トライア紀初期温室効果期における致命的な高温
Yadong Sun1, Michael M Joachimski, Paul B Wignall
1State Key Laboratory of Geobiology and Environmental Geology, China University of Geosciences (Wuhan), Wuhan 430074, People's Republic of China. eeys@leeds.ac.uk
まとめ
温暖化が原因でペルミア期末の大量絶滅が起こり,急激に気温が上昇し,赤道上の生物に害を与え,生態系の回復を妨げました. この出来事は,トライアス紀初期に海と陸の生態系に大きな影響を及ぼした.
科学分野:
- パレオントロジー・パレオントロジー
- 気候科学 気候科学
- エコロジー エコロジー エコロジー
背景:
- 地球温暖化は,過去の生物学的危機における既知の要因である.
- ペルム紀末期の大量絶滅は,地球の歴史における重要な出来事である.
研究 の 目的:
- 初期トライアス期の急速な気温上昇が,ペルミア期末の大量絶滅に果たした役割を調査する.
- これらの高温が赤道生態系と生態系回復に与える影響を理解する.
主な方法:
- トライアス初期からの化石記録の分析.
- 温度変動を決定するために,古気候の再構築.
- 海洋と陸上の分類の生態学的分析.
主要な成果:
- ペルム紀末期の大量絶滅は,地球温暖化の急激な上昇と一致した.
- 赤道緯度では生命に不都合な温度が発生し,石灰藻や魚類が絶滅した.
- 生態系の回復は抑制され,熱的マキシマムの間,小さな無脊椎動物の分類が優位であった.
結論:
- トライアス初期における急速で極端な気温上昇は,ペルミア期末の大量絶滅の主要な原動力であった.
- 高温により,陸上の植物や動物は赤道地域から移住を余儀なくされた.
- これらの熱現象は,生態系の回復を大幅に妨害し,抑制しました.
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