| Literature DB >> 25713387 |
Takuro Nunoura1, Yoshihiro Takaki2, Miho Hirai3, Shigeru Shimamura4, Akiko Makabe5, Osamu Koide3, Tohru Kikuchi6, Junichi Miyazaki4, Keisuke Koba7, Naohiro Yoshida8, Michinari Sunamura9, Ken Takai4.
Abstract
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.Entities:
Keywords: Challenger Deep; hadal; niche separation; nitrification; trench
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Year: 2015 PMID: 25713387 PMCID: PMC4371994 DOI: 10.1073/pnas.1421816112
Source DB: PubMed Journal: Proc Natl Acad Sci U S A ISSN: 0027-8424 Impact factor: 11.205