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水旱轮作对稻田土壤中产甲烷古菌群落结构的影响。

Effect of paddy-upland rotation on methanogenic archaeal community structure in paddy field soil.

作者信息

Liu Dongyan, Ishikawa Hiroki, Nishida Mizuhiko, Tsuchiya Kazunari, Takahashi Tomoki, Kimura Makoto, Asakawa Susumu

机构信息

Soil Biology and Chemistry, Graduate School of Bioagricultural Sciences, Nagoya University, Chikusa, Nagoya, Aichi, 464-8601, Japan,

出版信息

Microb Ecol. 2015 Jan;69(1):160-8. doi: 10.1007/s00248-014-0477-3. Epub 2014 Aug 12.

Abstract

Methanogenic archaea are strict anaerobes and demand highly reduced conditions to produce methane in paddy field soil. However, methanogenic archaea survive well under upland and aerated conditions in paddy fields and exhibit stable community. In the present study, methanogenic archaeal community was investigated in fields where paddy rice (Oryza sativa L.) under flooded conditions was rotated with soybean (Glycine max [L.] Merr.) under upland conditions at different rotation histories, by polymerase chain reaction (PCR)-denaturing gradient gel electrophoresis (DGGE) and real-time quantitative PCR methods targeting 16S rRNA and mcrA genes, respectively. Soil samples collected from the fields before flooding or seeding, during crop cultivation and after harvest of crops were analyzed. The abundance of the methanogenic archaeal populations decreased to about one-tenth in the rotational plots than in the consecutive paddy (control) plots. The composition of the methanogenic archaeal community also changed. Most members of the methanogenic archaea consisting of the orders Methanosarcinales, Methanocellales, Methanomicrobiales, and Methanobacteriales existed autochthonously in both the control and rotational plots, while some were strongly affected in the rotational plots, with fatal effect to some members belonging to the Methanosarcinales. This study revealed that the upland conversion for one or longer than 1 year in the rotational system affected the methanogenic archaeal community structure and was fatal to some members of methanogenic archaea in paddy field soil.

摘要

产甲烷古菌是严格厌氧菌,需要高度还原的条件才能在稻田土壤中产生甲烷。然而,产甲烷古菌在旱地和稻田通气条件下能很好地存活,并呈现出稳定的群落。在本研究中,通过聚合酶链反应(PCR)-变性梯度凝胶电泳(DGGE)以及分别针对16S rRNA和mcrA基因的实时定量PCR方法,对不同轮作历史下,淹水条件下的水稻(Oryza sativa L.)与旱地条件下的大豆(Glycine max [L.] Merr.)进行轮作的田间产甲烷古菌群落进行了调查。分析了在淹水或播种前、作物种植期间以及作物收获后从田间采集的土壤样本。与连续稻田(对照)地块相比,轮作地块中产甲烷古菌种群的丰度下降到约十分之一。产甲烷古菌群落的组成也发生了变化。由甲烷八叠球菌目、甲烷微菌目、甲烷杆菌目组成的大多数产甲烷古菌成员在对照地块和轮作地块中均为本地存在,而在轮作地块中一些成员受到强烈影响,对属于甲烷八叠球菌目的一些成员产生致命影响。本研究表明,轮作系统中旱地转换一年或更长时间会影响产甲烷古菌群落结构,并对稻田土壤中产甲烷古菌的一些成员产生致命影响。

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