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Updated: Apr 21, 2026

Laser-Induced Fluorescence Emission L.I.F.E. as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats
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パレオセアノグラフィー 古代海洋学 北半球氷河化における南極の役割

Stella C Woodard1, Yair Rosenthal2, Kenneth G Miller3

  • 1Department of Marine and Coastal Sciences, Rutgers University, 71 Dudley Road, New Brunswick, NJ 08901, USA. woodard@marine.rutgers.edu.

Science (New York, N.Y.)
|October 25, 2014
PubMed
まとめ

北半球の氷河期は2,730万年前から始まった. 南極の氷の増加によって引き起こされた太平洋の冷たい水域と海洋循環の変化は,この主要な気候変動の移行を容易にした.

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