ドレイク海峡の開通のタイミングと気候上の影響
Howie D Scher1, Ellen E Martin
1Department of Geological Sciences, University of Florida, Gainesville, FL 32611, USA. howie@earth.rochester.edu
まとめ
ドレーク海峡は約4100万年前に開き,太平洋の水が南洋に流入した. この出来事は,海洋循環,生産性,地球温暖化に影響を与え,重要な南極経路を確立しました.
科学分野:
- パレオセアノグラフィー
- 気候科学 気候科学
- 地質学 地質学 地質学
背景:
- ドレイク海峡開通のタイミングは議論されていて,海洋循環と地球温暖化の理解に影響を及ぼしている.
- ネオジムイソトープデータは,過去の海洋学的な状況についての洞察を提供します.
研究 の 目的:
- ドレイク海峡の開口時期と海洋循環への影響を決定する.
- 海洋学的な変化と地球規模の気候変化の関係を調査する.
主な方法:
- Agulhas Ridgeのネオジムイソトープ比における長期変動の分析.
- 海洋ゲートウェイの地質年代測定.
主要な成果:
- 証拠によると,約4100万年前,太平洋の海水が南洋に流入したとされています.
- ドレイク海峡の開通と深まりは,生物の生産性の向上と気候の変動と一致しました.
- ドレイク・パサッジの開口は,タスマニア・ゲートウェイより前のもので,初期の環南極流を示している.
結論:
- ドレイク海峡の開通は南洋の循環と地球温暖化に大きな影響を与えました.
- 海洋循環と生物生産性の変化は,大気中の二酸化炭素の減少と関連していた.
- エオセンの終わりまでに,完全な環南極経路が確立されました.
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