海拔高度对北京侧柏人工林土壤氮循环功能基因的影响

Effects of Elevation on Functional Genes of Soil Nitrogen Cycling in Beijing Platycladus orientalis Plantation

  • 摘要:
    目的 土壤微生物介导的氮循环过程是决定森林生态系统N2O等温室气体排放的关键生物因素,揭示北京市森林土壤微生物氮循环功能基因及其驱动因子对森林温室气体减排至关重要。
    方法 本研究以北京市昌平区十三陵林场侧柏人工林为研究对象,采用宏基因组学方法研究不同海拔高度(100 m、300 m、500 m)土壤微生物氮循环功能基因。
    结果 海拔高度显著影响了侧柏人工林土壤氮循环功能基因β-多样性,其主要受土壤pH所驱动。微生物硝化作用、反硝化作用、同化硝酸盐还原为亚硝酸盐(ANRN)和异化亚硝酸盐还原为铵(DNRA)途径的基因丰度均在100 m处显著富集,且与土壤pH呈显著正相关。微生物编码的nosZnirKnorB(反硝化)、nrfAnrfH基因(DNRA)在100 m处丰度最高,其中pH显著影响了nirKnorBnrfAnrfH基因的丰度。
    结论 揭示了pH是驱动侧柏人工林土壤微生物氮循环的关键环境因子,且低海拔土壤具有更高的DNRA基因丰度,其是决定N2O产生的关键氮循环过程。

     

    Abstract:
    Objective Soil microbial mediated nitrogen cycling processes are the key biological factors that determine the emissions of greenhouse gases of N2O in forest ecosystems. The aim was to reveal microbial nitrogen cycling processes and their driving factors for the reduction of greenhouse gas emissions in the forest.
    Method By focusing on Platycladus orientalis plantation in the Ming Dynasty Tombs Forest Farm of Changping District in Beijing, this study applied the metagenomic method to investigate the microbial nitrogen cycling functional genes at different elevations (100 m, 300 m, and 500 m).
    Result Elevation significantly influenced the β-diversity of the soil nitrogen cycling genes in the Platycladus orientalis plantation, which was mainly driven by the soil pH. The abundance of the gene encoding for the pathways of microbial nitrification, denitrification, ANRN, and DNRA were significantly enriched at the elevation of 100 m, and showed a significant positive correlation with the soil pH. The abundances of the genes nosZ, nirK, norB (denitrification), nrfA and nrfH (DNRA) were the highest at the elevation of 100 m, among which the pH significantly affected the relative abundances of the nirK, norB, nrfA and nrfH.
    Conclusion This results reveal that pH is a key environmental factor driving the soil microbial-mediated nitrogen cycle in the Platycladus orientalis plantation, and the soil at low elevations has a higher abundance of functional genes related to the DNRA process, which is a key nitrogen cycling process of determining the production of N2O.

     

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