纪末期的灭绝和现代新热带雨林的起源
Mónica R Carvalho1,2, Carlos Jaramillo3,4,5, Felipe de la Parra6
1Smithsonian Tropical Research Institute, Panama.
概括
甲纪末期的事件导致热带森林的植物灭绝了45%,导致了600万年的恢复期. 这一事件改变了新热带雨林的形状,
科学领域:
- 古植物学
- 古生态学
- 新热带森林的演变
背景情况:
- 克里塔纪末期对热带森林的影响尚不清楚.
- 晚白纪 (马斯特里希特纪) 的热带森林有开放的树冠和丰富的植物-昆虫相互作用.
研究的目的:
- 量化热带森林的植物灭绝和生态变化.
- 重建白纪 - 古纪边界对新热带植物的长期影响.
主要方法:
- 分析了超过5万个化石花粉.
- 考察来自哥伦比亚遗址的6000多个化石树叶标本.
主要成果:
- 在白纪和古纪的边界,植物多样性下降了45%.
- 热带森林经历了600万年的低多样性时期.
- 古世森林演变为封闭的树冠和多层结构,由芽植物主导,类似于现代的新热带雨林.
结论:
- 纪末期的事件显著减少了新热带地区的植物多样性.
- 这场灾难性事件推动了现代,高度多样化的新热带雨林生态系统的进化.
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