西

Matthew W Schmidt1, Howard J Spero, David W Lea

  • 1Department of Geology, University of California, Davis, California 95616, USA. schmidt@geology.ucdavis.edu

Nature
|March 12, 2004
PubMed
まとめ

カリブ海の塩分は,最後の氷河期の北大西洋の深水形成とともに変動した. 低塩分度が温暖化イベントに先行し,熱帯水のアドベクションが気候変動を拡大したことを示唆しています.

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