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メガ・エルニーニョは,ペルミア期末の大量絶滅を引き起こした
Yadong Sun1,2, Alexander Farnsworth3,4, Michael M Joachimski2
1State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (Wuhan), Wuhan 430074, P.R. China.
まとめ
炭素二酸化物の増加によって引き起こされた エルニーニョ現象が激化し ペルミア期末の大量絶滅を引き起こしました 森林伐採やサンゴ礁の崩壊など 連続した環境災害が起き 大規模な種の絶滅に繋がりました
科学分野:
- 古代気候学
- 地質科学
- 気候科学
背景:
- ペルミア期末の大量絶滅の主な原因は 議論の余地があります
- パンゲアの独特の地理は 絶滅のダイナミクスに影響を及ぼしたのかもしれません
研究 の 目的:
- ペルミア期末の大量絶滅の 統一理論を提案する
- エルニーニョ現象が 絶滅を促す役割を明らかにする
主な方法:
- マルチプロキシデータ分析
- 古代気候モデリング
主要な成果:
- 大気中のCO2は 最新のペルミアン期に倍増し 循環の変化を引き起こし エルニーニョを強めた
- エルニーニョの激化により 森林破壊,サンゴ礁の消滅,プランクトン危機が起こりました
- 炭素の貯蔵量が減ると 温暖化やエルニーニョ現象を 増幅させるような ポジティブなフィードバックループが生まれました
結論:
- 気候の変動と温暖化による影響は 陸地と海で壊滅的な損失をもたらしました
- エルニーニョ現象の拡大は ペルミア期末の大量絶滅の 重要な要因でした
- この研究は,人為的なCO2上昇と大量絶滅の間のリンクを確立しています.
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