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エオセンの末期に彗星が降ったという地化学的な証拠
K A Farley1, A Montanari, E M Shoemaker
1Division of Geological and Planetary Sciences, California Institute of Technology, MS 170-25, Pasadena, CA 91125, USA. farley@gps.caltech.edu
まとめ
地球は,地球外生命体ヘリウム-3 (塵の追跡物質) の増加を,エオセンの末期に経験した. この250万年の流れは,大きな小惑星の衝突と一致し,太陽系の塵や地球を横切る物体の短時間的な増幅を示唆しています.
科学分野:
- 地質化学 地質化学
- 惑星科学は惑星科学である.
- 古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは
背景:
- ペラジック石灰岩には,惑星間塵のトレーサーである地球外ヘリウム-3が含まれています.
- ポピガイとチェサピーク湾のクレーターのような大きな衝突イベントは,約3600万年前に起こった.
- エオセンの末期は,重要な地質学的,天文学的出来事を経験した.
研究 の 目的:
- 地球外のヘリウム-3濃度について,ペラジック石灰岩を分析するために.
- ヘリウム3の流れと,地球の歴史における主要な衝突イベントを相関させるため.
- 地球を横切る物体と太陽系内部の塵性の動態を調査する.
主な方法:
- ペラジック石灰岩のサンプルを地化学分析.
- ヘリウム-3濃度を定量化するための同位体分析.
- 出来事の間の時間的な関係を確立するために,年代測定法による年代測定.
主要な成果:
- エオセンの終わりに,地球外での強化されたヘリウム-3流の250万年 (My) の期間が特定されました.
- ヘリウム3の強化は,ポピガイとチェサピーク湾の衝突事故の1ミリ前に始まり,1.5ミリ後に終わった.
- ヘリウム-3濃度の上昇は大きな衝突イベントと相関しており,地球を横切る物体と太陽系内部の塵の同時,短い増幅を示しています.
結論:
- 同時の相関は,オート雲の乱れによって引き起こされた彗星シャワーを示唆しています.
- 地球を横切る物体と惑星間塵は,エオセンの後半に一時的な増加を経験しました.
- このイベントは,地球に影響を与える太陽系内のダイナミックなプロセスの証拠を提供します.
関連する概念動画
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