首页> 外文期刊>Microbial Ecology: An International Journal >Abundance and Co-Distribution of Widespread Marine Archaeal Lineages in Surface Sediments of Freshwater Water Bodies across the Iberian Peninsula
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Abundance and Co-Distribution of Widespread Marine Archaeal Lineages in Surface Sediments of Freshwater Water Bodies across the Iberian Peninsula

机译:伊比利亚半岛淡水水体表面沉积物中广泛海洋古谱的丰富与共同分配

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Archaea inhabiting marine and freshwater sediments have a relevant role in organic carbon mineralization, affecting carbon fluxes at a global scale. Despite current evidences suggesting that freshwater sediments largely contribute to this process, few large-scale surveys have been addressed to uncover archaeal diversity and abundance in freshwater sedimentary habitats. In this work, we quantified and high-throughput sequenced the archaeal 16S rRNA gene from surficial sediments collected in 21 inland waterbodies across the Iberian Peninsula differing in typology and trophic status. Whereas methanogenic groups were dominant in most of the studied systems, especially in organic-rich sediments, archaea affiliated to widespread marine lineages (the Bathyarchaeota and the Thermoplasmata) were also ubiquitous and particularly abundant in euxinic sediments. In these systems, Bathyarchaeota communities were dominated by subgroups Bathyarchaeota-6 (87.95 +/- 12.71%) and Bathyarchaeota-15 (8.17 +/- 9.2%) whereas communities of Thermoplasmata were mainly composed of members of the order Thermoplasmatales. Our results also indicate that Archaea accounted for a minor fraction of sedimentary prokaryotes despite remarkable exceptions in reservoirs and some stratified lakes. Copy numbers of archaeal and bathyarchaeotal 16S rRNA genes were significantly different when compared according to system type (i.e., lakes, ponds, and reservoirs), but no differences were obtained when compared according to their trophic status (from oligotrophy to eutrophy). Interestingly, we obtained significant correlations between the abundance of reads (Spearman r = 0.5, p = 0.021) and OTU richness (Spearman r = 0.677, p 0.001) of Bathyarchaeota and Thermoplasmata across systems, reinforcing the hypothesis of a potential syntrophic interaction between members of both lineages.
机译:古老的海洋和淡水沉积物在有机碳矿化中具有相关的作用,影响全球范围的碳通量。尽管目前的证据表明,淡水沉积物在很大程度上为这一过程做出了贡献,但已经解决了很少的大规模调查,以发现淡水沉积栖息地的古代多样性和丰富。在这项工作中,我们量化和高通量测序来自在伊比利亚半岛的21个内陆水上的曲面沉积物中测序古代16S rRNA基因,这是不同类型的类型学和营养状况的不同。虽然甲烷基团在大多数研究的系统中占主导地位,特别是在有机富含有机沉积物中,亚古亚的沉积物(碱性archeAtaota和热固体)在杂质沉积物中也普遍且特别丰富。在这些系统中,碱性archaeoTa群落由亚组碱基酸群-6(87.95 +/- 12.71%)和碱性archaeoTa-15(8.17 +/- 9.2%),而热压粒管的社区主要由秩序热正丙基成员组成。我们的结果还表明,尽管水库和一些分层的湖泊有着显着异常,但古老的沉积原核性占沉积原核性的一小部分。根据系统类型(即湖泊,池塘和储层)相比,拟临时和浴性archyArchaeotal 16s rRNA基因的拷贝数目显着不同,但根据其营养状况(从of OligoTrophy对Eutrophy)相比,没有获得差异。有趣的是,我们在综合读取(Spearman r = 0.5,p = 0.021)和Otu Richness(Spearman r = 0.677,P <0.001)之间的浴性archaeota和Thermoplasmata之间的显着相关性,加强了潜在的同步相互作用的假设两个谱系的成员之间。

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