| 岩性对喀斯特灌丛土壤固氮菌与丛枝菌根真菌群落结构及丰度的影响 |
| 摘要点击 2634 全文点击 907 投稿时间：2016-06-30 修订日期：2016-10-12 |
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| 中文关键词 喀斯特 灌丛生态系统 岩性 固氮菌 丛枝菌根真菌 群落结构 |
| 英文关键词 karst shrub ecosystem lithology nitrogen-fixing bacteria arbuscular mycorrhizal fungi community structure |
| 作者 | 单位 | E-mail | | 梁月明 | 中国科学院亚热带农业生态研究所, 亚热带农业生态过程重点实验室, 长沙 410125
中国地质科学院岩溶地质研究所, 国土资源部、广西壮族自治区岩溶动力学重点实验室, 桂林 541004 | yueming0919@163.com | | 苏以荣 | 中国科学院亚热带农业生态研究所, 亚热带农业生态过程重点实验室, 长沙 410125 | yrsu@isa.ac.cn | | 何寻阳 | 中国科学院亚热带农业生态研究所, 亚热带农业生态过程重点实验室, 长沙 410125 | | | 陈香碧 | 中国科学院亚热带农业生态研究所, 亚热带农业生态过程重点实验室, 长沙 410125 | |
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| 中文摘要 |
| 运用末端限制性片段长度多态性（terminal restriction fragment length polymorphism，T-RFLP）和荧光定量PCR（real-time PCR）法，检测喀斯特灌丛生态系统中不同岩性条件下土壤固氮菌与丛枝菌根（arbuscular mycorrhizal，AM）真菌群落结构与丰度的变化，揭示岩性对灌丛生态系统土壤中固氮菌与AM真菌群落结构与丰度的影响.结果表明不同岩性条件下，土壤固氮菌与AM真菌丰度存在显著差异，其中，固氮菌与AM真菌丰度在石灰岩土壤中最大，白云岩土壤中最小，石灰岩-白云岩夹层土壤介于两者之间；同样，不同岩性土壤中固氮菌与AM真菌群落结构存在显著性差异.土壤Olsen-P、有机碳、黏粒含量与固氮菌丰度存在显著正相关关系，而土壤全氮、黏粒含量与AM真菌丰度存在显著正相关.RDA分析表明，植物均匀度影响固氮菌群落组成结构，而植物均匀度、香农多样性指数及丰富度指数影响AM真菌群落组成结构.以上的研究结果表明：岩性主要是通过影响植物与土壤养分来影响土壤固氮菌与AM真菌群落组成结构及丰度. |
| 英文摘要 |
| Lithology is a key factor when used to restore vegetation in karst degraded ecosystems, and arbuscular mycorrhizal (AM) fungi and nitrogen-fixing bacteria play an important role in improving plant growth. However, little information is available regarding the effects of lithology on these two groups of microorganisms. To test whether these microbial communities are impacted by lithology, the abundance and composition of soil AM fungal and nitrogen-fixing bacteria communities were determined through terminal restriction fragment length polymorphism (T-RFLP) and real-time fluorescence-based quantitative PCR (real-time PCR). Three types of lithology (dolomite, limestone and dolomite-limestone) were selected in this study. The diversity, richness, and evenness of plant species were evaluated through field surveys and soil properties were measured. The results showed that the abundances of soil nitrogen-fixing bacteria and arbuscular mycorrhizal fungal communities were significantly influenced by lithology. The abundances of these two groups of microorganisms were the lowest in dolomite soil, inferior to dolomite-limestone soil, while highest in limestone soil. Similarly, the composition of soil nitrogen-fixing bacteria and AM fungi communities varied among lithology. A significant linear correlation was observed among soil organic carbon, available phosphorus, clay content and nitrogen-fixing bacterial abundance (P<0.05), and a significant linear correlation among total nitrogen, clay content and AM fungal abundance (P<0.05). Redundancy analysis showed that the composition of nitrogen-fixing bacterial community was closely linked to plant evenness, and the AM fungal community composition was closely linked to plant diversity (plant evenness, Shannon-wiener and richness). These results indicated that lithology influenced the abundances and compositions of soil nitrogen-fixing bacteria and arbuscular mycorrhizal (AM) fungal communities mainly through plant and soil properties. |
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