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Updated: Jul 11, 2026

Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
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Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria

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古代末期生物圏の酸素化と大気の進化

Alan J Kaufman1, David T Johnston, James Farquhar

  • 1Departments of Geology and Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD 20742-4211, USA.

Science (New York, N.Y.)
|September 29, 2007
PubMed
まとめ

25億年前のマックレイ山のシェイルは,古代の酸化硫黄循環を明らかにしています.

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