- Copyright © 1998 American Society of Plant Physiologists
Abstract
Ca2+ in rooting medium is essential for root elongation, even in the absence of added toxicants. In the presence of rhizotoxic levels of Al3+, H+, or Na+ (or other cationic toxicants), supplementation of the medium with higher levels of Ca2+alleviates growth inhibition. Experiments to determine the mechanisms of alleviation entailed measurements of root elongation in wheat (Triticum aestivum L. cv Scout 66) seedlings in controlled medium. A Gouy-Chapman-Stern model was used to compute the electrical potentials and the activities of ions at the root-cell plasma membrane surfaces. Analysis of root elongation relative to the computed surface activities of ions revealed three separate mechanisms of Ca2+ alleviation. Mechanism I is the displacement of cell-surface toxicant by the Ca2+-induced reduction in cell-surface negativity. Mechanism II is the restoration of Ca2+ at the cell surface if the surface Ca2+has been reduced by the toxicant to growth-limiting levels. Mechanism III is the collective ameliorative effect of Ca2+ beyond mechanisms I and II, and may involve Ca2+-toxicant interactions at the cell surface other than the displacement interactions of mechanisms I and II. Mechanism I operated in the alleviation of all of the tested toxicities; mechanism II was generally a minor component of alleviation; and mechanism III was toxicant specific and operated strongly in the alleviation of Na+toxicity, moderately in the alleviation of H+ toxicity, and not at all in the alleviation of Al3+ toxicity.
Ca2+ in rooting medium is essential for root elongation, even in the absence of added toxicants (Hanson, 1984; present study). In the presence of rhizotoxic levels of Al3+, H+, or Na+ (or other cationic toxicants), supplementation of the medium with higher levels of Ca2+ alleviates growth inhibition (LaHaye and Epstein, 1969; Hanson, 1984; Kinraide and Parker, 1987; Yan et al., 1992; Yermiyahu et al., 1997a; present study). Several separate mechanisms for Ca2+ alleviation of mineral toxicity have been proposed. A commonly proposed, or at least implied, mechanism is the restoration of toxicant-displaced Ca2+ (LaHaye and Epstein, 1969; Hanson, 1984;Cramer et al., 1985; Lynch et al., 1987; Shortle and Smith, 1988;Schulze, 1989; Läuchli, 1990; Rengel, 1992; Yan et al., 1992;Yermiyahu et al., 1997a). The present investigation attempts to identify the mechanisms by which Ca2+ alleviates mineral rhizotoxicity and to determine the relative importance of these mechanisms.
Several previous investigations have demonstrated the importance ofψ 0 in root-mineral interactions (Wagatsuma and Akiba, 1989; Suhayda et al., 1990; Kinraide, 1994;Yermiyahu et al., 1997a). Because PM surfaces are usually negatively charged (Wagatsuma and Akiba, 1989), the ion concentrations at root PM surfaces can differ significantly from the concentrations in the rooting medium. Treatments that reduce PM surface negativity, such as increases in the ionic strength or decreases in the pH of the rooting medium, reduce the effectiveness of cationic toxicants and increase the effectiveness of at least one anionic toxicant (Kinraide, 1994). Presumably, the effectiveness of ionic nutrients and ameliorants such as Ca2+ are similarly modified.
Because of the importance of ψ0, a model for its computation has been developed specifically for root cells of the experimental subject, an Al-sensitive wheat cultivar (Triticum aestivum L. cv Scout 66) (Yermiyahu et al., 1997b). Although developed specifically for cv Scout 66 on the basis of ion sorption, the model appears to be suitable for the estimation of ψ0 (or values that are at least proportional to ψ0) for plants in general. This model has been refined to improve its compatibility with published ζ potentials from diverse plant sources (Kinraide et al., 1998).
Knowledge of ψ0 allows the computation of {I Ζ}0. Use of {I Ζ}0 rather than ion activities in the bulk-phase rooting medium ({I Ζ}∞) has enabled the separate analysis of three mechanisms for the Ca2+ alleviation of mineral rhizotoxicity.
MATERIALS AND METHODS
Growth Experiments
Root elongation in response to combinations of toxic and nontoxic minerals was assessed by the cultivation of 2-d-old seedlings of an Al-sensitive wheat cultivar (Triticum aestivum L. cv Scout 66) in aerated solutions at 25°C in the dark for 2 d according to methods described previously (Kinraide, 1997). The composition of specific solutions will be presented with the results of the experiments.
Computation of Ion Activities at the PM Surface
{I Ζ}0 was computed from {I Ζ}∞ and ψ0 after the latter was computed with a Gouy-Chapman-Stern model that was developed specifically for cv Scout 66 (Yermiyahu et al., 1997b) and then refined to improve its compatibility with published ζ potentials from diverse plant sources (Kinraide et al., 1998). A diskette with a computer program for the Gouy-Chapman-Stern model, together with a manual for its use, may be obtained from the author.
Analysis of Root Elongation
Root elongation will be expressed in several ways. RLis the mean length of roots from a solution in which the two longest roots from each of five seedlings were measured.RRL C is defined as 100(RL T −RL S)/(RL C −RL S), where RL Tis the RL in the presence of toxicant,RL C is the RL in the corresponding toxicant-free control (or low-toxicant control in the case of H+), and RL Sis the RL in the presence of toxicant sufficient to maximize its growth-inhibitory effects (RL S is nearly equal to RL at the time of seedling transfer to the test solutions). In each particular experimentRL S is a single value, but eachRL T has its correspondingRL C.
RRL C is problematical because of an implication that the difference in RL T andRL C is attributable solely to toxicant. In Al3+ toxicity, for example, an Al-bearing solution and its Al-free control may be at an equally low pH, but it is not true that the two solutions impose similar H+stresses. H+ stress is higher in the control solutions because Al3+ displaces H+ from the PM surface (Kinraide, 1997). Consequently, another designation for root elongation in response to toxicants is defined here. RRL max is defined as 100(RL T −RL S)/(RL max −RL S), whereRL max is RL in toxicant-free, Ca2+-sufficient solutions. In this formulationRL max is a single value within each experiment.
When growth is plotted against measures of toxicant intensity, such as {T}0, the resulting curves are often downwardly sigmoidal and can be expressed by a Weibull equation that has been used previously to describe growth responses to toxicants (Kinraide, 1997; Yermiyahu et al., 1997a). If growth is limited only by {T}0, then:
If {Ca2+}0 is limiting (because of toxicant displacement of Ca2+ from the PM surface or for some other reason), the addition of Ca2+ may enhance growth, and plots of growth versus {Ca2+}0 may be upwardly sigmoidal. If growth is limited only by {Ca2+}0 insufficiency, then:
It is acknowledged here that Equations 1 through 4 are not mechanistically derived, and the coefficients have no special physiological meaning. However, they can serve to quantify both toxicant strengths and Ca2+-toxicant interactions, as demonstrated later. Although the coefficients may seem numerous, they are the minimal number for the required shapes, two for each sigmoidal curve plus an additional coefficient for each interaction.
Replication and Statistics
To compile data from a sufficient range of values for each of the variables, data were pooled from growth experiments performed under similar conditions. Not every experiment added to the pool was replicated, but considerable overlap among treatment variables occurred among experiments. An attempt was made to minimize intercorrelations among independent variables within a pool (data are presented below). A statistics program (SYSTAT, version 6, Systat, Evanston, IL) was used for multiple, nonlinear regression analyses. All values for coefficients presented in Results are significantly different from 0 (95% confidence intervals do not encompass 0).
RESULTS
Ca2+ Alleviation of Al3+ Toxicity
Ca2+ alleviates Al3+toxicity, but recent studies indicate that, ordinarily, the alleviation is not caused by the restoration of Al3+-inhibited Ca2+ uptake (Ryan et al., 1994) or by the restoration of Al3+-displaced cell-surface Ca2+ (Kinraide et al., 1994; Ryan et al., 1997). Ca2+ and other cations are ameliorative in the following order: Tris(ethylenediamine)cobalt3+ > Ca2+ ≈ Mg2+ ≈ Sr2+ > Na+ ≈ K+ (Kinraide and Parker, 1987; Kinraide et al., 1992, 1994; Ryan et al., 1994, 1997). Thus, it was concluded that Ca2+ and other cations relieve Al3+ toxicity solely by the displacement of Al3+ from the cell surface by electrostatic effects, i.e. by the reduction of cell-surface negativity and the consequent reduction of {Al3+}0. Alleviation of toxicity by the electrostatic displacement of toxicant will be referred to as mechanism I. The use of {T}0 instead of {T}∞ in Equation 1 is an attempt to express that mechanism quantitatively.
If mechanism I is the sole means by which Ca2+relieves Al3+ toxicity, then Equation 1 will describe adequately root elongation, and an attempt to evaluate Equation 3 will lead to nonsignificant values fora 2 and b 2, as has been observed for all data published previously (analyses not presented). Nevertheless, Al3+ does displace Ca2+ from cell or PM surfaces (Reid et al., 1995;Ryan et al., 1997, Yermiyahu et al., 1997b), and Kinraide et al. (1994)predicted that under conditions of sufficiently low Ca2+, the addition of Al3+may induce a state of cell-surface Ca2+insufficiency.
To test that hypothesis, new experiments were performed to assess Al3+ intoxication in a Ca2+-Mg2+ replacement series in which [CaCl2] + [MgCl2] = 1 mm (Fig.1). This experimental design eliminated mechanism I as a variable because of the similar effects of Ca2+ and Mg2+ on ψ0 (Kinraide et al., 1998). Figure 1 (top panel) demonstrates that [CaCl2] > 0.1 mm([MgCl2] < 0.9 mm) supported full root elongation in the absence of Al, but in the presence of 2 μm AlCl3, [CaCl2] > 0.2 mm was required. As [CaCl2] declined below 0.2 mm,RRL C also declined. This indicates that Al3+ caused a Ca2+insufficiency between 0.1 and 0.2 mmCaCl2, and that Al3+aggravated the Ca2+ insufficiency already expressed in the controls below 0.1 mmCaCl2. Alleviation of toxicity by Ca2+ restoration of toxicant-displaced Ca2+ will be referred to as mechanism II. The use of {Ca2+}0 instead of {Ca2+}∞ in Equation 2 is an attempt to express that mechanism. Mechanism II is related to the Ca2+-displacement hypothesis for toxicity, which states that a cation is toxic because it displaces Ca2+ from the cell surface.
Root elongation in response to CaCl2, MgCl2, and AlCl3 in the rooting medium. [CaCl2] + [MgCl2] = 1 mm and pH = 4.6. RRL C is the root length in Al solutions relative to Al-free solutions with similar CaCl2and MgCl2. The data were compiled from six experiments, with each point on the graph based on one to six values. Each of these values was based on the measured lengths of 10 roots, as described inMethods.
If mechanisms I and II both operate in the alleviation of Al3+ toxicity, then Equation 3 (not incorporating Eq. 4) should be appropriate. The experiments presented in Figure 1were pooled with the new experiment presented in TableI. Because the pH was only moderately low in these experiments (4.6) and the sum of the divalent cations was moderately high (1 mm), the roots were under no H+ stress (Kinraide et al., 1992; present study). Regression analysis according to Equation 3 yielded the results presented for Al3+ in TableII. When Equation 4 was incorporated into Equation 3, a nonsignificant value for a 4was obtained. Figure 2 presents model-generated curves for RRL max and 1 − 1/exp[(a 2{Ca2+}0)b2] based on the coefficients in Table II. Because all solutions for a given toxicant are electrostatically similar, mechanism I does not influence the trends in Figure 2.
Effects of Al3+, Ca2+, and Mg2+ on root elongation in cv Scout 66 seedlings
Summary of statistics from regression analyses according to the equation RRLmax = 100(1/exp[(a1{T}0)b1])(1 − 1/exp[(a2{Ca2+}0)b2])
Calculated root responses to CaCl2, MgCl2, and toxicants in the rooting medium. [CaCl2] + [MgCl2] = 1 mm and pH = 4.5, except where H+ was the designated toxicant. Toxicant levels (AlCl3 = 3.06 μm, pH = 4.12, and NaCl = 132.2 mm) were chosen so thatRRL max = 50 at [CaCl2]/([CaCl2] + [MgCl2]) = 0.5. ψ0 was −14, −15, and −10 mV for the added Al3+, H+, and Na+, respectively. The constancy of ψ0 for a toxicant means that electrostatic displacement of toxicant by Ca2+ (mechanism I) played no role in the computed trends. A 2= 1 − 1/exp[(a 2{Ca2+}0)b2] and is an expression of mechanism II alleviation. The continued increase in RRL max for Na+ and H+ in the top panel signifies the action of mechanism III.
Ca2+ Alleviation of H+ Toxicity
Ca2+ alleviates H+toxicity, and mechanism I appears to operate because toxicity is also alleviated by Na+, Mg2+, and Tris(ethylenediamine)cobalt3+ and other cations whose effectiveness increases with increasing charge (Kinraide et al., 1992). Nevertheless, the pattern of Ca2+alleviation is different from that of the Ca2+alleviation of Al3+ toxicity because Ca2+ is a more effective ameliorant than Mg2+, even at relatively high [Ca2+]∞, where mechanism II would not be expected to operate. In Ca2+-Mg2+ replacement experiments, RRL C continued to increase with increasing [Ca2+]∞(Kinraide et al., 1994). Growth experiments with H+ indicate that the effectiveness of the toxicant may be reduced by Ca2+ by mechanisms beyond those already described. For that reason, we introduce a third class of mechanisms: the alleviation of toxicity by Ca2+ by one or more mechanisms other than I and II will be referred to asmechanism III. The incorporation of Equation 4 into Equation3 is an attempt to express these mechanisms.
If mechanism III does operate, then Equation 3 (not incorporating Eq.4) will be incomplete, and incorporation of Equation 4 into Equation 3may improve the description of root elongation. These ideas were tested by pooling results from several published experiments (Kinraide et al., 1994) with results from new experiments such as those presented in Table III. The data were evaluated in terms of Equation 3 (incorporating Eq. 4). The results of the regression analysis are presented in Table II and Figure 2, where the effects of mechanism III on H+ toxicity can be seen in the continued increase of RRL maxfor H+.
Effects of pH and Ca2+ on root elongation in cv Scout 66 seedlings
RL max = 68.5 mm and RL S = 23.2 mm. A 1 = 1/exp[(a3 /(a4 {Ca 2+ } 0 + 1){T} 0 ) b 1],A2 = 1 − 1/exp[(a2 {Ca 2+ } 0 b2], and computed RRLmax = 100A1 · A2 . The data are from an experiment performed twice. The coefficients for the computation of RRLmax are based on 117 measurements (see Table II).
Ca2+ Alleviation of Na+ Toxicity
Ca2+ alleviates Na+toxicity, but a preliminary inspection of the data indicates that Ca2+ alleviation is not dominated by mechanism I to the extent that it is in Al3+ toxicity or even H+ toxicity. The diagnostic feature of mechanism I alleviation is that cations other than Ca2+ are effective ameliorants. Mg2+ and Sr2+ do reduce Na+toxicity, but the effects are weak compared with the effect of Ca2+ (Fig. 3). Furthermore, high Na+ can impose an osmotic stress that Ca2+ is unable to relieve.
Effects of NaCl, CaCl2, and MgCl2 on root elongation. A factorial array of 27 solutions contained 80, 105, or 130 mm NaCl, 0.15, 0.30, or 0.45 mm CaCl2, and 0, 1, or 2 mmMgCl2 (all at pH 5.0). Areas of circles are proportional to [CaCl2]. The data are from a single experiment representative of several similar but not identical Na+-Ca2+-Mg2+ experiments.
Data from several experiments were pooled (including the data from Fig.3, which were published previously [Kinraide, 1994]), and data from some new experiments in which [Na+]∞ ranged from 0 to 200 mm were also used. In addition, data were examined from an experiment in which mannitol ranged from 0 to 400 mm. Mannitol concentrations < 250 mm were not inhibitory, and Ca2+ could relieve Na+toxicity completely when the [NaCl] was <135 mm, indicating that osmotic stress was not a factor in root elongation in solutions with an osmolarity <250 mm. Consequently, only data from solutions with [NaCl] < 135 mm were retained in the pool. Regression analysis of these data yielded the results presented in Table II and Figure 2, where strong mechanism III effects can be seen in the steep and continuous increase ofRRL max for Na+.
The coefficient a
1 can be defined to include a Mg2+ term. If the equation:
A Reevaluation of a H+-Toxicity Study in an Attempt to Discern Mechanism II
The analytical techniques described above were also applied to several published studies in which a role for mechanism II was asserted or implied. In most cases mechanism I accounted for most of the alleviation, and mechanism II could not be confirmed. The following example illustrates some important points of experimental design and analysis.
In a study of H+ toxicity, Yan et al. (1992)concluded that the inhibition of corn root elongation was likely to have been a consequence of H+ influx inadequately compensated for by H+ secretion, resulting in the acidification of the cytoplasm. H+ displacement of Ca2+ was thought likely to have enhanced H+ influx, an effect that could be offset by the addition of Ca2+ to the medium.
To determine whether inhibition of corn-root growth by H+ was demonstrably a function of Ca2+ displacement, data were pooled from the figures and tables of Yan et al. (1992). Growth was scaled toRRL max, {H+}0 and {Ca2+}0 were computed, and RRL max was plotted against the surface ion activities in Figure 4. Growth appeared to be inhibited by {H+}0 and enhanced by {Ca2+}0, but in this study, as in most others, {H+}0 and {Ca2+}0 were intercorrelated (Fig. 4c), so an effect of Ca2+other than the mechanism I effect is difficult to discern. Analysis in terms of Equation 3 (incorporating Eq. 4) yielded statistically significant values for a 1 (4.38),b 1 (3.00), anda 2 (5.68). b 2and a 4 could not be evaluated so they were deleted (effectively setting b 2 equal to 1). Apparently, the correlation of {H+}0 with {Ca2+}0 was not strong enough to prevent the evaluation of both a 1and a 2, so one may conclude, in agreement with Yan et al. (1992), that H+-induced Ca2+ displacement accounts for some of the intoxication. Nevertheless, the data set is inadequate for extensive analyses, mainly because of {H+}0 and {Ca2+}0intercorrelations.
Growth of corn seedling roots in response to H+ and Ca2+. Data were taken from Yan et al. (1992). Growth measurements were scaled toRRL max, and activities in the medium and at the PM surface were computed as described elsewhere in the present study. Areas of circles are proportional to {Ca2+}0 or {H+}0, as indicated.
DISCUSSION
The coefficients shown in Table II quantitatively express several characteristics of the studied toxicities and the ameliorative effects of Ca2+. Coefficientsa 1 and a 3relate to the strength of the toxicants. Therefore, Al3+ is at least 10 times more toxic than H+, and H+ is about 1000 times more toxic than Na+ to short-term root elongation in seedlings of cv Scout 66. These relative toxicities may be termed intrinsic because they refer to toxicant activities at the PM surface. Coefficients a 2 andb 2 refer to the requirement for {Ca2+}0 modeled as though it were independent of {T}0. The coefficienta 4 indicates interactions between {Ca2+}0 and {T}0 that are toxicant specific. {Ca2+}0 and {T}0 do not interact in the case of Al3+ toxicity, and the interaction in Na+ toxicity is at least 6-fold greater than in the case of H+ toxicity. The coefficienta 7 indicates that {Mg2+}0 and {Na+}0 also interact and that Ca2+ is about 8 times more effective than Mg2+ as a mechanism III ameliorant.
Electrostatic principles make it almost inevitable that mechanism I would play an important role in the Ca2+alleviation of toxicity by cations, especially multivalent cations. It is surprising, therefore, that such a role for Ca2+ has been stated only rarely (Foy, 1983;Kinraide et al., 1992, 1994; Ryan et al., 1997; Yermiyahu, 1997a). This statement by Foy (1983) clearly differentiates toxicant displacement from Ca2+ replacement: “Beneficial effects of increased concentrations of these elements [Ca, Mg, K, and Na] were probably due to a competitive reduction in Al-root contact, rather than supplying deficient nutrients.” In contrast, mechanism II has been invoked frequently as an explanation for the ameliorative effectiveness of Ca2+ (LaHaye and Epstein, 1969; Hanson, 1984;Cramer et al., 1985; Lynch et al., 1987; Shortle and Smith, 1988;Schulze, 1989; Läuchli, 1990; Rengel, 1992; Yan et al., 1992;Yermiyahu et al., 1997a). However, the present study indicates that mechanism I plays a much more significant role than mechanism II, as illustrated in the following computational analysis (TableIV).
Components of toxicity computed for media supplemented with Al3+, H+, and Na+
An infertile, moderately acidic soil may have a soil solution with a [Ca2+] of 0.5 mm, a pH of 4.5, and an ionic strength of 5 mm (Wright and Wright, 1987) (simulated by 0.5 mm [CaCl2] and 3.5 mm [NaCl] acidified with HCl; Table IV). Three stresses were imposed: addition of 4.3 μmAlCl3, reduction of pH to 4.124, or elevation of NaCl to 126 mm. Each change reducedRRL max to 50 (computed using the coefficients in Table II), but the stress imposed by Ca2+ displacement was minor (A 2 ranged from 0.91 to 0.99). Elevation of CaCl2 relieved the stress, but only insignificantly by mechanism II. MgCl2 was almost as effective as CaCl2 in the alleviation of Al3+ toxicity (compare rows 3 and 4 in Table II), where Mg2+ alleviation can be attributed only to mechanism I. Although trivial, mechanism II contributed more to the alleviation of Na+ toxicity than to the alleviation of H+ or Al3+toxicities (the increase in A 2 from 0.91 to 0.97 in rows 8 and 9 is greater than comparable increases for the other toxicants). Mechanism III was a large component of the alleviation of Na+ (A 1 declined from 0.85 to 0.61 in rows 9 and 10).
Results presented by Cramer et al. (1985) can be interpreted as evidence that Ca2+ is displaced from the root-cell PM surface by high Na+, and Yermiyahu et al. (1997a) measured directly the displacement of Ca2+ by Na+ from the surfaces of PM vesicles. Thus, Na+ toxicity appears to correlate negatively with {Ca2+}0, as do other toxicities (Fig. 4). However, these correlations need not be interpreted as evidence that intoxication is mainly the consequence of Ca2+ displacement. Two alternative explanations for negative correlations between {Ca2+}0 and toxicity are possible. First, high incidental negative correlations between {Ca2+}0 and {T}0 are likely (Yermiyahu et al., 1997a; Fig. 4c) but can be avoided (present study; see Table II). Second, a negative correlation between toxicity and {Ca2+}0 is likely to occur whenever mechanism III alleviation is important. It is important to realize that these correlations do not necessarily demonstrate a mechanism II alleviation. Consequently, correlations between Ca2+ displacement and toxicity may be observed even if Ca2+ displacement plays a small role.
The toxicant-specific nature of mechanism III is not surprising. Consider, as a possibility, that the PM is not very permeable to Al3+, so Al3+ exerts its principal effects at the cell surface, that H+has major effects at the cell surface and in the cell interior, and that Na+ exerts its principal effects intracellularly. If Ca2+ reduces PM leakiness in general (Fawzy et al., 1954; Hanson, 1984; Cramer et al., 1985) and blocks Na+-permeable channels in particular (for reviews and new data, see a special collection of articles by Amtmann et al., 1997; deBoer and Wegner, 1997; Maathuis and Sanders, 1997;Roberts and Tester, 1997; Tyerman et al., 1997; White, 1997), then a differential effectiveness of mechanism III is likely (Fig. 2).
When Ca2+ and toxicant are considered in terms of their bulk-phase intensities, interactions are generally observed, but much of that interaction is indirect and can be attributed to mechanisms I and II. The unmasking of more specific interactions can occur only after these mechanisms have been taken into account. The following steps were used in the present study and may be helpful to others: (1) compute {Ca2+}0 and {T}0; (2) use experimental designs that ensure an adequate range of values for {Ca2+}0 and {T}0 without introducing unwanted correlations between those variables (Ca2+-Mg2+ replacement solutions may be used to vary {Ca2+}0 without varying {T}0); and (3) use statistical methods that incorporate reasonable, descriptive models such as sigmoidal growth responses rather than linear responses, which extrapolate to absurd values.
Mechanisms I, II, and III have been presented in terms of ionic responses at the PM surface, but ion activities in the cell walls may respond similarly, and some of the intoxication and alleviation may originate from that phase. Additionally, the cell wall and the PM may interact to influence ion activities at the PM surface. Almost certainly, the cell surface is the initial site of ionic perturbations, but intoxication and alleviation may be implemented by Ca2+-dependent processes in the cell interior (Rengel, 1992).
CONCLUSIONS
Ca2+ appears to alleviate the effects of rhizotoxic cations by multiple mechanisms. First, the electrostatic displacement of toxicant from PM surfaces may be the most important mechanism in most cases, although it is less important for Na+ toxicity than for Al3+and H+ toxicities. Second, the restoration of toxicant-displaced Ca2+ at PM surfaces is unlikely to be an important mechanism in most cases, although it is more important for Na+ toxicity than for Al3+ and H+ toxicities. Third, a class of interactions between Ca2+ and toxicants is highly specific and may reflect in part the Ca2+ blockade of PM channels that admit toxicants. These conclusions are based on short-term root-growth experiments with wheat seedlings. Growth by other species or organs or growth over longer periods may exhibit other patterns of Ca2+ alleviation of toxicity. Forest decline has been attributed to an insufficient supply of divalent cations to leaves or other tree parts induced by high Al3+ and H+ in soils (Shortle and Smith, 1988; Schulze, 1989). Shoots and roots respond differently to Na+ stress. In the present study leaf and coleoptile stunting persisted after the total alleviation by Ca2+ of root-growth inhibition at high Na+ concentrations, indicating a greater sensitivity of shoot growth to osmotic stress (data not presented). Therefore, roots that express few signs of intoxication may fail to provide adequate water, nutrients, or other growth factors to the shoots.
Footnotes
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↵* E-mail kinraide{at}asrr.arsusda.gov; fax 1–304–256–2921.
Abbreviations:
- ψ0
- electrical potential at the PM surface
- {IΖ}0 and {IΖ}∞
- activity of ionI with charge Ζ at the PM surface and in the bulk-phase medium, respectively
- [IΖ]0 and [IΖ]∞
- concentration of ion I with charge Ζ at the PM surface and in the bulk-phase medium, respectively
- PM
- plasma membrane
- RRLmax
- root elongation in toxicant-bearing solutions relative to maximum elongation in toxicant-free, Ca2+-sufficient solutions
- {T}0
- activity of toxicant at the PM surface
- Received March 9, 1998.
- Accepted June 24, 1998.