クレータ紀・パレオゲン紀の大量絶滅後の生物の回復に関する例外的な大陸記録
T R Lyson1, I M Miller2, A D Bercovici2,3
1Denver Museum of Nature & Science, 2001 Colorado Boulevard, Denver, CO 80205, USA. tyler.lyson@dmns.org.
まとめ
クレータ紀・旧紀の大量絶滅 (KPgE) の後の早期の哺乳類の回復は急速であり,最初の100万年以内に多様性と体量が大幅に増加した. 気候変動が この生物の復活に 影響を与えているようです
科学分野:
- 古生物学
- 古代生態学
- 気候科学
背景:
- クレータ紀・旧紀の大量絶滅 (KPgE) の後の最初の100万年はよくわかっていない.
- この時期の化石記録は 完ぺきでないことが多いので 生物的回復の詳細な分析が困難である.
研究 の 目的:
- 初期パレオゲンにおける生物の回復の原動力と速度を明らかにする.
- 哺乳類と植物の進化と気候との関係を分析する.
主な方法:
- コロラド州の時間調整された層図の分析
- 哺乳類,爬虫類,植物の例外的に完全な化石の調査.
主要な成果:
- 哺乳類の分類学的な豊かさは,KPgE後の10万年以内に倍増した.
- 哺乳類の最大体積はKPgE後の300 kaで大きく増加し,メガフララの多様性が増加した.
- 大規模な哺乳類の多様化とレギュミノサエの出現は,KPgE後700カ年頃に発生し,温暖化間隔と一致した.
結論:
- 哺乳類の回復は,体量と食事の専門性を含め,初期のパレオゲンでは迅速でした.
- 気候の温暖化間隔は,KPgE後の植物と哺乳類の同時進化と回復に重要な役割を果たした.
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