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武夷山自然保护区不同海拔梯度木荷叶片钙形态变化特征

Variation Characteristics of Calcium Forms in Leaves of Schima superba at Different Altitudes in Wuyi Mountain Nature Reserve

  • 摘要:
    目的 探讨武夷山不同海拔梯度下木荷叶片钙形态的分布特征及其与环境因子的关系,为亚热带地区林地生态保护与可持续经营提供理论依据。
    方法 在武夷山自然保护区海拔800~1 700 m范围内设置10个梯度样地,采集木荷成熟叶片和对应土壤样品,测定硝酸钙/氯化钙(AIC-Ca)、水溶性钙(H2O-Ca)、果胶酸钙(NaCl-Ca)、磷酸钙(HAC-Ca)、草酸钙(HCl-Ca)和硅酸钙(Res-Ca)共6种钙形态含量,结合土壤理化指标(pH、有效钙等),通过方差分析、相关性分析和冗余分析(RDA)揭示其分异规律。
    结果 (1)钙形态分布呈现显著海拔分异(p<0.05):AIC-Ca在海拔1 201~1 400 m含量较高;H2O-Ca在海拔900和1 200 m含量较高,由于该海拔内种间竞争压力大,需要活性钙动态调节环境适应;Res-Ca在海拔800~1 000 m时占比较高,形成钙沉积库,目的在于发挥抗氧化功能和调节植物体有机酸平衡。(2)冗余分析表明,海拔与所有钙形态呈负相关,土壤有效钙与各钙形态正相关,pH与AIC-Ca、NaCl-Ca呈负相关,与其他形态正相关。
    结论 木荷通过钙形态的协同分配实现对环境的适应,其分异格局受海拔梯度与土壤有效钙共同驱动。研究结果为亚热带山地植被钙代谢调控机制及生态适应性研究提供科学依据。

     

    Abstract:
    Objective To explore the distribution characteristics of calcium forms in leaves of Schima superba along an altitude gradient in the Wuyi Mountain and to examine their relationship with environmental factors, thereby providing a theoretical basis for ecological protection and sustainable forest management in subtropical areas.
    Method Ten elevation-gradient plots were set up across 800~1 700 m in the Wuyi Mountain Nature Reserve. Mature leaves and corresponding soil samples of S.superba were collected. The contents of six calcium forms, including calcium nitrate/calcium chloride (AIC-Ca), water-soluble calcium (H2O-Ca), calcium pectinate (NaCl-Ca), calcium phosphate (HAC-Ca), calcium oxalate (HCl-Ca) and calcium silicate (Res-Ca), were determined. Combined with soil physical and chemical indexes (pH, available calcium, etc.), the differentiation rules were revealed by variance analysis, correlation analysis and redundancy analysis (RDA).
    Results (1) Leaf Ca forms showed significant altitude differentiation: AIC-Ca reached its highest proportion at 1 201~1 400 m; H2O-Ca reached its highest proportion at 900 and 1 200 m, coinciding with stronger interspecific competition within this altitude gradient, suggesting a greater requirement for active calcium to adjust to environmental conditions. Res-Ca accounted for a relatively high proportion at 800~1 000 m, indicating a “deposited” Ca pool, that may support antioxidant function and regulate the balance of organic acids in plants. (2) Redundancy analysis showed that altitude was negatively correlated with all calcium forms, soil available calcium was positively correlated with each Ca forms, pH was negatively correlated with AIC-Ca and NaCl-Ca, and positively correlated with other forms.
    Conclusion S.superba appears to adapt to changing environments through the synergistic distribution of calcium forms, with patterns primarily driven by altitude and soil available Ca. These findings provide a scientific basis for the study of calcium metabolism regulation mechanism and ecological adaptability of subtropical mountain vegetation.

     

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