Improved signal-to-noise is achieved through preservation of all coherence transfer pathways and application of the TROSY principle. The application of the [¹⁵N,¹³C]-DQ/ZQ-[¹⁵N,¹H]-TROSY-E.COSY experiment to the 16 kDa apo-form of the E. coli Heme Chaperon protein CcmE is described. Overall good agreement is achieved between and angles measured with the new experiment and the average values determined from an ensemble of 20 NMR conformers.     

Stable carbon and oxygen isotopic compositions of recent charophyte oosporangia and water from Malham Tarn,U.K.: palaeontological implications

Charophyte oosporangia and water samples from a highly calcareous lake were measured for stable carbon and oxygen isotopic composition. The time period over which the oosporangia calcify is short, thus any biochemical relationship between the water and oosporangia"s calcite represents only one time window (late Summer in Malham Tam). This important temporal restraint must also apply to interpretations of all fossil material measured. The ¹⁸O_c of the charophyte oosporangia is deduced to be in equilibrium with the ¹⁸O of the water for a given temperature. The ¹³ C_c of the charophyte oosporangia was approximately 2.5 per mil lower than the ¹³C_DIC in the water we measured. With the release Of CO₂ with phosphoric acid from the charophyte oosporangia, there was no significant difference in the ¹⁸O_c values obtained, regardless of whether or not the carbonate was separated from the organic center, however ¹³C_c values were marginally lower for carbonate plus organic center measurements. Our results indicate that fossil charophyte gyrogonites can be used to elucidate the geochemistry of the ancient water body in which they lived.     

δ15N as an indicator of N2-fixation by cyanobacterial mats in tropical marshes

Cyanobacterial mats (CBM) are important components of wetland ecosystems in limestone-based regions of the Caribbean. During two sampling periods (July 1999 and January 2000) we measured N₂-fixation in samples from 23 different marshes simultaneously with measurements of relevant environmental factors. Samples were evaluated for abundance of five groups of cyanobacteria: (1) Leptolyngbya, (2) Oscillatoria, (3) Chroococcales, (4) Nostoc-& Stigonematales, and (5) dead sheaths. Differences in nitrogen fixation, expressed as nitrogenase activity in nmol C₂H₄ cm^–2 h^–1, were best explained by the proportion of heterocyst-forming cyanobacteria. The samples were analyzed for the natural abundance of ¹⁵N. ¹⁵N values ranged from –1.99 to 11.44 and were strongly negatively correlated with N₂-fixation. With all data included, ¹⁵N was also strongly correlated with nitrates in water. With the samples from Little Belize (high nitrate content marshes) excluded, the effect of nitrate became insignificant. N₂-fixation predicted from ¹⁵N measured on an independent data set from September 2000 was moderately accurate (r² = 0.68, 0.52 and 0.54 for predictions based on July 1999, January 2000 and combined data sets, respectively). When individual sample sets were divided into two groups with ¹⁵N < 2 and ¹⁵N > 2, the two groups were always highly significantly different in terms of their N₂-fixation. The presented evidence suggests that ¹⁵N can be used as a reliable indicator of N₂-fixation by CBM.     

Characterization of second site mutations show that fast proton transfer to QB − is restored in bacterial reaction centers of Rhodobacter sphaeroides containing the Asp-L213 → Asn lesion

The structural basis for proton coupled electron transfer to Q_B in bacterial reaction centers (RCs) was studied by investigating RCs containing second site suppressor mutations (Asn M44 Asp, Arg M233 Cys, Arg H177 His) that complement the effects of the deleterious Asp L213 Asn mutation [DN(L213)]. The suppressor RCs all showed an increased proton coupled electron transfer rate k _AB ⁽²⁾(Q_A ^–Q_B ^– + H⁺ Q_AQ_BH^–) by at least 10³ (pH 7.5) and a recombination rate k _BD (D⁺Q_AQ_B ^– DQ_AQ_B) 15–40 times larger than the value found in DN(L213) RCs. Proton transfer was studied by measuring the dependence of k _AB ⁽²⁾ on the free energy for electron transfer (G_et). k _AB ⁽²⁾ was independent of G_et in DN(L213) RCs, but dependent on G_et in native and all suppressor RCs. This shows that proton transfer limits the k _AB ⁽²⁾ reaction with a rate of 0.1s^–1 in DN(L213) RCs but is not rate limiting and at least 10⁸-fold faster in native and 10⁵-fold faster in the suppressor RCs. The increased rate of proton transfer by the suppressor mutations are proposed to be due to: (i) a reduction in the barrier to proton transfer by providing a more negative electrostatic potential near Q_B ^–; and/or (ii) structural changes that permit fast proton transfer through the network of protonatable residues and water molecules near Q_B.     

Temporal variability in <Superscript>13</Superscript>C of respired CO<Subscript>2</Subscript> in a pine and a hardwood forest subject to similar climatic conditions

Temporal variability in the ¹³C of foliage (¹³C_F), soil (¹³C_S) and ecosystem (¹³C_R) respired CO₂ was contrasted between a 17.2-m tall evenly aged loblolly pine forest and a 35-m tall unevenly aged mature second growth mixed broadleaf deciduous forest in North Carolina, USA, over a 2-year period. The two forests are located at the Duke Forest within a kilometer of each other and are subject to identical climate and have similar soil types. The ¹³C_F, collected just prior to dawn, was primarily controlled by the time-lagged vapor pressure deficit (VPD) in both stands; it was used for calculating the ratio of intercellular to ambient CO₂ (Ci/Ca). A remarkable similarity was observed in the relationship between Ci/Ca and time-lagged VPD in these two forests despite large differences in hydraulic characteristics. This similarity emerged as a result of physiological adjustments that compensated for differences in plant hydraulic characteristics, as predicted by a recently proposed equilibrium hypothesis, and has implications to ecophysiological models. We found that in the broadleaf forest, the ¹³C of forest floor CO₂ efflux dominated the ¹³C_R, while in the younger pine forest, the ¹³C of foliage respired CO₂ dominated ¹³C_R. This dependence resulted in a more variable ¹³C_R in the pine forest when compared to the broadleaf forest due to the larger photosynthetic contribution. Given the sensitivity of the atmospheric inversion models to ¹³C_R, the results demonstrate that these models could be improved by accounting for stand characteristics, in addition to previously recognized effects of moisture availability, when estimating ¹³C_R.     

The expression of mouse T-cell receptor TCRDV genes in BALB/c spleen

The rearrangement and expression of six different mouse T-cell receptor TCRDV (V) gene subfamilies have been studied in BALB/c mouse spleen. The results show that all the TCRDV gene segments studied can be rearranged and expressed with both the TCRA () and the TCRD () chain. The apparently restricted and separated V gene repertoire for the TCRD and TCRAT-cell receptor may result from thymus and peripheral selection rather than from selective rearrangement in the DNA level. Several J gene segment show how much higher concentration in spleen with TCRDV gene segments, however, these J gen segments do not tend to be located at either end of the J gene cluster.     

Characterization of inside-out oriented H+-ATPases in cholate-pretreated renal brush-border membrane vesicles

Summary Exposure of porcine renal brush-border membrane vesicles to 1.2% cholate and subsequent detergent removal by dialysis reorients almost all N-ethylmaleimide (NEM)-sensitive ATPases from the vesicle inside to the outside. ATP addition to cholate-pretreated, but not to intact, vesicles causes H⁺ uptake as visualized by the pH indicator, acridine organge. The reoriented H⁺-pump is electrogenic because permeant extravesicular anions or intravesicular K⁺ plus valinomycin enhance H⁺ transport. ATP stimulates H⁺ uptake with an apparentK _m of 93 m. Support of H⁺ uptake andP _i liberation by ATP>GTPITP> UTP indicates a preference for ATP and utilization of other nucleotides at lower efficiency. ADP is a potent, competitive inhibitor of ATP-driven H⁺ uptake,(K _i , 24 m). Mg²⁺ and Mn^2– support ATP-driven H⁺ uptake, but Ca²⁺, Ba²⁺ and Zn²⁺ do not. Imm Zn²⁺ inhibits MgATP-driven H⁺ transport completely. NEM-sensitiveP _i liberation is stimulated by Mg²⁺ and Mg^2– and, unlike H⁺ uptake, also by Ca²⁺ suggesting Ca²⁺-dependent ATP hydrolysis unrelated to H⁺ transport. The inside-out oriented H⁺-pump is relatively insensitive toward oligomycin, azide, N,N-dicyclohexylcarbodiimide (DCCD) and vanadate, but efficiently inhibited by NEM (apparentK _i , 0.77 m), and 4-chloro-7-nitro-benzoxa-1,3-diazole (NBD-Cl; apparentK _i , 0.39 m). Taken together, the H⁺-ATPase of proximal tubular brush-border membranes exhibits characteristics very similar to those of vacuolar type (V-type) H⁺-ATPases. Hence,V-type H⁺-ATPases occur not only in intracellular organelles but also in specialized plasma membrane areas.     

Interpretations of gradients in δ13C value in thick photosynthetic tissues of plants with Crassulacean acid metabolism

In Ceropegia dichotoma, Crassula argentea, Esheveria colorata, Kalanchoë beharensis, Opuntia ficus-indica, Sansveria stuckyi and Opuntia inermis the carbon-isotope ratio ( ¹³C) of tissues close to the epidermis is 2–4.3 more negative than those in the centre of the leaf or cladode. The greatest change in ¹³C value occurs between the epidermal layer and the layer of mesophyll tissue immediately underneath. Analysis of major metabolic and structural components in successive layers of Crassula argentea grown under controlled environmental conditions conducive to Crassulacean acid metabolism confirmed that much of the variation in ¹³C values of bulk carbon is caused by differences in chemical composition. Thus the steep gradient in ¹³C value at the epidermis reflects, in part, the contribution of more-negative ¹³C values of lipids in these tissues. Moreover, during nocturnal CO₂ fixation the amount of malic acid synthesised decreases with depth and the ¹³C value of the methanol-soluble fraction is less negative with distance away from the upper epidermis. These results are consistent with diffusion limitation to CO₂ uptake in these thick leaf tissues, which also contributes to the observed gradients in ¹³C value.Abbreviation CAM Crassulacean acid metabolism - FW fresh weight - PEPCase phospoenolpyruvate carboxylase - Rubisco ribulose-1,5-bisphosphate carboxylase-oxygenase - ¹³C carbon-isotope ratio This work was supported by grants from the North Carolina Biotechnology Centre to Duke University, National Science Foundation (NSF) grant DCB90-06830, Department of Energy, Division of Energy Biosciences grant DE-FG05-89 ER 14005, and NSF grant BSR 87-06429 to Duke University Phytotron.     

Oxygen and carbon isotope composition of parasitic plants and their hosts in southwestern Australia

We measured leaf dry matter ¹⁸O and ¹³C in parasitic plants and their hosts growing in southwestern Australia. Parasite/host pairs included two mistletoe species, three species of holoparasites, and five species of root hemiparasites. Among these parasite functional types, significant variation was observed in parasite/host isotopic differences for both ¹⁸O (P<0.0001, n=65) and ¹³C (P<0.0001, n=64). Mistletoes were depleted in both ¹⁸O and ¹³C compared to their hosts; parasite/host differences were –4.0 for ¹⁸O (P<0.0001) and –1.9 for ¹³C (P<0.0001). The lower ¹⁸O in mistletoe leaf dry matter compared to their hosts is consistent with the frequently observed high transpiration rates of these parasites. Root hemiparasites were also depleted in ¹⁸O and ¹³C compared to their hosts, but not to the same extent as mistletoes; parasite/host differences were –1.0 for ¹⁸O (P=0.04) and –1.2 for ¹³C (P=0.0006). In contrast to mistletoes and root hemiparasites, holoparasites were enriched in both ¹⁸O and ¹³C compared to their hosts; parasite/host differences were +3.0 for ¹⁸O (P<0.0001) and +1.5 for ¹³C (P=0.02). The enrichment in ¹⁸O for holoparasite dry matter did not result from more enriched tissue water; holoparasite tissue water ¹⁸O was less than host leaf water ¹⁸O by a difference of –3.8 when sampled at midday (P=0.0003). Enrichment of holoparasites in ¹³C compared to their hosts is consistent with a generally observed pattern of enrichment in heterotrophic plant tissues. Results provide insights into the ecology of parasitic plants in southwestern Australia; additionally, they provide a context for the formulation of specific hypotheses aimed at elucidating mechanisms underlying isotopic variations among plants.     

Factors influencing the stable carbon and oxygen isotopic composition ofPorites lutea coral skeletons from Phuket,South Thailand

We determined the ¹⁸O and ¹³C composition of the same fixed growth increment in severalPorites lutea coral skeletons from Phuket, South Thailand. Skeletal growth rate and ¹⁸O are inversely related. We explain this in terms of McConnaughey's kinetic isotopic disequilibria model. Annual trends in ¹⁸O cannot be solely explained by observed variations in seawater temperature or salinity and may also reflect seasonal variations in calcification rate. Coral tissue chlorophylla content and ¹³C of the underlying 1 mm of skeleton are positively related, suggesting that algal modification of the dissolved inorganic carbonate pool is the main control on skeletal ¹³C. However, in corals that bleached during a period of exceptionally high seawater temperatures in the summer of 1991, ¹³C of the outer 1 mm of skeleton and skeletal growth rate (over 9 months up to and including the bleaching event) are inversely related. Seasonal variations in °¹³C may reflect variations in calcification rate, zooxanthellae photosynthesis or in seawater ¹³C composition. Bleached corals had reduced calcification over the 9-month period up to and including the bleaching event and over the event they deposited carbonate enriched in¹³C and¹⁸O compared with unaffected corals. However, calcification during the event was limited and insufficient material was deposited to influence significantly the isotopic signature of the larger seasonal profile samples. In profile, overall decreases in ¹⁸O and ¹³C were observed, supporting evidence that positive temperature anomalies caused the bleaching event and reflecting the loss of zooxanthellae photosynthesis.     

Trophic interactions of Antarctic seals as determined by stable isotope signatures

The diets and trophic interactions among Weddell, crabeater, Ross, and leopard seals in the eastern Ross Sea, Antarctica, were investigated by the use of stable isotope techniques during the 1999–2000 summer seasons. The ¹³C and ¹⁵N values in seal serum clearly distinguished the three Antarctic pack-ice seal species at different trophic positions (Weddell>Ross>crabeater). These patterns appeared to reflect a close linkage to their known foraging ecology and diving behaviors, and agreed well with their presumed dietary diversity. The more enriched ¹³C and ¹⁵N values in male Weddell seals than those in females suggested differences in foraging preferences between them. Significant differences in ¹⁵N were also found among different age groups of Weddell seals. A strong correlation between the C:N ratios and serum cholesterol was probably due to extremely high cholesterol levels in phocids. Comparisons of isotope data with harbor seals revealed distinct differences between Antarctic phocids and the northern seal species.     

Carbon-isotope discrimination by leaves of Flaveria species exhibiting different amounts of C3-and C4-cycle co-function

Carbon-isotope ratios were examined as ¹³C values in several C₃, C₄, and C₃–C₄ Flaveria species, and compared to predicted ¹³C, values generated from theoretical models. The measured ¹³C values were within 4 of those predicted from the models. The models were used to identify factors that contribute to C₃-like ¹³C values in C₃–C₄ species that exhibit considerable C₄-cycle activity. Two of the factors contributing to C₃-like ¹³C values are high CO₂ leakiness from the C₄ pathway and pi/pa values that were higher than C₄ congeners. A marked break occurred in the relationship between the percentage of atmospheric CO₂ assimilated through the C₄ cycle and the ¹³C value. Below 50% C₄-cycle assimialtion there was no significant relationship between the variables, but above 50% the ¹³C values became less negative. These results demonstrate that the level of C₄-cycle expression can increase from, 0 to 50% with little integration of carbon transfer from the C₄ to the C₃ cycle. As expression increaces above 50%, however, increased integration of C₃- and C₄-cycle co-function occurs.Abbreviations and symbols RuBP carboxylase ribulose-1,5-bisphosphate carboxylase (EC 4.1.1.39) - PEP carboxylase phosphoenolpyruvate carboxylase (EC 4.1.1.31) - pa atmospheric CO₂ partial pressure - pi intercellular CO₂ partial pressure - isotope ratio - quantum yield for CO₂ uptake     

One-bond carbon-proton coupling constants: Angular dependence in β-linked oligosaccharides

Summary The angular dependence of¹J_C,H in model compounds related to -linked oligosaccharides has been established by FPT INDO quantum chemical calculations. Values calculated for models of (1 1)-, (1 2)-, (1 3)- and (1 4)-linked disaccharides were compared, and the effect of the orientation of HO-2 elucidated. The angular dependence of¹J_C,H on the torsional angles ^H and ^H and the solvent dielectric constant (s) was characterized in the form:¹J_C,H = A cos2+B cos + C sin2 + D since + E + Fe. The¹J_C,H values, measured by DEPT methods for C-1-H-1 and C-X-H-X in cellobiose, cyclic trisaccharide and hexopyranoses were used to adjust the calculated angular dependences. Based on the occurrence of the conformers for agarobiose, neoagarobiose, mannobiose and methyl -xylobioside, the thermodynamically averaged <¹J_C,H > values were calculated. The results obtained (<¹J_C-1,H-1 > 162.4, <¹J_{C-4, H-4} > 147.6 Hz for methyl -xylobioside; <¹J_C-1,H-1 > 162.4 and <¹J_C-4,H-4] > 147.6 Hz for mannobiose; <¹J_C-1,H-1 > 162.8 Hz for neo agarobiose and <¹J_C-1,H-1 > 163.2 Hz for agarobiose) agree well with the experimental values of 162.7, 147.5, 160.4, 147.2, 160.9 and 165.7 Hz, respectively.     

Effects of competition and N and P supply on carbon isotope discrimination and <Superscript>15</Superscript>N-natural abundance in four grassland species

The effect of interspecific competition and element additions (N and P) on four grassland species (Poa pratensis, Lolium perenne, Festuca valida, Taraxacum officinale) grown under field conditions was studied. Two grasses (L. perenne, F. valida) grown in monoculture (absence of competition) showed lower carbon isotope discrimination (¹³C) and enriched ¹⁵N values. Nitrogen addition (as urea) had inconsistent effects on species ¹³C while caused enrichment of ¹⁵N of P. pratensis and F. valida but strong depletion of ¹⁵N of T. officinale. Phosphorous had no significant effect on ¹³C but depleted ¹⁵N of all species.     

The mechanism of Na+ transport by rabbit urinary bladder

Summary The mechanism of Na⁺ transport in rabbit urinary bladder has been studied by microelectrode techniques. Of the three layers of epithelium, the apical layer contains virtually all the transepithelial resistance. There is radial cell-to-cell coupling within this layer, but there is no detectable transverse coupling between layers. Cell coupling is apparently interrupted by intracellular injection of depolarizing current. The cell interiors are electrically negative to the bathing solutions, but the apical membrane of the apical layer depolarizes with increasingI _sc. Voltage scanning detects no current sinks at the cell junctions or elsewhere. The voltage-divider ratio, , (ratio of resistance of apical cell membrane,R _a, to basolateral cell membrane,R _b) decreases from 30 to 0.5 with increasingI _sc, because of the transportrelated conductance pathway in the apical membrane. Changes in effective transepithelial capacitance withI _sc are predicted and possibly observed. The transepithelial resistance,R _t, has been resolved intoR _a, R_b, and the junctional resistance,R _j, by four different methods: cable analysis, resistance of uncoupled cells, measurements of pairs of (R _t, ) values in the same bladder at different transport rates, and the relation betweenR _t andI _sc and between andI _sc.R _j proves to be effectively infinite (nominally 300 k F) and independent ofI _sc, andR _a decreases from 154 to 4 k F with increasingI _sc. In the resulting model of Na⁺ transport in tight epithelia, the apical membrane contains an amiloride-inhibited and Ca⁺⁺-inhibited conductance pathway for Na⁺ entry; the basolateral membrane contains a Na⁺–K⁺-activated ATPase that extrudes Na⁺; intracellular (Na⁺) may exert negative feedback on apical membrane conductance; and aldosterone acts to stimulate Na⁺ entry at the apical membrane via the amiloride-sensitive pathway.