在古世 - 世边界的过渡性花变化和快速的全球变暖
Scott L Wing1, Guy J Harrington, Francesca A Smith
1Department of Paleobiology, Smithsonian Museum of Natural History, 10th Street and Constitution Avenue, NW, Washington, DC 20560, USA. wings@si.edu
概括
来自古世 - 世热极限 (PETM) 的植物化石揭示了快速,大规模的植物迁移和显著的花变化,与现代气候变化影响相当.
科学领域:
- 古植物学是古植物学.
- 气候科学 气候科学
- 古气候学 古气候学
背景情况:
- 古世 - 世热极值 (PETM) 是一个全球快速变暖 (5-10°C) 的时期.
- 以前的研究表明,PETM期间的花变化很小,与脊椎动物动物周转形成鲜明对比.
- 了解过去的气候事件可以预测未来的植被反应.
研究的目的:
- 在PETM期间调查花组成和动态.
- 根据化石植物证据重建古气候条件.
- 为了比较PETM花对现代和未来气候变化的反应.
主要方法:
- 来自美国怀俄明州的植物化石的分析.
- 检查花组成,叶子形状和叶子大小.
- 基于花数据的古气候重建.
主要成果:
- PETM植物包括本地植物和迁徙植物的两种系系.
- 有证据表明植物范围发生了大规模和快速的变化 (在1万年内).
- 气候变暖约为5°C,降水模式变化 (最初低,然后增加) 由花数据推断出来.
结论:
- 对变暖和二氧化碳增加的PETM花反应是快速而显著的.
- PETM花变化的速度和程度与冰川后的植物相似.
- PETM植被动态为人类气候变化对未来植被的预测影响提供了洞察力.
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