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Carbon and nitrogen allocation shifts in plants and soils along aridity and fertility gradients in grasslands of China

机译:中国草地上土壤和土壤中碳氮分配的变化沿干旱和肥力梯度变化

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摘要

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.
机译:植物碳(C)和氮(N)的化学计量在维持生态系统结构和功能中起重要作用。为了解释次大陆规模环境变化对植物C和N化学计量的影响,我们研究了在2200 km气候梯度下中国草原两个分布广泛且占优势的属的枝,根C和N化学计量。研究了碳氮浓度与土壤气候变量因子之间的关系。与以前的理论相反,茎秆和根中的植物碳浓度和碳氮比随着土壤肥力的增加而增加,而随着干旱的增加而降低。随着干旱的增加,相对氮素的分配从土壤转移到植物,从根部转移到芽。 C∶N比的变化与N浓度的变化有关。植物碳浓度和碳氮比的动态变化主要是由生物量再分配和植物-土壤系统中的养分稀释效应引起的。我们的结果表明,在不断变化的环境下,碳和氮分配到不同生态系统区室的转移可能会改变植物-土壤系统对这些元素的整体利用。

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