[热带森林恢复期间氨氧化细菌群落的季节性变化]。

Q3 Environmental Science
Ming-Liu Wang, Qian-Bin Cao, Mei Lu, Qian-Qian Zuo, Shuang Zhao, Min-Kun Chen, Ping Wang
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引用次数: 0

摘要

本研究采用高通量测序技术调查了西双版纳热带森林生态系统三个恢复阶段[即Mallotus paniculatus群落(早期)、Millettia leptobotrya群落(中期)和Syzygium oblatum群落(后期)]土壤氨氧化细菌(AOB)群落的干湿季节变化特征。我们分析了热带森林恢复过程中土壤理化特征对AOB群落组成和多样性的影响。结果表明,热带森林恢复显著影响了优势AOB门类的相对丰度及其干湿季节变化。在恢复早期,变形菌的相对丰度最高(71.3%),而放线菌的相对丰度则在恢复晚期(1.0%)。变形菌和放线菌的丰度在早期和晚期的干湿季节变化范围分别最大。在热带森林恢复阶段,优势 AOB 属的丰度及其干湿季节变化各不相同。亚硝基螺菌和亚硝基单胞菌在恢复后期的平均相对丰度最大值分别为 66.2% 和 1.5%。相比之下,亚硝基弧菌的丰度在恢复初期达到最大值(25.6%)。亚硝基螺旋体和亚硝基单胞菌相对丰度的最大干湿季节变化出现在恢复初期,而亚硝基弧菌的相对丰度最大干湿季节变化出现在恢复中期。AOB 群落的 Chao1、Shannon 和 Simpson 多样性指数随恢复阶段而增加,雨季明显高于旱季。典型对应分析结果表明,土壤易氧化碳是控制 AOB 群落多样性和放线菌丰度的主要因素。土壤容重和温度是影响蛋白质细菌丰度的主要因素。土壤 pH 值、微生物生物量碳、含水量、铵态氮、容重和温度是控制亚硝基螺菌、亚硝基单胞菌和亚硝基弧菌丰度的主要因素。因此,热带森林恢复可通过调节土壤温度、容重和易氧化碳的变化来调节优势AOB类群相对丰度的变化,从而导致土壤AOB群落多样性的增加。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
[Seasonal changes of ammonia-oxidizing bacterial communities during tropical forest restoration].

In this study, we used a high-throughput sequencing technology to survey the dry-wet seasonal change characteristics of soil ammonia-oxidizing bacteria (AOB) communities in the three restoration stages [i.e., Mallotus paniculatus community (early stage), Millettia leptobotrya community (middle stage), and Syzygium oblatum community (later stage)] of Xishuangbanna tropical forest ecosystems. We analyzed the effects of soil physicochemical characteristics on AOB community composition and diversity during tropical forest restoration. The results showed that tropical forest restoration significantly affected the relative abundance of dominant AOB phyla and their dry-wet seasonal variation. The maximum relative abundance of Proteobacteria (71.3%) was found in the early recovery stage, while that of Actinobacteria was found in the late recovery stage (1.0%). The abundances of Proteobacteria and Actinobacteria had the maximum ranges of dry-wet seasonal variation in the early and late stages, respectively. The abundance of dominant AOB genera and its dry-wet seasonal variation varied across tropical forest restoration stages. The maximum average relative abundance of Nitrosospira and Nitrosomonas in the late recovery stage was 66.2% and 1.5%, respectively. In contrast, the abundance of Nitrosovibrio reached its maximum (25.6%) in the early recovery stage. The maximum dry-wet seasonal variation in relative abundance of Nitrosospira and Nitrosomonas occurred in the early recovery stage, while that of Nitrosovibrio occurred in the middle recovery stage. The Chao1, Shannon, and Simpson diversity indices of AOB communities increased along the restoration stages, which were significantly higher in the wet season than in the dry season. The results of canonical correspondence analysis showed that soil easily oxidized carbon was the main factor controlling AOB community diversity and Actinobacteria abundance. Soil bulk density and temperature were the main factors affecting Proteobacteria abundance. Soil pH, microbial biomass carbon, water content, ammonium nitrogen, bulk density, and temperature were the main factors controlling the abundances of Nitrosospira, Nitrosomonas, and Nitrosovibrio. Therefore, tropical forest restoration can regulate the change of relative abundance of dominant AOB taxa via mediating the changes of soil temperature, bulk density, and readily oxidized carbon, leading to an increase in soil AOB community diversity.

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应用生态学报
应用生态学报 Environmental Science-Ecology
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2.50
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