长江流域资源与环境 >> 2023, Vol. 32 >> Issue (7): 1467-1478.doi: 10.11870/cjlyzyyhj202307010

• 生态环境 • 上一篇    下一篇

不同退耕年限菜子湖湿地土壤微生物量及古菌群落结构变化

俞姗姗1,张平究1,梁川1,周利1,杨艳芳2,张金花1,陈芳1
  

  1. (1.安徽师范大学地理与旅游学院/江淮流域地表过程与区域响应安徽省重点实验室,安徽 芜湖 241002;2. 安徽师范大学生态与环境学院,安徽 芜湖 241002)

  • 出版日期:2023-07-20 发布日期:2023-07-21

Changes of Soil Microbial Biomass and Archaeal Community Structures in Wetlands With Various Restoration Ages in Caizi Lake

YU Shan-shan1, ZHANG Ping-jiu1, LIANG Chuan1, ZHOU Li1,  YANG Yan-fang2, ZHANG Jin-hua1, CHEN Fang1   

  1. (1. School of Geography and Tourism, Anhui Normal University/Key Laboratory of Surface Processes and Regional Response in Jianghuai Basin, Anhui Province, Wuhu 241002, China; 2. School of Ecology and Environment, Anhui Normal University, Wuhu 241002, China)

  • Online:2023-07-20 Published:2023-07-21

摘要: 土壤微生物对湿地生态系统运行和功能维持均具有重要地位。采用PLFAs分析方法和高通量测序技术获取土壤微生物和古菌群落结构信息,探讨了退耕还湖后湿地生态恢复过程中土壤微生物和古菌群落结构的变化规律及其土壤环境影响因素。结果表明,随着退耕年限增加,湿地表层土壤微生物总量、放线菌、细菌和真菌(除退耕11 aW)生物量不断升高,而亚表层均呈先降后增再降的趋势,但均未达原始湿地水平;相对于油菜地,退耕后湿地表层土壤细菌占比有先降后增再降的趋势,而亚表层则有先升后降趋势;土壤真菌占比和真菌细菌比总体上呈先升后降再升的趋势,而土壤放线菌占比逐渐上升。广古菌门(相对丰度:47.61%~85.29%)是研究区湿地土壤古菌的优势菌门,奇古菌门(相对丰度:14.58%~52.33%)为次优势菌门,泉古菌门(相对丰度:0.01%~0.81%)较小;退耕后表层土壤广古菌门相对丰度有先升后降的趋势,亚表层整体有升高趋势;表层土壤奇古菌门相对丰度存在先降后升的趋势,而亚表层则有降低趋势。利用相关性分析和冗余分析发现有效氮、全氮与有机质是解释退耕后土壤微生物量、微生物群落结构与古菌群落结构变化的主要环境因子,其中有效氮是退耕还湖后湿地土壤微生物量和群落结构变化累积解释量最大的环境因子。微生物通过微生物量和群落结构特征响应和指示着退耕后湿地土壤生态恢复过程。

Abstract: Soil microorganisms play an important role in the operation and maintenance of wetland ecosystems. In this paper, the PLFAs analysis method and high-throughput sequencing technology were used to obtain the community structure information of soil microorganisms and archaea. The changes of soil microbial biomass and archaeal community structure, and the influencing factors during the ecological restoration during returning farmland to wetland were discussed. The results showed that along the wetland restoration age, the biomass of soil total microorganisms, actinomycetes, bacteria and fungi (except for the 11 aW) in the surface layer increased continuously, while they showed a decreasing-increasing-decreasing trend in the subsurface layer. Compared with rapeseed field, the proportion of bacteria showed a decreasing-increasing-decreasing tendency in the surface soils of restoration wetlands, and showed a trend of increasing-decreasing in the subsurface soils. The proportion of fungi, and the ratio of fungi to bacteria showed a trend of increasing-decreasing-increasing along the restoration ages. The proportion of soil actinomycetes gradually increased along the restoration ages. Euryarchaeota (relative abundance: 47.61%-85.29%) was the first dominant phylum of archaea in the studied area, and Thaumarchaeota (relative abundance: 14.58%-52.33%) was the second dominant phylum. The relative abundance of the Crenarchaeota phyla was small (relative abundance: 0.01%-0.81%). The relative abundance of Euryarchaeota in the surface soil increased first and then decreased, and in the subsurface showed an upward trend during the wetland restoration period. The relative abundance of Thaumarchaeota showed a trend of decreasing-increasing in the surface soils, while has a decreasing trend in the subsurface soils. Correlation analysis and redundancy analysis results indicated that available nitrogen, total nitrogen and organic matter were the main environmental factors for explaining the changes of soil microbial biomass, microbial community structure and archaeal community structure during wetland restoration. However, the environmental factor with the largest cumulative explanations for changes of microbial biomass and community structure was soil available nitrogen. Microorganisms respond to the soil ecological restoration process in wetlands after returning farmland to wetland by adjusting microbial biomass and community structure.

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