Multiphasic Uptake of Sulfate by Barley Roots

Uptake of sulfate by excised barley roots increases upon their washing in aerated water or dilute CaCl₂ solutions. Washing increases the values for V_max and the sulfate concentrations required for transition between the lower phases, but the K_M-values remain essentially constant. At low sulfate concentrations, phase transitions do not occur in the absence of calcium or other divalent cations. These ions are about equally effective in enhancing short-term sulfate uptake. Phase transitions were not principally altered by sulfhydryl or protein reagents. These concentration-dependent transitions appear unrelated to temperature-dependent phase transitions as evidenced by similar multiphasic patterns at low and high temperature.     

Multiphasic Uptake of Amino Acids by Barley Roots

Concentration-dependence and other characteristics of uptake of ³H-labeled l -lysine, l -methionine and l -proline by excised roots of barley (Hordeum vulgare L.) were studied. Use of relatively short uptake and wash periods and low solute concentrations ensured good estimates of influx across the plasmalemma. Uptake in the range of 10^?7M– 6.3 × 10^?3M can be precisely represented by four or five phases of single, multiphasic mechanisms. The mechanisms appear to be relatively specific as judged from the competition by unlabeled analogues. Structural requirements for interaction of a compound with the uptake site for methionine are given, as are the effects of analogues on the phase pattern for this amino acid. There is no indication of separate uptake and transition sites for methionine or lysine. i.e. phase transitions seem in this case to be caused by binding of molecule(s) to the uptake site. Uptake, but not phase patterns, was highly pH-dependent. The optima were pH 5 for lysine, pH 3–5 (a broad peak) for methionine and about pH 5.5 for proline. Uptake of the three amino acids was strongly inhibited by 2,4-dinitrophenol. sulfhydryl reagents and deoxycholate.     

Ammonium and Potassium Uptake by Citrus Roots

Multiphasic kinetics were indicated for uptake of ammonium and potassium by intact cirtrus seedlings as measured by a continuous flow technique. Uptake at low concentration, below 10^?3M, was biphasis. The patterns for ammonium uptake by 60-day-old and 180-day-old seedlings were similar, but the rates of uptake per g dry weight of root were greater for the younger plants.     

Ammonium Uptake by Rice Roots (III. Electrophysiology)

The transmembrane electrical potential differences ([delta][psi]) were measured in epidermal and cortical cells of intact roots of 3-week-old rice (Oryza sativa L. cv M202) seedlings grown in 2 or 100 [mu]M NH4+ (G2 or G100 plants, respectively). In modified Johnson's nutrient solution containing no nitrogen, [delta][psi] was in the range of -120 to -140 mV. Introducing NH4+ to the bathing medium caused a rapid depolarization. At the steady state, average [delta][psi] of G2 and G100 plants were -116 and -89 mV, respectively. This depolarization exhibited a biphasic response to external NH4+ concentration similar to that reported for 13NH4+ influx isotherms (M.Y. Wang, M.Y. Siddiqi, T.J. Ruth, A.D.M. Glass [1993] Plant Physiol 103: 1259-1267). Plots of membrane depolarization versus 13NH4+ influx were also biphasic, indicating distinct coupling processes for the two transport systems, with a breakpoint between two concentration ranges around 1 mM NH4+. The extent of depolarization was also influenced by nitrogen status, which was larger for G2 plants than for G100 plants. Depolarization of [delta][psi] due to NH4+ uptake was eliminated by a protonophore (carboxylcyanide-m-chlorophenylhydrazone), inhibitors of ATP synthesis (sodium cyanide plus salicylhydroxamic acid), or an ATPase inhibitor (diethylstilbestrol). The results of these observations are discussed in the context of the mechanisms of NH4+ uptake by high- and low-affinity transport systems operating across the plasma membranes of root cells.     

Kinetics of Potassium and Magnesium Uptake by Intact Soybean Roots

The kinetics of uptake of K⁺ and Mg²⁺ were studied by using intact soybean [Glycine max (L.) Merr. cv. Amsoy] roots. Uptake of K⁺ in the concentration range 1.29 × 10^?5 to 1.82 × 10^?3 M can be represented by two phases of a single, multiphasic mechanism. Similarly, uptake of Mg²⁺ in the concentration range 4.10 × 10^?6 to 2.49 × 10^?4M was biphasic.     

Uptake of Sulfate by Roots and Leaf Slices of Barley: Mediated by Single, Multiphasic Mechanisms

The uptake of 10^?1M–2.5 × 10^?1M sulfate by roots and leaf slices of barley can be described by a single isotherm having, respectively, 8 and 5 phases with regularly increasing kinetic constants. Each phase covers a limited concentration range and obeys Michaelis-Menten kinetics. The uptake of sulfate is proposed to be rate-limited by a single mechanism or structure which is located in the plasmalemma (or cytoplasm) and which changes characteristics at certain discrete external concentrations (inflection points). Examination of published data indicates that the uptake of other inorganic ions by higher plant cells is also mediated by single, multi-phasic mechanisms.     

Multiphasic Uptake of Sulfate by Barley Roots I. Effects of Analogues, Phosphate, and pH

For sulfate uptake by barley roots, competition studies reveal that uptake and phase transitions are caused by interaction of ions with separate sites on or in the plasmalemma. Uptake is competitively, and unequally, inhibited by sulfate analogues but not by other divalent anions. In contrast, divalent phosphate and di- and trivalent pyrophosphate are equally effective in causing transitions. Phosphate is taken up mainly or entirely as H₂PO₄^? by a similar but separate multiphasic mechanism. At pH 8, sulfate uptake is mediated by fewer phases than at low and intermediate pH.     

Multiphasic Hexose Uptake in Chlorella

The model proposed by E. Komor and W. Tanner for hexose proton cotransport in Chlorella (Planta 123: 195–198. 1975) is shown to be incorrect. Their data cannot represent hexose uptake via a protonated and a deprotonated form of the carrier, but may be precisely represented by a single bi- or triphasic mechanism.     

Uptake of Proteins by Plant Roots

The patterns of uptake of fluorescein-labelled lysozyme (Fl-lysozyme) by barley, maize, onion, tomato and vetch are similar as revealed by fluorescence microscopy. Penetration of the root cap and through the epidermis into the cortex increases with time of exposure and decreases with higher salt concentrations. In fact, one molar ethylammonium chloride can remove most of the absorbed protein from treated roots and the space observed to be stained by Fl-lysozyme in this manner can be visualized as “free space”. Results with sterile and non-sterile barley roots were indistinguishable. At low ionic strength, Fl-lysozyme can penetrate cells and complex with nucleoli. Such cell protoplasts appear “coagulated”. Uptake results with fluorescein per se were unlike those with protein. The uptake of a much larger molecule, ferritin, is confined to the epidermis and root cell walls. Localized, absorbed protein and root growth inhibition by basic proteins have yet to be related.     

Effect of Phloem-Translocated Malate on NO(3) Uptake by Roots of Intact Soybean Plants

In soybean (Glycine max L. Merr. cv Kingsoy), NO₃⁻ assimilation in leaves resulted in production and transport of malate to roots (B Touraine, N Grignon, C Grignon [1988] Plant Physiol 88: 605-612). This paper examines the significance of this phenomenon for the control of NO₃⁻ uptake by roots. The net NO₃⁻ uptake rate by roots of soybean plants was stimulated by the addition of K-malate to the external solution. It was decreased when phloem translocation was interrupted by hypocotyl girdling, and partially restored by malate addition to the medium, whereas glucose was ineffective. Introduction of K-malate into the transpiration stream using a split root system resulted in an enrichment of the phloem sap translocated back to the roots. This treatment resulted in an increase in both NO₃⁻ uptake and C excretion rates by roots. These results suggest that NO₃⁻ uptake by roots is dependent on the availability of shoot-borne, phloem-translocated malate. Shoot-to-root transport of malate stimulated NO₃⁻ uptake, and excretion of HCO₃⁻ ions was probably released by malate decarboxylation. NO₃⁻ uptake rate increased when the supply of NO₃⁻ to the shoot was increased, and decreased when the activity of nitrate reductase in the shoot was inhibited by WO₄²⁻. We conclude that in situ, NO₃⁻ reduction rate in the shoot may control NO₃⁻ uptake rate in the roots via the translocation rate of malate in the phloem.     

Ammonium Uptake by Rice Roots (I. Fluxes and Subcellular Distribution of 13NH4+)

The time course of 13NH4+ uptake and the distribution of 13NH4+ among plant parts and subcellular compartments was determined for 3-week-old rice (Oryza sativa L. cv M202) plants grown hydroponically in modified Johnson's nutrient solution containing 2,100, or 1000 [mu]M NH4+ (referred to hereafter as G2, G100, or G1000 plants, respectively). At steady state, the influx of 13NH4+ was determined to be 1.31, 5.78, and 10.11 [mu]mol g-1 fresh weight h-1, respectively, for G2, G100, and G1000 plants; efflux was 11, 20, and 29%, respectively, of influx. The NH4+ flux to the vacuole was calculated to be between 1 and 1.4 [mu]mol g-1 fresh weight h-1. By means of 13NH4+ efflux analysis, three kinetically distinct phases (superficial, cell wall, and cytoplasm) were identified, with t1/2 for 13NH4+ exchange of approximately 3 s and 1 and 8 min, respectively. Cytoplasmic [NH4+] was estimated to be 3.72, 20.55, and 38.08 mM for G2, G100, and G1000 plants, respectively. These concentrations were higher than vacuolar [NH4+], yet 72 to 92% of total root NH4+ was located in the vacuole. Distributions of newly absorbed 13NH4+ between plant parts and among the compartments were also examined. During a 30-min period G100 plants metabolized 19% of the influxed 13NH4+. The remainder (81%) was partitioned among the vacuole (20%), cytoplasm (41%), and efflux (20%). Of the metabolized 13N, roughly one-half was translocated to the shoots.     

Manganese Uptake by Excised Oat Roots

Uptake of ⁵⁴Mn by excised oat roots from dilute manganese chloridesolutions has been investigated. The time-course of uptake hasbeen analysed into the customary but somewhat arbitrary fastand slow phases. Uptake is not metabolic in either of these.The fast phase (‘exchangeable’ manganese) is essentiallycomplete in about 30 minutes and represents the attainment ofequilibrium in a process of ion-exchange. It is shown that analysesappropriate for enzyme kinetics cannot be applied in this situation,and an alternative formulation is based on Donnan equilibration,taking account of the selectivity of the ion exchanger towardsdifferent counter-ions; the predictions of this latter theoryare compared with the experimentally determined uptake. Theslow phase (‘absorbed’ manganese) may also involveexchange sites, either chemically different from, or more difficultof access than, those involved in the fast phase, or both. Equilibriumwas certainly not reached in three hours in this slow-phaseprocess. Release of manganese, taken up by the roots from manganese chloridesolutions, into calcium chloride solutions does not seem tobe simply the reversal of uptake, particularly with very dilutesolutions. This is particularly shown by the kinetics of uptakeand release, uptake being a much faster process than release.Manganese may transfer from the first phase to the second phase,but there is no evidence that uptake by the roots proceeds inseries from first to second phase. It is considered more likelythat the two phases function independently, linked by the surroundingsolution.     

Boron Uptake by Excised Barley Roots

Active uptake of boron (B) by excised barley roots is linear with time for at least 1.5 h. Although no evidence was found for accumulation of B against a concentration gradient. this component of B uptake does satisfy other criteria for an active transport process. Transport is inhibited by 0.05 mM 2,4-dinitrophenol, 0.05 mM azide, 5 mM arsenate and 5 mM dicoumarol. Also, uptake is temperature-sensitive, being nil at 2°C and maximal at 34 to 38°C. Boron uptake by barley roots increases with time when they are washed in aerated 0.5 mM CaSO₄ solution. A double reciprocal plot of the B uptake data manifests a series of phases separated by sharp transitions or “jumps”, and is compatible with the concept of multiphasic uptake mechanisms. Kinetic constants and transition points for the various phases were calculated accordingly. The fit of these data was compared statistically to three other relevant models, viz, the dual model, the “single + diffusion” model (a Michaelis–Menten term and a diffusion term), and the negative cooperativity model. In each case, the data were better represented by the multiphasic model.     

Uptake of Iodide by Excised Bean Roots

Mesophyll cells of leaf slices of bean (Phaseolus vulgaris L.) absorb six to ten times more K⁺ than Rb⁺ from 0.1 mM single chlorides of these cations. Absorption of ⁴²K⁺ from 0.1 mM⁴²KCl is much more inhibited by low concentrations of Rb₂SO₄ than by K₂SO₄. The isotherm for K⁺ absorption is biphasic in the range 0.1–1.1 mM, and K⁺ is more effective than Rb⁺ in causing transition from phase 1 to phase 2.     

Characteristics of Zinc Uptake by Barley Roots

The linear uptake of zinc by excised barley roots (Hordeum distichon L.) in the time range from 20–120 min is not continued over periods of 20–28 h. In concentration dependent uptake experiments with intact barley roots three phases in the range up to 1.38 mM zinc could be detected independent of the tested uptake period. The kinetic constants increased with higher phases and the transition points were lowered with increasing time. The presence of copper did not inhibit the uptake of zinc competitively. On the contrary a slight stimulation in the uptake rates was observed indicating an interaction with the transition site. It is concluded that zinc and copper are taken up by separate mechanisms.     

Fatty Acid Composition and Nitrate Uptake of Soybean Roots during Acclimation to Low Temperature

Fatty acid composition of old and new roots was determined for soybeans (Glycine max [L.] Merr. cv Ransom) at root-zone temperatures of 14, 18, and 22°C during a 26-day period. New roots had a greater concentration of polyunsaturated fatty acids than old roots. The ratio of polyunsaturated to saturated fatty acid concentration in new roots exposed to 14 and 18°C peaked at 16 days and declined, while the corresponding ratio in old roots increased throughout the treatment period. Apparently the response of fatty acid composition in old and new roots to low temperature was mediated by tissue aging or differentiation. These findings were contrary to the concept that modifications in fatty acid composition remain constant at lower temperatures.

The function of root tissues exposed to lower temperature was evaluated with respect to the ability of the root systems to absorb NO₃⁻. Over the relatively long periods of exposure, the ability of whole root systems to absorb NO₃⁻ was similar at cool and warm temperatures. The effect of cool temperature on functioning of roots appeared to involve reductions in the rates of initiation and differentiation of young root tissues rather than changes in membrane permeability related to alteration of fatty acid composition.

     

Ammonium Uptake by Rice Roots (II. Kinetics of 13NH4+ Influx across the Plasmalemma)

Short-term influxes of 13NH4+ were measured in intact roots of 3-week-old rice (Oryza sativa L. cv M202) seedlings that were hydroponically grown at 2, 100, or 1000 [mu]M NH4+. Below 1 mM external concentration ([NH4+]0), influx was saturable and due to a high-affinity transport system (HATS). For the HATS, Vmax values were negatively correlated and Km values were positively correlated with NH4+ provision during growth and root [NH4+]. Between 1 and 40 mM [NH4+]0, 13NH4+ influx showed a linear response due to a low-affinity transport system (LATS). The 13NH4+ influxes by the HATS, and to a lesser extent the LATS, are energy-dependent processes. Selected metabolic inhibitors reduced influx of the HATS by 50 to 80%, but of the LATS by only 31 to 51%. Estimated values for Q10 (the ratio of rates at temperatures differing by 10[deg]C) for HATS were greater than 2.4 at root temperatures from 5 to 10[deg]C and were constant at approximately 1.5 between 5 and 30[deg]C for the LATS. Influx of 13NH4+ by the HATS was insensitive to external pH in the range from 4.5 to 9.0, but influx by the LATS declined significantly beyond pH 6.0. The data presented are discussed in the context of the kinetics, energy dependence, and the regulation of ammonium influx.     

Micronutrient Cation Sorption by Roots and Uptake by Plants

The sorption of ferric iron, copper, zinc and manganese by wheatseedling roots and by discs of cellulose filter paper was measured.The magnitude of sorption at pH 5-0 was Fe(III) > Cu(II)> Zn(II) > Mn(II). Sorption of Cu(II), Zn(II) and Mn(II)increased with increasing pH whilst sorption of Fe(III) decreased.The patterns of sorption are discussed in the light of our knowledgeof the hydrolysis of the metal ions. It is suggested that metalsadsorbed on root surfaces may be remobilized by organic ligandswhich leak from the root cells. Where an external liquid diffusionpath away from the root does not exist, soluble metal ligandcomplexes might accumulate in the water free space and superficialwater film of the root, thus facilitating their uptake intoroot cells and translocation within the plant. Under such conditionsthe amounts of metal translocated to the shoots of wheat seedlingsare shown to be related to the amounts of metal adsorbed bytheir roots. Key words: Adsorption, Micronutrients, Roots