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プレストセンの初期以来,北部の氷床の変動に対するプレセッションの持続的な影響
Stephen Barker1, Aidan Starr1, Jeroen van der Lubbe2
1School of Earth and Environmental Sciences, Cardiff University, Cardiff, UK.
まとめ
氷の量の変化は主に 100万年前までの傾きによって引き起こされた. プレセーションは,特にプレイストセンの中期から後半にかけて,氷河期の氷床の融解に影響した.
科学分野:
- 古代気候学
- 四半期地質学
- 気候の動態
背景:
- 地球の軌道の周期と 歴史的に結びついています
- 氷河期における傾きとプレセッションの相対的な影響は,特に100万年前までは,研究の対象であり続けています.
研究 の 目的:
- 過去170万年の氷河周期を 推し進める際の 傾斜とプレセッションの役割を調べる
- 軌道の力に反応して氷床の膨張と縮小のタイミングとメカニズムを決定する.
主な方法:
- 北大西洋のラフトの記録を分析しました
- アイスラフティングイベントと地球の軌道パラメータの相関 (傾きとプレセーション).
主要な成果:
- 氷床の膨張は傾きが低下する時に一貫して発生した.
- 氷の大量流出 (流出) は一貫してプレセションにおける最小値と関連していた.
- プレセーションによる断層と氷河期の終結との関連は,プレイストセンの中期から後半にかけて顕著である.
結論:
- 100万年前までは 氷河周期の主な原動力でした
- 北半球の氷床が約100万年前に南に広がった後,プレセッションは氷河の終結において重要になった.
- 氷河期の軌道強制は,四年生期を通して異なる段階を示しています.
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