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クレータ紀・パレオゲン紀の境界と関連してデッカの火山の噴火速度

Courtney J Sprain1,2, Paul R Renne3,4, Loÿc Vanderkluysen5

  • 1Department of Earth and Planetary Science, University of California, Berkeley, 307 McCone Hall, Berkeley, CA 94720-4767, USA. c.sprain@liverpool.ac.uk.

Science (New York, N.Y.)
|February 23, 2019
PubMed
まとめ
この要約は機械生成です。

デッカン・トラップス (DT) 噴火

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科学分野:

  • 地理科学
  • 古代気候学
  • 火山学

背景:

  • デッカントラップ (DT) の火山は,白亜紀・旧紀境界 (KPB) の生態系危機に寄与したと推測されている.
  • この仮説を検証するには,DT内のKPBの正確な位置づけが不可欠です.

研究 の 目的:

  • デッカン・トラップのマグマ活動に関連して,KPBの正確な年代を決定する.
  • デッカン・トラップの噴火の歴史と 時間の経過におけるその量分布を 精査する.

主な方法:

  • 高精度アルゴン-40/アルゴン-39ジオクロノロジーは,火山単位を年代測定するために使用されました.
  • KPB に関する噴火量分布の分析

主要な成果:

  • KPBはデッカン・トラップの マグマ管道システムの変化と一致しています
  • DTの90%は100万年未満で噴火し,約75%はKPBの後に埋め込まれた.
  • 最小のDT段階は白期の気候変化記録と一致する.

結論:

  • デッカントラップの火山は主にKPBの後で発生し,KPBの生態系危機の主な原動力としての役割に挑戦した.
  • 気候を変化させるガス放出のタイミングは噴火量と直接相関しないかもしれないし,DTの火山活動が白期の気候変化の源ではなかった.