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Updated: Jul 13, 2026

Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats
13:38

Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats

Published on: October 26, 2019

チリ沖とパタゴニアの氷床への反応による地表水の変化の南極のタイミング

Frank Lamy1, Jérôme Kaiser, Ulysses Ninnemann

  • 1GeoForschungsZentrum-Potsdam, Telegrafenberg, 14473 Potsdam, Germany. flamy@gfz-potsdam.de

Science (New York, N.Y.)
|June 26, 2004
PubMed
まとめ

海洋沈殿物は,海氷と風の移転に関連した南極のタイミングによる海洋変化を明らかにしています. パタゴニアの氷床の広がりは,これらの変化を反映しているが,氷河の反応が遅れており,南米の記録の不一致を説明している.

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