Tang Yuan, Cheng Jian-Zhong, Lian Bin
State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, PR China.
Jiangsu Key Laboratory for Microbes and Functional Genomics, Jiangsu Engineering and Technology Research Center for Microbiology, College of Life Science, Nanjing Normal University, Nanjing, PR China.
Pol J Microbiol. 2017 Jan 2;65(4):413-423. doi: 10.5604/17331331.1227667.
The endolithic environment is a ubiquitous habitat for microorganisms and a critical interface between biology and geology. In this study, a culture-based method and the phylogenetic analysis based on 16S rRNA and internal transcribed spacer (ITS) sequences were used to investigate the diversity of endolithic bacteria and fungi in two main types of carbonate rocks (namely dolomite and limestone) from Nanjiang Canyon in Guizhou karst area, China. The results of bacterial diversity indicated that all bacteria isolated from dolomite and limestone rocks were divided into 4 bacterial groups, including Proteobacteria, Actinobacteria, Firmicutes and Bacteroidetes. For these two kinds of rocks, Proteobacteria was the first dominant group, and Gammaproteobacteria occupied the greatest proportion which might be closely related to Pseudomonas in phylogeny to be the most dominant genera after isolation. Actinobacteria and Bacillus bacteria were also widespread in these two kinds of rock environments. There were only 9 and 8 strains of fungi isolated from dolomite and limestone respectively, which all belonged to Ascomycota. To the best of our knowledge, this is the first report on diversity of endolithic culturable bacteria and fungi in carbonate rocks in Guizhou karst region. These microorganisms may play an important and unprecedented role in the carbonate rock weathering during the long history of geological evolution.
石内环境是微生物普遍存在的栖息地,也是生物学与地质学之间的关键界面。在本研究中,采用基于培养的方法以及基于16S rRNA和内部转录间隔区(ITS)序列的系统发育分析,对中国贵州喀斯特地区南江峡谷两种主要类型碳酸盐岩(即白云岩和石灰岩)中的石内细菌和真菌多样性进行了研究。细菌多样性结果表明,从白云岩和石灰岩中分离出的所有细菌被分为4个细菌类群,包括变形菌门、放线菌门、厚壁菌门和拟杆菌门。对于这两种岩石,变形菌门是第一优势类群,其中γ-变形菌纲占比最大,在系统发育上可能与假单胞菌密切相关,是分离后最主要的属。放线菌和芽孢杆菌在这两种岩石环境中也广泛存在。从白云岩和石灰岩中分别仅分离出9株和8株真菌,它们均属于子囊菌门。据我们所知,这是关于贵州喀斯特地区碳酸盐岩石内可培养细菌和真菌多样性的首次报道。在漫长的地质演化历史中,这些微生物可能在碳酸盐岩风化过程中发挥重要且前所未有的作用。