Anda Dóra, Makk Judit, Krett Gergely, Jurecska Laura, Márialigeti Károly, Mádl-Szőnyi Judit, Borsodi Andrea K
Department of Microbiology, Eötvös Loránd University, Pázmány P. sétány 1/C, Budapest, 1117, Hungary.
Extremophiles. 2015 Jul;19(4):787-97. doi: 10.1007/s00792-015-0754-1. Epub 2015 May 8.
In this study, scanning electron microscopy (SEM) and 16S rRNA gene-based phylogenetic approach were applied to reveal the morphological structure and genetic diversity of thermophilic prokaryotic communities of a thermal karst well located in Budapest (Hungary). Bacterial and archaeal diversity of the well water (73.7 °C) and the biofilm developed on the inner surface of an outflow pipeline of the well were studied by molecular cloning method. According to the SEM images calcium carbonate minerals serve as a surface for colonization of bacterial aggregates. The vast majority of the bacterial and archaeal clones showed the highest sequence similarities to chemolithoautotrophic species. The bacterial clone libraries were dominated by sulfur oxidizer Thiobacillus (Betaproteobacteria) in the water and Sulfurihydrogenibium (Aquificae) in the biofilm. A relatively high proportion of molecular clones represented genera Thermus and Bellilinea in the biofilm library. The most abundant phylotypes both in water and biofilm archaeal clone libraries were closely related to thermophilic ammonia oxidizer Nitrosocaldus and Nitrososphaera but phylotypes belonging to methanogens were also detected. The results show that in addition to the bacterial sulfur and hydrogen oxidation, mainly archaeal ammonia oxidation may play a decisive role in the studied thermal karst system.
在本研究中,应用扫描电子显微镜(SEM)和基于16S rRNA基因的系统发育方法,揭示位于布达佩斯(匈牙利)的一个热喀斯特泉中嗜热原核生物群落的形态结构和遗传多样性。通过分子克隆方法研究了井水(73.7°C)以及泉流出管道内表面形成的生物膜中的细菌和古菌多样性。根据SEM图像,碳酸钙矿物是细菌聚集体定殖的表面。绝大多数细菌和古菌克隆与化能自养型物种具有最高的序列相似性。细菌克隆文库中,水中以硫氧化菌硫杆菌属(β-变形菌纲)为主,生物膜中以嗜氢硫杆菌属(产水菌门)为主。生物膜文库中相对较高比例的分子克隆代表嗜热栖热菌属和细螺旋菌属。水和生物膜古菌克隆文库中最丰富的系统发育型与嗜热氨氧化菌亚硝化暖球菌属和亚硝化球形菌属密切相关,但也检测到属于产甲烷菌的系统发育型。结果表明,除了细菌的硫和氢氧化作用外,主要是古菌的氨氧化作用可能在研究的热喀斯特系统中起决定性作用。