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Fungi in perennial ice from Scărișoara Ice Cave (Romania)

机译:Scărișoara Ice Cave(罗马尼亚)多年生冰中的真菌

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摘要

Screening of 1,000-years old ice layers from the perennial ice block of Scărișoara Ice Cave (NW Romania) revealed the presence of fungal communities. Using culture-dependent methods and molecular techniques based on DGGE fingerprinting of 18S rRNA gene fragments and sequencing, we identified 50 cultured and 14 uncultured fungi in presently-forming, 400 and 900 years old ice layers, corresponding to 28 distinct operational taxonomic units (OTUs). The dominant ice-contained fungal OTUs were related to Ascomycota, Basidiomycota and Cryptomycota phyla. Representatives of Mucoromycota and Chytridiomycota were also isolated from recent and 400 years old ice samples. The cryophilic Mrakia stokesii was the most abundant fungal species found in the cave ice samples of all prospected ages, alongside other cryophilic fungi also identified in various glacial environments. Ice deposits formed during the Little Ice Age (dated between AD 1,250 and 1,850) appeared to have a higher fungal diversity than the ice layer formed during the Medieval Warm Period (prior to AD 1,250). A more complex fungal community adapted to low temperatures was obtained from all analyzed ice layers when cultivated at 4 °C as compared to 15 °C, suggesting the dominance of cold-adapted fungi in this glacial habitat. The fungal distribution in the analyzed cave ice layers revealed the presence of unique OTUs in different aged-formed ice deposits, as a first hint for putative further identification of fungal biomarkers for climate variations in this icy habitat. This is the first report on fungi from a rock-hosted cave ice block.
机译:从Scărișoara冰洞(罗马尼亚西北部)多年生冰块中筛选出1000年历史的冰层,发现存在真菌群落。使用基于文化的方法和基于18S rRNA基因片段的DGGE指纹图谱的分子技术和测序,我们鉴定了目前形成的400和900年历史的冰层中的50种培养真菌和14种未培养真菌,分别对应于28个不同的操作分类单位(OTU) )。占优势的含冰真菌OTU与子囊菌,担子菌和隐孢子虫门有关。还从最近和400年历史的冰样品中分离出了毛霉菌和梭菌的代表。嗜冷性Mrakia stokesii是在所有潜在年龄的洞穴冰样中发现的最丰富的真菌物种,以及在各种冰川环境中也鉴定出的其他嗜冷性真菌。在小冰期(公元1,250至1,850之间)形成的冰层似乎具有比中世纪温暖时期(公元1,250之前)形成的冰层更高的真菌多样性。当在4 C与15 C相比时,从所有分析的冰层中获得了一个更适应低温的真菌群落,这表明在这种冰川生境中冷适应真菌的优势。被分析的洞穴冰层中的真菌分布揭示了在不同年龄形成的冰层中存在独特的OTU,这为进一步确定该冰冷栖息地气候变化的真菌生物标志物提供了第一个提示。这是关于岩石洞穴冰块中真菌的首次报道。

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