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北極からのクレタセア紀後半の季節的な海洋の変動
Andrew Davies1, Alan E S Kemp, Jennifer Pike
1National Oceanography Centre Southampton, School of Ocean and Earth Science, University of Southampton, Southampton, SO14 3ZH, UK.
Nature
|July 10, 2009
まとめ
クレタ紀の北極海からの記録は,季節的なダイアトムの生産を明らかにし,上流ではなく,層分かれした水域で発生しました. これは,地球温暖化の下で将来の海洋生産性の潜在的なモデルを示唆しています.
科学分野:
- 古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは
- 海洋学 海洋学とは
- マリン・バイオロジー マリン・バイオロジー
背景:
- 北極海は,地球規模の気候変動の重要な指標である.
- 過去の北極の条件を理解することは,将来の気候シナリオを予測するために不可欠です.
- 温室効果期間の後期白期の北極海の状態についてはほとんど知られていない.
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