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Updated: May 4, 2026

09:39
Technique to Collect Fungiform Taste Papillae from Human Tongue
Published on: September 19, 2010
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現代の赤道太平洋の冷たい舌の出現への亜極のリンク
Alfredo Martínez-Garcia1, Antoni Rosell-Melé, Erin L McClymont
1Geological Institute, ETH Zürich, 8092 Zürich, Switzerland. alfredo.martinez-garcia@erdw.ethz.ch
まとめ
太平洋の冷たい舌は,亜南極圏と亜北極圏の冷却により発生した. この冷却はまた,気候パターンを変化させ,プレオセーン-プレイストセンの移行期における海洋学的変化の仮説を支持した.
科学分野:
- パレオセアノグラフィー
- 気候科学 気候科学
- 海洋学 海洋学とは
背景:
- 東方赤道太平洋の冷たい舌は,世界の気候に影響を与える重要な海洋の特徴です.
- そのプレオセン-プレイストセンの発展は,熱帯域外冷却によって引き起こされた熱クリンの群集と関連しています.
研究 の 目的:
- 寒い舌の発達による亜南極および亜北極地域における同期的な冷却を調査する.
- 軌道変動に対する亜南極気候反応の変化を調査する.
主な方法:
- 亜南極と亜北極地域からの古気候プロキシデータの分析.
- 地域的な冷却のタイミングと冷たい舌の出現の比較.
- 地球の軌道周期に対する気候反応の変化の評価.
主要な成果:
- 亜南極と亜北極の地域では,冷たい舌の発達と一致する大幅な冷却が発生しました.
- サブ南極の気候は,軌道力への反応パターンとして,亜熱帯から亜極圏に変化した.
- 海洋の冷却が熱帯の群れと渦巻の収縮につながったという仮説を証拠が裏付けている.
結論:
- エクストラトロピカル冷却は,太平洋の冷たい舌のプレオセーン-プレイストセンの発展に重要な役割を果たしました.
- 観測された気候の変化は,海洋の温水球と亜熱帯圏の回転の収縮を示しています.
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