減少した北大西洋の深い水域は,アガシズ湖氷河の淡水噴出と同時期である

Helga Kikki Flesche Kleiven1, Catherine Kissel, Carlo Laj

  • 1Bjerknes Centre for Climate Research, University of Bergen, N-5007 Norway. kikki@uib.no

Science (New York, N.Y.)
|December 8, 2007
PubMed
まとめ

約8,380年前,アガシズ湖から大量の淡水噴出が起こり,大西洋の循環が著しく弱まった. このイベントは,約100年間続いたが,北大西洋地域の深水の流れと気候に影響を与えた.

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