Regulation of ion transport in mitochondria by respiratory chain enzymes and ATPase

The effects of the respiratory chain inhibitors as well as those of the inhibitors and substrates of ATP-synthetase in Ca2+ and K+ transport induced in the mitochondria upon the medium acidification in the presence of phosphate or arsenate, were investigated. Evidence has been obtained suggesting that under the experimental conditions used the transmembrane fluxes of K+ and Ca2+ are paralleled with H+ leakage through the proton channel of ATPase. It was found also that the system inducing cation fluxes at low pH values included peroxidation and hydrolysis of phospholipids. A scheme of regulation of ion transport in the mitochondria involving oxidative phosphorylation and oxidation and hydrolysis of lipids is proposed.     

Effects of inorganic nitrogen application on the dynamics of the soil solution composition in the root zone of maize

The effect of inorganic nitrogen (N) fertilizer on the ionic composition of the soil solution under maize (Zea mays L.) was studied. A pot experiment was carried out with two treatments combined factorially, with or without N application (Ca(NO₃)₂; +N and –N treatments, respectively), and with or without plants. Three looped hollow fiber samplers were installed in each pot to sample soil solutions nondestructively from the root zone, seven times during the 50-day growth period. Plants were harvested on the 50th day, and their nutrient contents determined.Effects of N fertilizer on the soil solutions were observed by the first sampling, 2 days after sowing. The concentrations of Ca and NO₃ ^– and electrical conductivity (EC) increased significantly in the +N treatments as direct effects of fertilizer application. In addition, the concentrations of Mg, K, Na and H⁺ also increased and that of P decreased significantly as indirect effects caused by the re-establishment of chemical equilibria. This suggested the greater supply as well as the greater possibility of leaching loss not only of NO₃ ^– but also of Ca, Mg and K. In the treatments with plants, the concentrations of NO₃ ^–, Ca, Mg and K decreased with time and pH increased significantly compared with the unplanted soil. The depletion of N in the soil solution roughly agreed with the amount of N taken up by the plant. The depletions of K from the soil solution amounted to less than 10% of the amount of the K taken up, suggesting intensive replenishment of K from exchange sites in the soil. Depletions of Ca and Mg were several times higher than the amounts taken up, indicating that the depletions resulted from the adsorption of the divalent cations by the soil rather than uptake by plants. Because NO₃ ^– is hardly absorbed by exchange sites in soil and was the dominant anion in solution, it was concluded that NO₃ ^– had a major role in controlling cation concentrations in the soil solution and, consequently, on their availability for uptake by plants as well as their possible leaching loss. ei]H Marschner     

Simultaneous and intermittent measurement of K,Ca and NO3-ion absorption by intact bean plant (Phaseolus vulgaris L.) in aerobic and anaerobic condition

Summary Simultaneous and intermittent measurement of K, Ca and NO₃-ion absorption by intact bean plants was made under both aerobic and anaerobic conditions. Anaerobiosis was found to have a more direct and pronounced effect on K-ion absorption rather than NO₃ ion. Significant ionic efflux (particularly of K ion) occurred in anaerobic condition. This was explained on the basis of direct effect of ATP-ase on cation absorption by inducing an electrochemical and pH gradient. No effect, however, has been found on the rate of Ca ion absorption due to anaerobiosis.     

Effects of fertilization and liming on the chemical soil conditions and element distribution in forest soils

Summary The distribution and storage of major elements in acid soils from a spruce and a beech forest was investigated after fertilization of NH₄NO₃ and KCl followed by Ca and Mg fertilization by 2 liming applications. All fertilizers were applied on top of the soil without mixing. Most of the added Ca and Mg was detected in the humus layer, a significant part of it still in carbonatic form. The effect of liming on mineral soil pH is very low, and was only observed in the 0–10 cm layer. However, base saturation of the mineral soil increased. The storage of C and N of the humus layer was not affected. N fertilization increased the N storage of the soil only under beech, but was followed by heavy NO₃-losses with seepage water under spruce. High leaching rates for K were also found in the spruce stand. The amount of K that was not leached increased the pool of exchangeable K in the deeper soil layer.     

New insights into maitotoxin action

Maitotoxin (3 ng/mol) induced a massive uptake of 45Ca2+ into BC3H1 cells. This effect exhibits a lag phase of 3 min. Inositol diphosphate formation occurred concomittantly with the 45Ca2+ uptake but inositol monophosphate formation was found only after a 5-min delay following toxin addition. Maitotoxin-induced 45Ca2+ influxes could not be blocked by either 1 microM verapamil, 1 microM nifedipine or 1 mM La3+ but was blocked by Zn2+ (IC50 = 41 microM). In addition to inositol phosphate formation and 45Ca2+ uptake, maitotoxin stimulated a large uptake of Na+ and a great loss of K+ in BC3H1 cells. In the absence of Ca2+ (1 mM EGTA) none of the four maitotoxin effects could be detected. After restoration of Ca2+, the maitotoxin effects reappeared even when the toxin itself was no longer present. The divalent cation, Co2+ (1 mM), inhibited ion movements induced by maitotoxin and also digitonin (8.1 microM). The toxin action showed a very pronounced pH dependence. At low pH, maitotoxin was inactive. The dose-response curves for H+ ion inhibition of maitotoxin-induced Ca2+ uptake showed a shift to the right when determined in the absence of HCO3- and HCO3-/Cl- ions. It was concluded that the primary action of maitotoxin in BC3H1 cells was a pore-forming or channel-forming activity of a non-classical type. Some properties of maitotoxin resemble those of alpha-latrotoxin, others those of pore-forming agents such as melittin or alpha-toxin of Staphylococcus aureus.     

A calcium- and pH-regulated protein from Dictyostelium discoideum that cross-links actin filaments

We have purified an actin binding protein from amebas of Dictyostelium discoideum which we call 95,000-dalton protein (95K). This protein is rod shaped, approximately 40 nm long in the electron microscope, contains two subunits measuring 95,000 daltons each, and cross-links actin filaments. Cross-linking activity was demonstrated by using falling-ball viscometry, Ostwald viscometry, and electron microscopy. Cross-linking activity is optimal at 0.1 microM Ca++ and pH 6.8, but is progressively inhibited at higher Ca++ and pH levels over a physiological range. Half-maximal inhibition occurs at 1.6 microM free Ca++ and pH 7.3, respectively. Sedimentation experiments demonstrate that elevated Ca++ and pH inhibit the binding of 95K to F-actin which explains the loss of cross-linking activity. Electron microscopy demonstrates that under optimal conditions for cross-linking, 95K protein bundles actin filaments and that this bundling is inhibited by microM Ca++. Severing of actin filaments by 95K was not observed in any of the various assays under any of the solution conditions used. Hence, 95K protein is a rod-shaped, dimeric, Ca++- and pH-regulated actin binding protein that cross-links but does not sever actin filaments.     

Calcium transport into the vacuole of oat roots. Characterization of H+/Ca2+ exchange activity

Calcium (Ca2+) is sequestered into vacuoles of oat root cells through a H+/Ca2+ antiport system that is driven by the proton-motive force of the tonoplast H+-translocating ATPase. The antiport has been characterized directly by imposing a pH gradient in tonoplast-enriched vesicles. The pH gradient was imposed by diluting K+-loaded vesicles into a K+-free medium. Nigericin induced a K+/H+ exchange resulting in a pH gradient of 2 (acid inside). The pH gradient was capable of driving 45Ca2+ accumulation. Ca2+ uptake was tightly coupled to H+ loss as increasing Ca2+ levels progressively dissipated the steady state pH gradient. Ca2+ uptake displayed saturation kinetics with a Km(app) for Ca2+ of 10 microM. The relative affinity of the antiporter for transport of divalent cations was Ca2+ greater than Sr2+ greater than Ba2+ greater than Mg2+. La3+ or Mn2+ blocked Ca2+ uptake possibly by occupying the Ca2+-binding site. Ruthenium red (I50 = 40 microM) and N,N'-dicyclohexylcarbodiimide (I50 = 3 microM) specifically inhibited the H+/Ca2+ antiporter. When driven by pH jumps, the H+/Ca2+ exchange generated a membrane potential, interior positive, as shown by [14C]SCN accumulation. Furthermore, Ca2+ uptake was stimulated by an imposed negative membrane potential. The results support a simple model of one Ca2+ taken up per H+ lost. The exchange transport can be reversed, as a Ca2+ gradient (Ca2+in greater than Ca2+out) was effective in forming a pH gradient (acid inside). We suggest that the H+/Ca2+ exchange normally transports Ca2+ into the vacuole; however, under certain conditions, Ca2+ may be released into the cytoplasm via this antiporter.     

Ion flux interaction with cytoplasmic streaming in branchlets of Chara australis

Both parts of the actin-myosin complex involved in cytoplasmic streaming could be regulated by mineral ions. The main goal of this study was to find a relationship between cyclosis and ion transport across the cell wall and plasma membrane. The transport of K(+) and Ca(2+) along pH bands in Chara branchlet internodal cells was characterized by using the MIFE system for non-invasive microelectrode measurement of ion fluxes. Branchlets formed acidic and alkaline bands with the pH ranging from 5 to 8. Different pH patterns were observed for different sides of the branchlets. Sides with cyclosis streaming acropetally generally showed greater variation in the profiles of pH and H(+) fluxes. Although a high correlation was not found between pH bands and Ca(2+) or K(+) fluxes, there was a positive correlation between Ca(2+) and K(+) fluxes themselves for both sides of the branchlets. Application of cytochalasin D, an inhibitor of cyclosis, had no immediate effect on pH and ion fluxes, however, the time of cyclosis cessation corresponded with a dramatic change in Ca(2+) and K(+) fluxes; pH profiles and H(+) fluxes were affected within 2 h. The evidence suggests that, in Chara branchlets, pH band formation and Gd(3+)-insensitive Ca(2+) transport systems are linked to the cyclosis machinery: (i) the pH band amplitude for the acropetally streaming side was larger than that for the basipetally streaming side; (ii) cessation of cytoplasmic streaming after cytochalasin D application resulted in changed pH banding profiles and H(+), Ca(2+) and K(+) fluxes; and (iii) the application of GdCl(3) or incubation in GdCl(3) solutions did not lead to the cessation of cytoplasmic streaming, although external Ca(2+) fluxes changed.     

Manganese can inhibit or potentiate contractile responses in mesenteric portal vein

The effects of a number of agents believed to interfere with Ca were examined on contraction induced by noradrenaline (NA) or K in rat mesenteric portal veins. The organic calcium antagonists nifedipine, verapamil, methoxyverapamil, and felodipine slowly produced maximum inhibitory effects, nifedipine being fastest with a T1/2 of 20 min. In contrast, the inhibitory effects of Mn were immediate but disappeared on continued exposure of the tissue to Mn. After removal of Mn from the bath fluid, an above normal contraction was produced by K or NA. Measurement of Mn by atomic absorption spectrometry showed that the concentrations of EDTA-resistant Mn increased in parallel with the loss of inhibitory effects of Mn. This is consistent with an external inhibitory effect of Mn but a potentiating effect of Mn once it reaches an EDTA-inaccessible site. The potentiating effect of Mn was not seen with other ions such as Cd, Ni, Co, Mg, and La, which produced only inhibition of responses to NA or K. Contractile responses to Ba were examined in the absence of external Ca and it was found that the responses decreased with time. The presence of Mn not only prevented the loss of contractility but produced a marked increase in the response to Ba. Relaxation rates were also studied and it was found that Mn speeds the relaxation of contractures produced by NA or Ba as long as Mn is present in the bath fluid, but Mn slows relaxation when it is present (presumably) intracellularly. Mn does not alter relaxation rates of K contractures.(ABSTRACT TRUNCATED AT 250 WORDS)     

Self-aggregation of surfactant protein A

Environmental factors of physiological relevance such as pH, calcium, ionic strength, and temperature can affect the state of self-aggregation of surfactant protein A (SP-A). We have studied the secondary structure of different SP-A aggregates and analyzed their fluorescence characteristics. (a) We found that self-aggregation of SP-A can be Ca(2+)-dependent. The concentration of Ca(2+) needed for half-maximal self-association (K(a)(Ca)()2+) depended on the presence of salts. Thus, at low ionic strength, K(a)(Ca)()2+ was 2.3 mM, whereas at physiological ionic strength, K(a)(Ca)()2+ was 2.35 microM. Circular dichroism and fluorescence measurements of Ca(2+)-dependent SP-A aggregates indicated that those protein aggregates formed in the absence of NaCl are structurally different from those formed in its presence. (b) We found that self-aggregation of SP-A can be pH-dependent. Self-aggregation of SP-A induced by H(+) was highly influenced by the presence of salts, which reduced the extent of self-association of the protein. The presence of both salts and Ca(2+) attenuated even more the effects of acidic media on SP-A self-aggregation. (c) We found that self-aggregation of SP-A can be temperature-dependent. At 20 degrees C, SP-A underwent self-aggregation at physiological but not at low ionic strength, in the presence of EDTA. All of these aggregates were dissociated by either adding EDTA (a), increasing the pH to neutral pH (b), or increasing the temperature to 37 degrees C (c). Dissociation of Ca(2+)-induced protein aggregates at low ionic strength was accompanied by an irreversible loss of both SP-A secondary structure and SP-A-dependent lipid aggregation properties. On the other hand, temperature-dependent experiments indicated that a structurally intact collagen-like domain was required for either Ca(2+)- or Ca(2+)/Na(+)-induced SP-A self-aggregation but not for H(+)-induced protein aggregation.     

Effects of Ca2+ on the sodium pump observed in cardiac myocytes isolated from guinea pigs

It is presently unknown whether Ca2+ plays a role in the physiological control of Na+/K+-ATPase or sodium pump activity. Because the enzyme is exposed to markedly different intra- and extracellular Ca2+ concentrations, tissue homogenates or purified enzyme preparations may not provide pertinent information regarding this question. Therefore, the effects of Ca2+ on the sodium pump were examined with studies of [3H]ouabain binding and 86Rb+ uptake using viable myocytes isolated from guinea-pig heart and apparently maintaining ion gradients. In the presence of K+, a reduction of the extracellular Ca2+ increased specific [3H]ouabain binding observed at apparent binding equilibria: a half-maximal stimulation was observed when extracellular Ca2+ was lowered to about 50 microM. The change in [3H]ouabain binding was caused by a change in the number of binding sites accessible by ouabain instead of a change in their affinity for the glycoside. Ouabain-sensitive 86Rb+ uptake was increased by a reduction of extracellular Ca2+ concentration. Benzocaine in concentrations reported to reduce the rate of Na+ influx failed to influence the inhibitory effect of Ca2+ on glycoside binding. When [3H]ouabain binding was at equilibrium, the addition of Ca2+ decreased and that of EGTA increased the glycoside binding. Mn2+, which does not penetrate the cell membrane, had effects similar to Ca2+. In the absence of K+, cells lose their tolerance to Ca2+. Reducing Ca2+ concentration prevented the loss of rod-shaped cells but failed to affect specific [3H]ouabain binding observed in the absence of K+. These results indicate that a large change in extracellular Ca2+ directly affects the sodium pump in cardiac myocytes isolated from guinea pigs.     

Effect of Ca2+ and K+ on the intracellular pH of an Escherichia coli L-form.

The L-form NC7, derived from Escherichia coli K12, grew in a complex medium containing 0.2 M-CaCl2 as osmotic stabilizer, but not at pH values above 7.8. The cessation of growth at alkaline pH was not due to cell death. In complex media containing K+ or Na+, the L-form grew ove a wide pH range. Growth at alkaline pH was inhibited by 1 mM-amiloride, indicating that Na+/H+ antiport activity was required for growth at alkaline pH. The internal pH (pHi) of the L-form in media containing K+, Na+ or Ca2+ was constant at about 7.8 to 8.0 at external pH (pHo) values of 7.2 and 8.2. The rates of O2 consumption by intact cells, lactate oxidation by membrane vesicles from cells grown in Ca(2+)-containing medium, and cell division were all strongly repressed under alkaline conditions.     

Factors affecting soil acidification under legumes I. Effect of potassium supply

This study examined the effect of K (as K₂SO₄) supply on acid production under N₂-fixing plants of lupin (Lupinus angustifolius L. cv. Gungurru) and clover (Trifolium subterraneum L. cv. Dalkeith) grown in a K-deficient soil with a low pH buffer capacity for 55 days in the glasshouse at 20/12 °C (day/night). Increasing K supply up to 240 mg K kg^-1 soil markedly increased plant growth of both species but clover growth was more responsive than lupin. Growing plants for 55 days decreased soil pH by 0.65–0.85 units under lupin and 0.45–0.83 units under clover. The amounts of H⁺ produced per kg biomass (specific acid production) were the highest at the nil K supply, generally decreased with increasing K level up to 30 mg K kg^-1 under lupin and up to 120 mg K kg^-1 soil under clover and only slightly increased with further increasing K under lupin. Increasing K₂SO₄ supply proportionally increased plant uptake of K and SO ₄ ^2- but generally decreased concentrations of Ca, Mg, Na, P and Cl. Specific acid production correlated well with concentrations of excess cations and ash alkalinity, and total acid production was strongly correlated with total excess cations and total ash alkalinity in plants. These relationships were not affected by K treatment and species. Specific acid production also correlated with plant Ca concentration but not with K concentration. In addition, lupin and clover extruded similar amounts of H⁺ per kg biomass produced. It is suggested that application of K₂SO₄ does not have a significant impact on acid production by lupin and clover.     

The effect of hydrogen peroxide on isolated body wall of the lugworm Arenicola marina (L.) at different extracellular pH levels

The effect of hydrogen peroxide on the rate of tissue oxygen consumption, on intracellular pH (pH(i)) and on malondialdehyde (MDA) accumulation was studied in isolated body wall tissue of the lugworm Arenicola marina (L.). H2O2 effects were investigated at various levels of pH(i) by changing medium pH (pH(e)). The largest decrease of tissue oxygen consumption (by 17% below controls), as well as the highest degree of MDA accumulation (four-fold compared to control values) after H2O2 exposure were found at acidic pH(e) of 6.4. This was attributed to the higher redox potential of H2O2 in acidic solutions. Oxygen consumption at alkaline pH(e) (8.5) was not affected by H2O2. MDA accumulation in the tissue was considerably lower than at pH(e) 7.4 or 6.4. Despite pH dependent alterations of H2O2 redox potential, we observed more or less constant pH(e) independent acidification of the tissue upon exposure to H2O2. We attributed the acidification to an inhibition of ATP consuming proton equivalent ion transport across the cellular membrane. Inactivation of carrier proteins is discussed to be responsible for the decrease in tissue oxygen consumption. However, with a larger effect on oxygen consumption at acidic pH(e) values, the latter may not be the only explanation, but additional impairment of other energy demanding processes may be involved.     

Evidence for a nutritional disorder of Oxalis acetosella L. on acid forest soils; II. Diagnostic field experiments and nutrient solution studies

Different field experiments were performed to discover the main factor(s) responsible for the poor leaf growth, moderate propagation and leaf chlorosis of Oxalis acetosella in an old Norway spruce stand with acid soil (Höglwald Forest). A previous study had suggested, that Ca (or Mg) deficiency or Mn toxicity could be involved.In a Main Diagnostic Field Experiment with an intact population, Ca and Mg were either applied as sulphate or carbonate to distinguish between nutritional and pH effects. Mn and Si were also applied to aggravate or overcome possible effects of Mn toxicity. Enhancement experiments with different amounts of CaSO₄ were conducted to investigate the Ca dose-effect relationship under field conditions. Additional trials with SrCO₃, BaCO₃ and NaHCO₃ had the goal to raise the soil pH without supply of nutrients.Greenhouse experiments with Oxalis acetosella supplemented the field studies by investigating the Ca and Mn dose-effect relationships under controlled conditions. Growth, vitality and nutrition of Oxalis were studied in a nutrient solution culture at pH 4.0 over a range of concentrations of Ca (20 to 5000 mol L_-1) and Mn (5 to 1000 mol L_-1) respectively. Furthermore, the effects of two contrasting ammonium/nitrate ratios were tested. The nutritional composition of the basal nutrient solution and the microclimate in the greenhouse were as far as possible adjusted to the environmental conditions of the plant in the Höglwald Forest.All these studies led to the conclusion, that the moderate growth and vitality of Oxalis in the Höglwald Forest was mainly due to an insufficient Ca supply, rather than an effect of Mg deficiency, low soil pH or Mn toxicity. The application of CaSO₄ caused a similar stimulation of the growth as CaCO₃. A clearly positive, close CaSO₄ dose-effect relationship was detected in field experiments as well as in the nutrient solution study. The same type of leaf chloroses as in the field was reproduced through low Ca nutrient solutions. Predominant ammonium nutrition may significantly impair Ca uptake.Oxalis acetosella displayed a relatively high leaf tissue tolerance of excessive Mn. There was no indication for a Mn-induced Ca deficiency in the Höglwald Forest. Enhanced Si uptake led to a partial vitalization of Oxalis; the reason for that remained unclear.     

Time-resolved charge translocation by sarcoplasmic reticulum Ca-ATPase measured on a solid supported membrane

Sarcoplasmic reticulum vesicles were adsorbed on an octadecanethiol/phosphatidylcholine mixed bilayer anchored to a gold electrode, and the Ca-ATPase contained in the vesicles was activated by ATP concentration jumps both in the absence and in the presence of K(+) ions and at different pH values. Ca(2+) concentration jumps in the absence of ATP were also carried out. The resulting capacitive current transients were analyzed together with the charge under the transients. The relaxation time constants of the current transients were interpreted on the basis of an equivalent circuit. The current transient after ATP concentration jumps and the charge after Ca(2+) concentration jumps in the absence of ATP exhibit almost the same dependence upon the Ca(2+) concentration, with a half-saturating value of approximately 1.5 microM. The pH dependence of the charge after Ca(2+) translocation demonstrates the occurrence of one H(+) per one Ca(2+) countertransport at pH 7 by direct charge-transfer measurements. The presence of K(+) decreases the magnitude of the current transients without altering their shape; this decrease is explained by K(+) binding to the cytoplasmic side of the pump in the E(1) conformation and being released to the same side during the E(1)-E(2) transition.     

The effects of short-term laboratory pH depressions on molting,mortality and major ion concentrations in the mayflies Stenonema femoratum and Leptophlebia cupida

Field surveys of the distribution of mayfly nymphs suggest that Stenonema femoratum are more acid-sensitive than Leptophlebia cupida. To assess whether this apparent difference in sensitivity of nymphs is reflected in differences in the degree of whole-body loss of [Na], [Cl], [Ca] or [K] under laboratory conditions, we exposed nymphs of both species to low pH for 96–192 h in soft water ([Ca] = 0.1 mM). Although mortality and loss of whole-body [Na] and [Cl] occurred in both species at pH 3.5, unexpectedly they were considerably greater in L. cupida than in S. femoratum. Ion loss was not size related within the range of nymphal weights used (2–14 mg dry wt) for S. femoratum. Exposure to the environmentally more common pH 4.5 had no effect on whole-body [Na] and [Cl] or on mortality in either species. However, in L. cupida, molting by nymphs increased at both pH 3.5 and 4.5. A decrease in whole-body [Ca] occurred, and the loss of whole-body [Na] and [Ca] at pH 3.5 appeared to cease following the period of molting. In S. femoratum no molting or Ca loss occurred and whole-body [Na] and [Cl] decreased between 96 and 192 h exposures.     

Inhibition by calcium of senescence of detached cucumber cotyledons: effect on ethylene and hydroperoxide production

The effect of Ca on senescence was followed in detached cucumber (Cucumis sativus L.) cotyledons floating on various solutions in the dark. Compared with those in water, cotyledons in 10⁻⁴ molar CaCl₂ exhibited reduced chlorophyll loss and H₂O₂ production, reduced and delayed ethylene production, and did not undergo a burst in CO₂ production. In contrast, Mg had little effect on cotyledon senescence, whereas K stimulated chlorophyll loss but did not increase H₂O₂ accumulation of ethylene and CO₂ production. This reduction in the rate of senescence by Ca could also be achieved by increasing the endogenous levels of Ca in the cotyledons before excision, although the reduction was less than that with Ca in the external solution. The addition of H₂O₂ to the solutions on which cotyledons were floated stimulated chlorophyll breakdown, but effects on ethylene and CO₂ were not consistent.     

Salinity-induced calcium deficiencies in wheat and barley

Salinity-calcium interactions, which have been shown to be important in plants grown in dryland saline soils of the Canadian prairies, were studied in two species differing in salt tolerance. In solution culture, wheat showed a greater reduction in growth and a higher incidence of foliar Ca deficiency symptoms than barley when grown under MgSO₄ or Na₂SO₄ plus MgSO₄ salt stress. Amendment of the saline solution with Ca to increase the Ca/(Na+Mg) ratio ameliorated the effects of salt, but more so in wheat than in barley. At least part of the difference in salt tolerance between the two species must therefore relate to species differences in the interaction of salinity and Ca nutrition. The greater response of wheat to Ca was not due to a lower Ca status in leaf tissue; on the contrary, although Ca amendments improved tissue Ca/(Na+Mg) ratios in both species, salinized wheat had equivalent or higher Ca content, and higher Ca/(Na+Mg) ratios than did barley. The higher Ca requirement of wheat is apparently specific to a saline situation; at low salinity, wheat growth was not reduced as extensively as that of barley as Ca/(Na+Mg) ratio was decreased. High night-time humidity dramatically improved wheat growth under saline conditions, but increasing the Ca concentration of the saline solution had no effect on growth in the high humidity treatment. Membrane leakage from leaf tissue of wheat grown under saline conditions was increased compared to tissue from non-saline plants. Plants grown in Ca-amended saline solutions showed no increase in membrane leakage. These results confirm the importance of Ca interaction with salinity stress, and indicate differences in species response.     

Vegetation-soil relations in the lowlands of south-west Tasmania

A geographic survey of 14 south-west Tasmanian sedgeland-heaths revealed that soil organic matter is related to: water content: total nitrogen (N): total and exchangeable sodium (Na), calcium (Ca) and magnesium (Mg); exchangeable potassium (K) cation exchange capacity; and total exchangeable bases. However, total and available phosphorus (P), total K and Iron (Fe). pH level and percentage base saturation were found to be Independent of organic content. Most of the soil nutrient capital is contained In the A₀ horizon, the depth of which was found to be positively related to the time elapsed since the last fire. There is no clear relationship between rock type and soil fertility, but there is evidence of soil-vegetation interaction. The sedgeland-heath species have lower concentrations of P, Ca and Mg in their foliage and are more efficient In the withdrawal of P and K upon tissue senescence than the surrounding scrub and forest species. Over a vegetation transition from sedgeland-heath to forest on uniform geology there was a change in soil type. The forest was found to have more fertile soils and a higher concentration of nutrients in the above-ground biomass than the adjacent sedgeland-heath. The ecotone was burnt between 20–30 years prior to sampling, but the fire did not kill all the forest trees, and the structural differences suggest a mare rapid recovery of forest species. Soil fertility appears to be an important factor in controlling the rate of recovery and succession following a fire, especially if the nutrient-rich organic layer is burnt.