喀斯特地区稻田土壤剖面微生物群落对土壤深度的响应
作者:
作者单位:

(1.贵州大学农学院,贵州 贵阳 550025;2.贵州省山地畜禽养殖污染控制与资源化技术工程实验室,贵州 贵阳 550025)

作者简介:

钟卓妍(2000-),硕士研究生,主要从事土壤微生物研究。E-mail:gs.zyzhong22@gzu.edu.cn。

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基金项目:

基金项目:国家重点专项部省联动计划课题(2022YFD1901505);贵州省特色杂粮优质高效机械化科技创新人才团队建设(BQW[2024]009);山地特色农业绿色丰产关键技术研究与集成应用([2023]07)。


Microbial response to soil depth in rice paddy soil profiles in karst areas
Author:
Affiliation:

(1.College of Agriculture,Guizhou University,Guiyang Guizhou 550025;2.Guizhou Engineering Laboratory of Mountainous Livestock and Poultry Breeding Pollution Control and Resource Technology,Guiyang Guizhou 550025)

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    摘要:

    土壤微生物群落沿土壤深度发挥作用,了解土壤微生物群落剖面动态的信息对于预测喀斯特地区稻田土壤微生物群落长期在各土壤诊断层的活动具有重要价值。采用16S rRNA 和ITS 扩增子的高通量测序技术,研究了喀斯特地区稻田土壤深度的变化对土壤微生物群落的影响。结果表明:土壤深度的变化对土壤酶活性的影响较大,同时改变了细菌和真菌的群落组成和微生物多样性。共鉴定了61 个细菌门和18 个真菌门,土壤中占主导地位的细菌门是酸杆菌门(Acidobacteriota,相对丰度为22.54%)、绿弯菌门(Chloroflexi,相对丰度为16.67%)和变形菌门(Proteobacteria,相对丰度为16.58%),其中底层土壤中富营养菌的相对丰度较低(变形菌门相对丰度从表层的20.10% 降至底层的16.04%),寡营养菌的相对丰度较高(酸杆菌门相对丰度从表层的20.27% 增至底层的26.88%);优势真菌门包括子囊菌门(Ascomycota,相对丰度为43.22%)和担子菌门(Basidiomycota,相对丰度为21.04%)。碱解氮和磷酸酶是细菌群落的重要驱动因素(R2 分别为0.5391 和0.5085,P<0.001),蔗糖酶和有效磷是真菌群落的重要驱动因素(R2 分别为0.2577 和0.2032,P<0.05)。相较于真菌群落,细菌群落与环境因子的相关性更为显著。随着剖面深度的增加,理化指标呈下降趋势;土壤微生物多样性和共现网络随着剖面深度呈先下降后上升的趋势,表层土壤微生物网络包括324 个节点和754 条边,随着剖面深度呈下降趋势,而在底层土壤又上升至79 个节点和94 条边。本研究为喀斯特地区稻田土壤微生物群落随土壤深度变化提供新的见解。

    Abstract:

    Soil microbial communities change along the soil depth,and information on the dynamics of soil microbial community profiles is valuable for predicting the long-term activities of soil microbial communities in rice fields in karst regions at various soil diagnostic layers. The effects of changes in soil depth on soil microbial communities in paddy fields in karst areas were investigated using high-throughput sequencing of 16S rRNA and ITS amplicons. The results indicated that changes in soil depth significantly affected soil enzyme activity and altered the composition and microbial diversity of bacterial and fungal communities. A total of 61 bacterial phyla and 18 fungal phyla were identified. The dominant bacterial phyla in the soil were Acidobacteriota(relative abundance of 22.54%),Chloroflexi(relative abundance of 16.67%),and Proteobacteria(relative abundance of 16.58%). In deeper soil layers,the relative abundance of eutrophic bacteria was lower(Proteobacteria decreased from 20.10% in surface soil to 16.04% in deeper soil),while the relative abundance of oligotrophic bacteria was higher(Acidobacteriota increased from 20.27% in surface soil to 26.88% in deeper soil). The dominant fungal phyla included Ascomycota(relative abundance of 43.22%)and Basidiomycota(relative abundance of 21.04%). Alkali-hydrolyzable nitrogen and acid phosphatase enzyme were significant drivers of bacterial communities(R2 = 0.5391 and 0.5085,respectively,P<0.001),while sucrase and available phosphorus were key drivers of fungal communities(R2=0.2577 and 0.2032,respectively,P<0.05). Compared to fungal communities,bacterial communities showed a stronger correlation with environmental factors. As soil depth increased,physicochemical indicators exhibited a declining trend. Soil microbial diversity and co-occurrence networks initially decreased and then increased with soil depth. The surface soil microbial network comprised 324 nodes and 754 edges,showing a declining trend with depth,but increased again to 79 nodes and 94 edges in the deeper soil. This study provided new insights into the changes in soil microbial communities with soil depth in paddy fields in karst regions.

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钟卓妍,郭子成,李雪儿,龚徐,周盈盈,韦小了,刘飘,杨三维,何腾兵,何冠谛.喀斯特地区稻田土壤剖面微生物群落对土壤深度的响应[J].中国土壤与肥料123,2025,(8):119-130

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  • 收稿日期:2025-01-16
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  • 录用日期:2025-03-17
  • 在线发布日期: 2025-10-11
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