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Updated: Feb 17, 2026

Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
09:45

Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria

Published on: July 24, 2016

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オリゴセンの深海の酸素イソトープの変動は,主に温度によって引き起こされる

Flavia Boscolo-Galazzo1, Victoria E Taylor2, Eirik V Galaasen2

  • 1MARUM, Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany.

Nature geoscience
|February 16, 2026
PubMed
まとめ

オリゴセンの気候の変化は,南極の氷の量の変化ではなく,海洋の温度によって引き起こされた. 新しく集積された同位体データは,軌道のペースで進む深海温暖化が顕著であることを明らかにし,南極の氷床の動態に関する過去の解釈を解決している.

キーワード:
パレオセアノグラフィーパレオ気候とは,古代の気候です.

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