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Responses of Methanogenic and Methanotrophic Communities to Elevated Atmospheric CO2 and Temperature in a Paddy Field

机译:稻田产甲烷和甲烷营养群落对大气CO2和温度升高的响应

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摘要

Although climate change is predicted to affect methane (CH4) emissions in paddy soil, the dynamics of methanogens and methanotrophs in paddy fields under climate change have not yet been fully investigated. To address this issue, a multifactor climate change experiment was conducted in a Chinese paddy field using the following experimental treatments: (1) enrichment of atmospheric CO2 concentrations (500 ppm, CE), (2) canopy air warming (2°C above the ambient, WA), (3) combined CO2 enrichment and warming (CW), and (4) ambient conditions (CK). We analyzed the abundance of methanogens and methanotrophs, community structures, CH4 production and oxidation potentials, in situ CH4 emissions using real-time PCR, T-RFLP, and clone library techniques, as well as biochemical assays. Compared to the control under CE and CW treatments, CH4 production potential, methanogenic gene abundance and soil microbial biomass carbon significantly increased; the methanogenic community, however, remained stable. The canopy air warming treatment only had an effect on CH4 oxidation potential at the ripening stage. Phylogenic analysis indicated that methanogens in the rhizosphere were dominated by Methanosarcina, Methanocellales, Methanobacteriales, and Methanomicrobiales, while methanotrophic sequences were classified as Methylococcus, Methylocaldum, Methylomonas, Methylosarcina (Type I) and Methylocystis (Type II). However, the relative abundance of Methylococcus (Type I) decreased under CE and CW treatments and the relative abundance of Methylocystis (Type II) increased. The in situ CH4 fluxes indicated similar seasonal patterns between treatments; both CE and CW increased CH4 emissions. In conclusion results suggest that methanogens and methanotrophs respond differently to elevated atmospheric CO2 concentrations and warming, thus adding insights into the effects of simulated global climate change on CH4 emissions in paddy fields.
机译:尽管预计气候变化会影响稻田土壤中的甲烷(CH4)排放,但尚未对气候变化下稻田中产甲烷菌和甲烷营养菌的动力学进行充分研究。为了解决这个问题,我们在中国稻田采用以下实验方法进行了多因素气候变化实验:(1)富集大气中的CO2浓度(500 ppm,CE),(2)冠层空气变暖(高于地面2°C) (3)合并CO2富集和变暖(CW),以及(4)环境条件(CK)。我们使用实时荧光定量PCR,T-RFLP和克隆文库技术以及生化分析方法,分析了甲烷菌和甲烷营养菌的丰度,群落结构,CH4的产生和氧化电位,CH4的原位排放。与CE和CW处理相比,CH4的生产潜力,产甲烷基因的丰度和土壤微生物量碳显着增加。然而,产甲烷群落保持稳定。冠层空气加温处理仅对成熟阶段的CH4氧化电位有影响。系统发育分析表明,根际中的产甲烷菌主要为甲烷藻,甲烷球菌,甲烷细菌和甲烷微粒,而甲烷营养序列被分类为甲基球菌,甲基本地细菌,甲基单孢菌,甲基甲虫(I型)和甲基囊虫(II型)。但是,在CE和CW处理下,甲基球菌(I型)的相对丰度降低,而甲基囊藻(II型)的相对丰度升高。原位CH4通量表明处理之间的相似季节性模式。 CE和CW都增加了CH4排放。总之,结果表明,产甲烷菌和甲烷营养生物对升高的大气CO2浓度和变暖的反应不同,从而增加了对模拟的全球气候变化对稻田CH4排放影响的见解。

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