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氨氧化古菌中亚硝酸盐还原酶的同源物:多样性和基因组背景。

Homologues of nitrite reductases in ammonia-oxidizing archaea: diversity and genomic context.

机构信息

Department of Biology, Centre for Geobiology, University of Bergen, PO Box 7803, 5020 Bergen, Norway.

出版信息

Environ Microbiol. 2010 Apr;12(4):1075-88. doi: 10.1111/j.1462-2920.2010.02153.x. Epub 2010 Feb 3.

DOI:10.1111/j.1462-2920.2010.02153.x
PMID:20132279
Abstract

Ammonia-oxidizing archaea are frequent and ubiquitous inhabitants of terrestrial and marine environments. As they have only recently been detected, most aspects of their metabolism are yet unknown. Here we report on the occurrence of genes encoding potential homologues of copper-dependent nitrite reductases (NirK) in ammonia-oxidizing archaea of soils and other environments using metagenomic approaches and PCR amplification. Two pairs of highly overlapping 40 kb genome fragments, each containing nirK genes of archaea, were isolated from a metagenomic soil library. Between 68% and 85% of the open reading frames on these genome fragments had homologues in the genomes of the marine archaeal ammonia oxidizers Nitrosopumilus maritimus and Cenarchaeum symbiosum. Extensions of NirK homologues with C-terminal fused amicyanin domains were deduced from two of the four fosmids indicating structural variation of these multicopper proteins in archaea. Phylogenetic analyses including all major groups of currently known NirK homologues revealed that the deduced protein sequences of marine and soil archaea were separated into two highly divergent lineages that did not contain bacterial homologues. In contrast, another separated lineage contained potential multicopper oxidases of both domains, archaea and bacteria. More nirK gene variants directly amplified by PCR from several environments indicated further diversity of the gene and a widespread occurrence in archaea. Transcription of the potential archaeal nirK in soil was demonstrated at different water contents, but no significant increase in transcript copy number was observed with increased denitrifying activity.

摘要

氨氧化古菌是陆地和海洋环境中常见且广泛存在的微生物。由于它们最近才被发现,其代谢的大多数方面还不为人知。本研究采用宏基因组学方法和 PCR 扩增技术,报告了土壤和其他环境中氨氧化古菌中潜在铜依赖亚硝酸盐还原酶(NirK)基因的存在。从土壤宏基因组文库中分离到了两对高度重叠的 40 kb 基因组片段,每个片段都包含古菌的 NirK 基因。这两个基因组片段上的开放阅读框有 68%-85%与海洋古菌氨氧化菌 Nitrosopumilus maritimus 和 Cenarchaeum symbiosum 的基因组中的同源物有同源性。从这 4 个fosmid 中的两个中推导出了 NirK 同源物的 C 端融合的蓝铜蛋白结构域延伸,表明这些多铜蛋白在古菌中的结构存在差异。包括目前已知所有主要 NirK 同源物组的系统发育分析表明,海洋和土壤古菌推导的蛋白序列分为两个高度分化的谱系,这些谱系不包含细菌同源物。相比之下,另一个独立的谱系包含了两个域的潜在多铜氧化酶,古菌和细菌。从几个环境中直接通过 PCR 扩增的更多 nirK 基因变体表明了该基因的进一步多样性,并在古菌中广泛存在。在不同的含水量下证明了土壤中潜在的古菌 nirK 的转录,但随着脱氮活性的增加,转录物拷贝数没有明显增加。

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