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Updated: Mar 21, 2026

Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
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古代の微小隕石は,酸素に富んだアルカイア上層大気を示唆している

Andrew G Tomkins1, Lara Bowlt1, Matthew Genge2,3

  • 1School of Earth, Atmosphere and Environment, Monash University, Melbourne, Victoria 3800, Australia.

Nature
|May 13, 2016
PubMed
まとめ

初期の地球の上層大気圏は,現在の酸素レベルに似ている可能性があり,以前の仮定に異議を唱えた. 化石の微小隕石は 27億年前に高濃度の酸素が存在していたことを示唆しています

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