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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

ペルーの南海岸沿いのプレカンブリア期後半の変形地下の20億年前の粒子が発見されました

B Dalmayrac, J R Lancelot, A Leyreloup

    Science (New York, N.Y.)
    |October 7, 1977
    PubMed
    まとめ

    ウラン鉛による年代測定により,ペルーで20億年前のオロゲン現象が明らかになった. この古代の変形複合体は,現代の火山活動に影響を与え,ペルー・チリ溝に沿ったストロンチウム同位体比に影響を与えています.

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