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Methane emission from feather moss stands

机译:羽毛苔藓林分的甲烷排放

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Data from remote sensing and Eddy towers indicate that forests are not always net sinks for atmospheric CH4. However, studies describing specific sources within forests and functional analysis of microorganisms on sites with CH4 turnover are scarce. Feather moss stands were considered to be net sinks for carbon dioxide, but received little attention to their role in CH4 cycling. Therefore, we investigated methanogenic rates and pathways together with the methanogenic microbial community composition in feather moss stands from temperate and boreal forests. Potential rates of CH4 emission from intact moss stands (n = 60) under aerobic conditions ranged between 19 and 133 pmol CH4 h(-1) gdw(-1). Temperature and water content positively influenced CH4 emission. Methanogenic potentials determined under N-2 atmosphere in darkness ranged between 22 and 157 pmol CH4 h(-1) gdw(-1). Methane production was strongly inhibited by bromoethane sulfonate or chloroform, showing that CH4 was of microbial origin. The moss samples tested contained fluorescent microbial cells and between 10(4) and 10(5) copies per gram dry weight moss of the mcrA gene coding for a subunit of the methyl CoM reductase. Archaeal 16S rRNA and mcrA gene sequences in the moss stands were characteristic for the archaeal families Methanobacteriaceae and Methanosarcinaceae. The potential methanogenic rates were similar in incubations with and without methyl fluoride, indicating that the CH4 was produced by the hydrogenotrophic rather than aceticlastic pathway. Consistently, the CH4 produced was depleted in C-13 in comparison with the moss biomass carbon and acetate accumulated to rather high concentrations (3-62 mM). The delta C-13 of acetate was similar to that of the moss biomass, indicating acetate production by fermentation. Our study showed that the feather moss stands contained active methanogenic microbial communities producing CH4 by hydrogenotrophic methanogenesis and causing net emission of CH4 under ambient conditions, albeit at low rates.
机译:来自遥感和涡流塔的数据表明,森林并不总是大气CH4的净汇。然而,描述森林内特定来源的研究和对CH4周转地点微生物的功能分析很少。羽毛苔藓林分被认为是二氧化碳的净汇,但很少关注它们在CH4循环中的作用。因此,我们研究了温带和北方森林羽毛苔藓的产甲烷率和途径以及产甲烷微生物群落组成。在有氧条件下,完整苔藓林分(n = 60)的潜在CH4排放速率在19至133 pmol之间,CH4 h(-1) gdw(-1)。温度和含水量对CH4排放有正相关影响。在黑暗的N-2气氛下测定的产甲烷电位范围为22至157 pmol CH4 h(-1) gdw(-1)。溴乙烷磺酸盐或氯仿强烈抑制甲烷的产生,表明CH4是微生物来源的。测试的苔藓样品含有荧光微生物细胞和每克 10(4) 至 10(5) 份干重苔藓的 mcrA 基因编码甲基 CoM 还原酶亚基。苔藓林分中的古细菌16S rRNA和mcrA基因序列是古细菌科Methanobacteriaceae和Methanosarcinaceae的特征。在有和没有氟化甲烷的孵育中,潜在的产甲烷率相似,表明CH4是由氢营养途径而不是乙酸碎屑途径产生的。与苔藓生物质碳和乙酸盐积累到相当高的浓度(3-62 mM)相比,产生的CH4在C-13中持续耗尽。醋酸盐的δC-13与苔藓生物质的δC-13相似,表明通过发酵生产乙酸盐。我们的研究表明,羽毛苔藓林分含有活跃的产甲烷微生物群落,通过氢合成甲烷作用产生CH4,并在环境条件下引起CH4的净排放,尽管速率较低。

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