Bharali Bhagawan, Bates Jeffrey W
Department of Biological Sciences, Imperial College at Silwood Park, Ascot, Berkshire, UK.
Ann Bot. 2002 Sep;90(3):337-43. doi: 10.1093/aob/mcf192.
The hypothesis that metal ions absorbed by bryophytes from the underlying soil may ameliorate adverse effects of SO2 was investigated in the terricolous moss species Pleurozium schreberi (Brid.) Mitt. and Rhytidiadelphus triquetrus (Hedw.) Warnst. Dilute sodium bisulfite solutions (equivalent to dissolved SO2) were applied to shoots isolated from soil or in contact with artificial substrata. Marked inhibition of net photosynthesis was observed within 2 h of treatment with 0.3 mM bisulfite in both mosses. Progressive recovery of net photosynthesis occurred 2-8 h after bisulfite treatment, although the extent of this depended on the concentration and pH of the solution. When R. triquetrus and P. schreberi were grown on artificial substrata (calcareous, acid-mineral or acid-organic) with weekly bisulfite applications, the only significant effect was poorer growth of P. schreberi receiving bisulfite on the calcareous and acid-organic substrata. In both species, growth on the calcareous substratum led to increased concentrations of exchangeable Ca2+, whereas exchangeable Fe3+ concentrations increased following growth on the acid-mineral soil. In another experiment the two mosses were pre-treated with either Ca2+ or Fe3+ before incubation with bisulfite. In P. schreberi, the depression of net photosynthetic rate caused by bisulfite was ameliorated from 33 to 64% of the control by pre-treatment with Fe3+, but it was unaffected by Ca2+ pre-treatment. In R. triquetrus, the amelioration caused by Fe3+ pre-treatment was from 16 to 60% of the control, but pre-treatment with Ca2+ gave a greater amelioration, to 75% of the control value. The responses are discussed in terms of soil preferences of the mosses and possible underlying bisulfite amelioration mechanisms.
关于苔藓植物从下层土壤中吸收的金属离子可能会减轻二氧化硫不良影响的假说,在土生苔藓物种高山金发藓(Pleurozium schreberi (Brid.) Mitt.)和立碗藓(Rhytidiadelphus triquetrus (Hedw.) Warnst.)中进行了研究。将稀亚硫酸氢钠溶液(相当于溶解的二氧化硫)施用于从土壤中分离出的或与人工基质接触的茎枝上。在用0.3 mM亚硫酸氢盐处理两种苔藓后的2小时内,观察到净光合作用受到明显抑制。亚硫酸氢盐处理后2 - 8小时,净光合作用逐渐恢复,不过恢复程度取决于溶液的浓度和pH值。当立碗藓和高山金发藓生长在人工基质(钙质、酸性矿物或酸性有机基质)上并每周施用亚硫酸氢盐时,唯一显著的影响是在钙质和酸性有机基质上接受亚硫酸氢盐处理的高山金发藓生长较差。在这两个物种中,在钙质基质上生长会导致可交换Ca2+浓度增加,而在酸性矿物土壤上生长后可交换Fe3+浓度增加。在另一个实验中,两种苔藓在与亚硫酸氢盐一起培养之前先用Ca2+或Fe3+进行预处理。在高山金发藓中,亚硫酸氢盐引起的净光合速率降低通过Fe3+预处理从对照的33%改善到64%,但不受Ca2+预处理的影响。在立碗藓中,Fe3+预处理引起的改善从对照的16%到60%,但Ca2+预处理带来了更大的改善,达到对照值的75%。根据苔藓的土壤偏好和可能的潜在亚硫酸氢盐改善机制对这些反应进行了讨论。