快速全球变暖在古世 - 世边界对新热带植被的影响
Carlos Jaramillo1, Diana Ochoa, Lineth Contreras
1Smithsonian Tropical Research Institute, Box 0843-03092, Balboa, Ancon, Republic of Panama. jaramilloc@si.edu
概括
热带雨林在古世 - 世热量最大 (PETM) 期间勃发展,尽管温度上升了3°5°C. 新的植物物种出现,表明它们对变暖和高二氧化碳水平有弹性.
科学领域:
- 古气候学 古气候学
- 古植物学是古植物学.
- 新热带生态新热带生态学
背景情况:
- 古世 - 世热极值 (PETM) 导致了全球快速变暖,热带气温上升了3°5°C.
- 了解热带生态系统对极端变暖事件的反应对于预测未来气候影响至关重要.
研究的目的:
- 调查热带森林在PETM期间对快速变暖的反应.
- 评估新热带雨林植物多样性和起源率的变化.
主要方法:
- 分析了来自哥伦比亚东部和委内瑞拉西部三个平流图段的古生物学记录.
- 在PETM期间评估植物多样性和起源率.
主要成果:
- 观察到植物多样性和起源率的显著增加.
- 植物群中增加了新的血管种类,表明了快速的适应和多样化.
- 在北方新热带地区没有发现干旱度增加的证据.
结论:
- 热带雨林在PETM期间持续存在并多样化,尽管气候变暖显著,二氧化碳水平高.
- 与一些假设相反,热带生态系统表现出弹性,而不是由于热应激而严重妥协.
- 这项研究强调了热带动植物对过去气候变化事件的适应能力.
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