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Updated: May 26, 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

"大酸化イベント"に続く有機物質の大規模な酸化の同位体証拠

Lee R Kump1, Christopher Junium, Michael A Arthur

  • 1Department of Geosciences, Pennsylvania State University, University Park, PA 16802, USA.

Science (New York, N.Y.)
|December 7, 2011
PubMed
まとめ

プロテロゾーイクエオンは,極端な炭素循環の変動を経験しました. パレオプロテロゾーイク時代の炭素同位体異常は,後のネオプロテロゾーイク時代の出来事と類似した,初期の酸素豊富な大気条件を示唆しています.

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