シベリアのトラップとペルミアン-トリアス期の境界の同期
まとめ
ペルム・トライアス期の絶滅は,シベリアの洪水火山活動によって引き起こされた可能性が高い. この大規模な噴火は二酸化硫黄を放出し,地球温暖化と海面の変化を引き起こし,絶滅を引き起こした.
科学分野:
- 地質学 地質学 地質学
- パレオントロジー・パレオントロジー
- 気候科学 気候科学
背景:
- ペルミウム-トライアス (P-Tr) 境界は,大規模な大量絶滅のイベントを象徴しています.
- シベリアのトラップは,洪水ベースタルト火山活動に関連した大規模な火山地帯を表しています.
研究 の 目的:
- ノリルスク1号の侵入のタイミングを,P-Tr境界線と比較して調査する.
- シベリアの洪水火山活動とP-Tr絶滅を結びつける仮説を検証する.
主な方法:
- イオン探査機を用いたジルコンのウラン鉛年代測定.
- ノリルスクIの侵入とP-Tr境界タフからのジルコンのジオクロノロジック分析.
主要な成果:
- ノリルスクI侵入からのジルコンの年齢は,P-Tr境界のタフからの年齢と密接に一致しています (+/- 4百万年以内).
- この発見は,ノリルスク1号の侵入とシベリアトラップのコマグマ的関係を支持する.
結論:
- シベリアの洪水火山活動が,P-Tr絶滅の原因である可能性が高い.
- 火山による排出物 (硫黄二酸化物など) は,地球温暖化,氷河の膨張,酸雨,海面変動を引き起こし,大量絶滅に寄与した可能性がある.
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