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Fungal and Prokaryotic Activities in the Marine Subsurface Biosphere at Peru Margin and Canterbury Basin Inferred from RNA-Based Analyses and Microscopy

机译:基于RNA的分析和显微术推断秘鲁边界和坎特伯雷盆地海洋地下生物圈中的真菌和原核生物活动。

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摘要

The deep sedimentary biosphere, extending 100s of meters below the seafloor harbors unexpected diversity of Bacteria, Archaea, and microbial eukaryotes. Far less is known about microbial eukaryotes in subsurface habitats, albeit several studies have indicated that fungi dominate microbial eukaryotic communities and fungal molecular signatures (of both yeasts and filamentous forms) have been detected in samples as deep as 1740 mbsf. Here, we compare and contrast fungal ribosomal RNA gene signatures and whole community metatranscriptomes present in sediment core samples from 6 and 95 mbsf from Peru Margin site 1229A and from samples from 12 and 345 mbsf from Canterbury Basin site U1352. The metatranscriptome analyses reveal higher relative expression of amino acid and peptide transporters in the less nutrient rich Canterbury Basin sediments compared to the nutrient rich Peru Margin, and higher expression of motility genes in the Peru Margin samples. Higher expression of genes associated with metals transporters and antibiotic resistance and production was detected in Canterbury Basin sediments. A poly-A focused metatranscriptome produced for the Canterbury Basin sample from 345 mbsf provides further evidence for active fungal communities in the subsurface in the form of fungal-associated transcripts for metabolic and cellular processes, cell and membrane functions, and catalytic activities. Fungal communities at comparable depths at the two geographically separated locations appear dominated by distinct taxa. Differences in taxonomic composition and expression of genes associated with particular metabolic activities may be a function of sediment organic content as well as oceanic province. Microscopic analysis of Canterbury Basin sediment samples from 4 and 403 mbsf produced visualizations of septate fungal filaments, branching fungi, conidiogenesis, and spores. These images provide another important line of evidence supporting the occurrence and activity of fungi in the deep subseafloor biosphere.
机译:深海沉积生物圈在海底下延伸了数百米,它具有细菌,古细菌和微生物真核生物的出乎意料的多样性。尽管对地下真核生物的微生物真核生物知之甚少,尽管有几项研究表明,真菌在微生物真核生物中占主导地位,并且在高达1740 mbsf的样品中检测到了真菌分子特征(包括酵母和丝状形式)。在这里,我们比较并对比了秘鲁Margin站点1229A的6和95 mbsf的沉积物核心样品以及坎特伯雷盆地站点U1352的12和345 mbsf的沉积物核心样品中存在的真菌核糖体RNA基因特征和整个群落的转录组。元转录组分析显示,与营养丰富的秘鲁边缘地区相比,营养丰富的坎特伯雷盆地沉积物中氨基酸和肽转运蛋白的相对表达更高,而秘鲁边缘样本中的活力基因表达更高。在坎特伯雷盆地沉积物中检测到与金属转运蛋白,抗生素抗性和生产相关的基因的更高表达。为345 mbsf的坎特伯雷盆地样品生产的poly-A聚焦元转录组,以真菌相关转录本的形式,为代谢和细胞过程,细胞和膜功能以及催化活性提供了地下活性真菌群落的进一步证据。在两个地理上分开的位置处,深度相当的真菌群落似乎以不同的分类单元为主。分类学组成和与特定代谢活动有关的基因表达上的差异可能是沉积物有机物含量以及海洋省份的函数。对4和403 mbsf的坎特伯雷盆地沉积物样品进行的显微镜分析显示了分离的真菌细丝,分支真菌,分生孢子和孢子的图像。这些图像提供了另一重要证据,证明了深海海底生物圈中真菌的发生和活动。

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