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Updated: Sep 11, 2025

Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
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鉄酸化物から溶けた海洋有機炭素の地質史

Nir Galili1,2, Stefano M Bernasconi3, Alon Nissan4,5

  • 1Geological Institute, Department of Earth and Planetary Sciences, ETH Zurich, Zurich, Switzerland. ngalili@ethz.ch.

Nature
|August 13, 2025
PubMed
まとめ

海洋溶解有機炭素 (DOC) レベルは地質学的な時間とともに大きく変動した. この研究は古代のDOC濃度を再構築し,海洋化学,酸素化,複雑な海洋生物の進化の間のリンクを明らかにします.

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