Limnological Station, Institute of Plant Biology, University of Zurich, Seestr. 187, CH-8802, Kilchberg, Switzerland.
Environ Microbiol. 2010 Apr;12(4):1061-74. doi: 10.1111/j.1462-2920.2009.02151.x. Epub 2010 Jan 27.
We studied bacterial diversity and community composition in three shallow pools of a Swiss karst cave system with contrasting hydrological and hydrochemical properties. The microbial assemblages in the pools were remarkably different, and only one operational taxonomic unit of 16S rRNA genes (OTU, 97% similarity) was shared between the three of them (total OTU number in all pools: 150). Unexpectedly high microbial phylotype richness was found even in the two pools without groundwater contact and with low concentrations of organic carbon and total cell numbers (< 10(4) ml(-1)). One of these seepage water fed systems harboured 15 distinct OTUs from several deeply branching lineages of the candidate phylum OP3, whereas representatives of this group were not detected in the other two pools. A tentative phylogeographic analysis of available OP3-related sequences in the context of our data set revealed that there was generally little agreement between the habitats of origin of closely related sequence types. Two bacterial clades affiliated with the obligate methylamine utilizer Methylotenera mobilis were only found in the pool that was exposed to repeated flooding events. These bacteria formed relatively stable populations of up to 6% of total cell counts over periods of several months irrespective of inundation by groundwater. This suggests that karst water may provide a means of transport for these bacteria from terrestrial to freshwater habitats.
我们研究了瑞士喀斯特洞穴系统中三个具有不同水文和水化学性质的浅水池中的细菌多样性和群落组成。水池中的微生物群落差异显著,只有一个 16S rRNA 基因(OTU,相似度为 97%)在这三个水池中共存(所有水池中的总 OTU 数:150)。即使在没有地下水接触且有机碳和总细胞数浓度较低(<10(4) ml(-1))的两个水池中,也发现了出乎意料的高微生物分类群丰富度。其中一个渗流水供养系统拥有来自候选门 OP3 的几个深分枝谱系的 15 个独特 OTU,而该组的代表在其他两个水池中未被检测到。在我们的数据集中,对可用的 OP3 相关序列进行的试探性系统地理学分析表明,密切相关的序列类型的起源栖息地之间通常没有多少一致性。仅在暴露于反复淹没事件的水池中发现了两个与专性甲胺利用菌 Methylotenera mobilis 有关的细菌类群。这些细菌形成了相对稳定的种群,在长达数月的时间内,无论是否被地下水淹没,其总细胞计数的比例高达 6%。这表明喀斯特水可能为这些细菌从陆地到淡水生境的迁移提供了一种途径。