T. Masunaga et al., MINERAL-COMPOSITION OF LEAVES AND BARK IN ALUMINUM ACCUMULATORS IN A TROPICAL RAIN-FOREST IN INDONESIA, Soil Science and Plant Nutrition (Tokyo), 44(3), 1998, pp. 347-358
Mineral composition including Al, Ca, Mg, P, S, and Si and relationshi
ps between Al and other elements such as Ca, Mg, P, S, and Si in leave
s and bark of trees in a tropical rain forest in West Sumatra were stu
died. Sixty five tree species and 12 unidentified trees were referred
to as Al accumulators based on Chenery's definition (more than 1 g kg(
-1) Al in leaves). For most of the Al accumulators, Al concentration i
n leaves was higher than in bark. However, some members of Euphorbiace
ae, Melastomataceae, and Ulmaceae families showed a reverse trend. Mos
t of the non-accumulators also showed a higher Al concentration in bar
k than in leaves. These results indicated that there was a difference
in the mechanism of Al accumulation in tree bodies. Some of the Al acc
umulators showed an extremely high Al concentration (more than 10 g kg
(-1)) not only in the mature leaves, but also in the new leaves. Analy
sis of the relationships between the concentration of Al and the other
5 elements in leaves, revealed that Al accumulators could be separate
d into two groups at the Al concentration of 3 g kg(-1). This finding
suggested that new criteria based on Al concentration (greater than or
equal to 3 g kg(-1)) or Al/Ca ratio in leaves could be proposed in or
der to define Al accumulators, apart from Chenery's criterion. Alumini
um accumulators with an Al concentration in leaves lower than 3 g kg(-
1) (Al accumulators <3 g kg(-1)) showed the same trend as the non-accu
mulators in terms of these elemental relationships, while Al accumulat
ors with an Al concentration in leaves higher than 3 g kg(-1) (AI accu
mulators greater than or equal to 3 g kg(-1)) showed a different trend
from the non-accumulators. The Al accumulators greater than or equal
to 3 g kg(-1) and the other trees (Al accumulators <3 g kg(-1) and non
-accumulators) showed separately positive correlations between the con
centrations of Al and Ca (or Mg) in the leaves. This observation seems
to be opposite to general findings in plant nutrition, i.e. inhibitio
n of Ca or Mg uptake by Al.,A positive correlation between Al and S wa
s also observed for all the trees. The Al accumulators greater than or
equal to 3 g kg(-1) showed positive correlations between the concentr
ations of Al and P (or Si) in the leaves, unlike the other trees. Thes
e findings suggested that Al stimulated P, S, or Si accumulation in le
aves or Al was transported with P, S, or Si for the Al accumulators gr
eater than or equal to 3 g kg(-1). No negative relationships between A
l and the other 5 elements in the leaves were observed for the Al accu
mulators greater than or equal to 3 g kg(-1).