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Plant Physiol, March 2001, Vol. 125, pp. 1473-1484
The High Level of Aluminum Resistance in Signalgrass Is Not
Associated with Known Mechanisms of External Aluminum Detoxification in
Root Apices1
Peter
Wenzl,2 *
Gloria M.
Patiño,
Alba L.
Chaves,
Jorge E.
Mayer, and
Idupulapati M.
Rao
Centro Internacional de Agricultura Tropical, A.A. 6713, Cali,
Colombia (P.W., G.M.P., A.L.C., I.M.R.); Institut für
Pflanzenphysiologie, Universität Wien, A-1090 Vienna, Austria
(P.W.); and Center for the Application of Molecular Biology to
International Agriculture, G.P.O. Box 3200, Canberra ACT 2601, Australia (J.E.M.)
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ABSTRACT |
Al resistance of signalgrass (Brachiaria
decumbens Stapf cv Basilisk), a widely sown tropical forage
grass, is outstanding compared with the closely related ruzigrass
(Brachiaria ruziziensis Germain and Evrard cv Common)
and Al-resistant genotypes of graminaceous crops such as wheat,
triticale, and maize. Secretion of organic acids and phosphate by root
apices and alkalinization of the apical rhizosphere are commonly
believed to be important mechanisms of Al resistance. However, root
apices of signalgrass secreted only moderately larger quantities of
organic acids than did those of ruzigrass, and efflux from signalgrass
apices was three to 30 times smaller than from apices of Al-resistant
genotypes of buckwheat, maize, and wheat (all much more sensitive to Al
than signalgrass). In the presence, but not absence, of Al, root apices
of signalgrass alkalinized the rhizosphere more than did those of
ruzigrass. The latter was associated with a shortening of the
alkalinizing zone in Al-intoxicated apices of ruzigrass, indicating
that differences in alkalinizing power were a consequence, not a cause
of, differential Al resistance. These data indicate that the main
mechanism of Al resistance in signalgrass does not involve external
detoxification of Al. Therefore, highly effective resistance mechanisms
based on different physiological strategies appear to operate in this species.
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INTRODUCTION |
Al toxicity is one of the most
important constraints to crop production on acid soils (Rao et al.,
1993 ; De la Fuente-Martínez and Herrera-Estrella, 1999 ).
Al3+ ions, the most toxic mononuclear Al species,
inhibit root elongation by injuring the root apex, particularly the
distal part of the transition zone (Ryan et al., 1993 ; Kinraide, 1997 ;
Sivaguru and Horst, 1998 ). Despite considerable research, the
mechanistic basis of Al toxicity is not well understood (Delhaize and
Ryan, 1995 ; Horst, 1995 ; Kochian, 1995 ; Rengel, 1996 ; Kochian and
Jones, 1997 ). It has been established that Al can cross the plasma
membrane, although the rate of uptake into the symplasm remains a
subject of controversy (Lazof et al., 1997 ; Rengel and Reid, 1997 ;
Taylor et al., 2000 ). Al resistance, accordingly, can be achieved
through "external" mechanisms, which minimize uptake of Al, or
"internal" mechanisms, which detoxify Al within the symplasm.
Two external Al resistance mechanisms based on Al detoxification in the
apoplast and rhizosphere have gained experimental support: (a)
formation of non-toxic Al chelates with Al ligands secreted by root
apices, and (b) alkalinization of the apical apoplast and rhizosphere,
which shifts the concentrations of mononuclear Al species in favor of
less toxic Al hydroxides.
Malate, citrate, and oxalate have been identified as important
Al-chelating ligands secreted by roots (Miyasaka et al., 1991 ; Delhaize
et al., 1993 ; Pellet et al., 1995 ; Ma et al., 1997 , 2000 ; Ma and
Miyasaka, 1998 ; Zheng et al., 1998a , 1998b ; Li et al., 2000 ; Ma, 2000 ;
Matsumoto, 2000 ). They are thought to be involved in Al resistance
because their secretion tends to be localized to apices and associated
with the level of Al resistance and the presence of genes conferring Al
resistance (Delhaize et al., 1993 ; Pellet et al., 1995 ; Ryan et al.,
1995b ; Zheng et al., 1998a ; Ma et al., 2000 ). Stimulation of
organic-acid secretion by overexpression of citrate synthase, or as a
result of mutagenesis, has confirmed this view (De la Fuente et al.,
1997 ; Larsen et al., 1998 ; Koyama et al., 1999 ). Chelation of
apoplastic and rhizospheric Al by phosphate appears to contribute to Al
exclusion in certain cultivars or species (Lindberg, 1990 ; Millard et
al., 1990 ; Pellet et al., 1996 , 1997 ). The isolation of an Al-resistant
Arabidopsis mutant that increases the pH of the apical rhizosphere
under Al stress has confirmed the long-standing hypothesis that a
stronger alkalinization of the rhizosphere can increase Al resistance
(Taylor, 1991 ; Degenhardt et al., 1998 ).
To date, most studies of Al-resistance mechanisms have focused on
Al-resistant genotypes of crops that have a long breeding history.
Because past breeding programs have rarely selected for Al resistance,
the single major resistance genes, frequently encountered in resistant
cultivars, may have resulted from random fixation or be a by-product of
selection for other agronomic features carried out on (moderately) acid
soils (McNeilly, 1994 ). Although virtually nothing is known about its
genetic basis in wild species (McNeilly, 1994 ), Al resistance is likely
to be a genetically and physiologically complex trait (Taylor, 1991 ;
Dvorák et al., 1992 ). Hence, physiological studies on bred crop
varieties may have over-emphasized resistance mechanisms that confer a
moderate level of Al resistance at best.
Signalgrass (Brachiaria decumbens Stapf cv Basilisk) is one
of the most widely sown forage grasses in the tropics with 26.4 million
ha in Brazil alone. Unlike most food crops, it is directly derived from a wild apomictic germplasm accession that is highly resistant to Al and well adapted to infertile acid soils (Sánchez and Salinas, 1981 ; Paulino et al., 1987 ; Keller-Grein et al., 1996 ; Rao
et al., 1996 ). Ruzigrass (Brachiaria ruziziensis Germain and
Evrard cv Common), a closely related species of the same agamic complex
(Miles and do Valle, 1996 ), is less Al-resistant and can thus be used
as a reference for comparative studies.
The aim of this study was to investigate whether Al resistance
mechanisms found in bred crops are responsible for the high level of Al
resistance in signalgrass. Our experimental set up was
multi-tiered. First, we quantified Al resistance levels of the two
Brachiaria species and compared them with Al-resistant genotypes of other plant species reported in the literature. We subsequently carried out a series of experiments to investigate whether
Al resistance of signalgrass could be attributed to more effective
external detoxification mechanisms.
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RESULTS |
Al Resistance of Brachiaria Spp.
Signalgrass and ruzigrass showed a highly significant difference
in Al resistance (P < 0.004 for species × Al
level, and P < 10 11 for
species; Fig. 1A). For quantitative
comparison, the Al3+ activity inhibiting root
elongation by 50%
({Al3+}50) was computed
for each species and compared with
{Al3+}50 of wheat,
triticale, maize, and Arabidopsis genotypes, calculated from data in
the literature. The
{Al3+}50 value of
signalgrass (49.5 ± 1.1 µM; mean ± SE) was several times greater than that of
Al-resistant genotypes of other species (Fig. 1B). Only limited
root-elongation data for buckwheat (Fagopyrum esculentum), which has been described as "highly
Al-resistant," is available (see figs. 1 and 9 in Zheng et al.,
1998a ). However, growth of buckwheat was inhibited in an Al-containing
nutrient solution that did not affect growth of ruzigrass, indicating
that Al resistance of signalgrass would be significantly superior to that of buckwheat (Osaki et al., 1997 ).

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Figure 1.
Al resistance of signalgrass (B. decumbens) and ruzigrass (B. ruziziensis), quantified
with a root elongation assay in simple salt solutions. A, Relative root
elongation (RRE; see Eq. 1 in "Materials and Methods") of 4-d-old
seedlings exposed to 200 µM
CaCl2 (pH 4.2), containing 0 to 200 µM AlCl3, for 3 d
(means ± SE of 27-36 seedlings).
RE0 was 40.8 mm (signalgrass) and 39.8 mm
(ruzigrass). RE was 9.8 mm for ruzigrass, but
could not be measured for signalgrass because this would have required
Al levels predicted to cause precipitation of
Al(OH)3. RE of
signalgrass was thus estimated, assuming a constant
RE0/RE ratio for both
species (10.0 mm). RRE values as a function of the Al3+
activity in the treatment solution were fitted to Equation 2 (solid
lines). Asterisks denote statistically significant interspecific
differences (P < 0.05). B, Comparison of Al resistance
of Brachiaria spp. with contrasting genotypes of other
species. RRE data were taken from the literature to determine
{Al3+}50, the
Al3+ activity causing a 50% inhibition in root
elongation (Eqs. 3 and 4). Assay conditions for these genotypes were as
follows: Arabidopsis, 0 to 2.5 µM
AlCl3, 100 µM
CaCl2 (pH 5.2) for 5 d (Toda et al., 1999 );
wheat, 0 to 10 µM AlCl3,
200 µM CaCl2 (pH 4.3) for
7 d (ES3 and ET3; Ryan et al., 1995b ) or 0 to 150 µM AlCl3, 400 µM CaCl2 (pH 4.5) for
2 d (Atlas 66; Kinraide et al., 1992 ); triticale, 0 to 50 µM AlCl3, 500 µM CaCl2 (pH 4.5) for
1 d (Ma et al., 2000 ); and maize, 0 to 142 µM AlCl3, approximately
230 µM CaCl2 (pH 4.3) for
3 d (Pellet, 1993 ).
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The effect of Al on root growth was also assessed in low-ionic-strength
nutrient solutions that simulate soil solutions of acid soils in
neotropical savannas. Growth in these solutions reflected the
differential Al resistance detected in the short-term root-elongation
assay. Fresh weight of roots of ruzigrass, classified as
"Al-tolerant" by Osaki et al. (1997) , was markedly more
affected by Al than that of signalgrass (P < 10 5 for species × Al level; Fig.
2B). Roots of ruzigrass, but not of
signalgrass, showed symptoms of Al injury at both Al levels, including
stubby appearance, a large number of short laterals close to the apex
of the main root axis, and deformed root apices that stained strongly
with hematoxylin (Fig. 2A). The mean apical diameter of adventitious
roots of ruzigrass increased from 0.39 to 0.55 mm, but the effect was
significantly smaller in the case of signalgrass (from 0.40 to 0.44 mm;
P < 10 5 for species × Al
level, Fig. 2C). Furthermore, ruzigrass accumulated more Al
(P < 0.03 for species × Al level and
P < 10 4 for species) and
callose (P < 10 19 for species)
in apices of adventitious roots than did signalgrass (Fig. 2, D and
E).

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Figure 2.
Differential manifestation of Al stress
symptoms in roots. Signalgrass (B. decumbens) and ruzigrass
(B. ruziziensis) were cultivated at increasing levels of Al
in low-ionic-strength nutrient solutions for 13 d. A, Al injury at
apices of adventitious roots, visualized by hematoxylin staining. B,
Root fresh weight per tray containing 200 seedlings (means ± SE; n = 6-7). C, Apical diameter
of adventitious roots (means ± SE for three
images containing 150-350 apices each). D, Al content of apices from
adventitious roots (means ± SE of 10-17
groups of five apices each). E, Callose concentration in apices of
adventitious roots expressed as Pachymann equivalents (means ± SE of 11 or 12 groups of five apices each).
Asterisks denote statistically significant interspecific differences
(P < 0.05).
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Organic-Acid Exudation by Whole Roots
Whole-root exudates contained citrate, malate, and oxalate in
addition to minor amounts of lactate, cis- and
trans-aconitate, maleate, and fumarate. All acids, except
cis-aconitate and fumarate, could also be detected in soil
solutions extracted by centrifugation from a sandy-loam Oxisol in which
ruzigrass had been cultivated (oxalate was not detectable because of
baseline problems; data not shown). In addition to these acids, there
were three unidentified peaks, for which pyruvate, tartrate, succinate,
malonate, L-glycerate, glycolate, quinate,
shikimate, phtalate, and ferulate were ruled out. Larger quantities of
these unknown compounds were secreted by ruzigrass than by signalgrass,
and Al stimulated their exudation in ruzigrass but not in signalgrass
(data not shown).
Although citrate exudation was stimulated in both species by
approximately 5 times under Al stress (P < 0.001),
ruzigrass secreted significantly larger amounts than signalgrass under
all conditions (P < 0.002; Fig.
3). Al also triggered a 10-fold increase in oxalate exudation by roots of ruzigrass but had no effect on oxalate
exudation from roots of signalgrass, which secreted oxalate at a higher
basal level (P < 10 3 for
species × Al level). Exudation of malate was not affected by Al
in either species (P < 0.9; Fig. 3). Al stress
stimulated the overall rate of organic-acid exudation of both species
(P < 0.04), but the data suggest that on exposure to
Al, ruzigrass secreted larger quantities than did signalgrass
(P < 0.09).

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Figure 3.
Efflux of oxalate, citrate, and malate from whole
roots of signalgrass (B. decumbens) and ruzigrass (B. ruziziensis) (means ± SE of five to six groups
of five plants each). Plants were cultivated as in Figure 2, and
exudates were collected during 1 h in the same nutrient solutions
in which the plants had been cultivated. Asterisks denote statistically
significant interspecific differences (P < 0.05).
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Secretion of Al Ligands by Root Apices
Root apices released less citrate, oxalate, and malate (up to 17 pmol mm 2 h 1; Fig.
4) than whole roots (up to 65 pmol
mm 2 h 1; Fig. 3). Levels
of organic acids in apical exudates consequently were close to the
limit of detection in some samples. Efflux of malate, only detectable
in signalgrass, was greater than efflux of other acids. It was
stimulated by Al present in the solution bathing root apices
(P < 10 5). Apices from plants
that had been cultivated in the presence of Al released greater amounts
of oxalate (P < 10 3) and
citrate (P < 10 9) but not
malate (Fig. 4).

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Figure 4.
Efflux of oxalate, citrate, and malate from root
apices (means ± SE of three to five groups of 30 apices each). Ruzigrass (upper row) and signalgrass (lower row) were
cultivated as in Figure 2. Organic acids secreted by root apices were
collected during a 2-h incubation of excised apices in 200 µM CaCl2 (pH 4.2),
containing a varying level of Al. Dotted lines indicate approximate
detection limits. Efflux of citrate from apices of plants cultivated in
the absence of Al, and efflux of malate from apices of ruzigrass, were
below the limit of detection.
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Measurement of organically complexed monomeric Al
(Alorg) confirmed that only a very small fraction
of the monomeric Al in treatment solutions was complexed by chelating
ligands secreted by root apices of either species (3 ± 2 µM; mean ± SD). The inferred efflux of
Al-chelating equivalents (7 to 10 pmol mm 2
h 1) was somewhat smaller than the combined
efflux of oxalate, citrate, and malate.
Phosphate efflux from root apices was smaller than organic-acid efflux
(measured range in the presence of Al: 1.2-5.9 pmol mm 2 h 1). Apices of
signalgrass tended to release less phosphate than those of ruzigrass.
The presence of Al during cultivation of plants stimulated phosphate
secretion from apices of ruzigrass up to 4-fold but had little effect
in signalgrass (data not shown).
Alkalinization of the Apoplast and Rhizosphere of Root Apices
Apices of intact roots, as well as excised root apices,
alkalinized the apoplast in a region up to approximately 1.2 mm from the tip, as indicated by the blue color of bromocresol green in the
apoplast (data not shown). Alkalinization was strongest in the
subapical region from approximately 0.4 to 1.2 mm, presumably the
transition zone between the meristem and the elongation zone because
cells started elongating just outside this zone. In contrast, acidification dominated in the elongation zone and more mature parts of
root apices, as indicated by the yellow color of the dye (data not
shown). The latter confirmed that the dye did not penetrate the
symplasm because this would have caused a uniform blue color as a
result of the high cytoplasmatic pH. Injured tissue at the site of
excision accumulated more dye, but did not contribute to
alkalinization, as indicated by the dye remaining yellowish green (data
not shown).
Excised root apices of both species, grown in the absence of Al, caused
a pH increase in the Al-free treatment solution of 0.0045 per
mm2 of apical surface area and hour (Fig.
5A, {Al3+} = 0 µM). This is equivalent to a net influx of
H+ equivalents into root apices of 219 pmol mm 2 h 1
(see "Materials and Methods"). Exposure to Al during cultivation reduced the alkalinizing power of apices in ruzigrass more than in
signalgrass (P < 10 5 for Al
level and P < 0.002 for species; Fig. 5A).
Furthermore, presence of Al during incubation of root apices appeared
to inhibit alkalinization in ruzigrass, as indicated by the
differential pH increase caused by apices of the two species grown in
the absence of Al (Fig. 5B, {Al3+} = 0 µM). Under continuous exposure to Al, root
apices of signalgrass therefore maintained a higher pH in the apoplast
and rhizosphere than did the apices of ruzigrass (P < 10 3; Fig. 5B,
{Al3+} > 0 µM).

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Figure 5.
Surface area-based rates of alkalinization of
solutions bathing excised root apices of signalgrass (B. decumbens) and ruzigrass (B. ruziziensis) (means ± SE of four to six groups of 30 apices each). Plants were
cultivated at increasing Al levels as in Figure 2. Excised root apices
were incubated for 2 h in 200 µM
CaCl2 (pH 4.2), containing either no Al or
{Al3+} = 115 µM. A,
Incubation of excised root apices without Al. B, Incubation of apices
at {Al3+} = 115 µM.
Asterisks denote statistically significant interspecific differences
(P < 0.05).
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DISCUSSION |
Al Resistance of Signalgrass Is Outstandingly High Compared with
Other Species
A widely used assay for quantifying Al resistance is based on the
measurement of root elongation of seedlings in simple salt solutions in
which the Al3+ activity
{Al3+} can be predicted with precision
(Kinraide et al., 1985 ). Using such an assay, we found Al resistance of
signalgrass to be markedly superior than that of ruzigrass, previously
classified as "Al-tolerant" (Osaki et al., 1997 ). Al resistance of
signalgrass is clearly outstanding compared with Al-resistant genotypes
of cereal crops (Fig. 1). The basal solution used for assaying Al
resistance of the most resistant cereal genotypes, i.e. Atlas 66 (wheat) and ST2 (triticale), contained at least twice as much
Ca2+ as the solution used for
Brachiaria spp. (400-500 versus 200 µM; see legend to Fig. 1). It is well
established that Ca2+ ions alleviate Al toxicity
(Kinraide, 1998 ). Because of this and the significantly smaller size of
Brachiaria seeds, which may therefore supply less nutrients
to the elongating primary root, the level of Al resistance of
signalgrass was almost certainly underestimated in the comparison.
The outstandingly high level of Al resistance of signalgrass was
underscored by the finding that growth was only moderately inhibited in
a low-ionic-strength nutrient solution at
{Al3+} = 115 µM
(Fig. 2B). This Al3+ activity, in terms of charge
equivalents, is comparable with the sum of activities of all cationic
macronutrients, plus Na+, in the nutrient
solution (Table I). It should be noted
that such high Al3+ activities are only rarely
found in soil solutions of acid soils (Wright et al., 1989 ; Menzies et
al., 1994 ). Interspecific differences in other well known Al-toxicity
symptoms, such as hematoxylin staining, lateral swelling of root
apices, and callose synthesis, also reflected the high resistance level
of signalgrass compared with ruzigrass (Fig. 2, A, C, and E).
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Table I.
Composition of the low-ionic-strength nutrient
solutions used for plant cultivation and the simple salt solutions used
for incubating excised root apices
Activities of major ions and ion complexes were predicted with GEOCHEM
2.0. The pH of all solutions was adjusted to 4.2 by adding calculated
amounts of HCl.
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A long evolutionary history of exposure to Al is likely to favor the
development of highly adapted genotypes with polygenic control of
resistance, because Al resistance can be modified by a considerable
number of genes (Larsen et al., 1996 ; Schott and Gardner, 1997 ; Ezaki
et al., 1999 , 2000 ). Species of agricultural interest tend to be less
Al-resistant than "wild species" (Wheeler et al., 1992 ; Crawford
and Wilkens, 1998 ). Even an acid-soil adapted cultivar of rice,
which is considered to be an Al-resistant species, was severely
affected by Al toxicity when grown in the nutrient solution
containing {Al3+} = 43 µM
(data not shown). These findings suggest that agricultural species may
not have been exposed to Al toxicity during their evolution. Resistance
genes originally present in species derived from acid soils,
alternatively, may have been lost in the course of genetic-improvement
programs aiming at other breeding objectives. In contrast, the root
elongation assay convincingly demonstrated that signalgrass has
preserved the high level of Al resistance that characterized the
original apomictic germplasm accession.
External Detoxification by Chelating Ligands Is Not Responsible
for the High Level of Al Resistance in Signalgrass
Root apices of signalgrass accumulated less Al than those of
ruzigrass (Fig. 2D). Whereas this might have been the result of a more
pronounced growth-induced dilution of Al in apices of rapidly
elongating signalgrass roots, it could also indicate that mechanisms
excluding Al from root apices contribute to the greater Al resistance
of signalgrass.
External Al detoxification by secreted organic acids is a
well-documented mechanism excluding Al from root apices. Elevated rates
of organic-acid secretion in response to Al stress can be detectable at
the level of the whole root system (Miyasaka et al., 1991 ; Ma et al.,
1997 ; Ma and Miyasaka, 1998 ; Zheng et al., 1998b ; Li et al., 2000 ).
This was also the case in the Brachiaria spp. (Fig. 3). Yet,
the stronger stimulation of citrate exudation by Al in ruzigrass, the
absence of a stimulatory effect of Al on oxalate exudation in
signalgrass, and the larger overall amount of organic acids exuded by
roots of ruzigrass at high Al levels (154 versus 59 pmol
mm 2 h 1), indicate that
a more intense exudation of organic acids by whole roots was not linked
to a higher level of Al resistance in these species.
This conclusion is not invalidated by the theoretical possibility that
organic-acid exudation may have been stimulated as a result of
Al-induced P deficiency, rather than Al toxicity itself (Miyasaka et
al., 1991 ), because control measurements showed that the P content of
shoots of both species was above the critical internal level for
Brachiaria (data not shown; Sánchez and Salinas, 1981 ). Furthermore, the phosphate concentration in nutrient solutions was probably too low ( 1 µM) to cause
depletion of phosphate due to precipitation with Al. In addition, the
more intense exudation of organic acids from roots of ruzigrass should
have contributed to its overall Al resistance, irrespective of whether
it was stimulated by Al itself or by Al-induced P deficiency.
Measurements of organic acids released by root apices ruled out the
possibility that in signalgrass organic-acid efflux was more confined
to root apices than in ruzigrass. Rates of organic-acid secretion,
calculated on a surface-area basis, were only approximately one-fifth
of those observed at the level of whole roots in either species,
despite the possibility that organic acids may have been released from
injured cells at the cut surface of excised apices (Figs. 3 and 4).
This finding contrasts sharply with the Al-stimulated efflux of malate
and citrate localized to root apices of wheat and maize, respectively
(Delhaize et al., 1993 ; Pellet et al., 1995 ; Ryan et al., 1995a ).
Quantification of organically complexed Al
(Alorg) in solutions bathing excised root apices
demonstrated that they did not release appreciable amounts of
unidentified Al ligands.
The absence of any apparent effect of excision on Al uptake by root
apices (see "Materials and Methods") suggests that the low rates of
organic-acid secretion were not an artifact of the experimental
protocol. This is because inhibition of an Al exclusion mechanism based
on organic-acid secretion as a result of excision should have
stimulated Al uptake. Low rates of organic-acid secretion from root
apices coincided with high concentrations within apices, whereas the
reverse was true at the whole-root level (P. Wenzl, A.L. Chaves, G.M.
Patiño, J.E. Mayer, and I.M. Rao, unpublished data). This
indicates that, in contrast to mature root sections, organic acids were
selectively retained within root apices.
These data suggest that detoxification of extracellular Al by
organic acids plays a secondary role in the outstanding
resistance of signalgrass to Al. This conclusion is based on several
lines of evidence. First, root apices of signalgrass secreted only
moderately larger amounts of organic acids than did those of
ruzigrass: The maximum efflux of Al-chelating equivalents was 26 pmol mm 2 h 1 in
signalgrass and 10 pmol mm 2
h 1 in ruzigrass (0.5 × oxalate + 1 × citrate + 1 × malate; Fig. 4). Second, the moderately greater
organic-acid efflux from apices of signalgrass was largely due to
malate, which is a poorer Al chelator than citrate and oxalate. Third,
maximum efflux of oxalate, citrate, and malate at root apices of
signalgrass was 3.4, 12, and 30 times lower than in buckwheat, maize
(cv South American 3), and wheat (near-isogenic line ET3),
respectively, all considerably more sensitive to Al (Pellet et al.,
1995 ; Ryan et al., 1995a ; Zheng et al., 1998a ). Finally, on exposure to
Al, whole roots of ruzigrass exuded larger quantities of organic acids
than did roots of signalgrass.
In certain Al-resistant plant varieties, phosphate released from root
apices is thought to generate an apoplastic sink for Al3+ ions in a manner similar to organic acids
(Lindberg, 1990 ; Millard et al., 1990 ; Pellet et al., 1996 , 1997 ). The
greatest efflux measured for apices of signalgrass in the presence of
Al was 22 pmol apex 1
h 1. This is 30-fold lower than the value
reported for the Al-resistant wheat cv Atlas 66 (680 pmol
apex 1 h 1; Pellet et
al., 1996 ). Root apices of less Al-resistant ruzigrass released similar
or greater amounts of phosphate (data not shown). These findings rule
out a significant contribution of phosphate efflux from root apices to
Al resistance of signalgrass.
The Greater Alkalinizing Power of Root Apices of Signalgrass
Is a Consequence, Not a Cause, of Its Greater Al Resistance
A long-standing hypothesis states that certain plants resist Al
toxicity by increasing the pH around their roots (Taylor, 1991 ;
Degenhardt et al., 1998 ). Using apices soaked in a pH sensitive dye, we
found that the transition zone and, to a lesser extent, the
meristematic zone alkalinize the apoplastic space (data not shown).
This pH increase is likely to reflect a transcellular proton current,
typically associated with polarized growth (Ryan et al., 1992 ).
Although wounding can generate a positive inward current similar to
that in the transition zone (Miller et al., 1988 ), the cut surface of
excised Brachiaria root apices did not contribute to
alkalinization (data not shown). Furthermore, the kinetics of
alkalinization of the apoplast was identical for excised and nonexcised
root apices (data not shown). We are therefore confident that
alkalinization of solutions bathing excised root apices was principally
caused by a proton influx in the transition zone, and was
representative of intact root apices.
Given the close association of apical proton current with active growth
of root apices, it has been argued that a greater H+ influx is a consequence, rather than a cause,
of Al resistance (Miyasaka et al., 1989 ; Ryan et al., 1992 ; Kollmeier
et al., 2000 ). Although this assumption is not generally valid, as
exemplified by an Arabidopsis mutant (Degenhardt et al., 1998 ), it is
consistent with the greater Al susceptibility of the influx of
H+ equivalents into root apices of ruzigrass.
The latter is evident from the weaker alkalinizing power of root
apices from ruzigrass cultivated in the presence of Al (Fig. 5A,
{Al3+} > 0 µM)
and ruzigrass apices exposed to Al after excision (Fig. 5B,
{Al3+} = 0 µM).
A likely reason for the reduced alkalinizing power of Al-stressed root
apices of ruzigrass was the shortening of the alkalinizing zone caused
by Al stress, which was only observed in this species (data not shown;
Kinraide, 1988 ). These data are therefore best explained by a greater
Al susceptibility of the growth-associated influx of
H+ equivalents into root apices of ruzigrass, a
view that accords with its greater Al sensitivity.
External Al Detoxification Mechanisms May Not Be Efficient Enough
for Highly Acidic Soils
The finding that Al resistance of signalgrass is independent of
external detoxification of Al by organic acids or phosphate raises the
question whether prolonged selective pressure exerted by Al-toxic soils
has favored other resistance strategies, because external
detoxification mechanisms are not sufficiently effective, or
metabolically economical, for highly acidic soils. Stoichiometric considerations would indeed suggest that the amount of organic acids
secreted by root apices of Al resistant wheat and maize genotypes might
only be adequate to detoxify Al at concentrations well below those
inhibiting root growth of signalgrass (Delhaize et al., 1993 ; Pellet et
al., 1995 , 1997 ; Ryan et al., 1995b ; Parker and Pedler, 1998 ). The
effectiveness of Al resistance mechanisms based on external chelation
of Al3+ by chelating ligands may also be limited
by other cell-surface ligands competing for Al ions (Parker and Pedler,
1998 ), the presence of other cations capable of forming complexes with
organic acids (Jones and Darrah, 1994 ), adsorption of organic acids to
the soil's exchange phase (Jones et al., 1996a ), and rapid microbial
degradation of organic acids in soils (Jones et al., 1996b ). In
addition, an Al exclusion mechanism based on the efflux of phosphate
may be of questionable adaptive value in highly weathered acid soils where P is the principal limiting nutrient.
 |
CONCLUSIONS |
We have presented evidence that currently prevailing models of Al
resistance mechanisms, based on external detoxification of Al by
chelating ligands or alkalinization, do not adequately account for the
outstanding resistance of signalgrass to Al. This suggests that
mechanisms based on other physiological strategies, for example a low
Al permeability of the plasma membrane, an active Al extrusion from the
symplasm, or a greater tolerance to symplastic Al, could be responsible
for the high resistance level of this species.
 |
MATERIALS AND METHODS |
Quantifying Al Resistance
Al resistance of signalgrass (Brachiaria
decumbens Stapf cv Basilisk) and ruzigrass (Brachiaria
ruziziensis Germain & Evrard cv Common) was quantified by
measuring elongation of primary roots of seedlings cultivated in 200 µM CaCl2 (pH 4.2), containing 0, 25, 50, 100, or 200 µM AlCl3. Al3+ activities
{Al3+} were calculated with GEOCHEM 2.0 (Parker et al.,
1987 ), using the stability constants given by Nordstrom and May (1989)
and the solubility constant for Al(OH)3 suggested by
Kinraide and Parker (1989) . The amount of HCl required for adjusting
the pH to 4.2 (64.9, 61.5, 58.1, 51.6, and 39.2 µM for
the control and the various Al treatments) was predicted with GEOCHEM
2.0 and confirmed empirically using high-quality de-ionized water (18 M ; measured range: 4.15-4.23).
Scarified seeds of signalgrass (tetraploid, apomictic; Agrosemillas,
Medellín, Colombia) and ruzigrass (CIAT 654; diploid, sexual;
CIAT, Cali, Colombia) were surface-sterilized in 70% (v/v) ethanol for 1 min and 2% (w/v) NaOCl, 0.1% (v/v) Triton
X-100 for 15 min. After 4 d of germination in 200 µM
CaCl2 (pH 4.2), uniform seedlings were transferred to
constantly aerated control and Al solutions. The seedlings were left to
grow in a growth chamber at 24°C and a 12-h diurnal cycle with a
photon-flux density of approximately 110 µmol m 2
s 1. Root elongation was measured after 3 d, during
which the pH of the control and Al treatments remained constant. Data
from three independent experiments were pooled to compute relative root
elongation (RRE) according to the following formula:
|
(1)
|
in which REAl is the root elongation in the
presence of Al, RE is the mean residual elongation at Al
levels sufficient to saturate growth inhibition, and RE0 is
the mean elongation in the Al-free control solution. To compare Al
resistance of Brachiaria with that of other species, RRE
values obtained in this and other studies conducted under comparable
conditions (see legend to Fig. 1B) were fitted to a Weibull-type
equation (Kinraide, 1997 ), using the Marquardt-Levenberg algorithm for
non-linear regression (r2 > 0.99 in
all cases):
|
(2)
|
The activity of Al3+ required to decrease RRE by
50% ({Al3+}50) was calculated from fitted
values of the empirical parameters a and
b according to the formula:
|
(3)
|
The SE of {Al3+}50 was
estimated by computing the propagation of the SEs of
a and b, estimated by the
Marquardt-Levenberg algorithm, that is:
|
(4)
|
Al3+ activities in treatment solutions described in
the literature were calculated, where necessary, with GEOCHEM 2.0 as outlined above, but disallowing precipitation of
Al(OH)3, although some of the treatment solutions were
over-saturated, according to the Kinraide and Parker constant
(1989) .
Obtaining Plant Materials
Cultivating Plants in Low-Ionic-Strength Nutrient Solutions
Plants were cultivated in large numbers in a glasshouse at CIAT
(Cali, Colombia; 3° 30' N, 76° 21' W; altitude, 965 m; typical maximum/minimum temperature and relative humidity, 36/19°C and 96/48%; typical maximum photon-flux density during the day, 1,100 µmol m 2 s 1). For germination, sterilized
seeds were distributed on mosquito nets glued to Styrofoam frames
floating on 10 L of an Al-free low-ionic-strength nutrient solution (pH
4.2). The solution contained low nutrient concentrations, comparable
with those found in soil solutions of the highly weathered Oxisols in
the Colombian savannas (P. Wenzl, J.E. Mayer, R. Albert, and I.M. Rao,
unpublished data). The composition was (in µM): 100 NO3 , 10 NH4+, 60 K+, 60 Ca2+, 30 Mg2+, 160 Na+, 1 H2PO4 , 100 SO42 , 5 Fe3+, 1 Mn2+,
1 Zn2+, 0.2 Cu2+, 6 H3BO3, 5 SiO32 , 0.001 MoO42 , 5 H2-EDTA2 ,
108.4 Cl (excluding HCl), and 65.4 HCl to adjust the pH
to 4.2 (GEOCHEM 2.0).
After 5 d, groups of 200 seedlings were transferred to fresh
floating devices and cultivated for another 12 d in continuously aerated nutrient solutions. These solutions contained identical nutrient concentrations as the solution used for germination and 0, 80, or 225 µM Al3+, 108.4, 348.4, or 783.4 µM Cl and 65.4, 55.4, or 38.4 µM HCl, respectively. These Al concentrations resulted in
{Al3+} = 0, 43, and 115 µM,
respectively (GEOCHEM 2.0; Table I). Solutions were renewed 2, 4, 6, 8, 9, 10, and 11 d after transfer of seedlings. The pH of nutrient
solutions showed a tendency to increase. The highest pH values were
observed at harvest on d 13: 4.5 ± 0.1, 4.3 ± 0.1, and
4.4 ± 0.1 for signalgrass and 4.7 ± 0.4, 4.3 ± 0.1, and 4.3 ± 0.1 for ruzigrass grown at {Al3+} = 0, 43, or 115 µM, respectively (means ± SD).
For each combination of species × treatment, we used three
independent cultivations with two to three containers, each holding 200 plants, resulting in 8,400 plants in all. The large number was needed
to obtain adequate measurements, because primary roots were too thin to
detect organic-acid efflux from apices, and only a part of the plants
developed adventitious roots by harvest time.
Harvesting Roots and Root Apices
To collect exudates from whole roots, a group of five plants was
selected at random from each container. Next, 3-mm apices were excised
from adventitious roots of approximately 20 plants from each container
and grouped for the following analyses: (a) to measure Al content, one
to three groups of five apices each were dried at 70°C for 48 h,
and (b) to quantify callose content, one to two groups of five apices
each were collected in 500 µL 100% (v/v) ethanol and stored
at 4°C. The remaining apices of adventitious roots (approximately 60 per container) were used to study both secretion of organic acids and
phosphate and to investigate alkalinization of the apoplast and rhizosphere.
Physiological Studies
Collecting Root Exudates from Whole Roots
Roots were gently rinsed with sterile 200 µM
CaCl2 (pH 4.2) and transferred to 40 mL of the same
(sterile) nutrient solution in which plants had been cultivated. Root
exudates, collected over 1 h under continuous aeration, were
concentrated in two steps under reduced pressure at 40°C to 60°C
and dissolved in 300 µL 0.3 N HCl to ensure that all Al
and Ca salts present in the concentrated nutrient solution were soluble
(GEOCHEM 2.0). Controls confirmed that this protocol did not degrade
organic acids and that HPLC retention times of organic acids did not
change in the presence of Al. Incubation tests similar to those of
Zheng et al. (1998a) showed that organic-acid-degrading micro-organisms
did not interfere with the collection of root exudates.
Collecting Organic Acids and Phosphate Released from Root
Apices
To quantify organic acids secreted by root apices, apices of
adventitious roots, previously washed in sterile nutrient solutions, were excised at 3 mm. They were collected in groups of 30 in 5-mL glass
vials containing 1 mL of sterile 200 µM CaCl2
(pH 4.2) on a rotary shaker at 100 rpm to permit recovery from injury
(Gronewald and Hanson, 1980 ). When excision of apices from a group of
plants was complete (approximately 30 min), they were continued to
incubate for another 30 min. They subsequently were rinsed once with 1 mL of sterile 200 µM CaCl2, containing 0, 68, or 200 µM AlCl3 at pH 4.2 (resulting in the
same Al3+ activities as in nutrient solutions; Table I),
and suspended in another 1 mL of either of these treatments. After a
secretion period of 2 h, the treatment solutions were removed.
Approximately two-thirds of them were dried in a SpeedVac centrifuge at
40°C and used to analyze secreted organic acids and phosphate. Some solutions were used in an incubation test (Zheng et al., 1998a ) to
ensure that microbial degradation of organic acids was not a problem.
Quantifying Secreted Organic Acids by HPLC
The residues containing root apical exudates were dissolved in
45 µL de-ionized water and centrifuged at 14,000g for
10 min. Aliquots (25 µL) were analyzed on an Aminex HPX 87H ion
exclusion column (300 × 7.8 mm), using isocratic elution with 12 mM H2SO4 at 0.4 mL
min 1 and 30°C. Organic acids were detected by
monitoring absorption at 210 nm and identified and quantified by
comparing retention times and peak areas with a mixture of standards
composed of cis- and trans-aconitate, citrate,
fumarate, lactate, maleate, malate, malonate, oxalate, succinate, and
tartrate. Concentrated exudates collected from whole roots were
analyzed under identical conditions after passing them through a
0.45-µm filter.
Quantifying Phosphate Secreted by Root Apices
Twelve microliters of the concentrated apical exudates was
diluted with de-ionized water to 100 µL. Phosphate was quantified by
measuring A622, after adding 10 µL of the
Malachite green reagent described by Shimogawara and Usuda (1995) .
Control experiments demonstrated that Al, present in some solutions,
did not interfere with this assay.
Investigating Alkalinization Caused by Root Apices
Intact adventitious roots, or excised root apices (3 mm) that
had been washed in 200 µM CaCl2 (pH 4.2) for
1 h, were used to visualize apoplastic pH. After being soaked in 2 mM bromocresol green (pKa = 4.7), 200 µM CaCl2 (pH 4.2) for 15 min, the apices were
transferred to the surface of slices of 0.7% (w/v) agarose, previously equilibrated with 200 µM CaCl2 (pH
4.2). They were photographed 20 min later when color development had
reached its maximum. The pH of approximately one-third of the solutions
containing apical exudates was determined using a pH electrode
specifically designed for low-ionic-strength solutions (Markson
LabSales, Hillsboro, OR; highest value measured in Al treatments:
4.54). In the case of the treatment solution lacking Al, the increase
in pH was converted into a net influx of H+ equivalents by
calculating the amount of protons that had to be removed from the
solution to adjust the pH to the measured values (GEOCHEM 2.0).
Quantifying the Amount of Al Chelated by Ligands Released from
Root Apices
The inorganic monomeric Al remaining in solutions after
incubation of excised root apices was quantified with pyrocatechol violet (Kerven et al., 1989 ; maximum depletion: 44.0 µM,
i.e. 22% of the initial 200 µM AlCl3). Total
monomeric Al (Almono) was measured, using the
pyrocatechol-violet assay described by Menzies et al. (1992) . The
concentration of monomeric Al complexed by Al ligands secreted from
root apices (Alorg), was calculated from the difference
between Almono and inorganic monomeric Al.
Measuring Al in Root Apices
Root apices were digested in a 2:1 mixture of 65% (w/w)
HNO3 and 70% (w/w) HClO4 at 200°C for
2 h, and their Al content was analyzed by atomic absorption
spectroscopy, using an UNICAM 969 spectrophotometer (UNICAM, Cambridge,
UK) equipped with a graphite furnace. Adventitious roots, selected at
random, were stained with hematoxylin according to Polle et al.
(1978) .
Testing the Effect of Excision of Root Apices on Al Uptake
Excised root apices have been widely used for physiological
studies of Al uptake and organic-acid metabolism (Chang and Roberts, 1989 ; Ryan et al., 1995a ; Pellet et al., 1996 , 1997 ; Archambault et
al., 1997 ; Pellet et al., 1996 , 1997 ; Zheng et al., 1998a ), but one
report suggested that excision might artificially stimulate Al uptake
by root apices (Samuels et al., 1997 ). Rates of Al uptake into intact
root apices, estimated from the apical Al content and the rate of root
elongation of adventitious roots measured during the last day of plant
cultivation, were found to be statistically indistinguishable from
rates of Almono depletion from solutions bathing excised
root apices (data not shown). Excision therefore did not significantly
stimulate Al uptake by root apices.
Determining Callose in Root Apices
Root apices, stored in ethanol at +4°C, were washed once with
de-ionized water, and callose was determined according to Köhle et al. (1985) , using Pachymann (Fluka, Milwaukee, WI) as a reference.
Root Image Analysis
We used root-image-analysis software (WinRHIZO; Régent
Instruments, Québec, Canada) to measure the surface area of whole roots and root apices, as well as to determine the mean diameter and
volume of root apices. The latter was converted into fresh weight,
based on the density of water. To obtain images, excised root apices
and whole roots used for collecting exudates were stained in 0.1%
(w/v) methylene blue, 0.1% (w/v) neutral red for at
least 24 h. They were then scanned with a flatbed scanner at optimized brightness and contrast settings, held constant throughout this study.
Statistical Analysis
Statistical analysis followed Sokal and Rohlf's (1995)
recommendations. Standardized deviates of each set of data (e.g. RRE, root fresh weight, organic-acid efflux) were tested for normality, using the Kolmogorov-Smirnov test. Potential outliers within
experimental groups (i.e. species × treatment) were winsorized if
confirmed with Dixon's test (two individual values in total).
Homogeneity of variance among experimental groups was tested, using
Bartlett's test, and data were transformed, in some cases, to reduce
heteroscedasticity (y = xa, with a = 0.3-0.5,
for apical callose content, phosphate efflux, and alkalinization, and
y = log(x) for organic-acid efflux
from whole roots). Two-way (species × Al level during
cultivation) or three-way (species × Al level during
cultivation × Al level during incubation of apices) model I
ANOVAs were computed, and differences among group means were tested for
significance, using the T test of Spjotvoll/Stoline.
 |
ACKNOWLEDGMENTS |
We thank Dr. David R. Parker (University of California,
Riverside) for providing us GEOCHEM 2.0. We are grateful to Dr.
Emmanuel Delhaize (CSIRO, Canberra, ACT, Australia) for his critical
review of the manuscript, and to Elizabeth de Páez for editorial
improvements of the text.
 |
FOOTNOTES |
Received September 6, 2000; returned for revision October 23, 2000; accepted November 27, 2000.
1
This work was supported by the Kommission
für Entwicklungsfragen of the Austrian Academy of Sciences, and
by the Colombian Ministry of Agriculture and Rural Development.
2
Present address: Center for the Application of Molecular
Biology to International Agriculture, G.P.O. Box 3200, Canberra ACT 2601, Australia.
*
Corresponding author; e-mail peter{at}cambia.org.au; fax
61-2-6246-4501.
 |
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