Mineral composition of leaves and bark in aluminum accumulators in a tropical rain forest in Indonesia

被引:38
作者
Masunaga, T [1 ]
Kubota, D
Hotta, M
Wakatsuki, T
机构
[1] Shimane Univ, Fac Life & Environm Sci, Matsue, Shimane 6908504, Japan
[2] Kagoshima Univ, Fac Sci, Kagoshima 8900065, Japan
关键词
Al accumulator; bark; leaves; mineral composition; tropical rain forest;
D O I
10.1080/00380768.1998.10414456
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
Mineral composition including Al, Ca, Mg, P, S, and Si and relationships between Al and other elements such as Ca, Mg, P, S, and Si in leaves and bark of trees in a tropical rain forest in West Sumatra were studied. 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 in leaves was higher than in bark. However, some members of Euphorbiaceae, Melastomataceae, and Ulmaceae families showed a reverse trend. Most of the non-accumulators also showed a higher Al concentration in bark than in leaves. These results indicated that there was a difference in the mechanism of Al accumulation in tree bodies. Some of the Al accumulators showed an extremely high Al concentration (more than 10 g kg(-1)) not only in the mature leaves, but also in the new leaves. Analysis of the relationships between the concentration of Al and the other 5 elements in leaves, revealed that Al accumulators could be separated 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 order to define Al accumulators, apart from Chenery's criterion. Aluminium 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-accumulators in terms of these elemental relationships, while Al accumulators with an Al concentration in leaves higher than 3 g kg(-1) (AI accumulators 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 concentrations of Al and Ca (or Mg) in the leaves. This observation seems to be opposite to general findings in plant nutrition, i.e. inhibition of Ca or Mg uptake by Al.,A positive correlation between Al and S was also observed for all the trees. The Al accumulators greater than or equal to 3 g kg(-1) showed positive correlations between the concentrations of Al and P (or Si) in the leaves, unlike the other trees. These findings suggested that Al stimulated P, S, or Si accumulation in leaves or Al was transported with P, S, or Si for the Al accumulators greater than or equal to 3 g kg(-1). No negative relationships between Al and the other 5 elements in the leaves were observed for the Al accumulators greater than or equal to 3 g kg(-1).
引用
收藏
页码:347 / 358
页数:12
相关论文
共 19 条
  • [1] NOTE ON EVOLUTIONARY STATUS OF ALUMINUM ACCUMULATORS AMONG DICOTYLEDONS
    CHENERY, EM
    SPORNE, KR
    [J]. NEW PHYTOLOGIST, 1976, 76 (03) : 551 - 554
  • [2] Foy C. D., 1978, ASA Special Publication, P301
  • [3] Foy C. D., 1974, The Plant Root and its Environment. Proceedings held at Virginia Polytechnic and State University, 1971. E.W.Carson (Editor), P601
  • [4] ALUMINUM-SILICON INTERACTIONS IN HIGHER-PLANTS
    HODSON, MJ
    EVANS, DE
    [J]. JOURNAL OF EXPERIMENTAL BOTANY, 1995, 46 (283) : 161 - 171
  • [5] HOTTA M, 1986, SUMATRA NATURE STUDY
  • [6] HOTTA M, 1984, SUMATRA NATURE STUDY
  • [7] Huang J.W., 1995, Plant-Soil Interactions at Low pH: Principles and Management, P297
  • [8] HUANG JWW, 1992, PLANTA, V188, P414, DOI 10.1007/BF00192809
  • [9] JORDAN CF, 1985, NUTRIENT CYCLING TRO, P77
  • [10] IDENTITY OF THE RHIZOTOXIC ALUMINUM SPECIES
    KINRAIDE, TB
    [J]. PLANT AND SOIL, 1991, 134 (01) : 167 - 178