Sun Jiarui, Hirai Miho, Takaki Yoshihiro, Evans Paul N, Nunoura Takuro, Rinke Christian
School of the Environment, The University of Queensland, St. Lucia, QLD, Australia.
Institute for Extra-cutting-edge Science and Technology Avant-garde Research (X-star), Japan Agency for Marine-Earth Science & Technology (JAMSTEC), Yokosuka, Kanagawa, Japan.
Microb Genom. 2025 Mar;11(3). doi: 10.1099/mgen.0.001351.
Marine sediments are vast, underexplored habitats and represent one of the largest carbon deposits on our planet. Microbial communities drive nutrient cycling in these sediments, but the full extent of their taxonomic and metabolic diversity remains to be explored. Here, we analysed shallow coastal and deep subseafloor sediment cores from 0.01 to nearly 600 metres below the seafloor, in the Western Pacific Region. Applying metagenomics, we identified several taxonomic clusters across all samples, which mainly aligned with depth and sediment type. Inferring functional patterns provided insights into possible ecological roles of the main microbial taxa. These included , the most abundant phylum across all samples, whereby the classes and dominated deep-subsurface and most shallow coastal sediments, respectively. and were the most abundant phyla among Archaea, contributing to high relative abundances of Archaea reaching over 50% in some samples. We recovered high-quality metagenome-assembled genomes for all main prokaryotic lineages and proposed names for three phyla, i.e. phyl. nov. (former RBG-13-66-14), phyl. nov. (former UBA6262) and phyl. nov. (former UBA8248). Metabolic capabilities across all samples ranged from aerobic respiration and photosynthesis in the shallowest sediment layers to heterotrophic carbon utilization, sulphate reduction and methanogenesis in deeper anoxic sediments. We also identified taxa with the potential to be involved in nitrogen and sulphur cycling and heterotrophic carbon utilization. In summary, this study contributes to our understanding of the taxonomic and functional diversity in benthic prokaryotic communities across marine sediments in the Western Pacific Region.
海洋沉积物是广阔且未被充分探索的栖息地,是地球上最大的碳沉积地之一。微生物群落驱动着这些沉积物中的养分循环,但其分类和代谢多样性的全貌仍有待探索。在这里,我们分析了西太平洋地区从海底以下0.01米到近600米的浅海沿岸和深海海底沉积物岩芯。应用宏基因组学,我们在所有样本中识别出几个分类群,它们主要与深度和沉积物类型相关。推断功能模式为主要微生物类群可能的生态作用提供了见解。其中包括所有样本中最丰富的门类,其 纲和 纲分别在深部次表层和大部分浅海沿岸沉积物中占主导地位。 和 是古菌中最丰富的门类,在一些样本中使得古菌的相对丰度高达50%以上。我们为所有主要原核生物谱系获得了高质量的宏基因组组装基因组,并为三个门类提出了名称,即 新门类(前RBG - 13 - 66 - 14)、 新门类(前UBA6262)和 新门类(前UBA8248)。所有样本的代谢能力范围从最浅沉积层中的有氧呼吸和光合作用到较深缺氧沉积物中的异养碳利用、硫酸盐还原和甲烷生成。我们还识别出了有可能参与氮和硫循环以及异养碳利用的类群。总之,这项研究有助于我们了解西太平洋地区海洋沉积物中底栖原核生物群落的分类和功能多样性。