Québec-Océan and Département de Biologie, Université Laval, Québec, QC, Canada.
Sci Rep. 2012;2:604. doi: 10.1038/srep00604. Epub 2012 Aug 28.
Meromictic lakes are useful biogeochemical models because of their stratified chemical gradients and separation of redox reactions down the water column. Perennially ice-covered meromictic lakes are particularly stable, with long term constancy in their density profiles. Here we sampled Lake A, a deep meromictic lake at latitude 83°N in High Arctic Canada. Sampling was before (May) and after (August) an unusual ice-out event during the warm 2008 summer. We determined the bacterial and archaeal community composition by high-throughput 16S rRNA gene tag-pyrosequencing. Both prokaryote communities were stratified by depth and the Bacteria differed between dates, indicating locally driven selection processes. We matched taxa to known taxon-specific biogeochemical functions and found a close correspondence between the depth of functional specialists and chemical gradients. These results indicate a rich microbial diversity despite the extreme location, with pronounced vertical structure in taxonomic and potential functional composition, and with community shifts during ice-out.
分层化学梯度和水柱中氧化还原反应的分离使得分层湖成为有用的生物地球化学模型。常年被冰覆盖的分层湖特别稳定,其密度剖面长期保持稳定。本研究在 2008 年温暖夏季异常融冰事件前后(5 月和 8 月)对加拿大高纬度北极地区 83°N 的深层分层湖 A 进行了采样。我们通过高通量 16S rRNA 基因标签焦磷酸测序确定了细菌和古菌群落的组成。两个原核生物群落都随深度分层,并且细菌在不同日期有所不同,表明存在局部驱动的选择过程。我们将分类群与已知的分类群特异性生物地球化学功能相匹配,发现功能专家的深度与化学梯度之间存在密切对应关系。这些结果表明,尽管地理位置极端,但仍存在丰富的微生物多样性,在分类和潜在功能组成方面具有明显的垂直结构,并在融冰期间发生群落变化。