Functional and structural response of the methanogenic microbial community in rice field soil to temperature change

被引:83
|
作者
Conrad, Ralf [1 ]
Klose, Melanie [1 ]
Noll, Matthias [1 ,2 ]
机构
[1] Max Planck Inst Terr Microbiol, D-35043 Marburg, Germany
[2] Fed Inst Mat Res & Testing, BAM, Div Biol Mat Protect & Environm Issues 5 1, D-12205 Berlin, Germany
关键词
PADDY SOIL; ARCHAEAL COMMUNITY; METHANE PRODUCTION; CARBON-DIOXIDE; CLUSTER-I; GENOTYPIC DIVERSITY; CLIMATE-CHANGE; RIBOSOMAL-RNA; EMISSION; BIODIVERSITY;
D O I
10.1111/j.1462-2920.2009.01909.x
中图分类号
Q93 [微生物学];
学科分类号
071005 ; 100705 ;
摘要
P>The microbial community in anoxic rice field soil produces CH(4) over a wide temperature range up to 55 degrees C. However, at temperatures higher than about 40 degrees C, the methanogenic path changes from CH(4) production by hydrogenotrophic plus acetoclastic methanogenesis to exclusively hydrogenotrophic methanogenesis and simultaneously, the methanogenic community consisting of Methanosarcinaceae, Methanoseataceae, Methanomicrobiales, Methanobacteriales and Rice Cluster I (RC-1) changes to almost complete dominance of RC-1. We studied changes in structure and function of the methanogenic community with temperature to see whether microbial members of the community were lost or their function impaired by exposure to high temperature. We characterized the function of the community by the path of CH(4) production measuring delta(13)C in CH(4) and CO(2) and calculating the apparent fractionation factor (alpha(app)) and the structure of the community by analysis of the terminal restriction fragment length polymorphism (T-RFLP) of the microbial 16S rRNA genes. Shift of the temperature from 45 degrees C to 35 degrees C resulted in a corresponding shift of function and structure, especially when some 35 degrees C soil was added to the 45 degrees C soil. The bacterial community (T-RFLP patterns), which was much more diverse than the archaeal community, changed in a similar manner upon temperature shift. Incubation of a mixture of 35 degrees C and 50 degrees C pre-incubated methanogenic rice field soil at different temperatures resulted in functionally and structurally well-defined communities. Although function changed from a mixture of acetoclastic and hydrogenotrophic methanogenesis to exclusively hydrogenotrophic methanogenesis over a rather narrow temperature range of 42-46 degrees C, each of these temperatures also resulted in only one characteristic function and structure. Our study showed that temperature conditions defined structure and function of the methanogenic microbial community.
引用
收藏
页码:1844 / 1853
页数:10
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