パレオセーヌ・エオセーヌ境界における衝突噴出物
Morgan F Schaller1, Megan K Fung2, James D Wright3
1Earth and Environmental Sciences, Rensselaer Polytechnic Institute (RPI), Troy, NY 12180, USA. schall@rpi.edu.
まとめ
地球外での衝突は 5千6百万年前の パレオセーヌ・エオセーヌ熱極期に発生しました この影響は地球における 重要な気候変動と進化のシフトに関連しています
科学分野:
- 地理科学
- 古代気候学
- 進化生物学
背景:
- 地球外からの影響は 地球の気候と進化に大きな影響を与えます
- 5千6百万年前のパレオセーヌ・エオセーヌ熱極 (P-E) イベントは,急速な地球温暖化と炭素循環の混乱を伴う.
- この時期には哺乳類の拡大と深海の絶滅など 進化の大きな変化が起こりました
研究 の 目的:
- 地球外衝突の証拠を調査する パレオセン-エオセンの境界で
- P-E 熱極期における観測された気候と進化的変化と相関する.
主な方法:
- 海のP-E境界部分からの地質サンプル分析
- シリケートガラス球体の識別と特徴付け
- 衝突のタイミングを 特定するために ストラティグラフィック分析
主要な成果:
- 複数のP-E境界部分の異なる層構造のシリケートガラス球体を発見した.
- これらの球粒をマイクロテクタイトとマイクロクリスタイトとして識別する.
- 炭素同位体発射と一致する 地球外衝突の確認
結論:
- 地球外での衝突は パレオセーン・エオセンの境界で 起こったのです
- この衝撃イベントは,P-E熱極の気候と進化の動態を理解する上で重要な要因です.
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