Nunoura Takuro, Takaki Yoshihiro, Hirai Miho, Shimamura Shigeru, Makabe Akiko, Koide Osamu, Kikuchi Tohru, Miyazaki Junichi, Koba Keisuke, Yoshida Naohiro, Sunamura Michinari, Takai Ken
Research and Development Center for Marine Biosciences, Japan Agency for Marine-Earth Science & Technology, Yokosuka 237-0061, Japan;
Research and Development Center for Marine Biosciences, Japan Agency for Marine-Earth Science & Technology, Yokosuka 237-0061, Japan; Department of Subsurface Geobiological Analysis and Research and.
Proc Natl Acad Sci U S A. 2015 Mar 17;112(11):E1230-6. doi: 10.1073/pnas.1421816112. Epub 2015 Feb 23.
Hadal oceans at water depths below 6,000 m are the least-explored aquatic biosphere. The Challenger Deep, located in the western equatorial Pacific, with a water depth of ∼11 km, is the deepest ocean on Earth. Microbial communities associated with waters from the sea surface to the trench bottom (0∼10,257 m) in the Challenger Deep were analyzed, and unprecedented trench microbial communities were identified in the hadal waters (6,000∼10,257 m) that were distinct from the abyssal microbial communities. The potentially chemolithotrophic populations were less abundant in the hadal water than those in the upper abyssal waters. The emerging members of chemolithotrophic nitrifiers in the hadal water that likely adapt to the higher flux of electron donors were also different from those in the abyssal waters that adapt to the lower flux of electron donors. Species-level niche separation in most of the dominant taxa was also found between the hadal and abyssal microbial communities. Considering the geomorphology and the isolated hydrotopographical nature of the Mariana Trench, we hypothesized that the distinct hadal microbial ecosystem was driven by the endogenous recycling of organic matter in the hadal waters associated with the trench geomorphology.
深度超过6000米的超深渊海洋是探索最少的水生生物圈。位于赤道西太平洋、水深约11千米的马里亚纳海沟是地球上最深的海洋。对马里亚纳海沟从海面到海沟底部(0至10257米)水体中的微生物群落进行了分析,在超深渊水体(6000至10257米)中鉴定出了前所未有的海沟微生物群落,这些群落与深海微生物群落不同。超深渊水体中潜在的化能无机营养种群比上层深海水体中的要少。超深渊水体中可能适应较高电子供体通量的化能无机营养硝化菌新出现成员也与适应较低电子供体通量的深海水体中的不同。在超深渊和深海微生物群落之间还发现了大多数优势类群在物种水平上的生态位分离。考虑到马里亚纳海沟的地貌以及其孤立的水文地形性质,我们推测独特的超深渊微生物生态系统是由与海沟地貌相关的超深渊水体中有机物的内循环驱动的。