Key Laboratory of Agrometeorology of Jiangsu Province, Department of Ecology, School of Applied Meteorology, Nanjing University of Information Science & Technology, Nanjing 210044, PR China.
Key Laboratory of Agrometeorology of Jiangsu Province, Department of Ecology, School of Applied Meteorology, Nanjing University of Information Science & Technology, Nanjing 210044, PR China.
Sci Total Environ. 2021 Sep 1;785:147357. doi: 10.1016/j.scitotenv.2021.147357. Epub 2021 Apr 26.
Mosses and lichens have been shown to play an important role in enhancing global chemical weathering of the surface rock. However, there are no studies concerning the effects of mosses and lichens on the microbial communities inhabiting rock surfaces. In this study, culture-dependent and culture-independent analyses were employed to compare the diversity, composition, and rock-weathering activity of bacterial communities inhabiting potash trachyte surfaces covered by mosses (MR) and lichens (LR) with those inhabiting surrounding bare rock surfaces (BR). Analyses of 16S rRNA gene Miseq sequencing revealed that the order of alpha (α) diversity indices, in terms of the number of unique operational taxonomic units (OTUs) and Faith's index of phylogenetic diversity, was MR > LR > BR. Moreover, α-diveristy indices were positively correlated with the content of available phosphorus (AP) in rock samples (r = 0.87-0.92), and this explained 70% of the variation in bacterial community structure. The culture-dependent analyses revealed that 100% of the culturable bacterial strains could enhance potash trachyte weathering, and the order of rock-weathering acitivity of bacterial strains was MR > LR > BR. Acidolysis was found to be the major mechanism involved in the bacteria-mediated weathering of potash trachyte. Moreover, bacterial strians related to the genera Dyella and Ralstonia showed the highest rock-weatheirng activity, and both Dyella and Ralstonia were enriched in MR. The results of this study enhance our understanding of the roles of bacteria facilitated by mosses and lichens in rock weathering, element cycling, and soil formation, and provide new insights into the interaction between non-vascular plants and the bacteria on rock surfaces.
苔藓和地衣已被证明在增强地表岩石的全球化学风化方面发挥着重要作用。然而,目前还没有研究关注苔藓和地衣对栖息在岩石表面的微生物群落的影响。在这项研究中,采用了依赖培养和非依赖培养的分析方法,比较了覆盖有苔藓(MR)和地衣(LR)的钾质粗面岩表面以及周围裸露岩石表面(BR)栖息的细菌群落的多样性、组成和岩石风化活性。16S rRNA 基因 Miseq 测序分析表明,根据独特操作分类单元(OTUs)数量和系统发育多样性 Faith 指数的 α 多样性指数的顺序为 MR>LR>BR。此外,α多样性指数与岩石样品中有效磷(AP)含量呈正相关(r=0.87-0.92),这解释了 70%的细菌群落结构变化。依赖培养的分析表明,100%的可培养细菌菌株能够促进钾质粗面岩风化,并且细菌菌株的岩石风化活性顺序为 MR>LR>BR。发现酸解是细菌介导钾质粗面岩风化的主要机制。此外,与 Dyella 和 Ralstonia 属相关的细菌菌株表现出最高的岩石风化活性,并且 Dyella 和 Ralstonia 都在 MR 中富集。本研究的结果增强了我们对苔藓和地衣促进的细菌在岩石风化、元素循环和土壤形成中的作用的理解,并为非维管束植物与岩石表面细菌之间的相互作用提供了新的见解。