トライアス・ジュラスの境界における大量絶滅と関連した突然の生産性の崩壊
P D Ward1, J W Haggart, E S Carter
1Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195, USA.
まとめ
トライア紀末期の大量絶滅は,海洋プランクトンの生産性に大きな崩壊を引き起こした. このイベントは,炭素同位体によって証明され,地球の歴史における他の主要な絶滅イベントを反映しています.
科学分野:
- パレオントロジー・パレオントロジー
- 地質化学 地質化学
- 地球科学 地球科学 地球科学
背景:
- トライア紀末期の大量絶滅は,地球の歴史上最大の5つの絶滅の出来事の1つです.
- この出来事の原因と影響を理解することは,ファネロゾーイク生物多様性の動態を理解するために不可欠です.
研究 の 目的:
- トライア紀末期の大量絶滅の原因を調査する.
- トライアス・ジュラスの境界における生産性の変化に関する炭素同位体証拠を分析する.
主な方法:
- カナダのブリティッシュ・コロンビア州クイーン・シャーロット諸島の断面のストラティグラフィック分析.
- 堆積物の記録の炭素同位体分析. 堆積物の記録の炭素同位体の分析. 堆積物の記録の炭素同位体の分析.
主要な成果:
- トライアスの終わりの境界で,海洋生産性の急激な崩壊の証拠.
- 他の主要な絶滅イベント (ペルミア-トライアス,白-三次) に類似する炭素同位体遠征が観察されました.
結論:
- トライア紀末期の大量絶滅は,海洋生態系の生産性の著しい崩壊と関連していた.
- 炭素同位体のデータは,この絶滅のイベント中に地球規模の環境ストレスのパターンを示唆しています.
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