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在疑似厌氧甲烷氧化古菌(ANME)中,存在甲烷净产生和氧化的环境证据。

Environmental evidence for net methane production and oxidation in putative ANaerobic MEthanotrophic (ANME) archaea.

机构信息

Center for Geomicrobiology, Ny Munkegade 114, Bldg 1540, Aarhus University, 8000-Aarhus C, Denmark.

出版信息

Environ Microbiol. 2011 Sep;13(9):2548-64. doi: 10.1111/j.1462-2920.2011.02526.x. Epub 2011 Aug 2.

DOI:10.1111/j.1462-2920.2011.02526.x
PMID:21806748
Abstract

Uncultured ANaerobic MEthanotrophic (ANME) archaea are often assumed to be obligate methanotrophs that are incapable of net methanogenesis, and are therefore used as proxies for anaerobic methane oxidation in many environments in spite of uncertainty regarding their metabolic capabilities. Anaerobic methane oxidation regulates methane emissions in marine sediments and appears to occur through a reversal of a methane-producing metabolism. We tested the assumption that ANME are obligate methanotrophs by detecting and quantifying gene transcription of ANME-1 across zones of methane oxidation versus methane production in sediments from the White Oak River estuary, North Carolina. ANME-1 consistently transcribe 16S rRNA and mRNA of methyl coenzyme M reductase (mcrA), the key gene for methanogenesis, up to 45 cm into methanogenic sediments. CARD-FISH shows that ANME-1 exist as single rod-shaped cells or pairs of cells. Integrating normalized depth distributions of 16S rDNA and rRNA (measured with qPCR and RT-qPCR respectively) shows that 26-77% of the rDNA (a proxy for ANME-1 cell numbers), and 18-76% of the rRNA (a proxy for ANME-1 activity) occurs within methane-producing sediments. These results, along with a re-assessment of the published Iiterature, change the perspective to ANME-1 as methanogens that are also capable of methane oxidation.

摘要

未培养的厌氧甲烷营养型(ANME)古菌通常被认为是专性甲烷营养型微生物,不能进行净甲烷生成,因此尽管其代谢能力存在不确定性,但在许多环境中仍被用作厌氧甲烷氧化的替代物。厌氧甲烷氧化调节海洋沉积物中的甲烷排放,似乎是通过逆转产甲烷代谢来实现的。我们通过在北卡罗来纳州的白河河口的沉积物中检测和定量分析 ANME-1 的基因转录,以检测 ANME 是否是专性甲烷营养型微生物,该基因转录横跨甲烷氧化区与甲烷生成区。ANME-1 始终转录 16S rRNA 和甲基辅酶 M 还原酶(mcrA)的 mRNA,mcrA 是产甲烷的关键基因,在产甲烷沉积物中可达 45 厘米。CARD-FISH 显示 ANME-1 以单个杆状细胞或成对细胞存在。整合 16S rDNA 和 rRNA 的归一化深度分布(分别用 qPCR 和 RT-qPCR 测量)表明,26-77%的 rDNA(代表 ANME-1 细胞数量)和 18-76%的 rRNA(代表 ANME-1 活性)发生在产甲烷沉积物中。这些结果,以及对已发表文献的重新评估,改变了对 ANME-1 作为既能进行甲烷氧化又能进行甲烷生成的微生物的看法。

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