大陆弧火山运动的强化侵蚀是坎布里亚爆炸的驱动因素
Yaowen Wu1,2, Hui Tian3, Haifeng Fan4
1State Key Laboratory of Deep Earth Processes and Resources, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, China.
Nature communications
|October 16, 2025
概括
坎布里亚爆炸期间的构造活动通过侵蚀年轻岩石释放了营养物质,提高了海洋生产力和氧气水平. 这一过程推动了早期的动物多样化,突出了构造学和生物地质化学循环之间的联系.
科学领域:
- 地质化学 地质化学
- 古生物学的古生物学
- 地球科学 地球科学 地球科学
背景情况:
- 坎布里亚爆炸 (约540-515万年前) 见证了动物的快速多样化,与营养的可用性和氧气水平的上升有关.
- 由气候和构造学驱动的增强的气候变化被提议满足这些条件.
- 在此期间,潜伏驱动的气候在营养循环中的特定作用仍然不清楚.
研究的目的:
- 为了调查探驱动的气候变化动力学和坎布里亚爆炸期间动物多样化的联系.
- 阐明潜伏和大陆弧火山运动在释放营养物质和随后的环境变化中的反作用.
主要方法:
- - (Li-Os) 同位素与现有的 (Sr) 同位素数据的整合.
- 分析岩石气候变化模式及其对营养流动的影响.
主要成果:
- 大约525-515万年前,气候模式发生了显著的转变.
- 初始阶段 (540-525万年前) 显示了与弧形相关的年轻岩石的侵蚀增强.
- 后期阶段 (525-515万年前) 表明,旧地的粘土形成气候变化的转变.
结论:
- 潜伏驱动的升温和升起可能加速了富含的年轻岩石的侵蚀.
- 这种营养物质的释放促进了海洋生产力和通过有机埋葬的氧化.
- 在坎布里亚爆炸期间,对生物地质化学循环的构造控制在推动早期动物多样化方面发挥了关键作用.
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