Department of Molecular Genetics, Forsyth Institute, Cambridge, MA, USA.
Geobiology. 2012 May;10(3):223-35. doi: 10.1111/j.1472-4669.2012.00317.x. Epub 2012 Feb 13.
Mahoney Lake, British Columbia, Canada, is a stratified, 15-m deep saline lake with a euxinic (anoxic, sulfidic) hypolimnion. A dense plate of phototrophic purple sulfur bacteria is found at the chemocline, but to date the rest of the Mahoney Lake microbial ecosystem has been underexamined. In particular, the microbial community that resides in the aphotic hypolimnion and/or in the lake sediments is unknown, and it is unclear whether the sulfate reducers that supply sulfide for phototrophy live only within, or also below, the plate. Here we profiled distributions of 16S rRNA genes using gene clone libraries and PhyloChip microarrays. Both approaches suggest that microbial diversity is greatest in the hypolimnion (8 m) and sediments. Diversity is lowest in the photosynthetic plate (7 m). Shallower depths (5 m, 7 m) are rich in Actinobacteria, Alphaproteobacteria, and Gammaproteobacteria, while deeper depths (8 m, sediments) are rich in Crenarchaeota, Natronoanaerobium, and Verrucomicrobia. The heterogeneous distribution of Deltaproteobacteria and Epsilonproteobacteria between 7 and 8 m is consistent with metabolisms involving sulfur intermediates in the chemocline, but complete sulfate reduction in the hypolimnion. Overall, the results are consistent with the presence of distinct microbial niches and suggest zonation of sulfur cycle processes in this stratified system.
加拿大不列颠哥伦比亚省的马霍尼湖是一个分层的、深 15 米的盐湖,具有贫氧(缺氧、硫化)的深层水。在化变层发现了一层密集的光养型紫色硫细菌,但迄今为止,马霍尼湖微生物生态系统的其余部分仍未得到充分研究。特别是,居住在无光的深层水和/或湖底沉积物中的微生物群落尚不清楚,也不清楚为光养作用提供硫化物的硫酸盐还原菌是否仅存在于板块内,还是也存在于板块下。在这里,我们使用基因克隆文库和 PhyloChip 微阵列对 16S rRNA 基因的分布进行了分析。这两种方法都表明,微生物多样性在深层水(8 米)和沉积物中最大。在光合板块(7 米)中多样性最低。较浅的深度(5 米,7 米)富含放线菌、α变形菌和γ变形菌,而较深的深度(8 米,沉积物)富含泉古菌、嗜盐厌氧菌和疣微菌。7 米和 8 米之间 δ变形菌和 ε变形菌的不均匀分布与化变层中涉及硫中间体的代谢物一致,但在深层水完全进行硫酸盐还原。总的来说,这些结果与存在不同的微生物小生境一致,并表明在这个分层系统中硫循环过程的分区化。