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Phylogenetic Characterization of Marine Benthic Archaea in Organic-Poor Sediments of the Eastern Equatorial Pacific Ocean (ODP Site 1225)

机译:赤道东太平洋有机贫困沉积物中海洋底栖古生菌的系统发育特征(ODP站点1225)

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摘要

Sequencing surveys of microbial communities in marine subsurface sediments have focused on organic-rich, continental margins; the database for organic-lean deep-sea sediments from mid-ocean regions is underdeveloped. The archaeal community in subsurface sediments of ODP Site 1225 in the eastern equatorial Pacific (3760 m water depth; 1.1 and 7.8 m sediment depth) was analyzed by PCR, cloning and sequencing, and by denaturant gradient gel electrophoresis (DGGE) of 16S rRNA genes. Three uncultured archaeal lineages with different depth distributions were found: Marine Group I (MG-I) within the Thaumarchaeota, its sister lineage Marine Benthic Group A (MBG-A), the phylum-level archaeal lineage Marine Benthic Group B (also known as Deep-Sea Archaeal Group or Lokiarchaeota), and the Deep-Sea Euryarchaeotal Group 3. The MG-I phylotypes included representatives of sediment clusters that are distinct from the pelagic members of this phylum. On the scale from fully oxidized, extremely organic carbon-depleted sediments (for example, those the South Pacific Gyre) to fully reduced, organic carbon-rich marine subsurface sediments (such as those of the Peru Margin), Ocean Drilling Program (ODP) Site 1225 falls into the non-extreme organic carbon-lean category, and harbors archaeal communities from both ends of the spectrum.
机译:海洋次表层沉积物中微生物群落的测序调查侧重于富含有机物的大陆边缘。来自海洋中部地区的富含有机物的深海沉积物数据库尚不完善。通过PCR,克隆和测序以及16S rRNA基因的变性梯度凝胶电泳(DGGE)分析了赤道东太平洋ODP站点1225(水深3760 m;沉积深度1.1和7.8 m)的地下沉积物中的古细菌群落。 。发现了三个具有不同深度分布的未养殖古细菌世系:Thaumarchaeota内的海洋I类(MG-I),其姊妹世系海洋底栖生物A组(MBG-A),门级古细菌世系海洋底栖生物B组(也称为深海古生物群或Lokiarchaeota群,以及深海古生物群3。MG-I系统型包括与该系统中上层成员不同的沉积物簇代表。从完全氧化的,极度有机耗碳的沉积物(例如,南太平洋环流)到完全还原的,富含有机碳的海洋地下沉积物(例如,秘鲁页岩的沉积物),海洋钻探计划(ODP)站点1225属于非极端有机贫碳类别,并且在频谱的两端都包含古细菌群落。

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