Department of Biology, Biotechnical Faculty, University of Ljubljana, Večna pot 111, 1000, Ljubljana, Slovenia.
Microb Ecol. 2013 Jul;66(1):5-18. doi: 10.1007/s00248-012-0172-1. Epub 2013 Jan 13.
The Vjetrenica cave in the Dinaric Karst hosts a worldwide extraordinarily high cave biodiversity. Beside a diverse and specialized cave fauna, sprout-like formations attached to the bed of the cave stream were observed and described, but not further characterized, almost a century ago. Here we investigated these sprout-like microbial aggregates by the rRNA approach and detailed microscopy. Based on fluorescence in situ hybridization and ultrastructural analysis, the sprout-like formations are morphologically highly organized, and their core consists of a member of a novel deep-branching lineage in the bacterial phylum Nitrospirae. This organism displays an interesting cellular ultrastructure with different kinds of cytoplasmic inclusions and is embedded in a thick extracellular matrix, which contributes to the stability and shape of the aggregates. This novel bacterium has been provisionally classified as "Candidatus Troglogloea absoloni." The surface of the sprout-like aggregates is more diverse than the core. It is colonized by a bacterial biofilm consisting primarily of filamentous Betaproteobacteria, whereas other microbial populations present in the crust include members of the Bacteriodetes, Gammaproteobacteria, Actinombacteria, Alphaproteobacteria, and Planctomycetes, which are intermingled with mineral inclusions. This study represents the first thorough molecular and ultrastructural characterization of the elusive sprout-like bacterial aggregates, which are also found in other cave systems of the Dinaric Karst. The discovery of Ca. Troglogloea absoloni contributes to the known biodiversity of subterranean ecosystems and especially of macroscopic structures formed in caves by microorganisms, whose composition and ecological function often remain enigmatic.
维特伦尼察洞穴(Vjetrenica cave)位于迪纳里克喀斯特(Dinaric Karst),拥有世界范围内极高水平的洞穴生物多样性。除了多样化和专业化的洞穴动物群外,近一个世纪前,人们还观察到并描述了附着在洞穴溪流底部的芽状结构,但没有进一步进行特征描述。在这里,我们通过 rRNA 方法和详细的显微镜研究了这些芽状微生物聚集体。基于荧光原位杂交和超微结构分析,芽状结构在形态上高度组织化,其核心由细菌门硝化螺旋菌(Nitrospirae)的一个深分支谱系的成员组成。这种生物体具有有趣的细胞超微结构,包含不同类型的细胞质内含物,并嵌入在厚厚的细胞外基质中,这有助于聚集体的稳定性和形状。这种新发现的细菌被暂时分类为“绝对穴居菌(Ca. Troglogloea absoloni)”。芽状聚集体的表面比核心更为多样化。它被主要由丝状贝塔变形菌(Betaproteobacteria)组成的细菌生物膜所定植,而在外壳中存在的其他微生物种群包括拟杆菌门(Bacteriodetes)、γ变形菌门(Gammaproteobacteria)、放线菌门(Actinombacteria)、α变形菌门(Alphaproteobacteria)和浮霉菌门(Planctomycetes)的成员,它们与矿物内含物交织在一起。这项研究首次对难以捉摸的芽状细菌聚集体进行了全面的分子和超微结构特征描述,这些聚集体也存在于迪纳里克喀斯特的其他洞穴系统中。绝对穴居菌(Ca. Troglogloea absoloni)的发现丰富了地下生态系统的已知生物多样性,尤其是由微生物形成的宏观洞穴结构的生物多样性,这些结构的组成和生态功能往往仍然神秘莫测。