クレタ紀末期の絶滅と現代の新熱帯雨林の起源
Mónica R Carvalho1,2, Carlos Jaramillo3,4,5, Felipe de la Parra6
1Smithsonian Tropical Research Institute, Panama.
まとめ
クレタ紀末期のイベントは 熱帯雨林の45%の植物絶滅を引き起こし,600万年の回復期をもたらした. 熱帯雨林を現代に変えた
科学分野:
- 古植物学
- 古代生態学
- 新熱帯森林の進化
背景:
- クレタ紀末期の熱帯雨林への影響はよくわかっていない.
- クレタ紀後期 (マストリヒチア期) の熱帯林は,開いた天蓋があり,植物と昆虫の相互作用が豊富でした.
研究 の 目的:
- クレータ紀末期以降の熱帯森林における植物絶滅と生態学的変化を定量化する.
- ネオトロピカル・フローラにおける白亜紀・古亜紀境界の長期的影響を再構築する.
主な方法:
- 5万以上の花粉の化石を分析した.
- コロンビアの遺跡から6,000以上の葉の化石を調査した.
主要な成果:
- 植物多様性の減少は白亜紀と旧亜紀の境界で45%であった.
- 熱帯雨林は600万年の低多様性期を 経験しました
- パレオセンの森林は,現代の新熱帯雨林に似ている,アンジオスペルムが支配する閉ざされた天幕と多層構造を進化させた.
結論:
- クレータ紀末期の出来事により ネオトロピカル植物の多様性が数百万年にわたって大幅に減少した.
- この悲惨な出来事が 進化の過程で現代の 多様な新熱帯雨林の 生態系を作り出したのです
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