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Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment
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初期のアルカイア期における微生物メタノゲネシスのための液体インクルージョンからの証拠

Yuichiro Ueno1, Keita Yamada, Naohiro Yoshida

  • 1Research Center for the Evolving Earth and Planet, Tokyo Institute of Technology, Meguro-ku, Tokyo 152-8551, Japan. yueno@depe.titech.ac.jp

Nature
|March 24, 2006
PubMed
まとめ

この研究は,メタノゲン,原始的な微生物の最も古い証拠を提供し,それは346億年以上にさかのぼります. これらの発見は,初期のメタノゲンが,メタンを生成することによって,地球の古代気候に影響を及ぼした可能性があることを示唆しています.

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