高寒嵩草草甸稳态特征及退化演替过程研究
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1.青海海北高寒草地生态系统国家野外科学观测研究站和中国科学院高原生物适应与进化重点实验室;2.中国科学院大学

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青海省科技厅青年项目“黄河源高寒草甸景观破碎化机制研究”(2023-ZJ-967Q);2023年度青海省“昆仑英才∙高端创新创业人才”培养拔尖人才项目[青人才字(2024)1号]


Study on steady-state characteristics and degradation succession process of Alpine Kobresia Meadow
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1.Northwest Institute of Plateau Biology,Chinese Academy of Sciences,Xining,810001;2.Qinghai Haibei National Field Research Station of Alpine Grassland Ecosystem and Key Laboratory of Adaptation and Evolution of Plateau Biota, Northwest Institute of Plateau Biology, Chinese Academy of Sciences, Xining, 810008, China

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    摘要:

    系统构件因子对干扰响应与适应过程是明晰生态系统稳定性维持及稳态转化的基础和核心,对退化生态系统修复研究具有重要的理论指导意义。本研究以高寒嵩草草甸退化演替模式序列为研究对象,探讨不同演替稳态植物群落数量特征、土壤养分特征、下垫面特征同退化演替的协同变化关系,研究发现:(1)高寒嵩草草甸退化演替过程中植物、土壤、下垫面特征对退化响应具有异步性,其中起负反馈效应的因子对系统特征的稳定性维持具有重要意义,是导致系统特征出现平台期的主要原因。(2)由于高寒嵩草草甸不同构件因子对退化响应的敏感性不同,导致高寒嵩草草甸随退化程度的加深,系统对退化响应敏感的因子逐渐被非敏感因子取代,进而造成系统稳态的转化和系统总体特征在整个退化演替中的阶梯性变化。因此,高寒嵩草草甸构件因子对退化干扰的异步性响应过程和负反馈效应维持了平台期系统特征的相对稳定,但在退化演替过程中,随着维持系统特征稳定的非敏感性因子逐渐被取代,系统将发生稳态转化。

    Abstract:

    The system response and adaptation under disturbance is the basis and core in clarifying the study of ecosystem stability maintenance and steady-state transformation, and has significance theoretical guiding for the restoration of degraded ecosystem. In order to determine the response process of each component factor and the overall characteristics in different steady stages in the alpine Kobresia meadow degradation succession process, and discuss the mechanism in ecosystem stability maintenance under the interference condition, a series of investigations and experiments were carried out on core distribution region of the Alpine Kobresia Meadow in Qinghai, and the characteristics of plant communities, soil nutrient contents, soil biological crust and mattic epipedon as representative index were discussed in the research. The results showed constituents of plant-soil system in different steady stages of the alpine Kobresia meadow was asynchronous in response to degradation, and the asynchronous response effect resulted in the relative stability of the system characteristics in different platform periods and led the characteristics of system into the stabilization in degradation succession process. For example, plant functional groups maintained the overall characteristics of the ecosystem in stable by adjusting the proportion of components and structures of the plant community in the process of degeneration succession. While the component characteristics of plant-soil system maintained of the overall characteristics of plant community in different steady stages in dynamic balance through adjusting the characteristics of soil nutrient, soil-microbial crust and soil-surface in asynchronous feedback to degradation. In addition, the sensitivity of component factors could be changed in degradation steady stages, and the non-sensitive component factors in eco-system could be gradually replaced to the sensitive component factors with the degree of degradation deepens, which was the main reason for steady-state transformation. Therefore, alpine Kobresia meadow maintained stabilization through the asynchronous responses and negative feedback effects of different component factors to degradation, and the negative feedback factors were the core to maintain the stability of the system in alpine Kobresia degradation process. However, when the disturbance exceeded the threshold range of non-sensitive factors of plant-soil system in degradation process, the non-sensitive factors could also be transformed into sensitivity factors, resulting in the transformation of ecosystem out-of-balance, resulting the meadow undergo steady-state transformation. Therefore, the factors with negative feedback effect in the degradation were the key to maintain the ecosystem in stabilization, and the reduction the number of negative feedback effect factors is easy to increase the risk of steady-state transformation in the ecosystem.

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林丽,兰玉婷,李本措,司梦可,樊博,张法伟,李以康,曹广民,李杰霞.高寒嵩草草甸稳态特征及退化演替过程研究.生态学报,,(). http://dx. doi. org/[doi]

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