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不同演替阶段岩溶石灰土可培养细菌的群落特征
引用本文:严嘉慧,周岐海,胡林安,钟菊新,李强. 不同演替阶段岩溶石灰土可培养细菌的群落特征[J]. 微生物学报, 2021, 61(6): 1666-1680
作者姓名:严嘉慧  周岐海  胡林安  钟菊新  李强
作者单位:广西师范大学珍稀濒危动植物生态与环境保护教育部重点实验室, 广西珍稀濒危动物生态学重点实验室, 广西 桂林 541006;中国地质科学院岩溶地质研究所, 自然资源部广西岩溶动力学重点实验室, 广西 桂林 541004;联合国教科文组织国际岩溶研究中心, 广西 桂林 541004
基金项目:中央引导地方科技发展专项(桂科ZY20198009)
摘    要:岩溶土壤是岩溶生态系统的重要组成部分,其母质碳酸盐岩在气候、地形、时间及生物等因素的综合作用下可依次演替出黑色石灰土、棕色石灰土、黄色石灰土和红色石灰土.[目的]了解可培养细菌群落对岩溶石灰土演替过程的响应,可为岩溶石漠化治理、生态恢复和重建等提供理论依据.[方法]以黑色石灰土、棕色石灰土、黄色石灰土和红色石灰土为研究...

关 键 词:岩溶  石灰土  土壤演替  可培养细菌
收稿时间:2021-02-08
修稿时间:2021-03-24

Community characteristics of culturable bacteria in calcareous soil at different succession stages
Jiahui Yan,Qihai Zhou,Lin''an Hu,Juxin Zhong,Qiang Li. Community characteristics of culturable bacteria in calcareous soil at different succession stages[J]. Acta microbiologica Sinica, 2021, 61(6): 1666-1680
Authors:Jiahui Yan  Qihai Zhou  Lin''an Hu  Juxin Zhong  Qiang Li
Affiliation:Key Laboratory of Ecology of Rare and Endangered Species and Environmental Protection, Ministry of Education, Guangxi Key Laboratory of Rare and Endangered Animal Ecology, Guangxi Normal University, Guilin 541006, Guangxi Zhuang Autonomous Region, China;Institute of Karst Geology, Chinese Academy of Geological Sciences, Key Laboratory of Karst Dynamics, Ministry of Natural Resources, Guilin 541004, Guangxi Zhuang Autonomous Region, China;International Research Center on Karst under the Auspices of United Nations Educational, Scientific and Cultural Organization, Guilin 541004, Guangxi Zhuang Autonomous Region, China
Abstract:Karst soil is an important part of karst ecosystem, and its parent material, carbonate rock, can successively evolve into black calcareous soil, brown calcareous soil, yellow calcareous soil and red calcareous soil under the comprehensive effect of climate, topography, time and biology. [Objective] To better understand the response of soil bacterial community to calcareous soil at different succession stages, which can provide the basic references for rocky desertification control and soil erosion control in karst area. [Methods] The contents of SOC, TN and TP, and the abundance and diversity of culturable bacteria in calcareous soils (black, brown, yellow and red) were determined. [Results] The contents of soil SOC and TN at different succession stages were in the order of black calcareous soil > brown calcareous soil > yellow calcareous soil > red calcareous soil. The content of TP was highest in black calcareous soil and lowest in red calcareous soil. A total of 144 strains of bacteria were isolated and purified, and R2A medium was the suitable medium. Then, the bacterial strains were classified into Actinobacteria, Bacteroidetes, Firmicutes and Proteobacteria. Pseudomonas, Cupriavidus and Bacillus were the dominant genera of culturable bacteria. At the genus level, the most strains were isolated from the black calcareous soil, and the dominant genera such as Arenimonas, Thermomonas, Achromobacter and Brevibacillus appeared. In the early succession stages, a large number of bacteria involved in carbon, nitrogen and phosphorus cycling appeared. [Conclusion] Based on the characteristics of parent material carbonate rock, black calcareous soil rich in organic matter is formed under the action of bacteria participating in carbon, nitrogen and phosphorus cycle. The physicochemical properties and culturable bacterial diversity of karst limestone soil decreased with the increase of leaching degree of limestone soil.
Keywords:karst  calcareous soil  soil succession  culturable bacteria
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