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[红壤稻田土壤中负责好氧甲烷氧化的活性微生物的下一代测序与稳定同位素探测]

[Next generation sequencing and stable isotope probing of active microorganisms responsible for aerobic methane oxidation in red paddy soils].

作者信息

Zheng Yan, Jia Zhongjun

机构信息

State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China.

出版信息

Wei Sheng Wu Xue Bao. 2013 Feb 4;53(2):173-84.

Abstract

OBJECTIVE

This study is aimed to establish an unbiased profiling strategy for investigating the microorganisms responsible for aerobic methane oxidation by pyrosequencing the total soil microbial communities at DNA and RNA levels, and to link aerobic methane oxidation activity with taxonomic identity of active microorganisms by DNA/RNA SIP in red paddy soils.

METHODS

Three red paddy soils derived from quaternary red clay were collected from Gushi and Taoyuan cities of Hunan province and Leizhou city of Guangdong province, were incubated with the labeled 13CH4 or 12CH4 for determination of aerobic methane oxidation kinetics. Pyrosequencing of the 16S rRNA andl6S rRNA gene at the whole microbial community levels were performed over the course of aerobic methane oxidation in soil microcosms. 13C-DNA and 13C-RNA were obtained through ultracentrifugation of the total soil DNA and RNA extracts, respectively. Clone library of pmoA genes in 13C-DNA and 16S rRNA genes in 13C-RNA were constructed.

RESULTS

Pyrosequencing of the total microbial communities revealed significant increase in the relative abundance of aerobic methanotrophs in soil microcosms upon the completion of aerobic methane consumption. The proportional increase of aerobic methanotrophs was significantly higher at RNA than DNA levels. Type I and II aerobic methanotrophs significantly increased in Gushi soil, while the significant increase of type II aerobic methanotrophs was observed in Taoyuan soil. In the meantime, type I aerobic methanotrophs appeared to be stimulated exclusively in Leizhou soil. Sequencing analysis of the 13C-labeled pmoA genes and 16S rRNA further demonstrate that phylogenetically distinct methanotrophs dominated aerobic methane oxidation activity in paddy soils of Gushi (Type I and II), Taoyuan (Type II) and Leizhou (Type I).

CONCLUSION

High-throughput pyrosequencing at the whole community level of 16S rRNA genes provides an almost unbiased profiling stragety for measuring characteristic changes in relative proportions of aerobic methanotrophs responsible for aerobic methane oxidation activity in red paddy soils, and higher sensitivity was observed at RNA than DNA levels. DNA/RNA-SIP can accurately reveal the active microorganisms responsible for aerobic methane oxidation in read soil, being largely consistent to pyrosequencing-based fingerprinting analysis of the total microbial communities.

摘要

目的

本研究旨在通过对红壤稻田土壤微生物群落的DNA和RNA水平进行焦磷酸测序,建立一种无偏差的分析策略,以研究参与好氧甲烷氧化的微生物,并通过DNA/RNA稳定同位素探针(SIP)将好氧甲烷氧化活性与活性微生物的分类身份联系起来。

方法

从湖南省的古丈市和桃源市以及广东省的雷州市采集了三种源自第四纪红粘土的红壤稻田土壤,用标记的13CH4或12CH4进行培养,以测定好氧甲烷氧化动力学。在土壤微宇宙好氧甲烷氧化过程中,对整个微生物群落水平的16S rRNA和16S rRNA基因进行焦磷酸测序。分别通过对土壤总DNA和RNA提取物进行超速离心获得13C-DNA和13C-RNA。构建13C-DNA中pmoA基因和13C-RNA中16S rRNA基因的克隆文库。

结果

对整个微生物群落的焦磷酸测序显示,在好氧甲烷消耗完成后,土壤微宇宙中好氧甲烷氧化菌的相对丰度显著增加。好氧甲烷氧化菌的比例增加在RNA水平上显著高于DNA水平。古丈土壤中I型和II型好氧甲烷氧化菌显著增加,而桃源土壤中仅观察到II型好氧甲烷氧化菌显著增加。同时,I型好氧甲烷氧化菌似乎仅在雷州土壤中受到刺激。对13C标记的pmoA基因和16S rRNA的测序分析进一步表明,系统发育上不同的甲烷氧化菌在古丈(I型和II型)、桃源(II型)和雷州(I型)的稻田土壤好氧甲烷氧化活性中占主导地位。

结论

在16S rRNA基因的整个群落水平上进行高通量焦磷酸测序,为测量红壤稻田土壤中参与好氧甲烷氧化活性的好氧甲烷氧化菌相对比例的特征变化提供了一种几乎无偏差的分析策略,并且在RNA水平上比DNA水平具有更高的灵敏度。DNA/RNA-SIP可以准确揭示红壤稻田中负责好氧甲烷氧化的活性微生物,这与基于焦磷酸测序的整个微生物群落指纹分析基本一致。

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