东非的提升作为中米欧纪动物过渡的催化剂
Niklas Werner1, Zhenqian Wang1, Lars Werdelin2
1Department of Physical Geography and Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden.
Science advances
|October 15, 2025
概括
东非的构造上升和二氧化碳水平的下降在米欧纪期间促进了草原的扩张,改变了生态系统. 这种转变影响了动物的分散和哺乳动物和早期人类的进化.
科学领域:
- 古气候学 古气候学
- 古生态学 古生态学
- 地球系统科学 地球系统科学
背景情况:
- 东非的米奥森时代的标志是巨大的构造上升.
- 这种提升影响了区域气候,生态系统和动物社区的演变.
- 在这个时期,从森林环境过渡到草原.
研究的目的:
- 为了模拟气候和植被对东非升起的反应,在关键的米奥森时期间隔.
- 研究大气二氧化碳水平的变化对这些环境变化的影响.
- 了解这些变化如何影响生物多样性和哺乳动物进化.
主要方法:
- 利用高分辨率的地球系统模型EC-Earth3与动态植被模型相结合.
- 模拟的气候和植被在25 ,20和1500万年前的升起场景下 (Ma).
- 综合地力学重建,古气候建模和化石数据.
主要成果:
- 构造上升和二氧化碳水平的下降大大减少了森林覆盖面.
- 草原的扩张在整个东非和中非得到了促进.
- 环境转型促进了动物的分散和生态周转.
结论:
- 东非升起和气候变化是米奥森生态系统转型的关键驱动因素.
- 这些环境变化为哺乳动物进化创造了新的机会,包括早期的原始人.
- 该研究整合了多个数据源,以重建过去的环境动态.
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