J Plant Ecol ›› 2024, Vol. 17 ›› Issue (2): rtae025.DOI: 10.1093/jpe/rtae025

• Research Articles •    

Mechanism of plant-soil feedback in a degraded alpine grassland on the Tibetan Plateau

Tiancai Zhou1,2,3,4, Jian Sun2, Peili Shi1,5,*   

  1. 1Key Laboratory of Ecosystem Network Observation and Modelling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China;
    2State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China;
    3Key Laboratory of Biodiversity and Environment on the Qinghai-Tibet Plateau, Ministry of Education, Lhasa 850011, China;
    4Tibet Research Academy of Eco-environmental Sciences, Lhasa 850000, China;
    5College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2024-01-11 Accepted:2024-04-02 Online:2024-04-10 Published:2024-02-22
  • Contact: E-mail: shipl@igsnrr.ac.cn
  • Supported by:
    National Key R&D Program of China (2023YFF1304304), the National Natural Science Foundation of China (31870406 and 42301071), the China Postdoctoral Science Foundation (2023M743633) and the Science and Technology Major Project of Tibetan Autonomous Region of China (XZ202201ZD0005G02).

青藏高原退化高寒草地的植物-土壤反馈机制

Abstract: Although biotic and abiotic factors have been confirmed to be critical factors that affect community dynamics, their interactive effects have yet to be fully considered in grassland degradation. Herein, we tested how soil nutrients and microbes regulated plant-soil feedback (PSF) in a degraded alpine grassland. Our results indicated that soil total carbon (STC; from 17.66 to 12.55 g/kg) and total nitrogen (STN; from 3.16 to 2.74 g/kg) exhibited significant (P < 0.05) decrease from non-degraded (ND) to severely degraded (SD). Despite higher nutrients in ND soil generating significantly (P < 0.05) positive PSF (0.52) on monocots growth when the soil was sterilized, a high proportion of pathogens (36%) in ND non-sterilized soil resulted in a strong negative PSF on monocots. In contrast, the higher phenotypic plasticity of dicots coupled with a higher abundance of mutualists and saprophytes (70%) strongly promoted their survival and growth in SD with infertile soil. Our findings identified a novel mechanism that there was a functional group shift from monocots with higher vulnerability to soil pathogens in the ND fertile soil to dicots with higher dependence on nutritional mutualists in the degraded infertile soil. The emerging irreversible eco-evolutionary in PSF after degradation might cause a predicament for the restoration of degraded grassland.

Key words: plant-soil feedback, plant function groups, degradation, alpine grassland, Tibetan Plateau

摘要:
虽然生物和非生物因素是驱动生态系统群落结构和组成变化的关键因素,但其交互作用如何调控青藏高原草地的退化尚未得到充分研究。鉴于此,本研究探索了退化高寒草地的土壤养分和微生物如何影响植物-土壤反馈(plant-soil feedback, PSF)和群落演变。结果表明,高寒草地从未退化到严重退化阶段,土壤全碳(17.66 vs. 12.55 g/kg)和全氮(3.16 vs. 2.74 g/kg)均显著(P < 0.05)降低。尽管未退化灭菌土壤中较高的养分对单子叶植物的生长产生显著(P < 0.05)正反馈效应(0.52),但其未灭菌土壤中较高比例的病原菌(36%)却介导了单子叶植物强烈的负反馈效应。相反,较高的表型可塑性以及退化土壤中较高的共生菌和腐生菌丰度(70%),共同促进了双子叶植物在退化贫瘠土壤中的存活和生长。综合而言,随着高寒草地退化程度的增加,植物群落从对未退化土壤病原菌敏感的单子叶植物转变为依赖退化土壤中共生菌的双子叶植物。高寒草地退化前后植物功能性状和微生物群落对退化环境的生态适应与协同演化可能给退化草地的恢复带来困境。

关键词: 植物土壤反馈, 植物功能群, 退化, 高寒草地, 青藏高原