[植被和土壤因子对退化的阿尔卑斯草原微生物群落的交互影响]。

Q2 Environmental Science Huanjing Kexue/Environmental Science Pub Date : 2024-07-08 DOI:10.13227/j.hjkx.202307217
Huan Xu, Ming-Jun Ding, Hua Zhang, Yue-Ju Zhang, Peng Huang, Yu-Ping Wu, Tian-E Zou, Neng-Yu Wang, Huan Zeng
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引用次数: 0

摘要

为了阐明植被和土壤因子对青藏高原退化高寒草原微生物群落的调控作用,我们选择了青藏高原三江源地区的高寒草原。我们分析了不同退化阶段(未退化、中度退化和严重退化)植被和土壤因子的差异,并检测了微生物群落的变化。并利用高通量测序技术检测了不同退化阶段高寒草原微生物群落特征的变化。最后,利用冗余分析(RDA)和多元回归矩阵(MRM)最终,利用冗余分析(RDA)和基于相似性或不相似性矩阵的多元回归矩阵(MRM),确定了降解过程中调控微生物(细菌和真菌)群落变化的关键环境因素。群落变化的关键环境因素。结果表明,高寒草原退化显著改变了群落覆盖度、高度、生物量和禾本科植物的重要价值;显著降低了土壤有机质、全氮、全磷和淤泥的含量;增加了土壤容重和含沙量。降解并没有改变细菌和真菌的组成,但它们的组成比例发生了变化,同时也导致了微生物丰富度(Chao1 指数和丰富度指数)的降低。但微生物多样性(Shannon 指数)没有发生明显变化。随着退化的发生,植被特征、土壤理化性质和微生物多样性呈现出一致的变化趋势。结合网络拓扑结构的变化特征(节点数和聚类系数显著下降),发现高寒草原退化导致物种间相互作用下降、网络分散化和微生物同质化,但物种间的合作关系保持不变(正相关联系在退化各阶段均占90%以上)。在高寒草原退化过程中,植被-土壤相互作用对土壤细菌群落的影响最大,而土壤理化性质对土壤真菌群落的影响最大。具体而言,植被群落高度、生物量和土壤容重是调节土壤微生物的相互因子,植被辛普森指数、禾本科重要值、土壤全磷、全钾和淤泥含量是影响土壤细菌群落的独特因子,土壤pH值和全氮含量是影响土壤真菌群落的特殊因子。
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[Interaction Effects of Vegetation and Soil Factors on Microbial Communities in Alpine Steppe Under Degradation].

To clarify the regulating effect of vegetation and soil factors on microbial communities in the alpine steppe under degradation on the Qinghai-Xizang Plateau, the alpine steppe in the Sanjiangyuan area of the Qinghai-Tibet Plateau was chosen. We analyzed the differences in vegetation and soil factors in different stages of degradation (non-degradation, moderate degradation, and severe degradation) and detected the variations in microbial community characteristics in the alpine steppe under different degradation stages using high-throughput sequencing technology. Eventually, redundancy analysis (RDA) and multiple regression matrixes (MRM) based on the similarity or dissimilarity matrix were used to identify key environmental factors regulating microbial (bacterial and fungal) community changes under degradation. The results showed that the degradation of the alpine steppe significantly changed the community coverage, height, biomass, and important value of graminae; significantly reduced the contents of soil organic matter, total nitrogen, total phosphorus, and silt; and increased the soil bulk density and sand content. Degradation did not change the composition of bacteria and fungi, but their composition proportions changed and also resulted in the loss of microbial richness (Chao1 index and Richness index) but did not significantly change the microbial diversity (Shannon index). With the occurrence of degradation, the vegetation characteristics, soil physicochemical properties, and microbial diversity showed a consistent change trend. Combined with the characteristics of the network topology changes (the number of nodes and clustering coefficient significantly decreased), it was found that degradation of the alpine steppe led to the decline of interspecies interactions, decentralization of network, and homogenization of microorganisms, but the cooperation relations among the species were maintained (positive correlation connections accounted for more than 90% in all degradation stages). Under the alpine steppe degradation, the vegetation-soil interaction had the greatest effect on soil bacterial community, whereas soil physicochemical properties had the greatest influence on soil fungal community. Specifically, vegetation community height, biomass, and soil bulk density were the mutual factors regulating soil microorganisms, whereas the vegetation Simpson index, important value of graminae, soil total phosphorus, total potassium, and silt content were the unique factors affecting the soil bacterial community, and soil pH and total nitrogen content were the particular factors affecting the soil fungal community.

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来源期刊
Huanjing Kexue/Environmental Science
Huanjing Kexue/Environmental Science Environmental Science-Environmental Science (all)
CiteScore
4.40
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15329
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