比較地球史とペルム後期の大量絶滅
A H Knoll1, R K Bambach, D E Canfield
1Botanical Museum, Harvard University, Cambridge, MA 02138, USA.
まとめ
ペルム後期の大量絶滅は,無酸素深海の転覆によって引き起こされ,二酸化炭素が放出され,生物に影響を及ぼした可能性があります. これはネオプロテロゾーイク時代に観測された条件を反映し,古代と最近の地質学的出来事を結びつける.
科学分野:
- パレオセアノグラフィー
- 地質学的な出来事は,地質学的な出来事です.
- 大量絶滅の出来事は,大量絶滅の出来事です.
背景:
- ネオプロテロゾーイク期の終わりには,炭素同位体の遠足,氷河化,そして異常な炭酸塩の降水が収束した.
- これらの現象は,ペルミア後期の地球における同様の条件を理解するためのモデルを提供します.
研究 の 目的:
- ペルミア後期におけるネオプロテロゾイク時代の状況の再現を解釈する.
- 古代海洋学的変化と大量絶滅の間の関連を説明する.
主な方法:
- パレオセアノグラフィモデルの開発.
- 層図と同位体データの分析.
- ネオプロテロゾイクとペルミア後期の地質学的記録の比較.
主要な成果:
- このモデルは,ペルミウム後期の無酸素深海の転覆が,高濃度の二酸化炭素を導入したことを示唆している.
- このCO2の放出は,表面環境と大気条件に影響を与えました.
結論:
- 予測された生理学的および気候的影響は,ペルム後期の大量絶滅の観測されたタイミングと選択性と一致しています.
- 海洋の転覆は,ペルミア後期絶滅の出来事の合理的なメカニズムです.
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