Refocusing revisited: An optimized,gradient-enhanced refocused HSQC and its applications in 2D and 3D NMR and in deuterium exchange experiments

Summary 2D ¹⁵N-¹H correlation spectra are ideal for measuring backbone amide populations to determine amide exchange protection factors in studies of protein folding or other structural features. Most protein NMR spectroscopists use HSQC, which has been shown to be generally superior to HMQC in both resolution and sensitivity. The refocused HSQC experiment is intrinsically less sensitive than the regular HSQC, due to T₂ relaxation during the refocusing delays. However, we show here that, when high ¹⁵N resolution is needed, an optimized refocused HSQC sequence that utilizes a semi-constant time evolution period and pulsed field gradients has better signal-to-noise ratio and resolution, and integrates more accurately, than a similar HSQC. The differences are demonstrated on a 20 kDa protein. The technique can also be applied to 3D NOESY experiments to eliminate strong NH₂ geminal peaks and their truncation artefacts at a modest cost in sensitivity.     

Glial α1-receptors probably inhibit the high-affinity uptake of noradrenaline into astrocytes in the rat brain in vivo

The effect of ₂-receptor blockage on the extraneuronal turnover of noradrenaline (NA) has been studied in the intact rat brain. Tropolone and yohimbine, along with reserpine or desmethylimipramine, were given 30 min after intracerebroventricular injection of [7-³H]NA, i.e. after the tracer had been stored or inactivated. Tropolone given alone did not change the fractions of³H-activity recovered as [³H]NA from hypothalamus, septum, striatum and pons-medulla, but in the presence of yohimbine improved the [³H]NA recovery in all areas except pons-medulla. The maximum effect was seen in the hypothalamus of reserpine-treated rats. Since the ₂-autoreceptors were blocked, the increased [³H]NA recovery does not reflect a down-regulated neuronal NA turnover. Instead it seems to show that a fraction greater than normal of neuronally released NA had been taken up into astrocytes and remained unmetabolized if catechol-O-methyltransferase was inactive. It is assumed that yohimbine enabled the protective tropolone effect by blocking astrocytic ₂-receptors that otherwise, either by itself or by antagonizing -receptor-induced hyperpolarization or cAMP formation, had impaired parameters that stimulate the high-affinity NA Uptake₁ of astrocytes (e.g. membrane potential, Na⁺, K⁺-ATPase) or control the gap junction permeability in the glial syncytium.     

Carbon isotope discrimination by plants follows latitudinal and altitudinal trends

Summary In an earlier paper we provided evidence that carbon isotope discrimination during photosynthesis of terrestrial C3 plants decreases with altitude, and it was found that this was associated with greater carboxylation efficiency at high altitudes. Changing partial pressures of CO₂ and O₂ and changing temperature are possible explanations, since influences of moisture and light were reduced to a minimum by selective sampling. Here we analyse plants sampled using the same criteria, but from high and low altitudes along latitudinal gradients from the equator to the polar ends of plant distribution. These data should permit separation of the pressure and temperature components (Fig. 1). Only leaves of fully sunlit, non-water-stressed, herbaceous C3 plants are compared. The survey covers pressure differences of 400 mbar (ca. 5000 m) and 78 degrees of latitude (ca 25 K of mean temperature of growth period). When habitats of similar low temperature (i.e. high altitude at low latitude and low altitude at polar latitude) are compared, discrimination increases towards the pole (with decreasing altitude and thus increasing atmospheric pressure). Latitudinally decreasing temperature at almost constant atmospheric pressure (samples from low altitude) is associated with a decrease in discrimination. So, polar low-altitude plants have ¹³C values half way between humid tropical lowland and tropical alpine plants. It is unlikely that latitudinal changes of the light regime had an effect, since low and high altitude plants show contrasting latitudinal trends in ¹³C although local altitudinal differences in overall light consumption were small. These results suggest that both temperature and atmospheric pressure are responsible for the altitudinal trends in ¹³C discrimination. Temperature effects may partly be related to increased leaf thickness (within the same leaf type) in cold environments. Theoretical considerations and laboratory experiments suggest that it is the oxygen partial pressure that is responsible for the pressure related change in discrimination. The study also provided results of practical significance for the use of carbon isotope data. Within a community of C3 plants, discrimination in species of similar life form, exposed to similar light, water and ambient CO₂ conditions ranges over 4, with standard deviations for 10–30 species of ±0.6 to 1.2. This natural variation has to be taken into account by using a sufficient sample size and standardization of sampling in any attempt at ecological site characterization using carbon isotope data. Evidence of a pronounced genotypic component of this variation in ¹³C discrimination in wild C3 plant species is provided. Correlations with dry matter partitioning, mesophyll thickness and nitrogen content are also present.     

Interactions of growth inhibitory factor with hydroxyl and superoxide radicals

To show the effects of growth inhibitory factor (Cu₄Zn₃MT-III) involved in the scavenging of reactive oxygen species (ROS), a pulse radiolytic study was employed using N₂O-saturated Cu₄Zn₃MT-III aqueous solutions. It was demonstrated that the oxidizing OH radical efficiently reacted with Cu₄Zn₃MT-III by forming a thiyl radical RS with a second-order constant of 1.46×10¹¹ mol l^–1s^–1, which was determined by competition kinetics against KSCN. The thiyl radical RS reacted rapidly and reversibly with a thiolate in Cu₄Zn₃MT-III to form radical anion RSSR ^– with a constant of 1.65×10⁹ mol lL^–1s^–1 per thiolate, while the constant of the decay of this radical anion was 2.72×10⁵ s^–1, and the equilibrium constant of the formation for RSSR ^– was 6.08×10³ mol^–1 l. These values were close to those of Cd₅Zn₂MT-II. The SOD activity of Cu₄Zn₃MT-III to quench O₂ ^–was assayed by the riboflavine-methionine-nitrobluetetrazolium (NBT) method which catalyzed the dismutation of superoxide (O₂ ^–) at pH 7.8 with an IC₅₀ value of 1.50×10^–6 M for Cu₄Zn₃MT-III and 1.62×10^–6 M for Cd₅Zn₂MT-II. Additionally, the down-regulation of GIF may be a main factor in the decrease of the scavenging ability for the free OH and O₂ ^–radicals, which is possibly associated with the pathogenesis of neurodegenerative disease.     

Sources of nitrate in rivers draining sixteen watersheds in the northeastern U.S.: Isotopic constraints

The feasibility of using nitrogen and oxygenisotope ratios of nitrate (NO₃ ^–) forelucidating sources and transformations ofriverine nitrate was evaluated in a comparativestudy of 16 watersheds in the northeastern U.S.A. Stream water was sampled repeatedly at theoutlets of the watersheds between January andDecember 1999 for determining concentrations,¹⁵N values, and ¹⁸Ovalues of riverine nitrate.In conjunction with information about land useand nitrogen fluxes,¹⁵N_nitrate and¹⁸O_nitrate values providedmainly information about sources of riverinenitrate. In predominantly forested watersheds,riverine nitrate had mean concentrations ofless than 0.4 mg NO₃ ^–-N L^–1,¹⁵N_nitrate values of lessthan +5, and ¹⁸O_nitratevalues between +12 and +19. This indicatesthat riverine nitrate was almost exclusivelyderived from soil nitrification processes withpotentially minor nitrate contributions fromatmospheric deposition in some catchments. Inwatersheds with significant agricultural andurban land use, concentrations of riverinenitrate were as high as 2.6 mg NO₃ ^–-NL^–1 with ¹⁵N_nitratevalues between +5 and +8 and¹⁸O_nitrate values generallybelow +15. Correlations between nitrateconcentrations, ¹⁵N_nitratevalues, and N fluxes suggest that nitrate inwaste water constituted a major, and nitrate inmanure a minor additional source of riverinenitrate. Atmospheric nitrate deposition ornitrate-containing fertilizers were not asignificant source of riverine nitrate inwatersheds with significant agricultural andurban land use. Although complementary studiesindicate that in-stream denitrification wassignificant in all rivers, the isotopiccomposition of riverine nitrate sampled at theoutlet of the 16 watersheds did not provideevidence for denitrification in the form ofelevated ¹⁵N_nitrate and¹⁸O_nitrate values. Relativelylow isotopic enrichment factors for nitrogenand oxygen during in-stream denitrification andcontinuous admixture of nitrate from theabove-described sources are thought to beresponsible for this finding.     

Interpretation of sulfur cycling in two catchments in the Black Forest (Germany) using stable sulfur and oxygen isotope data

The isotopic composition of SO ₄ ^2- in bulk precipitation, canopy throughfall, seepage water at three different soil depths, stream water, and groundwater was monitored in two forested catchments in the Black Forest (Germany) between November 1989 and February 1992. Isotope measurements on aqueous sulfate were complemented by ³⁴S-analyses on SO₂ in the air, total sulfur and inorganic sulfate in the soil, and bedrock sulfur, in order to identify sources and biogeochemical processes affecting S cycling in catchments with base poor, siliceous bedrock. Stable S isotope data indicated that atmospheric deposition and not mineral weathering is the major source of S in both catchments since ³⁴S-values for sulfate in the soil, in seepage water, and in stream water were generally found to be similar to the mean ³⁴S-values of precipitation SO ₄ ^2- (+2.1. However, ¹⁸O-values of seepage water SO ₄ ^2- at 30 cm and especially at 80 cm depth were depleted by several per mil with respect to those of the atmospheric deposition (+7.5 to +13.5. This indicates that in both catchments a considerable proportion of the seepage water SO ₄ ^2- is derived from mineralization of carbon-bonded soil S and must therefore have cycled through the organic soil S pool. ³⁴S-values for different S compounds in the solid soil were found to differ markedly depending on S fraction and soil depth. Since atmospheric S deposition with rather constant ³⁴S-values was identified as the dominant S source in both catchments, this is interpreted as a result ofin situ isotope fractionation rather than admixture of isotopically different S. The differences between the ³⁴S-values of seepage water and soil sulfate and those of organic soil S compounds are consistent with a model in which SO ₄ ^2- uptake by vegetation and soil microorganisms favours³⁴SO ₄ ^2- slightly, whereas during mineralization of organic soil S to aqueous SOSO ₄ ^2- ,³²S reacts preferentially. However, the data provide evidence for negligible isotope fractionation during physico-chemical S transformations such as adsorption/desorption in aerated forest soils.     

A global survey of carbon isotope discrimination in plants from high altitude

Summary Carbon 13/12 isotope ratios have been determined from leaves of a hundred C₃ plant species (or ecotypes) from all major mountain ranges of the globe, avoiding drought stressed areas. A general increase in ¹³C content was found with increasing altitude, i.e. overall discrimination against the heavy isotope is reduced at high elevation. The steepest decline of discrimination is observed in taxa typically ranging to highest elevations (e.g. the genus Ranunculus). Mean ¹³C for all samples collected between 2500 and 5600 m altitude is-26.15 compared to the lowland average of-28.80 (P<0.001). Forbs from highest elevations reach-24. According to theory of ¹³C discrimination this indicates decreasing relative limitation of carbon uptake by carboxylation. In other words, we estimate that the ratio of internal to external partial pressure of CO₂ (p _i /p _a )in leaves of high elevation plants is lower than in leaves of low altitude. These results confirm recent gas exchange analyses in high and low elevation plants.     

Effect of organic and inorganic fertigation on yields, δ15N values, and δ13C values of tomato (Lycopersicon esculentum Mill. cv. Saturn)

We examined the effects of fertilizer application, especially the effects of fertigation and types of fertilizer (inorganic and organic) on yields and ¹⁵N and ¹³C values of tomato (Lycopersicon esculentum Mill. cv. Saturn). Fertigation is a method in which an appropriate diluted liquid fertilizer is applied to the plants each time they are drip-irrigated. We developed a method of organic fertigation using corn steep liquor (CSL) as the liquid fertilizer, because it is an industrial byproduct of cornstarch manufacture and can be used very effectively. We compared fruit yield, mineral content, ¹⁵N value, and ¹³C value of tomatoes grown under three different fertilizer treatments, basal dressing: basal dressing with granular chemical fertilizer; inorganic fertigation: fertigation with liquid chemical fertilizer; and organic fertigation: fertigaion with CSL. Mineral contents of tomatoes grown with basal dressing were generally lower than those grown under either fertigation treatment. These results indicated that yields and mineral contents were influenced more by the method of fertilizer application than by whether the fertilizers were inorganic or organic. There were, however, significant differences in the ¹⁵N values of tomato fruits grown under different types of fertilizer applications, especially between inorganic and organic fertilizers. The ¹⁵N value of the chemical fertilizer used for basal dressing was 0.81 ± 0.45{}, that of the chemical fertilizer for fertigation was 0.00 ± 0.04{}, and that of CSL was 8.50 ± 0.71{}. The ¹⁵N values of the soils reflected the ¹⁵N values of the fertilizers. Moreover, the ¹⁵N values of the fruits corresponded to the ¹⁵N values of the applied fertilizers. The ¹⁵N values were 3.18 ± 1.34{} in the fruits grown with a basal dressing of chemical fertilizer, 0.30 ± 0.61 in those grown under inorganic fertigation, and 7.09 ± 0.68 in those grown under organic fertigation. On the other hand, although the ¹³C values in the soil also reflected the ¹³C values of the applied fertilizers, there was no significant difference in the ¹³C values of fruits among the different treatments. In conclusion, because the ¹⁵N values of fertilizers correlated well with those of the fruits, it may be possible to use ¹⁵N values as an indicator of organic products.     

Changes in soil organic matter with cropping as measured by organic carbon fractions and 13C natural isotope abundance

The decline in soil organic matter with cropping is a major factor affecting the sustainability of cropping systems. Changes in total C levels are relativelyinsensitive as a sustainability measure. Oxidation with different strength KMnO₄ has been shown to be a more sensitive indicator of change. The relative size of soil C fractions oxidised by 333 mM KMnO₄ declined with cropping, whilst the relative size of the unoxidised fraction increased. Changes in ¹³C ratio have been used to measure C turnover in systems which include C3 and C4 species.     

Photosynthetic Pathway Types in Rangeland Plant Species from Inner Mongolia,North China

Photosynthetic pathway types, based on ¹³C measurements, were determined for 125 species in 95 genera and 32 families growing in rangelands from Inner Mongolia. Of the total species, 4 species from 3 genera and 2 families had C₄ photosynthesis (2 species in Gramineae and 2 in Chenopodiaceae) and 118 species from 90 genera and 31 families had C₃ photosynthesis. The number of C₄ species differed significantly among four rangeland sites, 4 species in desert, 3 species in steppe, but no C₄ species were identified in meadow and dune. Six species [e.g. Agriophyllum arenarium Bieb., Bassia dasyphylla O. Kuntze, Saussurea japonica (Thunb.) DC.] earlier identified as C₄ species using the enzyme ratio method were found as C₃ species using the carbon isotope ratios (¹³C). Hence the enzyme ratio method for C₃ and C₄ identification may not always be reliable. The ¹³C values of 3 species of Crassulaceae, which had been considered as CAM species, differed remarkably [–25.79 for Sedum aizoon L., –24.42 for Osostachys fimbriatus (Turcz.) Berger, and –16.97 for O. malacophyllus (Pall.) Fisch], suggesting that the use of ¹³C method as a diagnosis for CAM photosynthetic pathway type may not always be reliable and supplementary measurements are needed.     

Effects of different nitrogen forms and combination with foliar spraying with 6-benzylaminopurine on growth,transpiration, and water and potassium uptake and flow in tobacco

NH₄ ⁺-N can have inhibitory effects on plant growth. However, the mechanisms of these inhibitory effects are still poorly understood. In this study, effects of different N forms and a combination of ammonium + 6-benzylaminopurine (6-BA, a synthetic cytokinin) on growth, transpiration, uptake and flow of water and potassium in 88-days-old tobacco (Nicotiana tabacum L. K 326) plants were studied over a period of 12 days. Plants were supplied with equal amounts of N in different forms: NO₃ ^–, NH₄NO₃, NH₄ ⁺ or NH₄ ⁺+6-BA (foliar spraying every 2 days after onset of the treatments). For determining flows and partitioning upper, middle and lower strata of three leaves each were analysed. During the 12 days study period, 50% replacement of NO₃ ^–-N by NH₄ ⁺-N (NH₄NO₃) did not change growth, transpiration, uptake and flow of water and K⁺ compared with the NO₃ ^–-N treatment. However, NH₄ ⁺-N as the sole N-source caused: (i) a substantial decrease in dry weight gain to 42% and 46% of the NO₃ ^–-N and NH₄NO₃ treatments, respectively; (ii) a marked reduction in transpiration rate, due to reduced stomatal conductance, illustrated by more negative leaf carbon-isotope discrimination (¹³C) compared with the NO₃ ^– treatment, especially in upper leaves; (iii) a strong reduction both in total water uptake, and in the rate of water uptake by roots, likely due to a decrease in root hydraulic conductivity; (iv) a marked reduction of K⁺ uptake to 10%. Under NH₄ ⁺ nutrition the middle leaves accumulated 143%, and together with upper leaves 206% and the stem 227% of the K⁺ currently taken up, indicating massive mobilisation of K⁺ from lower leaves and even the roots. Phloem retranslocation of K⁺ from the shoot and cycling through the root contributed 67% to the xylem transport of K⁺, and this was 2.2 times more than concurrent uptake. Foliar 6-BA application could not suppress or reverse the inhibitory effects on growth, transpiration, uptake and flow of water and ions (K⁺) caused by NH₄ ⁺-N treatment, although positive effects by 6-BA application were observed, even when 6-BA (10^–8 M) was supplied in nutrient solution daily with watering. Possible roles of cytokinin to regulate growth and development of NH₄ ⁺-fed plants are discussed.     

Interaction between perchlorate and nifedipine on insulin secretion from mouse pancreastic islets

In order to elucidate the mechanisms responsible for the stimulatory effect of perchlorate (ClO ₄ ^– ) on insulin secretion, we have investigated the interaction between this chaotropic anion and the organic calcium antagonist nifedipine. This drug, known as a blocker of L-type calcium channels, was chosen as a tool to test the idea that ClO ₄ ^– acts on insulin secretion by stimulating the gating of voltage-controlled Ca²⁺ channels. ClO ₄ ^– amplified the stimulatory effect of D-glucose on insulin release from perfused pancreas (first and second phases) as well as from isolated islets incubated in static incubations for 60 min. This indicates that ClO ₄ ^– amplifies physiologically regulated insulin secretion. Nifedipine reduced D-glucose-induced (20 mM) insulin release in a dose-dependent manner with half-maximum effect at about 0.8 M and apparent maximum effect at 5 M nifedipine. In the presence of 20 mM D-glucose, the inhibitory effects of 0.5, 1 or 5 M nifedipine were only slightly, if at all, counteracted by perchlorate. When 12 mM ClO ₄ ^– and 20 mM D-glucose were combined, calculation of the specific effect of ClO ₄ ^– revealed that nifedipine produced almost maximum inhibition already at 0.05 M. Thus, the perchlorate-induced amplification of D-glucose-stimulated insulin release shows higher sensitivity to nifedipine than the D-glucose-effect as such. This supports the hypothesis that perchlorate primarily affects the voltage-sensitive L-type calcium channel in the -cell.     

Improved lineshape and sensitivity in the HNCO-family of triple resonance experiments

A simple scheme is presented for the suppression of dispersive contributions to cross peaks in HNCO-type spectra where the ¹⁵N chemical shift is recorded in a constant-time manner immediately prior to the transfer from ¹⁵ N to ¹HN at the end of the sequence. These dispersive contributions arise when the delay for refocusing the ¹⁵N-¹³CO one-bond coupling is set to less than 0.5/¹J_N,CO and when ² J_HN,CO 0. Improvements in sensitivity in ¹HN detected experiments recorded on ¹⁵ N,¹³C-labeled samples can be realized by application of ¹³CO/¹³ decoupling during acquisition. Sensitivity gains on the order of 15% and 5% have been obtained for an SH3 domain (62 residues) and maltose binding protein (370 residues), respectively.     

Functional and neurochemical evidence that neurotensin-induced release of acetylcholine from Auerbach's plexus of guinea-pig ileum is presynaptically controlled via α2-adrenoceptors

The effect of neurotensin (NT) on [³H]acetylcholine release and contraction from isolated longitudinal muscle strip of guinea-pig ileum was examined. Neurotensin dose-dependently enhanced the release of [³H]-acetylcholine. This effect of neurotensin was inhibited by stimulation of ₂-adrenoceptors: noradrenaline, clonidine, xylazine or dexmedetomidine (₂-adrenoceptor agonists) inhibited neurotensin-induced release of acetycholine (ACh) as well as the contractions, while CH-38083 or yohimbine (₂-adrenoceptor antagonist) prevented this inhibitory effect. Our findings suggest that neurotensin may play a neuromodulatory role in the regulation of cholinergic neuronal activity in the gut and this modulatory effect is continuously controlled by the tonic activity of the sympathetic nervous system: endogenous noradrenaline release is capable of reducing the release of ACh and the consequent contraction of the gut enhanced by neurotensin.     

Response of Salvinia spp. to different nitrogen sources: the acid-base regulation approach

This paper shows the importance of acid-base analyses and ¹³C measurements in the evaluation of the responses of Salvinia species' responses to different N sources. It also highlights the importance of these methodologies as potential tools in the study of differences between habitats and nutrient acquisition, particularly N. This study used three different species of Salvinia cultured in the absence of combined N or in the presence of either NO _inf3 ^sup– or NH _inf4 ^sup+ as N sources. The interaction between NO _inf3 ^sup– or NH _inf4 ^sup+ as N source and organic acid metabolism, and the information on diazotrophy from the organic acid measurements, were also examined. Nevertheless, the results presented may not be used per se to assign diazotrophy. Carboxylate (C-A) levels in the different Salvinia species are much lower than the norm for bryophytes and tracheophytes, consistent with previously published work on Azolla. This might be related to the aquatic life form of these plants, since they seem to have no potential to increase the availability of Fe or P by the acidification of their rooting medium (water) that a larger net synthesis of organic acids, with cation-H⁺ exchange, could achieve.     

Determination of 3J(H infi supN,C infi sup′ ) coupling constants in proteins with the C′-FIDS method

Summary We introduce the C-FIDS-¹H,¹⁵N-HSQC experiment, a new method for the determination of ³J(H _infi ^supN ,C _infi ^sup ) coupling constants in proteins, yielding information about the torsional angle . It relies on the ¹H,¹⁵N-HSQC or HNCO experiment, two of the the most sensitive heteronuclear correlation experiments for isotopically labeled proteins. A set of three ¹H,¹⁵N-HSQC or HNCO spectra are recorded: a reference experiment in which the carbonyl spins are decoupled during t₁ and t₂, a second experiment in which they are decoupled exclusively during t₁ and a third one in which they are coupled in t₁ as well as t₂. The last experiment yields an E.COSY-type pattern from which the ²J(H _infi ^supN ,C _infi-1 ^sup ) and ¹J(N_i,C _infi-1 ^sup ) coupling constants can be extracted. By comparison of the coupled multiplet (obtained from the second experiment) with the decoupled multiplet (obtained from the first experiment) convoluted with the ²J(H _infi ^supN ,C _infi-1 ^sup ) coupling, the ³J(H _infi ^supN ,C _infi ^sup ) coupling can be found in a one-parameter fitting procedure. The method is demonstrated for the protein rhodniin, containing 103 amino acids. Systematic errors due to differential relaxation are small for ⁿJ(H^N,C) couplings in biomacromolecules of the size currently under NMR spectroscopic investigation.     

Estimation of symbiotic dinitrogen fixation in alder forest by the method based on natural15N abundance

Annual N₂-fixation in virgin forest ecosystems has been measured using a¹⁵N natural abundance (¹⁵N) procedure. This method was compared to a¹⁵N labelled fertilizer isotopic dilution method. For young alders (5–6 years old), ¹⁵N of leaves gave results in good agreement with the isotopic dilution of fertilizer method. Since ¹⁵N variability was expected according to plant physiology, for alder trees, leaves were collected at various heights after the end of the growing season, and, to take account of isotopic variations coming from derived inputs, ¹⁵N of leaves of a large number of other plants in the same are were measured to give control values. Following this procedure, the ¹⁵N method gave reliable evaluation of the nitrogen supply, by through N₂-fixation, to alders, which were found to maintain high nitrogen fixing capacity in a sequence ranging from first stage of establishment of climactic formation. Moreover, the same method is reported to discriminate various origins ofAlnus glutinosa grown in natural conditions, possibly in relation to the genetic diversity of this species.     

Molecular cloning and expression characterization of a rice K+ channel β subunit

K⁺ channel proteins native to animal membranes have been shown to be composed of two different types of polypeptides: the pore-forming subunit and the subunit which may be involved in either modulation of conductance through the channel, or stabilization and surface expression of the channel complex. Several cDNAs encoding animal K⁺ channel subunits have been recently cloned and sequenced. We report the molecular cloning of a rice plant homolog of these animal subunits. The rice cDNA (KOB1) described in this report encodes a 36 kDa polypeptide which shares 45% sequence identity with these animal K⁺ channel subunits, and 72% identity with the only other cloned plant (Arabidopsis thaliana) K⁺ channel subunit (KAB1). The KOB1 translation product was demonstrated to form a tight physical association with a plant K⁺ channel subunit. These results are consistent with the conclusion that the KOB1 cDNA encodes a K⁺ channel subunit.Expression studies indicated that KOB1 protein is more abundant in leaves than in either reproductive structures or roots. Later-developing leaves on a rice plant were found to contain increasing levels of the protein with the flag leaf having the highest titer of KOB1. Leaf sheaths are known to accumulate excess K⁺ and act as reserve sources of this cation when new growth requires remobilization of K⁺. Leaf sheaths were found to contain higher levels of KOB1 protein than the blade portions of leaves. It was further determined that when K⁺ was lost from older leaves of plants grown on K⁺-deficient fertilizer, the loss of cellular K⁺ was associated with a decline in both KOB1 mRNA and protein. This finding represents the first demonstration (in either plants or animals) that changes in cellular K⁺ status may specifically alter expression of a gene encoding a K⁺ channel subunit.     

Permeation of divalent cations through α-latrotoxin channels in lipid bilayers: steady-state current-voltage relationships

Summary -Latrotoxin, a polypeptide neurotoxin known to cause massive release of transmitter from vertebrate nerve terminals, is thought to act by forming cation-selective channels in plasma membranes. This paper describes the steady-state current carried by Ca²⁺, Sr²⁺ and Ba²⁺ through pores of -LaTx molecules incorporated in artificial bilayer membranes made of neutral lipids. Even when the solutions separated by the membrane are identical, theI-V relations rectify strongly, the current being higher when the side to which the toxin is added is positive. The polarity of the rectification is consistent with the hypothesis that the mechanism of action of the toxin is, at least in part, that of promoting inwardly directed flow of cations, and thus, accumulation of Ca²⁺ and other ions in the intracellular spaces. The dependence of theI-V characteristics on voltage and Ca²⁺ concentration is well described by a one-site, one-ion model for a channel. Three parameters of the model are deduced: the binding constant of the site for Ca²⁺,K=1.5m ^–1 (orK=7m ^–1 when activities are used instead of concentrations); the electrical distance of the site from the toxin-containing solution, =0.3; the free energy difference between the two barrier peaks, F =0.26 kT. The values of the parameters deduced by studying the channel in the presence of Ca²⁺ give theoretical curves that also fit the data with Sr²⁺ and Ba²⁺, indicating a low level of discrimination among these three cations.     

Evidence for voltage-dependent Cl− permeability in mouse pancreatic β-cells

Microdissected -cell-rich pancreatic islets fromob/ob-mice were used in studies of transmembrane³⁶Cl^– efflux. The mean rate coefficient for³⁶Cl^– efflux was stable at 0.158 min^–1 during the initial 10 min. Depolarization of the -cell plasma membrane by acute increases in extracellular K⁺ (5–130mM) stimulated the³⁶Cl^– efflux in a concentration-dependent manner. Glucose-induced (20mM) and K⁺-induced increases in³⁶Cl^– efflux were largely overlapping, but even at 135.9 mM K⁺, glucose slightly further enhanced the³⁶Cl^– efflux rate. The data suggest (1) that pancreatic -cells are equipped with a voltage-dependent Cl^– permeability, (2) that glucose-induced increase in Cl^– permeability may, at least partly, be mediated by primary membrane depolarization, and (3) that glucose in addition may activate other mechanisms for -cell Cl^– transport.