A New Approach to Understanding the Calcifuge Habit of Plants

Growth rate of the calcifuge plants Carex pilulifera, Deschampsiaflexuosa, Holcus mollis, Luzula pilosa, Nardus stricta, andVeronica officinalis, transplanted into an Ordovician limestonesoil of pH 8, increased by two to three times on addition of5 mol m^-3 of CaHPO₄ compared to untreated conditions. For Galiumsaxatile, however, P treatment was lethal and growth was possibleonly in soil supplied with Fe(III) citrate, which had littleor no effect on growth of the other six species. Phosphate treatmentof the limestone soil greatly increased plant uptake of P, whereasP concentration of shoots from untreated soil was very low andprobably highly deficient, compared to plants of field siteorigin. From this and two other recent studies it is now possibleto conclude that the calcifuge habit of plants, at least underclimatic conditions prevailing in northern Europe, is most oftendue to an inability of such plants to render the native phosphateof limestone soils available to plant uptake. Out of ten calcifugespecies tested, only one exception to this rule was identified.Copyright1994, 1999 Academic Press Carex pilulifera, Deschampsia flexuosa, Galium saxatile, Holcus mollis, Luzula pilosa, Nardus stricta, Veronica officinalis, calcifuge plants, phosphorus, iron, limestone soil, limiting factors     

Soluble inorganic tissue phosphorus and calcicole-calcifuge behaviour of plants

BACKGROUND AND AIMS: Natural and semi-natural, non-fertilized calcareous soils are consistently low in soluble and easily exchangeable phosphate. An over-utilization, or possibly an immobilization, of inorganic P in the tissues of calcifuge plants may take place, if such plants are forced to grow on a calcareous soil, though this has not been experimentally demonstrated. The objectives of this study are, therefore, to elucidate if calcifuge plants, when forced to develop on a calcareous soil, not only have lower total P (Ptot) concentrations in their leaves than calcicole plants grown on such soil, but also a lower proportion of Ptot as water-soluble, inorganic phosphate. Such differences may be of importance in understanding the calcicole-calcifuge behaviour of plants. MATERIALS AND METHODS: Plants of five calcicole and five calcifuge herbs and three calcicole and three calcifuge grasses were cultivated in a glasshouse on a moderately acid Cambisol and a calcareous Rendzic Leptosol using seeds of wild populations from southern Sweden. The calcifuges were: Corynephorus canescens, Deschampsia flexuosa, Holcus mollis, Digitalis purpurea, Lychnis viscaria, Rumex acetosella, Scleranthus annuus and Silene rupestris. The calcicoles were: Melica ciliata, Phleum phleoides, Sesleria caerulea, Arabis hirsuta, Sanguisorba minor, Scabiosa columbaria, Silene uniflora ssp. petraea and Veronica spicata. KEY RESULTS: At harvest, calcifuges had much lower leaf tissue concentrations of Ptot and Pi than calcicoles when grown on the calcareous soil, and biomass production of the calcifuges was poor on this soil. Moreover, the calcifuge herbs had, on average, a lower proportion of their Ptot as Pi than had the calcicole herbs. The calcifuge herbs were also unable to avoid excessive uptake of Ca from the calcareous soil. The calcifuge grasses maintained a similar proportion of Ptot as Pi as the calcicole grasses, but their growth was still poor on the calcareous soil. CONCLUSIONS: On calcareous soil, very little Pi in the tissues of calcifuge herbs is, at any time, available for use in various physiological functions. This is of importance to their photosynthesis, growth, competition and final survival on such soils.     

The Effects of Soil Moisture on Structural and Biomass Characteristics of Four Salt Marsh Plants

In a controlled greenhouse experiment young Deschampsia cespitosa,Grindelia integrifolia, Distichlis spicata and Salicornia virginicaplants were subjected to dry, field capacity, and saturatedsoil conditions. Plant height, stem diameter, stem density,number of leaves, number and length of internodes, and numberof primary and secondary branches varied among the three treatments.The quantity of aerenchyma in S. virginica was greatest in thesaturated treatment. In G. integrifolia the amount of secondaryxylem was greatest in the dry treatment. Maximum above- andbelow-ground biomass occurred under field capacity conditionsfor the four species. Root to shoot ratios of D cespitosa andS. virginica were not affected by changes in soil moisture whilethat of D. spicata was lowest in the saturated treatment andthat of G. integrifolia was lowest in the dry treatment. Key words: Salt marsh, soil moisture, plant structure     

An Experimental Study of Calcium Acquisition and its Effects on the Calcifuge Moss Pleurozium schreberi

In a field experiment to investigate the sources and effectson growth of Ca in the calcifuge moss Pleurozium schreberi,significant quantities of Ca reached the growing shoot apicesfrom a CaCO₃ layer placed on the mineral soil surface Top applicationsof 0.5 and 5 mol m^–3 CaCl₂ raised the exchangeable andintracellular Ca concentrations and displaced natural exchangeableK and Mg The 5 mol m^–3 CaCl₂ treatment also caused a significantreduction in intracellular Mg indicating that Mg uptake is dependenton an initial exchange step No growth differences were notedbetween treatments, possibly because ionic changes had not reacheda detrimental level within the 28 weeks of the experiment ina second experiment, shoot apices of Pleurozium schreberi, Pseudoscleropodiumpurum and Calliergon cuspidatum were grown on nylon gauze underintermittent distilled-water mist At weekly intervals the shootswere saturated with CaCl₂ solutions providing factorial combinationsof Ca and pH Growth of C cuspidatum and P purum from chalk soilwas reduced at high (0.01) Ca concentration whereas Pleuroziumschreberi and Pseudoscleropodium purum from acidic clay wereunaffected The pH treatments did not significantly affect mossgrowth Initial tissue levels of K and Mg were lower in the mossesfrom chalk and it is suggested that the CaCl₂ treatments causednutrient deficiencies in these plants Mosses from acidic soilcontained less exchangeable Ca than the chalk plants and grewpoorly in the absence of CaCl₂, perhaps due to the developmentof Ca deficiency Bryophyte growth, calcium uptake, pH, mineral nutrition, Pleurozium schreberi, Pseudoscleropodium purum, Calliergon cuspidatum     

Photosynthesis and Transpiration in Rice as Influenced by Soil Moisture and Air Humidity

The paper describes the effect of soil moisture content andair humidity on CO₂ exchange (P_N), CO₂ diffusion resistance(Cr) and transpiration (E) in four varieties of japonica rice(Oryza sativa L.). A decrease in soil moisture content reducedthe rate of photosynthesis to a varying degree in the varieties.Reduction in photosynthesis was attributed to increase in Cr.The effect of low soil moisture on photosynthesis and CO₂ diffusionwas further intensified by decrease in air humidity. By maintaininga high humidity in the air around the leaves however, the effectof soil moisture deficiency was reduced considerably, exceptin Rikuto Norin 21 which was very sensitive to soil-moisturedeficiency alone. Dryness of the air enhanced the transpirationrate, although the increase was relatively less in the plantsfacing a simultaneous water crisis at the root surface. In plantsgrowing under flooded conditions, a decrease in air humiditycaused a slight depression in P_N despite the simultaneous decreasein Cr. Oryza sativa L., rice, photosynthesis, transpiration, diffusion resistance, soil moisture, air humidity     

The Effect of Sulphur Dioxide on the Growth of Lolium perenne L., Lolium multiflorum Lam., Dactylis glomerata L., and Phleum pratense L.

Lockyer, D. R. 1985. The effect of sulphur dioxide on the growthof Lolium perenne L., Lolium multiflorum Lam., Dactylis glomerataL., and Phleum pratense L.?J. exp. Bot. 36: 1851-1859. Fouragriculturally important grasses, Lolium perenne L., Loliummultiflorum Lam., Dactylis glomerata L. and Phleum pratenseL. were exposed to sulphur dioxide (SO₂) in a system of exposurechambers. The plants were exposed for a total of 43 d to meanconcentrations of SO₂ in the air of 0,87 or 448 (µg m^–3and herbage was harvested twice. All four grasses showed chloroticlesions after exposure to the highest concentration of SO₂.The effect of SO₂ on the yield of herbage was statisticallysignificant only at the second harvest and at the highest concentration;the dry weights of shoots of D. glomerata and L. perenne werereduced by 33% and 16% respectively. Significant effects ofSO₂ were also found on the 'transpiration coefficients' measuredfor D. glomerata and P. pratense. The grasses differed in theiruptake of sulphur from the atmosphere but this was not relatedto their sensitivity to SO₂. Total–S concentration inthe shoots of L. perenne, L. multiflorum and D. glomerata increasedalmost linearly in response to increasing SO₂ concentration;with P. pratense only the highest SO₂ concentration raised total-Sabove the level in control plants. These increases were almostentirely due to the accumulation of sulphate–S. Key words: Sulphur diozide, Lolium perenne, Lolium multiflorum, Dactylis glomerata, Phleum pratense     

Soil Amendments Affecting Nickel and Cobalt Uptake by Berkheya coddii: Potential Use for Phytomining and Phytoremediation

Plants with inordinately high concentrations of heavy metals(‘hyperaccumulators’) can be used for phytoremediation(removal of contaminants from soils) or phytomining (growinga crop of plants to harvest the metals). Pot trials were usedto investigate the effects of MgCO₃, CaCO₃, sulphur, chelatingagents (NTA, DTPA, EDTA) and acid mine tailings on nickel andcobalt uptake by the South African nickel hyperaccumulator Berkheyacoddii. Plants were grown in a nickel-rich ultramafic (‘serpentine’)soil diluted with pumice. Both MgCO₃and CaCO₃caused significantdecreases in the uptake of both metals, as well as decreasingtheir solubility in the soil. After the addition of MgCO_3,therewas a significant increase in soil pH, so the reduction in plant-metaluptake could not be solely attributed to the action of magnesiumalone. Since CaCO₃had no significant effect on soil pH, thisindicated that calcium inhibits the uptake of both cobalt andnickel. All three chelating agents caused a significant reductionin plant uptake of nickel, despite increasing the solubility(plant availability) of these elements in the soil. Cobalt uptakewas unaffected. Sulphur, and the addition of acid mine tailings,caused a highly significant increase in nickel and cobalt uptake,relative to the controls. Sulphur could be used as a low-costsoil amendment to enhance the metal uptake of crops grown onultramafic soils. Thus, land management procedures would enhancephytoremediation and phytomining operations for nickel and cobalt.Copyright1999 Annals of Botany Company Nickel, cobalt, phytoremediation, phytomining.     

Plant Seeds as Mineral Nutrient Resource for Seedlings--A Comparison of Plants from Calcareous and Silicate Soils

Mineral nutrients of seeds constitute a significant source ofessential elements to seedlings and developing individuals ofvascular plants. In spite of their potential ecological significance,seed nutrient pools have attracted little attention with respectto calcifuge–calcicole behaviour of plants. The objectivesof this study were, therefore, to compare concentrations of13 macro- and micronutrients (K, Rb, Mg, Ca, Mn, Fe, Co, Cu,Zn, Mo, B, P and S) in seeds and leaves of 35 mainly herbaceousvascular plant species growing on both limestone (calcareous)and silicate (non-calcareous) soils. Concentrations of Rb andCo in seeds of plants originating from limestone soils were,on average, about half of those from silicate soils. Concentrationsof Mn, Mg, Zn and P of seeds were, or tended to be, lower orslightly lower in limestone-soil plants, whereas mean Ca andMo concentrations were higher. Comparing seed and leaf concentrationsof the same species from limestone and silicate soils generallydemonstrated a high P enrichment ratio, but a particularly lowK enrichment ratio in seeds, valid for both types of soil. Itwas also apparent that Fe and Mn, micronutrients which are lessreadily solubilized and taken up by plants on limestone soils,had significantly higher seed:leaf concentration ratios in plantsfrom limestone than from silicate soils, whereas the oppositewas true for Ca. This indicates a ‘strategy’ tosatisfy the demand of seedlings for elements which are lessreadily available in the soil.Copyright 1998 Annals of BotanyCompany Seed, leaf, plant, nutrient, content, calcareous, silicate, acid, soil.     

Studies with Liatris spicata Willd. 1. Effect of Temperature on Sprouting, Flowering and Gibberellin Content

Dormancy was induced during storage of Liatris spicata cormsgrown in Israeli summer conditions, but plants left in soilcontinued vegetative growth. Corms of winter-grown plants sproutedfreely. Treatment with GA₃ restored both sprouting and floweringin summer-grown corms, but in winter corms GA₂ was effectiveonly after corms were stored at low temperature. All the plantsflowered after 4 weeks at 2 °C and GA³ treatment. The content of gibberellins in the main bud of freshly excavatedcorms decreased during the first 18 d of storage but increasedto the initial level after 4 months of cold storage. The numberof flowering stems increased to 2.5 per corm when corms werecold-stored up to 75 d, but decreased with a longer storage. Liatris spicata, dormancy, flowering, gibberellin, sprouting     

Phosphorus Deficiency Impairs Early Nodule Functioning and Enhances Proton Release in Roots of Medicago truncatula L.

The effect of phosphorus supply (1–15 µM) on protonrelease and the role of P in symbiotic nitrogen fixation inmedic (Medicago truncatula L. ‘Jemalong’) was investigated.As P concentration in the nutrient solution increased, shootand root growth increased by 19 and 15%, respectively by day35, with maximal growth at 4 µM P. A P concentration of15 µM appeared to be toxic to plants. Phosphorus supplyhad no influence on nodule formation by day 12 but increasednodule number by day 35. Nitrogenase activity was estimatedby in situ measurement of acetylene reduction activity (ARA)in an open-flow system. During the assay, a C₂H₂-induced declineof ARA was observed under all P concentrations except 4 µM.Specific ARA (per unit nodule weight) doubled when P supplywas increased from 1 to 8 µM. This effect of P was muchgreater than the effects of P on nodulation and host plant growth.Concentrations of excess cations in plants decreased with increasingP concentration in the nutrient solution. Phosphorus deficiencystimulated uptake of excess cations over anions by the plantsand hence enhanced proton release. The results suggest thatP plays a direct role in nodule functioning in medic and thatP deficiency increases acidification which may facilitate Pacquisition. Copyright 2001 Annals of Botany Company Medicago truncatula L. (medic), P deficiency, C₂H₂-ID, nitrogenase activity, proton release, cation-anion balance, open-flow system     

Nutrient Relations of Groundsel (Senecio vulgaris) Infected by Rust (Puccinia lagenophorae) at a Range of Nutrient Concentrations II. Uptake of N, P and K and Shoot-Root Interactions

Groundsel (Senecio vulgaris), healthy or infected with rust,Puccinia lagenophorae, was grown at a range of nutrient concentrationsin sand culture. Specific absorption rates calculated on thebasis of root dry weight (SAR_W) were greater in rusted thancontrol groundsel for nitrogen, potassium and phosphorus. Whilethe magnitudes of these stimulations varied, they occurred acrossthe whole range of nutrient concentrations. By contrast, specificabsorption rate on the basis of root length (SAR_L) were littlechanged by rust at any external nutrient concentration; SAR_Lfor phosphate and potassium were slightly reduced when nutrientswere freely available. Water flux per unit dry root weight and length was stimulatedby rust because transpiration per unit leaf area was more rapidin infected plants after fungal sporulation. However, water-fluxand the rate of uptake of nutrients were correlated only whenexpressed on the basis of root weight and increased transpirationdid not appear to be the mechanism underlying increased rootactivity. Rather, increased SAR_W for N, P and K could very largelybe attributed to increased shoot demand per unit root, whichresulted from the higher shoot: root (S: R) ratios of infectedindividuals. Changes in S: R accounted for 92, 81 and 57% oftotal variation in SAR_W for K, P and N respectively. Greatervalues for SAR_W were possible because specific root length (SRL)increased, producing more functional root per unit root weight.The lack of stimulation in SAR_L in response to rust could beexplained since the higher SRL of infected plants resulted instable values of shoot weight per unit root length, i.e. shootdemand was not increased by infection on this basis. Senecio vulgaris, Puccinia lagenophorae, rust infection, nutrient uptake, water uptake, shoot: root interactions     

Soil O2 and CO2 Effects on Apparent Cell Viability for Roots of Desert Succulents

Roots of desert succulents occupy the upper layers of porous,well-aerated soils. However, roots of Agave deserti, Ferocactusacanthodes, and Opuntia ficus-indica all tolerated many daysof soil anoxia; 0% O₂ in the soil gas phase for 30 d reducedthe fraction of cells taking up the vital stain neutral red,an average of only 18% for the cortex and 6% for parenchymacells within the stele of perennial established roots. Ephemeralrain roots, induced by watering as branches on the establishedroots, were more susceptible to 0% O₂ in the soil gas phase;19 d abolished stain uptake for cortical cells and 32 d forstelar parenchyma cells. Soil CO₂ levels above the 0.1% observedin the root zone in the field rapidly reduced uptake of neutralred; the fraction of cortical cells taking up the stain decreased30% in 10 h at 0.5% CO₂ and was abolished in 9 h at 2% and 7h at 10% CO₂ averaged for the three species. Rain roots weresomewhat more susceptible than established roots to elevatedsoil CO₂ levels, and stelar parenchyma cells were much lesssusceptible than were cortical cells. When uptake of the vitalstain was abolished by elevated soil CO₂, no anatomical evidenceof cellular damage was observed. For A. deserti exposed to 2%CO₂, the pH of macerated root tissue decreased about 0.35 pHunit over 10 h; CO₂ apparently entered the cells, lowered theintracellular and/or cell wall pH, and prevented the accumulationof neutral red. Elevated soil CO₂ also inhibits root respirationfor the three desert succulents considered. Hence, the restrictionof such species to porous soils may reflect the relatively rapidinhibiting effects of elevated soil CO₂ levels rather than arequirement for high soil O₂ levels, consistent with the observationthat desert soils tend to have low gas-phase CO₂ levels near0.1% compared with 1% or more in the root zone of non-desertspecies. Key words: Agave deserti, Ferocactus acanthodes, neutral red, Opuntia ficus-indica, pH     

Cluster Roots in Casuarinaceae: Role and Relationship to Soil Nutrient Factors

N₂-fixing actinorhizal trees in the family Casuarinaceae areeconomically of great interest in tropical and sub-tropicalzones because they are used for many purposes including protectionagainst wind, stabilization of sand dunes and the productionof firewood and charcoal. They are usually able to grow in sandysoils with low fertility by virtue of their ability to fix N₂.The objective of this review is to discuss briefly the roleof mycorrhizas and, more extensively, that of cluster (proteoid)roots, developed by a number of species of Casuarinaceae toimprove the absorption of nutrients other than N from soil,especially those needed for N₂fixation and growth. After evaluatingthe actual relationships between mycorrhizas and the Casuarinaceae,we highlight the possible role of cluster roots as an effectivealternative to mycorrhizas, and as a means of improvement ofgrowth of the trees in nutrient-deficient soils. This raisesthe question of what triggers the formation of cluster rootsin the Casuarinaceae. In addition to phosphorus deficiency,iron deficiency seems to be a major factor inducing the formationof cluster roots in Casuarina glauca and C. cunninghamiana.The number of cluster roots and the precocity of their formationare directly related to plant chlorosis due to Fe deficiency,as expressed by the critical concentration of chlorophyll inthe shoot (0.60 mg g ^{- 1}shoot f.wt). The effect of the nitrogensource on cluster root formation is discussed in relation topH values in the plant culture solution. The number of clusterroots formed in nitrate-fed plants increases with pH in therange of 5 to 9. Experiments carried out with alkaline and acidicsoils show that cluster roots are only produced when they areneeded to overcome soil nutrient deficiency due to the immobilizationof nutrient elements (P and Fe) by soil alkalinity. The possibleinvolvement of ethylene in the initiation and/or the morphogenesisof cluster roots is discussed. Copyright 2000 Annals of BotanyCompany Casuarinaceae, Casuarina cunninghamiana, Casuarina glauca, cluster roots, ethylene, iron deficiency, phosphorus deficiency, proteoid roots     

Sagebrush (Artemisia tridentata Nutt.) roots maintain nutrient uptake capacity under water stress

Phosphorus and nitrogen uptake capacities were assessed during36–58 d drying cycles to determine whether the abilityof sagebrush (Artemisia tridentata Nutt.) to absorb these nutrientschanged as the roots were subjected to increasing levels ofwater stress. Water was withheld from mature plants in large(6 I) containers and the uptake capacity of excised roots insolution was determined as soil water potentials decreased from–0.03 MPa to –5.0 MPa. Phosphorus uptake rates of excised roots at given substrateconcentrations increased as preharvest soil water potentialsdecreased to –5.0 MPa. V_max and K_m also increased as soilwater potentials declined. Declining soil water potentials depressednitrogen uptake at set substrate concentrations, but uptakecapacity, calculated as the sum V_max for both NH⁺₄+NO^–₃,did not change significantly with drying. The sum V_max correlatedwith root nitrogen concentration. Root uptake capacity for nitrogen and phosphorus was extremelystable under severe water stress in this aridland shrub. Maintenanceof uptake capacity, coupled with a previously demonstrated abilityto conduct hydraulic lift, may enable A. tridentata better tomaintain nitrogen and phosphorus uptake as soil water availabilitydeclines. These mechanisms may be important in the ability ofA. tridentata to maintain growth, complete reproduction, andgain an advantage against competitors late in the season whenthe soil layers with higher nutrient availability are dry. Key words: Kinetics, nitrogen, phosphorus, roots, water stress     

Effects of Different Nitrogen Sources and Concentrations on CAM Photosynthesis in Kalanchoe blossfeldiana

When Kalanchoë blossfeldiana Poelln. cv. Hikan plants werecultured in solutions containing 0.2, 1.0, 5.0 or 10 mM of nitrateor ammonium under a long-day photoperiod, some criteria of CAM(Crassulacean acid metabolism) photosynthesis (diurnal changesof CO₂ uptake, titratable acidity and malate content in leaves)were examined. The plants absorbed 90 to 100% of CO₂ duringthe light phase regardless of the supplied nitrogen. Nitrate-grownplants absorbed about 10% of CO₂ during the dark phase regardlessof the supplied concentration, whereas in ammonium-grown plantsthe nocturnal CO₂ uptake occurred at 0.2 mM, at which the plantsdepleted nitrogen and no uptake was observed at the higher concentrations.Changes of nocturnal increase in titratable acidity and malatecontent almost corresponded with the changes in the amount ofnocturnal CO₂ uptake. Also K. daigremontiana plants suppliedwith 10 mM of ammonium had a less CAM-like pattern of diurnalCO₂ uptake than the plants supplied with 10 mM of nitrate. Theseresults suggest that a sufficient supply of ammonium depressesCAM photosynthesis.     

Suppression of the High Affinity Phosphate Uptake System: A Mechanism of Arsenate Tolerance in Holcus lanatus L.

In Holcus lanatus L. phosphate and arsenate are taken up bythe same transport system. Short-term uptake kinetics of thehigh affinity arsenate transport system were determined in excisedroots of arsenate-tolerant and non-tolerant genotypes. In tolerantplants the V_max of ion uptake in plants grown in phosphate-freemedia was decreased compared to non-tolerant plants, and theaffinity of the uptake system was lower than in the non-tolerantplants. Both the reduction in V_max and the increase in K_m ledto reduced arsenate influx into tolerant roots. When the twogenotypes were grown in nutrient solution containing high levelsof phosphate, there was little change in the uptake kineticsin tolerant plants. In non-tolerant plants, however, there wasa marked decrease in the V_max to the level of the tolerant plantsbut with little change in the K_m. This suggests that the lowrate of arsenate uptake over a wide range of differing rootphosphate status is due to loss of induction of the synthesisof the arsenate (phosphate) carrier. Key words: Arsenate, Holcus lanatus L., phosphate uptake, tolerance mechanisms, uptake mechanisms     

Soil chemical limitations to growth and development of Veronica officinalis L. and Carex pilulifera L.

Veronica officinalis and Carex pilulifera, widespread plants of acid soils in Europe, were grown in 50 soils of natural and seminatural ecosystems representing a wide range of soil chemical properties. The experiment was performed in a greenhouse at a soil moisture content of 55–65% WHC, ca. 60% R.H. of the air, temperature 14–16°C at night and 19–21°C by day; additional light 70 W m^-2 12 h d^-1. Properties closely related to soil acidity precluded growth of V. officinalis and limited the growth rate of C. pilulifera at soil pH-KCl < ca. 3.4. In slightly-moderately alkaline (calcareous) soils, growth was primarily limited by insufficient phosphate uptake. A low growth rate of C. pilulifera. in such soils was related to low concentrations of exchangeable soil phosphate and low tissue concentrations of phosphorus. However, in high-pH soils, secondary effects due to suboptimum trace element (probably Fe) conditions, giving rise to symptoms of chlorosis, were also indicated. The highest growth rates of both species were invariably measured in soils of intermediate acidity having very high concentrations of exchangeable phosphate. Multiple regression tests on the entire material indicated that 65–75% of the variability in several growth functions could be accounted for, when two or more soil characters were included in the equation. Besides phosphate, exchangeable Zn (in C. pilulifera) and nitrate (in V. officinalis) were of considerable importance in accounting for growth rates.     

Effect of Root Zone Temperature on the Mineral Composition of Xylem Sap and Plasma Membrane K+-Mg++-ATPase Activity of Grafted-Cucumber and -Figleaf Gourd Root Systems

Cucumber (Cucumis sativus L.) seedlings were grafted onto cucumber-(CG) or figleaf gourd- (FG, Cucurbita ficifolia Bouché)seedlings in order to determine the effect of solution temperature(12, 22, and 32°C) on the mineral composition of xylem sapand the plasma membrane K⁺-Mg⁺⁺-ATPase activities of the roots.Low solution temperature (12°C) lowered the concentrationof NO^–₃ and H₂PO^–₄ in xylem sap of CG plants butnot of FG plants. Concentrations of K⁺, Ca⁺⁺ and Mg⁺⁺ in xylemsap were less affected than anions by solution temperature.The plasma membrane of FG plants grown in 12°C solutiontemperature showed the highest K⁺- Mg⁺⁺-ATPase activity at allATP concentrations up to 3 mM and at low reaction temperatureup to 12°C, indicating resistance of figleaf gourd to lowroot temperature. (Received December 27, 1994; Accepted March 10, 1995)     

Phosphate uptake and transport in Agrostis capillaris L Effects of non-toxic levels of aluminium and the significance of P and Al speciation

Investigations on the effects of low levels of Al on P adsorption,uptake and translocation in seedlings of the indigenous grassAgrostis capillaris were undertaken. Apparent uptake and transportof H₂ ³²PO₄ from nutrient solutions containing 10 or 100mmolm^–3 phosphate were characterized as functions of timeand concentration. Experiments on ³²P uptake and transport insolutions containing no Al (control) or Al ranging from 3.7to 185 mmol m^–3 at pH ranging from 4.3 to 4.6, showedthat in 10 mmol m^–3 P, effects of Al at 3.7 and 37 mmolm^–3 on the size of the initial uptake shoulder were small,but some increase in subsequent P uptake to the roots was observed,though transport to the shoots was suppressed. With 37 mmolm^–3 Al in nutrient solution containing 100 mmol m^–3P, the uptake shoulder was much increased above the control.Subsequent root uptake was stimulated but transport was unaffected.Lack of toxicity of the Al concentrations used was indicatedby a lack of significant effect on plant fresh weight. AbsorbedAl was almost totally retained in the root in all treatments.Speciation calculations showed that the major species in Alamended nutrient solution at pH 4.4 were H₂PO₄^–, AI³⁺and AIHPO₄⁺, together with substantial amounts of AISO₄⁺ andsoluble aluminium hydroxy complexes (AIOH²⁺, AI(OH)₂⁺), dependingon the relative concentrations of P and Al. The effects of Al,with 10 mmol m^–3 P, on adsorption of complexed P werepartly accounted for in terms of preferential cell wall adsorptionof Al complexes not containing P. Conclusions were drawn aboutthe P-economy of A. capillaris plants growing on soils withlow levels of P and Al. Key words: Phosphorus, aluminium, speciation, Agrostis capillahs L     

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.