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Updated: Jul 12, 2026

Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
09:45

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

Published on: July 24, 2016

マグネシウムと鉄の代用は,無酸素海洋沈殿物の粘土鉱物におけるマグネシウムと鉄の代替である

J I Drever

    Science (New York, N.Y.)
    |June 25, 1971
    PubMed
    まとめ

    鉄は,無酸素堆積物中の海洋粘土鉱物から抽出され,硫化物を形成します. その後,マグネシウムは粘土の鉄を代用し,海水の組成と沈殿物の孔水化学を制御します.

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