Reim Andreas, Hernández Marcela, Klose Melanie, Chidthaisong Amnat, Yuttitham Monthira, Conrad Ralf
Max Planck Institute for Terrestrial MicrobiologyMarburg, Germany.
Centre for Biological Sciences, University of SouthamptonSouthampton, UK.
Front Microbiol. 2017 May 5;8:785. doi: 10.3389/fmicb.2017.00785. eCollection 2017.
Rice paddies in central Thailand are flooded either by irrigation (irrigated rice) or by rain (rain-fed rice). The paddy soils and their microbial communities thus experience permanent or arbitrary submergence, respectively. Since methane production depends on anaerobic conditions, we hypothesized that structure and function of the methanogenic microbial communities are different in irrigated and rain-fed paddies and react differently upon desiccation stress. We determined rates and relative proportions of hydrogenotrophic and aceticlastic methanogenesis before and after short-term drying of soil samples from replicate fields. The methanogenic pathway was determined by analyzing concentrations and δC of organic carbon and of CH and CO produced in the presence and absence of methyl fluoride, an inhibitor of aceticlastic methanogenesis. We also determined the abundance (qPCR) of genes and transcripts of bacterial 16S rRNA, archaeal 16S rRNA and methanogenic (coding for a subunit of the methyl coenzyme M reductase) and the composition of these microbial communities by T-RFLP fingerprinting and/or Illumina deep sequencing. The abundances of genes and transcripts were similar in irrigated and rain-fed paddy soil. They also did not change much upon desiccation and rewetting, except the transcripts of , which increased by more than two orders of magnitude. In parallel, rates of CH production also increased, in rain-fed soil more than in irrigated soil. The contribution of hydrogenotrophic methanogenesis increased in rain-fed soil and became similar to that in irrigated soil. However, the relative microbial community composition on higher taxonomic levels was similar between irrigated and rain-fed soil. On the other hand, desiccation and subsequent anaerobic reincubation resulted in systematic changes in the composition of microbial communities for both Archaea and Bacteria. It is noteworthy that differences in the community composition were mostly detected on the level of operational taxonomic units (OTUs; 97% sequence similarity). The treatments resulted in change of the relative abundance of several archaeal OTUs. Some OTUs of , , and increased, while some of and decreased. Bacterial OTUs within , and increased, while OTUs within other proteobacterial classes decreased.
泰国中部的稻田要么通过灌溉(灌溉水稻)要么通过降雨(雨养水稻)被淹没。因此,稻田土壤及其微生物群落分别经历长期或不定期的淹水。由于甲烷产生依赖于厌氧条件,我们推测产甲烷微生物群落的结构和功能在灌溉稻田和雨养稻田中有所不同,并且在干燥胁迫下反应也不同。我们测定了来自重复田间的土壤样品短期干燥前后氢营养型和乙酸裂解型甲烷生成的速率及相对比例。通过分析在有和没有氟甲烷(一种乙酸裂解型甲烷生成抑制剂)存在的情况下产生的有机碳、CH 和 CO 的浓度及 δC,确定了甲烷生成途径。我们还通过 T-RFLP 指纹图谱和/或 Illumina 深度测序确定了细菌 16S rRNA、古菌 16S rRNA 和产甲烷基因(编码甲基辅酶 M 还原酶的一个亚基)的基因和转录本丰度(qPCR)以及这些微生物群落的组成。灌溉稻田和雨养稻田土壤中的基因和转录本丰度相似。除了 的转录本增加了两个多数量级外,它们在干燥和再湿润后变化也不大。与此同时,CH 产生速率也增加了,雨养土壤中的增加幅度大于灌溉土壤。雨养土壤中氢营养型甲烷生成的贡献增加并与灌溉土壤中的相似。然而,灌溉土壤和雨养土壤在较高分类水平上的相对微生物群落组成相似。另一方面,干燥和随后的厌氧再培养导致古菌和细菌的微生物群落组成发生系统性变化。值得注意的是,群落组成差异大多在操作分类单元(OTU;97%序列相似性)水平上被检测到。这些处理导致几个古菌 OTU 的相对丰度发生变化。 、 、 和 的一些 OTU 增加,而 和 的一些 OTU 减少。 、 和 内的细菌 OTU 增加,而其他变形菌纲类别的 OTU 减少。