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  • 井原 廣一
    日本航空宇宙学会誌
    1987年 35 巻 407 号 561-568
    発行日: 1987/12/05
    公開日: 2010/12/16
    ジャーナル フリー
  • 地球生物圏のフロンテイア
    長沼 毅
    地学雑誌
    2003年 112 巻 2 号 226-233
    発行日: 2003/04/25
    公開日: 2009/11/12
    ジャーナル フリー
    The search for life on the edges (frontiers) of the global biosphere bridges earth-bound biology and exobiology. This communication reviews recent microbiological studies on selected “frontiers”, i.e., deep-sea, deep subsurface, and Antarctica. Deep-sea is characterized as the aphotic (non-photosynthetic) habitat, and the primary production is mostly due to the chemosynthetic autotrophy at the hydrothermal vents and methane-rich seeps. Formation of the chemosynthesis-dependent animal communities in the deep leads to the idea that such communities may be found in the “ocean” of the Jovian satellite, Europa. An anoxic (no-O2), as well as aphotic, condition is characteristic of the deep subsurface biosphere. Microorganisms in the deep subsurface biosphere exploit every available oxidant for anaerobic respiration. Sulfate, nitrate, iron (III) and CO2 are the representative oxidants in the deep subsurface. Below the 3000 m-thick glacier on Antarctica, >70 lakes having liquid water are entombed. One of such sub-glacial lakes, Lake Vostok, has been a target of “life in extreme environments” and is about to be drill-penetrated for microbiological studies. These biospheric frontiers will provide new knowledge about the diversity and the potential of life on Earth and facilitate the capability of astrobiologial exploration.
  • 稲場 典康
    人工知能
    2006年 21 巻 1 号 14-19
    発行日: 2006/01/01
    公開日: 2020/09/29
    解説誌・一般情報誌 フリー
  • 長沼 毅
    海の研究
    1995年 4 巻 5 号 423-432
    発行日: 1995/10/30
    公開日: 2008/04/14
    ジャーナル フリー
    Hydrothermal vents serve as the "oases" for the animals inhabiting the deep-sea "deserts". The biomass of the vent communities is outstanding in the sterile deep-sea habitats; it is remarkable even in the whole marine environment. The vent communities are primarily supported by microbial chemosynthetic production, largely based on sulfur oxidation. The fraction of sulfur-oxidizing bacteria in the microflora in the hydrothermally affected waters (plumes) was notably higher than that in non-plume waters. Planktonic bacteria in the plumes were shown to have high production rates and thus contribute to vent animals as particulate food sources. This contribution may be magnified by the capability of aggregate formation. Size is a food quality determining the food value, and the value of bacterial aggregates over bacterial cells is obviously high, considering rice grains and rice balls. Aggregate formation was often observed with the planktonic bacteria in and from the hydrothermal plumes. Thus, planktonic bacteria were thought to contribute to the vent communities at least in a dual manner: by high production and aggregate formation.
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