Luo Wentao, Li Mai-He, Sardans Jordi, Lü Xiao-Tao, Wang Chao, Peñuelas Josep, Wang Zhengwen, Han Xing-Guo, Jiang Yong
Erguna Forest-Steppe Ecotone Research Station Institute of Applied Ecology Chinese Academy of Sciences Shenyang China.
Swiss Federal Research Institute WSLBirmensdorf Switzerland.
Ecol Evol. 2017 Jul 28;7(17):6927-6934. doi: 10.1002/ece3.3245. eCollection 2017 Sep.
Plant carbon (C) and nitrogen (N) stoichiometry play an important role in the maintenance of ecosystem structure and function. To decipher the influence of changing environment on plant C and N stoichiometry at the subcontinental scale, we studied the shoot and root C and N stoichiometry in two widely distributed and dominant genera along a 2,200-km climatic gradient in China's grasslands. Relationships between C and N concentrations and soil climatic variables factors were studied. In contrast to previous theory, plant C concentration and C:N ratios in both shoots and roots increased with increasing soil fertility and decreased with increasing aridity. Relative N allocation shifted from soils to plants and from roots to shoots with increasing aridity. Changes in the C:N ratio were associated with changes in N concentration. Dynamics of plant C concentration and C:N ratios were mainly caused by biomass reallocation and a nutrient dilution effect in the plant-soil system. Our results suggest that the shifted allocation of C and N to different ecosystem compartments under a changing environment may change the overall use of these elements by the plant-soil system.
植物碳(C)和氮(N)化学计量比在维持生态系统结构和功能方面发挥着重要作用。为了在次大陆尺度上解读变化的环境对植物C和N化学计量比的影响,我们沿着中国草原2200公里的气候梯度,研究了两个广泛分布且占主导地位的属的地上部分和根系的C和N化学计量比。研究了C和N浓度与土壤气候变量因素之间的关系。与先前的理论相反,地上部分和根系中的植物C浓度和C:N比均随着土壤肥力的增加而增加,随着干旱程度的增加而降低。随着干旱程度的增加,相对N分配从土壤转移到植物,从根系转移到地上部分。C:N比的变化与N浓度的变化相关。植物C浓度和C:N比的动态变化主要是由植物-土壤系统中的生物量重新分配和养分稀释效应引起的。我们的结果表明,在变化的环境下,C和N向不同生态系统组分的分配转移可能会改变植物-土壤系统对这些元素的整体利用。