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冰岛瓦特纳冰川冰帽下的地下水中的微生物群落。

Microbial communities in the subglacial waters of the Vatnajökull ice cap, Iceland.

机构信息

MATIS, Department of Food Safety, Environment, and Genetics, Reykjavík, Iceland.

出版信息

ISME J. 2013 Feb;7(2):427-37. doi: 10.1038/ismej.2012.97. Epub 2012 Sep 13.

Abstract

Subglacial lakes beneath the Vatnajökull ice cap in Iceland host endemic communities of microorganisms adapted to cold, dark and nutrient-poor waters, but the mechanisms by which these microbes disseminate under the ice and colonize these lakes are unknown. We present new data on this subglacial microbiome generated from samples of two subglacial lakes, a subglacial flood and a lake that was formerly subglacial but now partly exposed to the atmosphere. These data include parallel 16S rRNA gene amplicon libraries constructed using novel primers that span the v3-v5 and v4-v6 hypervariable regions. Archaea were not detected in either subglacial lake, and the communities are dominated by only five bacterial taxa. Our paired libraries are highly concordant for the most abundant taxa, but estimates of diversity (abundance-based coverage estimator) in the v4-v6 libraries are 3-8 times higher than in corresponding v3-v5 libraries. The dominant taxa are closely related to cultivated anaerobes and microaerobes, and may occupy unique metabolic niches in a chemoautolithotrophic ecosystem. The populations of the major taxa in the subglacial lakes are indistinguishable (>99% sequence identity), despite separation by 6 km and an ice divide; one taxon is ubiquitous in our Vatnajökull samples. We propose that the glacial bed is connected through an aquifer in the underlying permeable basalt, and these subglacial lakes are colonized from a deeper, subterranean microbiome.

摘要

冰岛瓦特纳冰盖下的冰下湖中存在适应寒冷、黑暗和贫营养水的特有微生物群落,但这些微生物在冰下传播并在这些湖中定殖的机制尚不清楚。我们提供了来自两个冰下湖、一个冰下洪水和一个曾经是冰下但现在部分暴露于大气的湖的冰下微生物组的新数据。这些数据包括使用跨越 v3-v5 和 v4-v6 高变区的新型引物构建的平行 16S rRNA 基因扩增子文库。在两个冰下湖中均未检测到古菌,且群落主要由仅五个细菌分类群组成。我们的配对文库在最丰富的分类群上高度一致,但 v4-v6 文库中的多样性估计(基于丰度的覆盖率估计)比相应的 v3-v5 文库高 3-8 倍。优势类群与培养的厌氧菌和微需氧菌密切相关,并且可能在化能自养生态系统中占据独特的代谢生态位。尽管分离距离为 6 公里且存在冰分水岭,但冰下湖中主要类群的种群没有区别(>99%的序列同一性);一个分类群在我们的瓦特纳冰川样本中普遍存在。我们提出,冰川床通过下面可渗透玄武岩中的含水层相连,这些冰下湖是从更深的地下微生物组中定殖而来的。

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