在天文学上校准了早期的埃迪亚卡尔进化
Tan Zhang1,2,3, Chao Ma4,5, Yifan Li6
1State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation & Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, 610059, China.
Nature communications
|March 29, 2025
概括
早期埃迪亚卡尔时期的新天文学框架揭示了快速降冰和环境事件的全球同步性. 这增强了对早期生命进化和生态系统复杂性的理解.
科学领域:
- 古气候学 古气候学
- 古生物学的古生物学
- 地质时间学 (Geochronology)
背景情况:
- 早期埃迪亚卡尔的低分辨率的年代层图学阻碍了对环境变化和进化创新的理解.
- 确定精确的时间表对于将地质事件与生物进化联系起来至关重要.
研究的目的:
- 建立一个高分辨率的天文学时间框架,用于早期的埃迪亚卡拉时期.
- 精确地追溯关键的环境和生物事件,包括冰川,碳同位素游览和化石聚集.
- 为了完善早期埃迪亚卡兰生物进化的年龄模型.
主要方法:
- 天文学应用到中国南方的关键部分.
- 与多个放射性同位素日期集成以固定时间表.
- 日期事件与全球古气候和古环境标记的相关性.
主要成果:
- 为早期的埃迪亚卡朗建立了大约576万年高分辨率的天文年代学框架.
- 在中国南部的马里诺海冰川消融是快速的 (10^6-10^7年).
- 马里诺海的脱冰,埃迪亚卡的负碳同位素出行1和2 (EN1和EN2),以及关键的化石组合的全球同步性得到了强有力的证明.
结论:
- 精细的时间表为早期的埃迪亚卡尔生物进化提供了一个精确的年龄模型.
- 生态系统的复杂性在数百万年内逐渐增加.
- 快速向新型社区的过渡与生物地化学乱相吻合,尽管全球的分类学多样性稳定.
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