旱季
降水
雨季
气孔导度
沉积(地质)
光合作用
生长季节
园艺
蒸腾作用
亚热带
植物
化学
农学
动物科学
生物
生态学
古生物学
气象学
物理
沉积物
作者
Ting Wu,Yuting Song,David T. Tissue,Wei Su,Hanyu Luo,Xu Li,Shijie Yang,Xujun Liu,Junhua Yan,Jianxin Huang,Juxiu Liu
标识
DOI:10.1093/treephys/tpad114
摘要
Interspecific variations in phenotypic plasticity of trees affected by climate change may alter ecosystem function of forests. Seedlings of four common tree species (Castanopsis fissa, Michelia macclurei, Dalbergia odorifera and Ormosia pinnata) in subtropical plantations of southern China were grown in the field under rainout shelters and subjected to changing precipitation (48 L water every 4 days in the dry season, 83 L water every 1 day in the wet season; 4 g m-2 yr-1 nitrogen (N)), low N deposition (48 L water every 2 days in the dry season, 71 L water every 1 day in the wet season; 8 g m-2 yr-1 N), high N deposition (48 L water every 2 days in the dry season, 71 L water every 1 day in the wet season; 10 g m-2 yr-1 N) and their interactive effects. We found that the changes in seasonal precipitation reduced the light-saturated photosynthetic rate (Asat) for C. fissa due to declining area-based foliar N concentrations (Na). However, we also found that the interactive effects of changing precipitation and N deposition enhanced Asat for C. fissa by increasing foliar Na concentrations, suggesting that N deposition could alleviate N limitations associated with changing precipitation. Altered precipitation and high N deposition reduced Asat for D. odorifera by decreasing the maximum electron transport rate for RuBP regeneration (Jmax) and maximum rate of carboxylation of Rubisco (Vcmax). O. pinnata under high N deposition exhibited increasing Asat due to higher stomatal conductance and Vcmax. The growth of D. odorifera might be inhibited by changes in seasonal precipitation and N deposition, while O. pinnata may benefit from increasing N deposition in future climates. Our study provides an important insight into the selection of tree species with high capacity to tolerate changing precipitation and N deposition in subtropical plantations.
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