寒い北極海の海底に,多様な熱性細菌が絶えず流入しています
Casey Hubert1, Alexander Loy, Maren Nickel
1Biogeochemistry Group, Max Planck Institute for Marine Microbiology, Celsiusstrasse 1, D-28359 Bremen, Germany. chubert@mpi-bremen.de
まとめ
冷たい北極海の沈殿物は,毎年10^8以上の熱性細菌の胞子を吸収する. 温暖な地下環境から発生するこれらの休眠微生物は,気温が上昇すると有機物質を迅速に消費し,海洋微生物の多様性に影響を与えます.
科学分野:
- 微生物学 微生物学とは
- マリン・バイオロジー マリン・バイオロジー
- 地質化学 地質化学
背景:
- 微生物は,その代謝に適さない環境で生息する.
- 誤った位置に置かれたこれらの微生物を理解すると,分散メカニズムが明らかになり,微生物の多様性が形成されます.
研究 の 目的:
- 熱性細菌が北極海の沈殿物に流入する量を定量化するために.
- これらの熱性細菌の起源と輸送メカニズムを特定するために.
主な方法:
- 細菌の供給率を推定するために,エンドスポアの発芽実験が使用されました.
- 特定されたバクテリアの遺伝子解析と代謝分析が行われました.
主要な成果:
- 熱愛性のFirmicutesバクテリアの安定した供給 (10^8種子/m^2/年以上) は,北極海の堆積物で検出されました.
- これらのバクテリアは低温では代謝的に不活性ですが,50°Cでは有機物質を積極的に分解します.
- 系統遺伝学的分析は,暖かい地下の石油貯蔵庫と海洋殻の生態系からその起源を示しています.
結論:
- 海底の液体の流れは,熱性細菌を温暖な地下環境から冷たい海へと運ぶ可能性が高い.
- これらの輸送経路は,海洋微生物コミュニティの組成に大きな影響を与えます.
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