地中海の表面放射性炭素貯蔵庫の年齢の変化は,最後の氷河期最大期以来である
1Laboratoire des Sciences du Climat et de l'Environnement (LSCE), Unité Mixte de Service, CNRS, Avenue de la Terrasse, F-91118 Gif-sur-Yvette, France.
まとめ
海洋表面貯水池の年齢は,古気候の研究に不可欠であり,1万8000年間安定した状態でした. 北大西洋の循環の変化により,最後の脱氷期に年齢が倍増した.
科学分野:
- パレオセアノグラフィー
- 気候科学 気候科学
- 放射性炭素年代測定法による年代測定
背景:
- 海洋,大陸,そして冷気圏の古プロキシの共通の年代的枠組みを確立することは不可欠です.
- 海洋と大陸の気候関係と海洋の古風化を理解するには,正確な海面貯水池の年齢に依存します.
研究 の 目的:
- 地中海地域における過去1万8000年の炭素14年における海面貯水池の年齢を決定する.
- 過去の気候現象が海洋貯水池の年齢に及ぼす影響を調査する.
主な方法:
- プランクトン系フォラミニフェラの放射性炭素年代測定.
- 海洋と陸上の記録で同時に堆積したテフラの分析.
主要な成果:
- 海面貯水池の年齢は過去1万8000年の大半で一貫して約400年でした.
- 貯水池の年齢の有意な増加 (倍増) は,最後の脱氷の開始時に発生しました.
結論:
- ハインリッヒ1号事件に関連した北大西洋熱ハリン循環の変化は,地中海海面貯水池の年齢に影響を与えた.
- これらの発見は,古気候の再構築を精錬し,海洋の動態を理解するために重要である.
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