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[稻田土壤中亚硝酸盐依赖型厌氧甲烷氧化细菌群落结构的时空特征]

[Spatial and temporal characteristics of community structure of nitrite-dependent anaerobic methane-oxidizing bacteria in paddy soil].

作者信息

Tian Mao-Hui, Shen Li-Dong, Liu Xin, Yang Wang-Ting, Jin Jing-Hao, Yang Yu-Ling, Liu Jia-Qi

机构信息

School of Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing 210044, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2022 Jan;33(1):239-247. doi: 10.13287/j.1001-9332.202112.025.

DOI:10.13287/j.1001-9332.202112.025
PMID:35224946
Abstract

Paddy fields are one of the most important methane sources, which have great impacts on climate change. The nitrite-dependent anaerobic methane oxidation, by NC10 phylum bacteria- Methylomirabilis oxyfera ()-like bacteria, is a new process regulating methane emission from paddy fields. However, little is known about the spatial and temporal variations of -like bacterial communities and the regulating factors in paddy soils. We investigated the community composition, diversity, and abundance of -like bacteria in 0-40 cm depth of paddy soils at key growth stages of rice, including tillering, jointing, flowering, and milky stages. Results of high-throughput sequencing showed that community composition of -like bacteria differed significantly among different soil layers, while no significant variation was observed among different rice growth stages. The diversity of -like bacteria increased with soil depth. Real-time quantitative PCR showed that the 16S rRNA gene abundance of -like bacteria ranged from 5.73×10 to 2.56×10 copies·g (dry weight), with the highest gene abundance in the 10-20 cm layer. Further, the abundance of these bacteria showed a decreasing trend with rice growth. Soil organic carbon content and soil pH were correlated with the -like bacterial community structures and abundance. In all, our results suggested a certain degree of heterogeneity of spatial and temporal distribution of -like bacterial communities in paddy soils, which was largely influenced by soil organic carbon and soil pH.

摘要

稻田是最重要的甲烷排放源之一,对气候变化有重大影响。由NC10门细菌——嗜氧甲基奇异菌(Methylomirabilis oxyfera)类细菌进行的亚硝酸盐依赖型厌氧甲烷氧化,是一种调节稻田甲烷排放的新过程。然而,关于稻田土壤中嗜氧甲基奇异菌类细菌群落的时空变化及其调控因素,人们了解甚少。我们研究了水稻关键生长阶段(包括分蘖期、拔节期、开花期和乳熟期)稻田土壤0-40厘米深度内嗜氧甲基奇异菌类细菌的群落组成、多样性和丰度。高通量测序结果表明,嗜氧甲基奇异菌类细菌的群落组成在不同土层间存在显著差异,而在不同水稻生长阶段未观察到显著变化。嗜氧甲基奇异菌类细菌的多样性随土壤深度增加而增加。实时定量PCR结果显示,嗜氧甲基奇异菌类细菌的16S rRNA基因丰度范围为5.73×10至2.56×10拷贝·克(干重),在10-20厘米土层中基因丰度最高。此外,这些细菌的丰度随水稻生长呈下降趋势。土壤有机碳含量和土壤pH与嗜氧甲基奇异菌类细菌群落结构和丰度相关。总之,我们的结果表明稻田土壤中嗜氧甲基奇异菌类细菌群落的时空分布存在一定程度的异质性,这在很大程度上受土壤有机碳和土壤pH的影响。

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