Radial Water and Solute Flows in Roots of Zea mays: II. ION FLUXES ACEOSS ROOT CORTEX

Unidirectional fluxes of Na⁺, K⁺, Cl^–, and phosphate weremeasured across a preparation of hollow cylinder of a segmentof maize root. Cation fluxes are 2–3 orders of magnitudelarger than those of the anions. From the Ussing flux ratio,it was concluded that cations are moving passively while anionsare pumped actively across the root. The anion pumps are acceleratedby the uncoupler DNP and inhibited by cyanide. It is suggestedthat they are coupled directly to the electron transport system,rather than to ATP. From analysis of the diffusion coefficientsof the ions it was concluded that radial ion movement in theroot cortex must be through, rather than between, the cells.     

Radial Water and Solute Flows in Roots of Zea mays: IV. ELECTRICAL POTENTIAL PROFILES ACROSS THE ROOT

Techniques have been developed for continuous recording of electricalpotential difference in maize root preparations. In this waythe continuous p.d. profile along the lateral axis of the rootcould be obtained. The features of the profile are resolvedin terms of the root morphology. Analysis of the p.d. profile indicates (a) that the phases withinthe root are electrically negative with respect to the bathingmedium, (b) that the vacuoles are positive relative to the cytoplasm,i.e. a p.d. exists across the tonoplast, (c) that all cytoplasmicphases are equipotential, which indicates a continuity withinand between the cortical and stelar symplasms, (d) that theextracellular space of the root is presumably only slightlyinfluenced by the concentration of the external medium sincethe p.d. profile within the root does not react to changes ofconcentration in the external medium, (e) that the potentialof the stelar vacuoles is negative relative to the corticalone and this is consistent with the accumulation of surplusions in the stelar vacuoles. The implications of the present findings to the elucidationof ion transport mechanism across the root are briefly discussed.     

Radial Water and Solute Flow in Roots of Zea mays: III. EFFECT OF TEMPERATURE ON THO AND ION TRANSPORT

THO influx, ³⁶Cl^– influx and efflux and ²²Na influx throughmaize cortex sleeves were assayed under different temperaturesranging from 5 to 40 °C. The highest Q¹⁰ and H values forTHO influx were found between 12 and 32 °C. ³⁶Cl effluxand ²²Na influx were almost temperature independent. ³⁶Cl influxwas greatly increased above 20°C. These results are consistentwith previous conclusions that water flow through maize sleevesis metabolically mediated and that chloride is actively pumpedinwards.     

Relationship of Transplasmalemma Redox Activity to Proton and Solute Transport by Roots of Zea mays

Transplasmalemma redox activity, monitored in the presence of exogenous ferricyanide stimulates net H⁺ excretion and inhibits the uptake of K⁺ and α-aminoisobutyric acid by freshly cut or washed, apical and subapical root segments of corn (Zea mays L. cv “Seneca Chief”). H⁺ excretion is seen only following a lag of about 5 minutes after ferricyanide addition, even though the reduction of ferricyanide occurs before 5 minutes and continues linearly. Once detected, the enhanced rate of H⁺ excretion is retarded by the ATPase inhibitors N,N′-dicyclohexylcarbodiimide, diethylstilbestrol, and vanadate. A model is presented in which plasmalemma redox activity in the presence of ferricyanide involves the transport only of electrons across the plasmalemma, resulting in a depolarization of the membrane potential and activation of an H⁺-ATPase. Such a model implies that this class of redox activity does not provide an additional and independent pathway for H⁺ transport, but that the activity may be an important regulator of H⁺ excretion. The 90% inhibition of K⁺ (⁸⁶Rb⁺) uptake within 2 minutes after ferricyanide addition can be contrasted with the 5 to 15% inhibition of uptake of α-aminoisobutyric acid. The possibility exists that a portion of the K⁺ and most of the α-aminoisobutyric acid uptake inhibitions are related to the ferricyanide-induced depolarization of the membrane potential, but that the redox state of some component of the K⁺ uptake system may also regulate K⁺ fluxes.     

Axial and Radial Hydraulic Resistance to Roots of Maize (Zea mays L.)

A root pressure probe was employed to measure hydraulic properties of primary roots of maize (Zea mays L.). The hydraulic conductivity (Lp_r) of intact root segments was determined by applying gradients of hydrostatic and osmotic pressure across the root cylinder. In hydrostatic experiments, Lp_r was constant along the segment except for an apical zone of approximately 20 millimeters in length which was hydraulically isolated due to a high axial resistance. In osmotic experiments, Lp_r decreased toward the base of the roots. Lp_r (osmotic) was significantly smaller than Lp_r (hydrostatic). At various distances from the root tip, the axial hydraulic resistance per unit root length (R_x) was measured either by perfusing excised root segments or was estimated according to Poiseuille's law from cross-sections. The calculated R_x was smaller than the measured R_x by a factor of 2 to 5. Axial resistance varied with the distance from the apex due to the differentiation of early metaxylem vessels. Except for the apical 20 millimeters, radial water movement was limiting water uptake into the root. This is important for the evaluation of Lp_r of roots from root pressure relaxations. Stationary water uptake into the roots was modeled using measured values of axial and radial hydraulic resistances in order to work out profiles of axial water flow and xylem water potentials.     

Mechanisms of Inhibition of Water Movement in Anaerobically Treated Roots of Zea mays L.

Changes in water flux (Jv) across detopped, 7-d-old, maize rootswere characterized during the initial 24 h of being made anoxicby exposure to an anaerobic nutrient solution. Suction (50 kPa)was applied to the xylem and samples of the xylem sap were collectedat intervals and the osmolality and ionic content were measured. Values of Jv through anoxic roots fell below those of aerobiccontrols 1 h after the equilibrium oxygen partial pressure inthe bathing medium dropped below 20 kPa (air = 20.6 kPa). Thereduction in Jv was due primarily to a nullification of thediurnal rhythm in hydraulic conductivity (Lp) that was measuredin aerobic roots. However, about one-quarter of the reductionin Jv could be accounted for by a smaller osmotic componentof the driving force () on water movement. The significance of changes in Jv in anoxic roots is discussedin terms of the reliability of estimates of Lp, the reflectioncoefficient () and . Key words: Anaerobiosis, hydraulic conductivity, osmotic potential, water     

Nitrogen Enhancement of Phosphate Transport in Roots of Zea mays L. : I. Effects of Ammonium and Nitrate Pretreatment

The effect of nitrogen status on phosphorous uptake and translocation was examined in 6-day-old dark-grown decapitated maize seedlings exposed to 25 micromolar phosphorous. Transfer to complete solutions containing 1 millimolar ammonium resulted in an increase in phosphorous uptake rate after 6 to 8 hours. The stimulus remained effective for at least 5.5 hours upon subsequent transfer to nitrogen-free solutions. Pretreatments for 16 hours with either nitrate or ammonium resulted in enhanced rates of subsequent phosphorous uptake and in enhanced translocation to the xylem of the exogenously supplied phosphorous. Both processes reached a plateau following pretreatment with 0.1 to 1.0 millimolar concentrations of either nitrogen ion. Further enhancement occurred with 10 millimolar nitrate, but not with 10 millimolar ammonium pretreatment. Although nitrogen pretreatments slightly increased the quantity of exogenous phosphorous retained in the root tissue, most of the extra phosphorous taken up by the nitrogen-pretreated seedlings was translocated to the xylem. The enhanced translocation, however, did not totally account for the increase in uptake implying a specific stimulation of the uptake process.     

Radial Movement of Cations across Aerenchymatous Roots of Zea mays Measured by Electron Probe X-Ray Microanalysis

The radial movements of Rb⁺ and Sr²⁺ as analogues for K⁺ andCa²⁺ were followed by electron probe X-ray microanalysis inaerenchymatous roots of maize (Zea mays L. cv. LG 11). The objectwas to determine the possible pathways by which ions can reachthe xylem when degeneration and lysis of much of the root cortexhas taken place during formation of numerous gas-filled spacesin aerenchymatous roots. After 1, 6 and 24 h uptake of Rb⁺ andSr²⁺ from a full strength nutrient solution containing K⁺ andCa²⁺, the distribution of these elements was examined. Transverseroot sections, prepared by cryostat sectioning and lyophilization,were used for electron probe X-ray microanalysis. If the cellwalls lining gas-filled spaces become suberized (as reportedin earlier literature), this development might be expected toretard ion movement, but we found that Rb⁺ or Sr²⁺ could migrateas readily in the radial wall residues remaining after corticalcell lysis, as in the walls of intact cortical cells. The distributionsof Rb⁺ and Sr²⁺ differed, however. The lack of a concentrationgradient for Rb⁺ across the root was compatible with its transportmainly in the symplast, constituted by occasional files of intactcortical cells bridging the gas-filled spaces. The evident concentrationgradient for Sr²⁺ was accounted for by its movement to the endodermisby the apoplastic pathway constituted by the walls of intactand lysed cells. Key words: Aeration, aerenchyma, cations, electron probe X-ray microanalysis, Zea mays     

Metabolic Adaption in Mature Roots of Salt-stressed Zea mays

Respiratory gas exchange and incorporation of ¹⁴C-leucine intoprotein were studied in proximal root segments from 25-day-oldmaize plants grown for the last ten days in 50 mM Na₂SO₄. ¹⁴C-leucineincorporation, and oxygen uptake in the presence of glucose,were as large in Na₂SO₄-grown tissues tested under saline conditionsas in tissues exposed to non-saline solutions throughout Thisadaptation was attributed to an increased metabolic capacityof Na₂SO₄-treated tissues, because these tissues, when returnedto non-saline solutions, evolved oxygen and incorporated ¹⁴C-leucinefaster than tissues exposed continuously to non-saline solutions. These changes are interpreted as a ‘compensation’for the inhibitory effects found when non-adapted tissues wereexposed to 50 mM Na₂SO₄. Moreover, we have related them to ultrastructuralchanges observed previously in xylem parenchyma cells of thesetissues, and to the possible involvement of these xylem parenchymacells in the re-absorption of sodium from the ascending xylemfluid Zea mays L., maize, salt-stress, respiration, protein synthesis     

Pyruvate Decarboxylase from Zea mays L. : I. Purification and Partial Characterization from Mature Kernels and Anaerobically Treated Roots

Pyruvate decarboxylase (PDC) was purified from mature, dry maize kernels and from roots of anaerobically treated maize seedlings and partially characterized. PDC was purified to a specific activity of 96 units per milligram protein from kernels and to 41 units per milligram protein from root. The subunit molecular masses were estimated to be 61,000 and 60,000 for kernel PDC and 59,000 and 58,000 for root PDC. The pH optimum for each enzyme was 5.8. Since the pH optimum is nearly one pH unit below the value reported for the cytoplasm of anaerobically metabolizing maize roots (pH 6.7 ± 0.2), we investigated the effects of pH 5.8 and 6.6 on the cooperative kinetics observed for PDC from each source. The maximum Hill coefficients (n_H) were much greater at each pH for the kernel PDC (pH 5.8, n_H = 2.5 and pH 6.6, n_H = 3.2) than for the root PDC (pH 5.8, n_H = 1.4 and pH 6.6, n_H = 1.8). The cooperative kinetics observed with respect to pyruvate were asymmetric. Potassium inhibited maize PDC and was competitive with pyruvate (root PDC K_i = 16 millimolar and kernel PDC K_i = 10 millimolar).     

Water Deficit and Inflorescence Development in Zea mays L.

A water deficit imposed during the period of terminal male inflorescenceinitiation and early development reduced both the growth rateand the mature size of that organ in Zea mays (cv. Iochief).Growth and development of the axillary shoots, the potentialfemale inflorescences, was inhibited during the episode of waterdeficit but promoted thereafter. As a result, plants which hadbeen subjected to a water deficit at that period produced 2–3mature cobs and relatively large axillary shoots at the lowernodes, whereas plants supplied with water throughout produceda single mature cob and relatively small axillary shoots. A water deficit imposed during other growth phases did not producethis response and, moreover, a further period of deficit imposedlater in development, following a deficit at the sensitive stage,inhibited the enlargement of the axillary shoots invoked bythe earlier deficit. It did not, however, inhibit the enhancedfloral development of those axillary shoots nor reverse theinhibition of tassel growth. The data are discussed in relation to correlative inhibitionin Zea mays.     

Possible Linkage between NADH-Oxidation and Proton Secretion in Zea mays L. Roots

A possible involvement of two different systems in proton translocationand the correlation of this factor to growth rates were measuredsimultaneously by means of a pH stat and an optical system.Ferricyanide, which can accept electrons at the plasmalemma,led to an immediate increase of net H⁺ -efflux but also decreasedroot growth rate. The reduced form, ferrocyanide, inhibitednet H⁺ -effluxwithout changing the growth rate. Thus, corn rootgrowth was not determined by proton secretion exclusively. Vanadatestrongly inhibited net H⁺ -efflux by the roots but did not preventthe stimulating effect of fcrricyanide. Moreover, the extentof enhancement of net H⁺ -effluxby ferricyanide was exactlythe same in vanadate pretreated as in untreated roots. Alcoholswere used to try to increase the intracellular NADH level throughthe action of the cytoplasmic alcohol dehydrogenase presentin the roots and coleoptiles. Alcohols, known to be substratesfor alcohol dehydrogenase such as propan- 1-ol, ethanol andbutan-l -ol increased net H⁺ -effluximmediately but methanoland secondary alcohols which are not substrates had no effecton proton secretion. The K_m values of alcohol dehydrogenasefor the alcohols correspond only partly to their effects onproton secretion. However, the specificlty observed suggeststhat increased H⁺ -efflux arose from reduction of endogenousNAD by ADH and consequent increased membrane NADH-oxidasc activitytrans locating protons and electrons out of the cells. Decreased oxygen concentrations slowed proton secretion at valuesfar higher than are necessary to saturate cytochrome c oxidase.The results of these experiments suggest two distinct systemscontributing to proton efflux. Key words: ADH, proton transport, redox chain     

Ion Transport to the Xylem in Aerenchymatous Roots of Zea mays L.

Aerenchyma was induced in the developing nodal (adventitious)roots of maize (Zea mays L. cv. LG11) in solution culture bytreatment with an atmosphere of 5% (v/v) oxygen (oxygen partialpressure 5.0 k Pa). Ion uptake by aerenchymatous and ordinary(non-aerenchymatous) roots was then compared to determine theeffect of degeneration of much of the cortex in aerenchymatousroots on radial ion movement to the xylem. Rates of uptake andtransport of phosphate, potassium and chloride were followedby labelling 4–12mm length segments of intact roots usingradioactive tracers. In some experiments, enhanced rates ofphosphate transport were induced by means of a divided rootsystem and nutrient deprivation. For all three nutrient ions,and over a range of concentration for phosphate (10–100mmol m^–3 and potassium (0·25–5·0 molm^–3 and with enhanced rates of transport, aerenchymatousroots were at least as effective as ordinary roots (per mm³of root) and sometimes more effective (per mm root length).These findings are discussed in relation to hypotheses concerningthe pathways for radial ion movement across the cortex in ordinaryand aerenchymatous roots. Correspondence to: Long Ashton Research Station, Long Ashton,Bristol BS18 9AF, U.K. Key words: Aerenchyma, ion transport, mineral nutrition, oxygen deficiency, radio-isotopic tracers, roots, structure, Zea mays     

Effects of Salinity on Water Transport of Excised Maize (Zea mays L.) Roots

The root pressure probe was used to determine the effects of salinity on the hydraulic properties of primary roots of maize (Zea mays L. cv Halamish). Maize seedlings were grown in nutrient solutions modified by additions of NaCl and/or extra CaCl₂ so that the seedlings received one of four treatments: Control, plus 100 millimolar NaCl, plus 10 millimolar CaCl₂, plus 100 millimolar NaCl plus 10 millimolar CaCl₂. The hydraulic conductivities (Lp_r) of primary root segments were determined by applying gradients of hydrostatic and osmotic pressure across the root cylinder. Exosmotic hydrostatic Lp_r for the different treatments were 2.8, 1.7, 2.8, and 3.4·10⁻⁷ meters per second per megapascals and the endosmotic hydrostatic Lp_r were 2.4, 1.5, 2.7, and 2.3·10⁻⁷ meters per second per megapascals, respectively. Exosmotic Lp_r of the osmotic experiments were 0.55, 0.38, 0.68, and 0.60·10⁻⁷ meters per second per megapascals and the endosmotic Lp_r were 0.53, 0.21, 0.56, and 0.54·10⁻⁷ meters per second per megapascals, respectively. The osmotic Lp_r was significantly smaller (4-5 times) than hydrostatic Lp_r. However, both hydrostatic and osmotic Lp_r experiments showed that salinization of the growth media at regular (0.5 millimolar) calcium levels decreased the Lp_r significantly (30-60%). Addition of extra calcium (10 millimolar) to the salinized media caused ameliorative effects on Lp_r. The low Lp_r values may partially explain the reduction in root growth rates caused by salinity. High calcium levels in the salinized media increased the relative availability of water needed for growth. The mean reflection coefficients of the roots using NaCl were between 0.64 and 0.73 and were not significantly different for the different treatments. The mean values of the root permeability coefficients to NaCl of the different treatments were between 2.2 and 3.5·10⁻⁹ meters per second and were significantly different only in one of four treatments. Cutting the roots successively from the tip and measuring the changes in the hydraulic resistance of the root as well as staining of root cross-sections obtained at various distances from the root tip revealed that salinized roots had mature xylem elements closer to the tip (5-10 millimeters) compared with the controls (30 millimeters). Our results demonstrate that salinity has adverse effects on water transport and that extra calcium can, in part, compensate for these effects.     

Leaf Extension in Zea mays: I. LEAF EXTENSION AND WATER POTENTIAL IN RELATION TO ROOT-ZONE AND AIR TEMPERATURES

The temperature of the roots and shoots of Zea mays plants werevaried independently of each other and the rates of leaf extensionand leaf water potentials were measured. Restrictions of leafextension occurred when root temperatures were lowered from35 to 0 °C, but leaf water potentials were lowered onlyat root temperatures below 5 °C. Similar changes in ratesof leaf extension were measured at air temperatures from 30to 5 °. Between 30 and 35 °C air temperature, in anunsaturated atmosphere, restrictions of leaf extension wereassociated with low leaf water potentials. It was concluded that, at root temperatures 5 to 35 °C,and shoot temperatures 5 to 30 °C, water stress was notthe main factor restricting the extension of Zea mays leaves.     

Gravitropism of Primary Roots of Zea mays L. at Different Displacement Angles

Primary roots of Zea mays were oriented at various angles fromthe vertical ranging from 99° to 1° and their subsequentbending analysed from filmed records. The maximum rate of bendingand the time before bending commenced both varied two-fold,but showed no correlation with the initial angle of tip displacement.Roots orientated to small initial angles (< 40°) oftenovershot the vertical and proceeded to oscillate around thisorientation, whereas roots oriented to large initial angles(> 60°) often failed to achieve the vertical. Roots inthis latter group resumed bending after an indeterminate time,or did so immediately after a second displacement of their tip,showing that they were not intrinsically unable to bend. Theapparently spontaneous resumption of bending after a temporaryplagiogravitropic phase is suggested as being due to noise inthe graviperception system in the root cap. The tips of rootsgrowing vertically downwards showed oscillatory bending movementsup to 10° either side of vertical. This angle correspondsto the minimum angle of displacement which induces gravitropicbending. Only when roots were oriented 10-20° from verticaldid they begin unequivocally to show a gravitropism since atsuch angles the deflection of their tips exceeded that due totheir natural oscillation.Copyright 1993, 1999 Academic Press Gravitropism, roots, Zea mays     

Transport and Metabolism of Kinetin-8-14C in Zea mays L. Roots

The movement of kinetin has been investigated in roots of Zeaseedlings, grown in the dark, using kinetin-8-¹⁴C. Segments (10 and 11 mm) with and without an apex were used andthe following results obtained: The transport of kinetin is polarized basipetally. Kinetin-8-¹⁴C is transported in roots without vascular tissue,but the amount transported is always lower than in roots withvascular tissue. Thin-layer chromatography showed that the molecule of kinetinis metabolized in the root segments, adenine being one of theproducts.     

Pressure-Induced Water and Solute Flow Through Plant Roots

Water and salt flows through detopped sunflower, tomato andred kidney bean roots under applied pressure were studied usinga pressure chamber. Values of J_v for these root systems weremeasured applying variable pressure on the root medium, andL_p calculated. The K, Na and Cl fluxes under applied pressure were comparedwith those in intact plants at the same water flow rates. Tento 100 times higher Na and Cl fluxes were observed through detoppedroots under pressure as compared to those in the unpressurized,intact plants. It is suggested that the roots under pressureare not completely analogous to intact plant roots, and thatpressure-induced flow may not be a reliable method of determiningcharacteristics of ion flow in roots in relation to water flow. Key words: Volume flow, Hydraulic conductivity, K selectivity     

Polyamine Content and Action in Roots of Zea mays L. in Relation to Aerenchyma Development

Roots of Zea mays L. developed more aerenchyma (cortical gas-filledspace) when partially deficient in oxygen (3 kPa) than whensupplied with air (20·8 kPa oxygen) in association withfaster production of ethylene (ethene). The possibility wastested that the additional ethylene production resulted fromdecreases in spermidine (spd) and spermine (spm) which share,with ethylene, a common precursor, S-adenosylmethionine. However,no decreases in spd and spm were seen in root tissue up to 4d-old. Removing oxygen completely also had little effect onspd and spm, but strongly suppressed both ethylene productionand aerenchyma formation. Partial oxygen shortage (3 kPa) increased the concentrationof putrescine (put), the precursor of spd and spm. This increasewas not a response to the extra ethylene formed by such rootssince ethylene treatment did no reproduce the effect. Applicationof inhibitors of put biosynthesis, difluoromethylarginine anddifluoromethylornithine, led to increased aerenchyma formation.Exogenous put inhibited the development of aerenchyma whilestimulating rather than inhibiting ethylene production, whentested in either air or 3 kPa oxygen. Thus, put appears to limitaerenchyma formation by suppressing ethylene action rather thanits production.Copyright 1993, 1999 Academic Press Ethylene, ethene, roots, aerenchyma, polyamines, oxygen shortage, anaerobiosis, environmental stress, Zea mays     

The Diversity of Archaea and Bacteria in Association with the Roots of Zea mays L.

The diversity of bacteria and archaea associating on the surface and interior of maize roots (Zea mays L.) was investigated. A bacterial 16S rDNA primer was designed to amplify bacterial sequences directly from maize roots by PCR to the exclusion of eukaryotic and chloroplast DNA. The mitochondrial sequence from maize was easily separated from the PCR-amplified bacterial sequences by size fractionation. The culturable component of the bacterial community was also assessed, reflecting a community composition different from that of the clone library. The phylogenetic overlap between organisms obtained by cultivation and those identified by direct PCR amplification of 16S rDNA was 48%. Only 4 bacterial divisions were found in the culture collection, which represented 27 phylotypes, whereas 6 divisions were identified in the clonal analysis, comprising 74 phylotypes, including a member of the OP10 candidate division originally described as a novel division level lineage in a Yellowstone hot spring. The predominant group in the culture collection was the actinobacteria and within the clone library, the a-proteobacteria predominated. The population of maize-associated proteobacteria resembled the proteobacterial population of a typical soil community within which resided a subset of specific plant-associated bacteria, such as Rhizobium- and Herbaspirillum-related phylotypes. The representation of phylotypes within other divisions (OP10 and Acidobacterium) suggests that maize roots support a distinct bacterial community. The diversity within the archaeal domain was low. Of the 50 clones screened, 6 unique sequence types were identified, and 5 of these were highly related to each other (sharing 98% sequence identity). The archaeal sequences clustered with good bootstrap support near Marine group I (crenarchaea) and with Marine group II (euryarchaea) uncultured archaea. The results suggest that maize supports a diverse root-associated microbial community composed of species that for the first time have been described as inhabitants of a plant-root environment.