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Updated: May 2, 2026

Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
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最後の氷河期の亜南極海の鉄の肥料化

Alfredo Martínez-García1, Daniel M Sigman, Haojia Ren

  • 1Geological Institute, ETH Zürich, 8092 Zürich, Switzerland.

Science (New York, N.Y.)
|March 22, 2014
PubMed
まとめ

氷河期における南洋の植物プランクトンの粉末による鉄の肥料化により,生産性が向上し,大気中の二酸化炭素 (CO2) が減少しました. この発見は,氷河期CO2減少と千年スケールの気候振動に関する鉄の仮説を支持する.

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