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Leaf epicuticular wax and cuticle of the Polar Urals plants grown under contrasting geochemical conditions

机译:在相反地球化学条件下生长的极地乌拉尔植物的叶表皮蜡和表皮

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摘要

The epicuticular wax and cuticle structure of upper and lower leaf epidermal cells has been investigated in 11 plant species which grew under contrasting geochemical conditions (hypomatic, serpentinits, rocks with high concentrations of nickel and typical zonal acidic slate soils) in the Polar Urals. No difference in the structural types of wax deposits and cuticle of leaves in plants of the same species grown on different substrates was found. Structural type of cuticle and wax deposits is species_specific. However there are quantitative variations in the epicuticular wax density and cuticle thickness. The density of wax particles and the cuticle thickness are lower in plants grown on serpentinits, compared with those grown on slate soils. Based on a widespread concept of serpentinomorphosis and data obtained it is assumed that quantitative variations of the epicuticular wax density and cuticle thickness correlate with high concentrations of soil nickel. The notion of serpentinomorphosis is introduced.
机译:研究了极地乌拉尔地区11种植物的表皮蜡质和表皮结构,其中11种植物在相反的地球化学条件下生长(表观,蛇纹石,镍含量高的岩石和典型的带状酸性板岩土壤)。在不同底物上生长的相同物种的植物中,蜡沉积物和叶子的表皮的结构类型没有发现差异。表皮和蜡沉积物的结构类型是种特异性的。然而,表皮蜡密度和表皮厚度存在定量变化。与在石质土壤上生长的植物相比,在蛇纹石上生长的植物中蜡颗粒的密度和表皮厚度要低。基于广泛的蛇形变态概念和获得的数据,假定表皮蜡密度和表皮厚度的定量变化与土壤镍的高浓度相关。介绍了蛇形变态的概念。

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