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Revealing the unexplored fungal communities in deep groundwater of crystalline bedrock fracture zones in Olkiluoto, Finland

机译:揭示芬兰Olkiluoto结晶基岩断裂带深层地下水中未开发的真菌群落

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摘要

The diversity and functional role of fungi, one of the ecologically most important groups of eukaryotic microorganisms, remains largely unknown in deep biosphere environments. In this study we investigated fungal communities in packer-isolated bedrock fractures in Olkiluoto, Finland at depths ranging from 296 to 798 m below surface level. DNA- and cDNA-based high-throughput amplicon sequencing analysis of the fungal internal transcribed spacer (ITS) gene markers was used to examine the total fungal diversity and to identify the active members in deep fracture zones at different depths. Results showed that fungi were present in fracture zones at all depths and fungal diversity was higher than expected. Most of the observed fungal sequences belonged to the phylum Ascomycota. Phyla Basidiomycota and Chytridiomycota were only represented as a minor part of the fungal community. Dominating fungal classes in the deep bedrock aquifers were Sordariomycetes, Eurotiomycetes, and Dothideomycetes from the Ascomycota phylum and classes Microbotryomycetes and Tremellomycetes from the Basidiomycota phylum, which are the most frequently detected fungal taxa reported also from deep sea environments. In addition some fungal sequences represented potentially novel fungal species. Active fungi were detected in most of the fracture zones, which proves that fungi are able to maintain cellular activity in these oligotrophic conditions. Possible roles of fungi and their origin in deep bedrock groundwater can only be speculated in the light of current knowledge but some species may be specifically adapted to deep subsurface environment and may play important roles in the utilization and recycling of nutrients and thus sustaining the deep subsurface microbial community.
机译:真菌是生态学上最重要的真核微生物组之一,其多样性和功能作用在深层生物圈环境中仍然未知。在这项研究中,我们调查了芬兰Olkiluoto封隔器隔离的基岩裂缝中的真菌群落,其深度为地表以下296至798 m。真菌内部转录间隔区(ITS)基因标记的基于DNA和cDNA的高通量扩增子测序分析用于检查真菌的总多样性并鉴定不同深度的深部断裂带中的活性成员。结果表明,在所有深度的断裂带都存在真菌,真菌的多样性高于预期。观察到的大多数真菌序列都属于子囊门。 Phyla Basidiomycota和Chytridiomycota仅代表了真菌群落的一小部分。深基岩含水层中主要的真菌种类是来自子囊门的Sordariomycetes,Eurotiomycetes和Dothideomycetes,以及来自Basidiomycota phylum的Microbotryomycetes和Tremellomycetes类,也是在深海环境中最常发现的真菌类群。另外,一些真菌序列代表潜在的新颖真菌物种。在大多数骨折区域检测到活性真菌,这证明真菌能够在这些贫营养条件下维持细胞活性。真菌的作用及其在深基岩地下水中的起源只能根据现有知识推测,但某些物种可能专门适应深地下环境,并可能在养分的利用和循环利用中发挥重要作用,从而维持深地下微生物群落。

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