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首页> 外文期刊>Applied Microbiology >Alpha- and Gammaproteobacterial Methanotrophs Codominate the Active Methane-Oxidizing Communities in an Acidic Boreal Peat Bog
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Alpha- and Gammaproteobacterial Methanotrophs Codominate the Active Methane-Oxidizing Communities in an Acidic Boreal Peat Bog

机译:酸性和北方泥炭沼泽中的α-和γ-proteobacterial甲烷氧化菌共占活跃的甲烷氧化社区。

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The objective of this study was to characterize metabolically active, aerobic methanotrophs in an ombrotrophic peatland in the Marcell Experimental Forest, in Minnesota. Methanotrophs were investigated in the field and in laboratory incubations using DNA-stable isotope probing (SIP), expression studies on particulate methane monooxygenase ( pmoA ) genes, and amplicon sequencing of 16S rRNA genes. Potential rates of oxidation ranged from 14 to 17 μmol of CH_(4) g dry weight soil~(?1) day~(?1). Within DNA-SIP incubations, the relative abundance of methanotrophs increased from 4% in situ to 25 to 36% after 8 to 14 days. Phylogenetic analysis of the ~(13)C-enriched DNA fractions revealed that the active methanotrophs were dominated by the genera Methylocystis (type II; Alphaproteobacteria ), Methylomonas , and Methylovulum (both, type I; Gammaproteobacteria ). In field samples, a transcript-to-gene ratio of 1 to 2 was observed for pmoA in surface peat layers, which attenuated rapidly with depth, indicating that the highest methane consumption was associated with a depth of 0 to 10 cm. Metagenomes and sequencing of cDNA pmoA amplicons from field samples confirmed that the dominant active methanotrophs were Methylocystis and Methylomonas . Although type II methanotrophs have long been shown to mediate methane consumption in peatlands, our results indicate that members of the genera Methylomonas and Methylovulum (type I) can significantly contribute to aerobic methane oxidation in these ecosystems.
机译:这项研究的目的是表征明尼苏达州马塞勒实验森林中一个非营养养护泥炭地中具有代谢活性的好氧甲烷营养生物。在野外和实验室中,使用DNA稳定同位素探测(SIP),甲烷颗粒单加氧酶(pmoA)基因的表达研究以及16S rRNA基因的扩增子测序研究了甲烷氧化菌。 CH_(4)g干重土壤〜(?1)天〜(?1)的氧化潜力为14至17μmol。在DNA-SIP孵育中,在8至14天后,甲烷营养菌的相对丰度从原位的4%增加到25%至36%。对〜(13)C富集的DNA馏分进行的系统进化分析表明,活性甲烷氧化菌主要由甲基囊藻属(II型; Alphaproteobacteria),甲基单胞菌属和Methylovulum(均为I型;γproteobacteria)支配。在田间样品中,表面泥炭层中pmoA的转录本与基因之比为1到2,随着深度的增加而迅速衰减,表明最高的甲烷消耗量与0到10 cm的深度有关。从野外样品的基因组和cDNA pmoA扩增子的测序证实,主要的活性甲基嗜营养菌是甲基囊藻和甲基单胞菌。尽管长期以来,II型甲烷营养生物已被证明可以介导泥炭地的甲烷消耗,但我们的结果表明,甲基单孢菌属和甲基ovulum属(I型)的成员可以显着促进这些生态系统中的好氧甲烷氧化。

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