Relationship Between the Development and Growth of Rye (Secale cereale L.) and the Potassium Concentration in Solution

The development and growth of rye (Secale cereale L. cv. Rheidol)was studied in seedlings grown hydroponically in complete nutrientsolutions containing between 10 and 600 µM K⁺. The phyllochron(defined as the interval between the appearance of successiveleaves) was used as a developmental timescale to compare plants.The pattern of both shoot and root development was strictlyordered on a phyllochron basis and was unaffected by solutionK⁺ concentration, with the exception that tillers in plantsgrown at the lowest K⁺ concentrations were occasionally eithernot initiated or aborted at an early stage of development. However,both the rate of leaf appearance on the main stem and successivetillers and the rate of tiller appearance were slower in plantsgrown at lower K⁺ concentrations. The rate of leaf appearanceon the main stem was reduced to below 90% of its maximal valueat solution concentrations below about 50 µM K⁺. Plantrelative growth rate (RGR) was also reduced by lowering theK⁺ concentration of the nutrient solution and fell to below90% of its maximal value at solution concentrations below about200 µM K⁺. There was a complex relationship between tissueK⁺ concentration and the K⁺ concentration of the nutrient solution,which differed between leaves and root. Leaf K⁺ concentrationincreased steadily from about 50 µmol g^-1 f. wt to about200 µmol g^-1 f. wt as solution K⁺ concentration was increasedfrom 10 to 400 µM. In contrast, root K⁺ concentrationexhibited a sigmoidal dependence on solution K⁺ concentration,maintaining a minimal value of approximately 20 µmol g^-1f. wt at concentration below 100 µM K⁺, then increasingprogressively to about 120 µmol g^-1 f. wt at a solutionconcentration of 600 µM K⁺. The 'critical' leaf K⁺ concentration,i.e. the concentration at which either plant RGR or plant developmentwas reduced 90% of its maximal value, was 86 µmol g^-1f. wt for plant RGR and 150 µmol g^-1 f. wt for plant development.The 'critical' root K⁺ concentration was 24 µmol g^-1 f.wt K⁺ for both RGR and development. A decline in tissue K⁺ concentrationbelow these thresholds reduced plant growth considerably. RootK⁺ concentration was a sensitive indicator of the K⁺ statusof the plant with respect to potential growth since plant growthdeclined abruptly as root K⁺ concentration approached its 'critical'value, whereas plant growth showed a less defined relationshipwith shoot K⁺ concentration.Copyright 1993, 1999 Academic Press Critical K⁺ concentration, development, potassium, relative growth rate (RGR), rye, Secale cereale L. cv. Rheidol     

Net and Steady-state Cation Fluxes in Chlorella pyrenoidosa

The addition of K⁺ to Chlorella cells grown so as to be abnormallyrich in Na⁺ induces a net Na⁺ efflux and a concomitant uptakeof K⁺. The net Na⁺ extrusion shows first-order kinetics withtime constants of about 10 min for illuminated cells, and occursat rates in the region of 10 to 15 pmol cm1² s. The correspondingtime course for the net K⁺ influx also approximates to first-orderkinetics but is more complicated because it not only involvesa K⁺/Na⁺ component but also a K⁺/H⁺ exchange. The H⁺ extrusionusually represents less than 20 per cent of the net cation movementand may account both in magnitude and in rate for the differencebetween K⁺ and Na⁺ movements. The magnitudes of the net K⁺ andNa⁺ fluxes differed from steady-state flux rates in normal highK⁺-containing cells being as much as 20 times greater for K⁺and over 100 times greater for Na⁺. There is some indicationthat K⁺ competes for Na⁺ entry into Na⁺-rich cells, suggestingthat both the Na⁺/Na⁺ and K⁺/Na⁺ exchanges may share the sameentry site. The K⁺/Na⁺ exchange rates saturate at low externalK⁺ concentrations; the half-maximum rate was at about 0.2 mMK⁺. The Na⁺/K⁺ exchange is sensitive to temperature and between0 and 25 °C an activation energy of about 25 k cal/molewas calculated from the Arrhenius equation.     

Biosynthesis of folic acid compounds in plants VI. The occurrence and properties of the dihydrofolate-synthesizing enzyme in pea seedlings

An enzyme, which catalyzes the formation of dihydrofolate fromdihydropteroic acid and L-glutamic acid, was found in pea seedlings.The enzyme was purified approximately 25-fold from the crudeextracts of pea seedlings, and its some properties were investigated.Optimum pH for the enzyme activity was found to be 8.8. Pteroicand tetrahydropteroic acids were not active as substrate. Theenzymatic reaction required as cofactors ATP, divalent (Mg²⁺or Mn²⁺) and univalent (K⁺, NH₄⁺ or Rb⁺) cations. The productwas characterized as dihydrofolic acid by bioautography. MICHAELIS constants for L-glutamic acid, ATP, dihydropteroicacid and Mg²⁺ were 7.0x10^–4, 9.0x10^–5, 3.5x10^–6and 1.2x10^–3 M, respectively. The MICHAELIS constant forMn²⁺ was 3.0x10^–4. The enzyme was inhibited by PCMB orsilver nitrate and, to some extent, by L-aspartic acid. Inhibitionby PCMB was completely reversed by addition of 2-mercaptoethanol.Enzyme activity was distributed widely among plants. The importanceof magnesium and potassium ions for enzyme catalysis is discussed. ¹For the previous paper, Part V, see Reference (30). (Received March 28, 1970; )     

Matrix free Mg2+ and the regulation of mitochondrial volume

Mitochondria must maintain volume homeostasis inorder to carry out oxidative phosphorylation. It has been postulatedthat the concentration of freeMg²⁺([Mg²⁺]) serves as thesensor of matrix volume and regulates aK⁺-extrudingK⁺/H⁺antiport (K. D. Garlid. J. Biol. Chem.255: 11273-11279, 1980). To test this hypothesis, the fluorescentprobe furaptra was used to monitor[Mg²⁺] and freeCa²⁺ concentration ([Ca²⁺]) in the matrix ofisolated beef heart mitochondria, andK⁺/H⁺antiport activity was measured by passive swelling in potassium acetate. Concentrations that result in 50% inhibition of maximum activity of 92 µM matrix [Mg²⁺] and 2.2 µM[Ca²⁺] were determined for theK⁺/H⁺ antiport. Untreated mitochondria average670 µM matrix [Mg²⁺], a value that would permit <1%of maximumK⁺/H⁺antiport activity. Hypotonic swelling results in large decreases inmatrix [Mg²⁺], butswelling due to accumulation of acetate salts does not alter[Mg²⁺]. Swelling inphosphate salts decreases matrix[Mg²⁺], but not tolevels that permit appreciable antiport activity. We conclude that1) it is unlikely that matrix[Mg²⁺] serves as themitochondrial volume sensor, 2) ifK⁺/H⁺antiport functions as a volume control transporter, it is probably regulated by factors other than[Mg²⁺], and3) alternative mechanisms formitochondrial volume control should be considered.

     

Soil nitrogen form and plant nitrogen uptake along a boreal forest productivity gradient

We present results from a study of soil solution concentrations of ammonium (NH₄⁺), nitrate (NO₃^-), and amino acid N over one growing season along a local 90-m-long plant productivity gradient in a boreal forest. Three forest types are found along the gradient: an ericaceous dwarf-shrub type between 0 and 40 m, a low-herb type between 40 and 80 m, and a tall-herb type at 90 m. Soil sampling of the mor layer was performed in June, July, August and October in the three forest types. In addition, plant uptake of NH₄⁺, NO₃^- and the amino acid glycine was investigated. A mixture of the three N forms was injected into the soil; one N form at a time was labeled with ¹⁵N, and in the case of glycine also with ¹³C. In the dwarf-shrub forest, where plant productivity was low, the soil N pool was strongly dominated by amino acid N. There, plants took up more NH₄⁺ than NO₃^-. Glycine uptake did not differ significantly from either NH₄⁺ or NO₃^- uptake. Along the gradient, soil concentrations of NH₄⁺ and NO₃^- increased, as did plant productivity. In the low-herb forest NH₄⁺ comprised a major portion of the soil N pool, and plants took up more NH₄⁺ than NO₃^- or glycine. In the tall-herb forest, NO₃^- was as abundant as NH₄⁺, and together these two N forms dominated the soil N pool. Here, plants took up nearly equal amounts of NO₃^- and NH₄⁺, and this uptake exceeded that of glycine severalfold. Apart from the overall preference for NH₄⁺ that plants exhibited throughout the gradient, the results show a correlation between soil concentrations of amino acids and NO₃^- and plant preferences for these N forms.     

Distribution of sodium transporters and aquaporin-1 in the human choroid plexus

The choroid plexus epithelium secretes electrolytes and fluid in the brain ventricular lumen at high rates. Several channels and ion carriers have been identified as likely mediators of this transport in rodent choroid plexus. This study aimed to map several of these proteins to the human choroid plexus. Immunoperoxidase-histochemistry was employed to determine the cellular and subcellular localization of the proteins. The water channel, aquaporin (AQP) 1, was predominantly situated in the apical plasma membrane domain, although distinct basolateral and endothelial immunoreactivity was also observed. The Na⁺-K⁺-ATPase ₁-subunit was exclusively localized apically in the human choroid plexus epithelial cells. Immunoreactivity for the Na⁺-K⁺-2Cl^– cotransporter, NKCC1, was likewise confined to the apical plasma membrane domain of the epithelium. The Cl^–/HCO₃^– exchanger, AE2, was localized basolaterally, as was the Na⁺-dependent Cl^–/HCO₃^– exchanger, NCBE, and the electroneutral Na⁺-HCO₃^– cotransporter, NBCn1. No immunoreactivity was found toward the Na⁺-dependent acid/base transporters NHE1 or NBCe2. Hence, the human choroid plexus epithelium displays an almost identical distribution pattern of water channels and Na⁺ transporters as the rat and mouse choroid plexus. This general cross species pattern suggests central roles for these transporters in choroid plexus functions such as cerebrospinal fluid production. immunohistochemistry; metabolism; cerebrospinal fluid secretion     

Inorganic nitrogen uptake and regeneration in perennially icecovered Lakes Fryxell and Vanda, Antarctica

The isotope ¹⁵N was used to examine nitrogen dynamics in LakesFryxell and Vanda, two permanently ice-covered Antarctic lakes.Half-saturation constants for NH₄⁺. uptake in the shallow watersof both lakes were <10 µg N l^–1; uptake kineticexperiments on populations forming the deep-chlorophyll layersof these lakes showed zero-order kinetics and could not be fittedwith the Michaelis-Menten equation. Elevated uptake within thefirst few minutes following pulses of NH₄⁺. and NO₃^– occurredin both lakes. NH₄⁺ regeneration, determined from isotope dilutionexperiments, exceeded uptake at 4.6 m in Lake Fryxell, was lessthan uptake at 9 m in Lake Fryxell and was equal to uptake at10 m in Lake Vanda under the experimental conditions. NO₃^–uptake was suppressed by NH₄⁺ levels as low as 2 µg NH₄⁺-N l^–1 in Lake Fryxell; the suppression was strongestin the near-surface populations. Substrate-saturated C:N uptakeratios (g:g) in Lake Fryxell decreased from 8.4 near the surfaceto 1.8 at the bottom of the trophogenic zone. Overall, the nitrogendynamics in these lakes are similar to other lakes and the openocean in that biological productivity during the austral summeris supported by regenerated nutrients.     

Relative Importance of Ion Exclusion, Secretion and Accumulation in Spartina alterniflora Loisel.

The extent to which Spartina alterniflora Loisel. excluded,secreted or accumulated the major seawater ions (Cl^-, SO^2-₄,Na⁺, K⁺, Mg²⁺, and Ca²⁺) was investigated under varying salinitytreatments. From a quantitative viewpoint, ion exclusion wasmost prominent and accounted for 91–97% of the theoreticalmaximum ion uptake as a result of transpiration and growth.Of those ions taken up, approximately half was secreted fromthe shoots. Relative to K⁺, a disproportionate amount of Na⁺was excluded at the roots and secreted by the shoots. The concentrationwithin the tissues of S. alterniflora did not change with salinitytreatment for the majority of the ions examined, but Na⁺ wasmore than twice as concentrated at 40 g dm^-3 than at lOgdm^-3.Calculations of the flux of ions from salt marsh sediments tothe flood water via shoot secretion or stem/leaf turnover indicatethat these processes may be important to the ecology of S. alternifloraas mechanisms that limit the accumulation of salt within theroot zone.     

Movements of K+ during Shutting and Opening of the Trap-Lobes in Aldrovanda vesiculosa

K⁺ movements during the shutting and subsequent opening of trap-lobesin Aldrovanda vesiculosa were measured using ⁸⁶Rb as a tracerfor K⁺. Immediately after the shutting, a large amount of ⁸⁶Rbpre-loaded in the trap-lobes was detected in the hollow spaceinside the shut trap. This may indicate that much of the K⁺in the active motor cells leaks out during the shutting, resultingin turgor loss in the cells. ⁸⁶Rb(K⁺) uptake in the trap wasactive. During the opening process, enhanced ⁸⁶Rb uptake wasobserved. The time course of this uptake was similar to thatof the opening of the trap-lobes, and both courses were acceleratedby IAA. Enhanced K⁺ uptake may restore the turgor in activemotor cells. The quantity of K⁺ that moved during the shuttingor opening was estimated as 20% of that in the active motorcells in the open state of the trap-lobes. The K⁺ efflux acrossthe membranes of the active motor cells may be caused by a largeincrease in bulk flow triggered by an action potential, andwas estimated as 6,200 pmol.cm^–2. ¹ This paper is dedicated to the memory of Professor Joji Ashidawho established the physiology of rapid movement in Aldrovandavesiculosa. (Received July 22, 1982; Accepted November 11, 1982)     

Measurements of Ion Concentrations and Fluxes in Dunaliella parva

Measurements of K⁺, Na⁺, and Cl^– were made on a halotolerantstrain of Dunaliella growing at 500 mM NaCl, 25 ?C, and a relativelylow light intensity (6000 Lx). Much effort was spent in searchingfor a means of measuring the extracellular volume of fluid trappedbetween the cells of centrifuged pellets. All of the sugarstried as markers were rejected because they were found to bedigested in the cell suspension. The most suitable marker wasfound to be [¹⁴C]polyethylene glycol² (mol. wt. 4000); althoughthis substance was apparently adsorbed to the cell exterior,it was found possible to correct for adsorption and then obtaina reasonable figure for the trapped fluid. The final concentrationsof cell K⁺ and Na⁺ were 128 ? 53 mM and 131 ? 117 mM respectively.Cl^– balanced the sum of K⁺ Na⁺. Influxes of ²²Na⁺, ⁴²K⁺,and ³⁶C1^– were measured in cells in which the ions werein the steady state. Averages of 610 and 6.6 nmol m^–2s^–1 were obtained for Na⁺ and K⁺ respectively. Cl^–influx was divided into 2 phases with values of 1540 and 178mmol m^–2 s^–1. The faster influx was considered tobe across the outer cell membrane. The membrane responsiblefor the slower influx has not been identified. By comparingvalues of the potential difference calculated from the Nernstand Goldman equations, it was concluded that Na⁺ and K⁺ areprobably controlled by active mechanisms, whereas cell Cl^–is likely to be at thermodynamic equilibrium with the medium.     

H+/OH- Excretion and Nutrient Uptake in Upper and Lower Parts of Lupin (Lupinus angustifolius L.) Root Systems

The cultivation of narrow-leafed lupins (Lupinus angustifoliusL.) increase rates of subsoil acidification, and this is thoughtto be partly related to their pattern of nutrient uptake andH⁺/OH^- excretion. The main hypothesis of this study was thatH⁺ and OH^- excretion is not distributed evenly over the entirelength of the root system but is limited to zones where excesscation or anion uptake occur. Seedlings of nodulated lupinswere grown in solution culture using vertically split pots thatallowed the upper and lower zones of the root system to be suppliedwith varying concentrations of K⁺ and NO^-₃. Net H⁺/OH^- excretionwas equated to the addition of NaOH/HCl required to maintaina constant pH in the nutrient solution during a 4-d treatmentperiod and nutrient uptake was measured by depletion from solutionin each zone of the split pots. The excess of cation over anion uptake was positively correlatedwith H⁺ excretion in each rooting zone. In zones where K⁺ wassupplied at 1200 µM, cation uptake was dominated by K⁺and up to twice as much H⁺ was excreted than in zones whereK⁺ was absent. In zones where NO^-₃ was supplied at 750 µM,the anion/cation uptake was balanced, however H⁺ excretion continuedto occur in the zone. When NO^-₃ was supplied at 5000 µM,anion uptake exceeded cation uptake but there was no OH^- excretion.Organic acid anions may be excreted by lupins to maintain theirinternal electroneutrality when anion uptake exceeds cationuptake. Rhizosphere pH would not increase unless the pK_a ofthe excreted organic anions was greater than the external pH.Copyright1993, 1999 Academic Press Lupinus angustifolius L., H⁺/OH^- excretion, nutrient uptake, cation-anion balance, vertical split root     

Effects of univalent cations on the formation of nitrate reductase and nitrite reductase in rice seedlings

An investigation was made to determine the effects of univalentcations as activators on the formation of nitrate reductaseand nitrite reductase in rice seedlings. K⁺ functioned moreeffectively as a univalent cation activator than did other univalentcations examined. Substitution of Rb⁺ for K⁺ resulted in stimulationof nitrate reductase formation at about half the rate obtainedwith K⁺. There was no effect on nitrite reductase formation.Na⁺ could be partially substituted for K⁺ in the formation ofboth enzymes. NH₄⁺ slightly inhibited formation of the enzymes.In the absence of univalent cations, enzyme formation proceededat a slower rate during the initial 15-hr period, but thereafterproceeded at a higher rate. This delayed formation was not observedin the presence of K⁺. Results from inhibitor experiments suggestthat K⁺ stimulates the formation of nitrate reductase and nitritereductase. In conclusion, when nitrate nitrogen is supplied to rice plantsutilization of the nitrogen may be accelerated by increasedformation of enzymes involved in nitrate assimilation in thepresence of K⁺. (Received February 21, 1969; )     

Eddy diffusion of phytoplankton and nutrients: estimating coefficients from simulated and observed vertical distributions

A coupled, time-dependent, system of diffusion/advection equationswas used as the basis for estimating values of the eddy diffusioncoefficient K_x from simulated vertical distributions of fourstate variables, phytoplankton, nitrate, zooplanlcton and detritus.All concentrations were expressed in mmol m^–3 of nitrogen,and a conceptual 100 m water column was considered closed attop and bottom. The method was tested first with model output,then applied to quasi-steady-state distributions of chlorophylla and nitrate concentrations observed in the Celtic Sea on July7, 1982. Values of K_x in the simulated system were set at 30m² day^–1 above and below the thermoclme. Estimates forthe Celtic Sea were higher near the surface, lower just abovethe thermodine, and similar at depth. The model value withinthe thermocline was 0.2 m day^–1, whereas the estimatefor the Celtic Sea was 3 m² day^–1 Finally, equations weremodified to allow for non-steady-state conditions noted duringan upwelling period in the Tasman Sea between July 10 and July11, 1987, one tidal cycle apart. The estimated value of K, approached4700 m² day^–1 at 65 m     

Total Uptake and Incorporation into DNA of 3H-Thymidine, 3H-Deoxyuridine, and 3H-Thymine in the Primary Root of Vicia faba L.: II. EXCISED ROOTS

Total uptake of ³H-thymidine, ³H-thymine, and ³H-deoxyuridineand incorporation of these substances into DNA have been investigatedin excised roots in Vicia faba. Total uptake was found to behigher in excised roots than in intact ones. This was a consequenceof exogenous ³H-DNA precursors entering the excised roots throughthe cut surface. Where the cut surface was not immersed in the³H-thymidine solution ³H uptake was also higher than in intactroots. In this case ³H uptake scemed to be correlated with water-lossfrom the cut surface. Incorporation of ³H-thymidine, ³H-thymine,and ³H-deoxyuridine into DNA was found to be higher in excisedroots than in intact ones, probably as a result of a decreasein the size of the relevant endogenous precursor pools. It issuggested that this decrease resulted from the cessation ofthe supply of DNA precursors to these roots from the cotyledons.     

Incorporation of 3H-uridine and 3H-leucine during early embryogenesis of rice and barley in caryopsis culture

Incorporation of ³H-uridine and ³H-leucine during early embryogenesisin rice and barley was examined by culturing caryopses on White'smedium containing these isotopes. Grain counts showed that nodetectable amount of ³H-uridine was incorporated during theearly and middle periods of the globular embyo in both plants.³H-Uridine was detected in an embryo consisting of more than100 cells. ³H-Leucine, however, was incorporated from the beginningof embryogenesis. These results suggest that during early embryonicdevelopment in these plants, as in animal embryogenesis, RNAsynthesis is limited and the proteins will be synthesized byusing RNAs stored in the egg cell. The 100-cell stage is considered a critical point in early embryonicdevelopment, because at this stage cereal embryos start exponentialand dual rhythmic growth as well as uridine incorporation. (Received December 21, 1978; )     

Effect of NaCI Salinity on Flows and Partitioning of C, N, and Mineral Ions in Whole Plants of White Lupin, Lupinus albusL.

Plants of Lupinus albus L., cv. Ultra, were grown hydroponicallywith NO₃^–-nutrition for 51 d under control (0.05 mol m^–3Na⁺ and 10 mol m^–3 Cl^–) and saline (40 mol m^–3NaCI) conditions. Plants were harvested 41 and 51 d after germinationand analysed for content and net increment of C, N and the mineralcations K⁺, Na⁺, Mg²⁺, and Ca²⁺ and the anions Cl^–, NOJ,malate, phosphate, and SO₄^2–. Roots, stem interaodes,petioles and leaflets were analysed separately. During the studyperiod net photosynthesis, respiratory losses of CO₂ from shootand root and the composition of the spontaneously bleeding phloemsap and the root pressure xylem exudate were also determined.Using molar ratios of C over N in the transport fluids, incrementsof C and N, and photosynthetic gains as well as respiratorylosses of C, the net flows of C and N in the xylem and phloemwere then calculated as in earlier studies (Pate, Layzell andMcNeill, 1979a). Knowing the carbon flows, the ratios of ionto carbon in the phloem sap, and ion increments in individualorgans, net flows of K⁺, Na⁺, and Cl^– over the study periodwere also calculated. Salt stress led to a general decrease of all partial componentsof C and N partitioning indicating that inhibitions were notdue to specific effects of NaCI salinity on photosynthesis oron NO₃ uptake. However, there were differences between variouslyaged organs, and net phloem export of nitrogenous compoundsfrom ageing leaves was substantially enhanced under saline conditions.In addition, NO₃^–reduction in the roots was specificallyinhibited. Uptake and xylem transport of K⁺ was more severelyinhibited than photosynthetic carbon gain or NO₃^– uptakeby the root. K⁺ transport in the phloem was even more severelyrestricted under saline conditions. Na⁺ and Cl^– flowsand uptake, on the other hand, were substantially increasedin the presence of salt and, in particular, there were thenmassive flows of Na^– in the phloem. The results are discussedin relation to the causes of salt sensitivity of Lupinus albus.The data suggest that both a restriction of K⁺ supply and astrongly increased phloem translocation of Na⁺ contribute tothe adverse effects of salt in this species. Restriction ofK⁺ supply occurs by diminished K⁺ uptake and even more by reducedK⁺ cycling within the plant. Key words: Lupinus albus, salt stress, phloem transport, xylem transport, partitioning, carbon, nitrogen, K⁺, Na⁺, CI^–     

Effect of Sodium on Phosphate Uptake in Unicellular and Filamentous Cyanobacteria

The effect of Na⁺ on phosphate uptake was studied in four strainsof cyanobacteria: Synechococcus PCC 7942, Gloeothece PCC 6501,Phormidium sp. and Chlorogloeopsis PCC 6912. Phosphate uptakewas stimulated by Na⁺ in all cases. Li⁺ and K⁺ acted as partialanalogues for Na⁺. Half-saturation [K_1/2(Na⁺)] of phosphateuptake was reached with Na⁺ concentrations ranging from 317µM in Chlorogloeopsis to 659 µM in Phormidium. Theconcentration of phosphate required to reach half-saturationof phosphate uptake [K_1/2(P_i)]was not changed by the presenceof Na⁺. (Received April 11, 1994; Accepted July 5, 1994)     

Identification and characterization of a divalent cation-dependent glycosaminoglycan-binding protein from rat liver endothelium

Rat liver endothelial cells (LECs) express a membrane-associatedCa²⁺-dependent hyaluronan-binding activity (CaHA-BP) which isdistinct from the Ca²⁺-dependent, endocytic LEC HA receptor(Yannariello-Brown et al., J. Cell Biochem., 48, 73–80,1992). The CaHA-BP is specific for a subset of glycosaminoglycans,since Ca²⁺-dependent binding of ¹²⁵I-HA ({small tilde}80kDa)to LECs was competed with a 100-fold excess (w/w) of HA, chondroitinsulfate, and heparin, but not with chondroitin. The CaHA-BPactivity on intact LECs was pH-dependent. Optimal binding occurredat pH 6.0; no binding was detected at pH values 5 or 9. ¹²⁵I-HA,pre-bound in the presence of Ca²⁺ could also be dissociatedwith an acidic buffer (pH 5.0), as well as the divalent cationchelators EDTA and EGTA. ¹²⁵I-HA binding was stimulated by divalentcations other than Ca²⁺ such as Mg²⁺, Mn²⁺ and Ba²⁺; with theexception of Zn²⁺. A photoaffinity crosslinking reagent (¹²⁵I-ASD-HA)was used to identify specifically crosslinked polypeptides onLECs. In the absence of Ca²⁺ and in the presence of EGTA, onlybands at 175/166 kDa were consistently crosslinked. These bandshave been previously identified as the LEC Ca²⁺-independentendocytic HA receptor (Yannariello-Brown et al., J. Biol. Chem.,267, 20451/20455, 1992). In the presence of Ca²⁺, crosslinkingwas consistently seen to a 68 kDa polypeptide. Crosslinkingwas competed with a 100-fold excess (w/w) of HA. These and otherdata suggest that a 68 kDa protein is the most likely candidatefor the CaHA-BP in LECs. photoaffinity crosslinking hyaluronan calcium lectin     

Effect of K+, its Counter Anion, and pH on Sodium Efflux from Barley Root Tips

Sodium efflux from ²²Na⁺-loaded root tips root tips of Hordeumvulgare L. was markedly increased by replacing 10mM Na₂SO₄ inthe washing solution by K₂SO₄ with the same electrical conductivity.This increase was inhibited by both an uncoupler and an inhibitorof oxidative phosphorylation but not by ouabain. Potassium ionsdid not enhance Na⁺ efflux in the presence of a rapidly absorbedcounter anion, such as Cl^–, instead of . Efflux of ²²Na⁺ could also be enhanced by a low pH in theabsence of K⁺; this was prevented by uncouplers, but not byan inhibitor of the mitochondrial ATPase. It seems that K⁺ indirectly enhances Na⁺ efflux. It is suggestedthat metabolic K⁺ uptake in excess of the counter anion resultsin a proton gradient across the plasmalemma (acid outside) inducingH⁺/Na⁺ antiport.     

Function and contribution of the root tip in the induction of NO3- uptake along the barley root axis

The seminal roots of N-free-grown barley seedlings were ableto take up NO₃^– immediately upon initial exposure; theuptake rate in the tip was half of that in the older root zones(middle and base). A lag of 60 min was required in all rootzones before the uptake rates started to increase during inductionwith external NO₃^–. This increase could be prevented bythe addition of pFPA; we thus assume that additional NO₃^–transport proteins were synthesized during NO₃^– induction.During the time-course of NO₃^– induction different uptakerates were measured in morphologically different regions ofthe tip (1 mm segments) indicating a regulation of NO₃^–induction on a narrow local scale. In NO₃^– grown plants, NO₃^– uptake as well as NO₃^–content increased basipetally along the root axis concomitantlywith increasing vacuolization of the cells. Although NO₃^–uptake into the tip was only half of that into the older rootzones, this NO₃^– uptake was very important for the entireroot. Firstly, it provided the substrate for protein biosynthesisin the meristematic region: nitrate reductase activity and totalsoluble protein were highest in the first apical mm of the tip.Secondly, 3% of the NO₃^– taken up by the tip was foundin the base where it induced NO₃^– uptake: NO₃^– wastranslocated almost exclusively basipetally and as little as20nmolg^–1 root fr. wt. translocated from the tip weresufficient for acceleration of NO₃^– induction in the rootbase of N-free-grown plants. This clearly shows that the inductionof NO₃^– uptake does not depend exclusively on the availabilityof external NO₃^–, but can be mediated also with internallytranslocated NO₃^–.The root tip, therefore, may be consideredthe NO₃^– sensing region of the root. Key words: Barley, Hordeum vulgare L, internal NO₃^–, NO₃^– uptake, root zones