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Sources and selection of snow-specific microbial communities in a Greenlandic sea ice snow cover

机译:格陵兰岛海冰积雪中特定于雪的微生物群落的来源和选择

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摘要

Sea ice and its snow cover are critical for global processes including climate regulation and biogeochemical cycles. Despite an increase in studies focused on snow microorganisms, the ecology of snow inhabitants remains unclear. In this study, we investigated sources and selection of a snowpack-specific microbial community by comparing metagenomes from samples collected in a Greenlandic fjord within a vertical profile including atmosphere, snowpack with four distinct layers of snow, sea ice brine and seawater. Microbial communities in all snow layers derived from mixed sources, both marine and terrestrial, and were more similar to atmospheric communities than to sea ice or seawater communities. The surface snow metagenomes were characterized by the occurrence of genes involved in photochemical stress resistance, primary production and metabolism of diverse carbon sources. The basal saline snow layer that was in direct contact with the sea ice surface harbored a higher abundance of cells than the overlying snow layers, with a predominance of Alteromonadales and a higher relative abundance of marine representatives. However, the overall taxonomic structure of the saline layer was more similar to that of other snow layers and the atmosphere than to underlying sea ice and seawater. The expulsion of relatively nutrient-rich sea ice brine into basal snow might have stimulated the growth of copiotrophic psychro- and halotolerant snow members. Our study indicates that the size, composition and function of snowpack microbial communities over sea ice were influenced primarily by atmospheric deposition and inflow of sea ice brine and that they form a snow-specific assemblage reflecting the particular environmental conditions of the snowpack habitat.
机译:海冰及其积雪对于包括气候调节和生物地球化学循环在内的全球过程至关重要。尽管针对雪微生物的研究有所增加,但雪居民的生态仍然不清楚。在这项研究中,我们通过比较格陵兰峡湾中垂直分布的样本中的元基因组,调查了特定于积雪的微生物群落的来源和选择,该垂直剖面包括大气,积雪有四个不同层的积雪,海冰盐水和海水。所有积雪层中的微生物群落均来自海洋和陆地的混合来源,与大气群落相比,与海冰或海水群落更相似。表面雪元基因组的特征是存在与光化学胁迫抗性,初级生产和各种碳源代谢有关的基因。与海冰表面直接接触的基础盐雪层比上覆的雪层具有更高的细胞丰度,其中以Alteromonadales占优势,而海洋代表的相对丰度更高。但是,盐层的总体分类结构与其他雪层和大气的分类结构相比,与其下面的海冰和海水更相似。将相对营养丰富的海冰盐水排入基础雪中可能刺激了嗜营养性精神和卤代雪成员的生长。我们的研究表明,海冰上积雪微生物群落的大小,组成和功能主要受大气沉积和海冰盐水流入的影响,它们形成了特定于雪的集合,反映了积雪栖息地的特定环境条件。

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