クレータ紀・三次期のインパクターとそのタイプの同位体証拠
1Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093-0212, USA.
まとめ
クレタセウス-三次紀境界の堆積物におけるクロームの同位体は,宇宙衝突の出来事を確認している. この地外的なクロムシグネチャーは,K-Tインパクターとして炭酸性コンドライト小惑星を指しています.
科学分野:
- 地質化学 地質化学
- 宇宙化学 (コスモケミストリー)
- パレオントロジー・パレオントロジー
背景:
- クレータ紀-三次紀 (K-T) の境界線は,大量絶滅の出来事を示しています.
- K-T絶滅の原因は議論されており,宇宙の衝撃が主要な仮説である.
研究 の 目的:
- クロミウムイソトープ解析を用いてK-T境界現象の起源を調査する.
- K-T イベントの原因となる地球外生命体の衝突物質の性質を決定する.
主な方法:
- クロミウムイソトープの高精度質量スペクトロメトリック分析.
- デンマークのスティーヴンス・クリントとスペインのカラバカのK-T境界からの堆積物サンプル分析.
主要な成果:
- K-T境界標本におけるクロム同位体組成は,地球の同位体と著しく異なる.
- 同位体シグネチャーは,炭酸性コンドライト隕石に含まれるクロムと一致しています.
- これは,K-T境界物質の地球外の源であることを確認しています.
結論:
- K-T境界イベントは,宇宙の衝突によって引き起こされました.
- 衝突器は炭酸塩状のコンドライトだった可能性が高い.
- クロミウム同位体分析は,古代の衝撃物質を特定するための貴重なツールです.
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