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Complete-fosmid and fosmid-end sequences reveal frequent horizontal gene transfers in marine uncultured planktonic archaea

机译:完整的fosmid和fosmid末端序列揭示了海洋未培养的浮游古细菌中频繁的水平基因转移

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摘要

The extent of horizontal gene transfer (HGT) among marine pelagic prokaryotes and the role that HGT may have played in their adaptation to this particular environment remain open questions. This is partly due to the paucity of cultured species and genomic information for many widespread groups of marine bacteria and archaea. Molecular studies have revealed a large diversity and relative abundance of marine planktonic archaea, in particular of Thaumarchaeota (also known as group I Crenarchaeota) and Euryarchaeota of groups II and III, but only one species (the thaumarchaeote Candidatus Nitrosopumilus maritimus) has been isolated in pure culture so far. Therefore, metagenomics remains the most powerful approach to study these environmental groups. To investigate the impact of HGT in marine archaea, we carried out detailed phylogenetic analyses of all open reading frames of 21 archaeal 16S rRNA gene-containing fosmids and, to extend our analysis to other genomic regions, also of fosmid-end sequences of 12 774 fosmids from three different deep-sea locations (South Atlantic and Adriatic Sea at 1000 m depth, and Ionian Sea at 3000 m depth). We found high HGT rates in both marine planktonic Thaumarchaeota and Euryarchaeota, with remarkable converging values estimated from complete-fosmid and fosmid-end sequence analysis (25 and 21% of the genes, respectively). Most HGTs came from bacterial donors (mainly from Proteobacteria, Firmicutes and Chloroflexi) but also from other archaea and eukaryotes. Phylogenetic analyses showed that in most cases HGTs are shared by several representatives of the studied groups, implying that they are ancient and have been conserved over relatively long evolutionary periods. This, together with the functions carried out by these acquired genes (mostly related to energy metabolism and transport of metabolites across membranes), suggests that HGT has played an important role in the adaptation of these archaea to the cold and nutrient-depleted deep marine environment.
机译:海洋浮游原核生物之间水平基因转移(HGT)的程度以及HGT在其适应这种特定环境中可能发挥的作用仍然是尚待解决的问题。部分原因是由于许多广泛的海洋细菌和古细菌群体的养殖物种和基因信息不足。分子研究表明,海洋浮游古细菌,特别是Thaumarchaeota(也称为I Crenarchaeota组)和Euryarchaeota,属于第II和III组,具有很大的多样性和相对丰富性,但在该州仅分离出一个物种(thaumarchaeote念珠菌Nitrosopumilus maritimus)。到目前为止,纯文化。因此,宏基因组学仍然是研究这些环境群体的最有效方法。为了研究HGT对海洋古生菌的影响,我们对21种古生的含16S rRNA基因的fosmids的所有开放阅读框进行了详细的系统进化分析,并将其扩展到其他基因组区域,也包括12 774 fosmid末端序列来自三个不同深海位置(南大西洋和亚得里亚海的深度为1000µm,爱奥尼亚海的深度为3,000)的软体动物。我们发现海洋浮游性Thaumarchaeota和Euryarchaeota的HGT率均很高,通过完全fosmid和fosmid末端序列分析(分别为基因的25%和21%)估算出显着的收敛值。大多数HGT来自细菌供体(主要来自变形杆菌,硬毛菌和绿藻),也来自其他古细菌和真核生物。系统发育分析表明,在大多数情况下,HGT由研究组的几个代表共享,这表明它们是古老的,并且在相对较长的进化时期中得到了保存。这以及这些获得的基因所执行的功能(主要与能量代谢和代谢物跨膜运输有关)表明,HGT在这些古细菌适应寒冷和营养物质丰富的深海环境中发挥了重要作用。 。

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