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Updated: May 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

深海のシリケートの脱氷パルスは,亜熱帯北大西洋の北大西洋に流れ込みます

A N Meckler1, D M Sigman, K A Gibson

  • 1Geological Institute, ETH Zürich, 8092 Zürich, Switzerland. nele.meckler@erdw.ethz.ch

Nature
|March 30, 2013
PubMed
まとめ

氷河期には,大気の下部にある二酸化炭素が海に蓄積された. 脱氷は,海洋循環,特に北大西洋と南大洋の変化を通じて,このCO2を放出しました.

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