熱帯アフリカにおける白亜河流の流出の軌道強制と海洋への対応
Britta Beckmann1, Sascha Flögel, Peter Hofmann
1Department of Geosciences, University of Bremen, Klagenfurter Str., 28357 Bremen, Germany.
Nature
|September 9, 2005
まとめ
軌道前退によって引き起こされた熱帯気候の変化は,白亜紀の海洋無酸素化とブラック・シェール形成に大きく影響した. これらの発見は,温かい気候の海洋の縁の淡水排出の変動に対する感受性を強調しています.
科学分野:
- パレオセアノグラフィー
- 気候科学 気候科学
- 地質化学 地質化学
背景:
- クレタ紀は極度の高温を体験し,熱帯は潜在的に地球循環を推進しました.
- 温室効果条件下での軌道強制,淡水流出,大陸縁の生地化学の関連性を理解することは極めて重要です.
- 以前の研究では,これらの関連が完全に解明されていなかった.
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