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硝酸盐和硫酸盐依赖型甲烷厌氧共氧化作用:连接碳、氮和硫循环。

Simultaneous nitrate and sulfate dependent anaerobic oxidation of methane linking carbon, nitrogen and sulfur cycles.

机构信息

State Key Laboratory of Urban Water Resource and Environment, School of Environment, Harbin Institute of Technology, No.73, Huanghe Road, Nangang District, Harbin, Heilongjiang, 150090, China.

State Key Laboratory of Urban Water Resource and Environment, School of Environment, Harbin Institute of Technology, No.73, Huanghe Road, Nangang District, Harbin, Heilongjiang, 150090, China.

出版信息

Water Res. 2021 Apr 15;194:116928. doi: 10.1016/j.watres.2021.116928. Epub 2021 Feb 13.

Abstract

ANaerobic MEthanotrophic (ANME) archaea are critical microorganisms mitigating methane emission from anoxic zones. In previous studies, sulfate-dependent anaerobic oxidation of methane (AOM) and nitrate-dependent AOM, performed by different clades of ANME archaea, were detected in marine sediments and freshwater environments, respectively. This study shows that simultaneous sulfate- and nitrate-dependent AOM can be mediated by a clade of ANME archaea, which may occur in estuaries and coastal zones, at the interface of marine and freshwater environments enriched with sulfate and nitrate. Long-term (~1,200 days) performance data of a bioreactor, metagenomic analysis and batch experiments demonstrated that ANME-2d not only conducted AOM coupled to reduction of nitrate to nitrite, but also coupled to the conversion of sulfate to sulfide, in collaboration with sulfate-reducing bacteria (SRB). Sulfide was oxidized back to sulfate by sulfide-oxidizing autotrophic denitrifiers with nitrate or nitrite as electron acceptors, in turn alleviating sulfide accumulation. In addition, dissimilatory nitrate reduction to ammonium performed by ANME-2d was detected, providing substrates to Anammox. Metatranscriptomic analysis revealed significant upregulation of flaB in ANME-2d and pilA in Desulfococcus, which likely resulted in the formation of unique nanonets connecting cells and expanding within the biofilm, and putatively providing structural links between ANME-2d and SRB for electron transfer. Simultaneous nitrate- and sulfate-dependent AOM as observed in this study could be an important link between the carbon, nitrogen and sulfur cycles in natural environments, such as nearshore environments.

摘要

好氧甲烷营养型 (ANME) 古菌是减少缺氧区甲烷排放的关键微生物。在之前的研究中,分别在海洋沉积物和淡水环境中检测到硫酸盐依赖型厌氧甲烷氧化 (AOM) 和硝酸盐依赖型 AOM,由不同分支的 ANME 古菌执行。本研究表明,硫酸盐和硝酸盐依赖型 AOM 可以由 ANME 古菌的一个分支介导,该分支可能存在于富含硫酸盐和硝酸盐的河口和沿海地区,海洋和淡水环境的交界处。长期 (~1,200 天) 生物反应器性能数据、宏基因组分析和批量实验表明,ANME-2d 不仅进行了与硝酸盐还原为亚硝酸盐偶联的 AOM,还与硫酸盐还原细菌 (SRB) 合作进行了与硫酸盐转化为硫化物偶联的 AOM。硫化物被硫氧化自养反硝化细菌以硝酸盐或亚硝酸盐作为电子受体氧化回硫酸盐,从而缓解硫化物积累。此外,还检测到 ANME-2d 进行的异化硝酸盐还原为铵,为 Anammox 提供了底物。宏转录组分析显示,ANME-2d 中的 flaB 和 Desulfococcus 中的 pilA 显著上调,这可能导致形成连接细胞的独特纳米网,并在生物膜内扩展,并可能为 ANME-2d 和 SRB 之间提供电子转移的结构连接。本研究中观察到的同时依赖硝酸盐和硫酸盐的 AOM 可能是自然环境中碳、氮和硫循环之间的重要联系,例如近岸环境。

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