Shcherbakova Victoria, Yoshimura Yoshitaka, Ryzhmanova Yana, Taguchi Yukihiro, Segawa Takahiro, Oshurkova Victoria, Rivkina Elizaveta
Laboratory of Anaerobic Microorganisms, Skryabin Institute of Biochemistry and Physiology of Microorganisms, Russian Academy of Sciences, Prospect Nauki 5, Pushchino Moscow Region, 142290, Russian Federation
College of Agriculture, Tamagawa University, 6-1-1 Tamagawagakuen, Machida, Tokyo, 194-8610 Japan.
FEMS Microbiol Ecol. 2016 Oct;92(10). doi: 10.1093/femsec/fiw135. Epub 2016 Jun 15.
In the present study, we used culture-independent methods to investigate the diversity of methanogenic archaea and their distribution in five permafrost samples collected from a borehole in the Kolyma River Lowland (north-east of Russia). Total DNA was extracted from methane-containing permafrost samples of different age and amplified by PCR. The resulting DNA fragments were cloned. Phylogenetic analysis of the sequences showed the presence of archaea in all studied samples; 60%-95% of sequences belonged to the Euryarchaeota. Methanogenic archaea were novel representatives of Methanosarcinales, Methanomicrobiales, Methanobacteriales and Methanocellales orders. Bathyarchaeota (Miscellaneous Crenarchaeota Group) representatives were found among nonmethanogenic archaea in all the samples studied. The Thaumarchaeota representatives were not found in the upper sample, whereas Woesearchaeota (formerly DHVEG-6) were found in the three deepest samples. Unexpectedly, the greatest diversity of archaea was observed at a depth of 22.3 m, probably due to the availability of the labile organic carbon and/or due to the migration of the microbial cells during the freezing front towards the bottom.
在本研究中,我们使用非培养方法来研究产甲烷古菌的多样性及其在从科雷马河低地(俄罗斯东北部)一个钻孔采集的五个永久冻土样本中的分布情况。从不同年代的含甲烷永久冻土样本中提取总DNA,并通过PCR进行扩增。将得到的DNA片段进行克隆。对序列的系统发育分析表明,在所有研究样本中均存在古菌;60%-95%的序列属于广古菌门。产甲烷古菌是甲烷八叠球菌目、甲烷微菌目、甲烷杆菌目和甲烷盘菌目的新代表。在所研究的所有样本中,在非产甲烷古菌中发现了深古菌门(杂食泉古菌组)的代表。在上层样本中未发现泉古菌门的代表,而在最深的三个样本中发现了沃氏古菌门(以前称为DHVEG-6)。出乎意料的是,在22.3米深处观察到古菌的多样性最高,这可能是由于易分解有机碳源的存在和/或由于在冻结前沿微生物细胞向底部的迁移所致。