在古世 - 世热量最大时期的植被功能丧失
Julian Rogger1,2, Vera A Korasidis3, Gabriel J Bowen4
1Department of Earth and Planetary Sciences, ETH Zurich, Zurich, Switzerland. jul.rogger@gmail.com.
Nature communications
|November 27, 2025
概括
古世 - 世热极值 (PETM) 导致了显著的全球变暖,压倒了植被.
科学领域:
- 古气候学 古气候学
- 生态生态学 生态生态学
- 进化生物学 进化生物学
背景情况:
- 古世 - 世热极值 (PETM) 是一个大约5600万年前的全球变暖事件.
- 长期的气候干扰可能涉及生物圈碳库动态.
研究的目的:
- 测试PETM变暖是否超过了植被的适应能力.
- 评估对碳捕集和酸盐气候变化的影响.
主要方法:
- 生态进化植被模型.生态进化植被模型.
- 分析PETM棕花粉 (化石花粉和子).
主要成果:
- 尽管植被迁移和适应,但发生了广泛的生产力损失.
- 变暖超过了植被系统的反应能力.
结论:
- PETM变暖可能会损害植被的气候调节效率.
- 未来的变暖事件可能同样影响陆地生态系统.
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