全球冷却推动了多元化,而变暖导致了石灰岩 - 珀米亚时代型虫虫的灭绝
Shu-Han Zhang1, Ying-Ying Zhao1, Yu-Kun Shi1
1State Key Laboratory of Critical Earth Material Cycling and Mineral Deposits, School of Earth Sciences and Engineering and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China.
Science advances
|June 20, 2025
概括
化石藻的多样性动态令人惊地简单,显示两到三种多样化和四种下降. 长期冷却促进了生物多样性,而变暖事件导致了灭绝,突出了气候变化威胁.
科学领域:
- 古生物学的古生物学
- 气候科学 气候科学
- 进化生物学 进化生物学
背景情况:
- 化石记录是理解生物多样性在地质时间上的变化的关键.
- 复杂的生物多样性模式源于跨血统的特征-环境相互作用.
- 藻类 (Fusuline foraminifera) 是一个多样化的海洋化石群体,从石灰岩到波斯时期.
研究的目的:
- 通过使用高分辨率的全球数据集,分析藻类的多样性动态.
- 以史无前例的时间分辨率 (<4万5千年) 重建生物多样性模式.
- 研究气候 (冷却和变暖) 与生物多样化/灭绝事件之间的关系.
主要方法:
- 利用超级计算和人工智能算法.
- 分析了一组高分辨率的全球数据集,这些数据集是类菌化石.
- 重建了多样性的动态,而没有对数据进行分类,以揭示细微的模式.
主要成果:
- 鉴定出了一种意想不到的简单的多样性动态在类菌中.
- 记录了两个 (可能是三个) 截断的指数式多元化.
- 在石炭 - 珀米纪间隔期间观察到四个主要的多样性下降.
- 发现长期的冷却促进了生物多样化,而变暖事件与灭绝相关.
结论:
- 气候在石灰岩 - 波斯纪期间显著影响了海洋生物多样性的动态.
- 长期的冷却趋势支持了多元化,而变暖事件引发了灭绝.
- 目前的全球快速变暖对现代生态系统构成严重威胁,原因是人为二氧化碳排放.
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