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反硝化厌氧甲烷氧化菌和古菌的生态位分化导致西藏高寒湿地中甲烷的有效过滤。

Niche differentiation of denitrifying anaerobic methane oxidizing bacteria and archaea leads to effective methane filtration in a Tibetan alpine wetland.

机构信息

Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, 100085 Beijing, China; University of Chinese Academy of Sciences, 100049 Beijing, China.

Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, 100085 Beijing, China; University of Chinese Academy of Sciences, 100049 Beijing, China.

出版信息

Environ Int. 2020 Jul;140:105764. doi: 10.1016/j.envint.2020.105764. Epub 2020 May 1.

Abstract

Denitrifying anaerobic methane oxidation (DAMO) is a vital methane sink in wetlands. However, the interactions and niche partitioning of DAMO bacteria and archaea in freshwater wetland soils, in addition to the interactions among microorganisms that couple methane and nitrogen cycling is still unclear, despite that these factors may govern the fate of methane and nitrogen in wetlands. Here, we evaluated the vertical distribution of DAMO bacteria and archaea in soil layers along with the potential interactions among populations in the methane-coupled nitrogen cycling microbial community of Tibetan freshwater wetlands. A combination of molecular biology, stable isotope tracer technology, and microbial bioinformatics was used to evaluate these interrelated dynamics. The abundances and potential methane oxidation rates indicated that DAMO bacteria and archaea differentially occupy surface and subsurface soil layers, respectively. The inferred interactions between DAMO bacteria and nitrogen cycling microorganisms within their communities are complex, DAMO bacteria apparently achieve an advantage in the highly competitive environment of surface soils layers and occupy a specific niche in those environments. Conversely, the apparent relationships between DAMO archaea and nitrogen cycling microorganisms are relatively simple, wherein high levels of cooperation are inferred between DAMO archaea and nitrate-producing organisms in subsurface soils layers. These results suggest that the vertical distribution patterns of DAMO bacteria and archaea enable them to play significant roles in the methane oxidation activity of different soil layers and collectively form an effective methane filtration consortium.

摘要

反硝化厌氧甲烷氧化(DAMO)是湿地中重要的甲烷汇。然而,尽管这些因素可能控制湿地中甲烷和氮的命运,但淡水湿地土壤中 DAMO 细菌和古菌的相互作用和生态位划分,以及耦合甲烷和氮循环的微生物之间的相互作用仍不清楚。在这里,我们评估了西藏淡水湿地甲烷耦合氮循环微生物群落中 DAMO 细菌和古菌在土壤层中的垂直分布以及种群之间潜在相互作用。我们结合了分子生物学、稳定同位素示踪技术和微生物生物信息学来评估这些相互关联的动态。丰度和潜在甲烷氧化速率表明,DAMO 细菌和古菌分别占据了表层和次表层土壤。推测 DAMO 细菌和氮循环微生物在其群落内的相互作用是复杂的,DAMO 细菌显然在表层土壤的高度竞争环境中占据优势,并在这些环境中占据特定的生态位。相反,DAMO 古菌与氮循环微生物之间的明显关系相对简单,在次表层土壤中,DAMO 古菌和产生硝酸盐的生物之间推断存在高水平的合作。这些结果表明,DAMO 细菌和古菌的垂直分布模式使它们能够在不同土壤层的甲烷氧化活性中发挥重要作用,并共同形成有效的甲烷过滤联合体。

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