氮沉降对古尔班通古特沙漠土壤活性微生物群落的影响

Impact of Nitrogen Deposition on the Active Soil Microbial Community Structure in the Gurbantunggut Desert

  • 摘要:
    目的 大气氮沉降正深刻改变陆地生态过程,阐明土壤微生物群落响应氮沉降增加及其影响荒漠植物群落生长的机制,是理解全球变化对荒漠生态系统影响的关键之一。
    方法 依托氮添加长期定位试验,采用磷脂脂肪酸(PLFA)方法分析土壤微生物群落结构变化,探究土壤微生物群落响应规律,揭示氮沉降增加影响土壤微生物群落进而影响植物生长的机制。
    结果 ①随氮沉降增加,土壤pH从8.64(N0)降至8.35(N8),土壤养分呈增加趋势,在高氮处理(N8)下,土壤有机碳(SOC)、总氮(TN)、硝态氮(NO3-N)、铵态氮(NH4 + -N)和有效磷(Olsen-P)分别显著增加11.1%、13.3%、625.9%、128.1%、44.9%。②不同土壤微生物类群对氮沉降增加响应不同:N8处理下,放线菌(Act)、革兰氏阳性菌(G + )、革兰氏阴性菌(G)分别显著增加34.9%、33.2%、27.0%,但氮沉降增加未改变土壤微生物群落结构与多样性指数。③冗余分析表明土壤pH、TN和SOC是影响土壤微生物群落的主要因子;随机森林结果表明深色有隔内生菌(DSE)是影响荒漠植物生长的主要土壤微生物类群。结构方程模型进一步证明氮沉降增加通过降低土壤pH调控土壤微生物群落,pH降低促进DSE的生长,而DSE的增加显著抑制了植物生长。然而,氮添加促进了植物群落总生物量的增加。
    结论 本研究揭示了氮沉降增加通过降低土壤pH,调节土壤功能微生物生长,抑制尖喙牦牛儿苗生长但促进群落生物量增加的机制。

     

    Abstract:
    Objective Atmospheric nitrogen deposition is profoundly altering ecological processes in terrestrial ecosystems. Elucidating the mechanisms of soil microbial communities responding to the increased nitrogen deposition and how this affects the growth of desert plant communities were crucial for predicting and addressing the responses of desert ecosystems under global change.
    Method This study conducted a three-year in-situ observation experiment in a desert ecosystem, establishing nitrogen addition gradients. Phospholipid fatty acid (PLFA) analysis was used to examine changes in soil microbial community structure, combined with measurements of soil physicochemical properties and plant biomass, to investigate the response patterns of soil microbial communities and systematically reveal the mechanisms of the increased nitrogen deposition affecting soil microbial communities and plant growth.
    Result ① Increased nitrogen deposition significantly affected soil physicochemical properties: with the increasing nitrogen deposition, soil pH decreased from 8.64 (N0) to 8.35 (N8), and soil nutrients showed an increasing trend. Under the N8 treatment, soil organic carbon (SOC), total nitrogen (TN), nitrate nitrogen (NO3-N), ammonium nitrogen (NH4 + -N), and available phosphorus (Olsen-P) increased significantly by 11.1%, 13.3%, 625.9%, 128.1% and 44.9%, respectively. ② Different soil microbial groups responded differently to increased nitrogen deposition: under high nitrogen treatment (N8), Actinomycetes (Act), Gram-positive bacteria (G + ), and Gram-negative bacteria (G) increased significantly by 34.9%, 33.2% and 27.0%, respectively. However, the increased nitrogen deposition did not alter soil microbial community structure and diversity indices. ③ Redundancy analysis indicated that soil pH, TN, and SOC were the main factors influencing the soil microbial community. Random forest results showed that dark septate endophytes (DSE) were the primary soil microbial group affecting desert plant growth. Structural equation modeling further indicated that increased nitrogen deposition regulates the soil microbial community by reducing soil pH. The decrease in pH promoted the growth of DSE, and the increase in DSE significantly inhibited plant growth. However, nitrogen addition promoted an increase in total plant community biomass.
    Conclusion This study reveals the mechanism of the increased nitrogen deposition regulates the growth of soil functional microorganisms by lowering soil pH, inhibiting the growth of Erodium oxyrhinchum and promoting an increase in community biomass.

     

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