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经常性和长期的海洋性无氧导致了经过二叠纪-三叠纪危机后的生物恢复
Wenhao Li1,2, Bowei Yuan1,2
1National Key Laboratory of Deep Oil and Gas, China University of Petroleum (East China), Qingdao 266580, China.
Biology
|February 12, 2026
概括
在Chaohu地区的早期Triassic海洋无氧阻碍了生物的恢复. 然而,在斯米提亚/斯帕提亚边界气候降温事件期间,短暂的氧气条件促进了海洋生物的显著恢复.
科学领域:
- 古海洋学是古海洋学.
- 海洋地质化学海洋地质化学
- 古生物学的古生物学
背景情况:
- 在经历了珀米亚-特里亚斯危机后,早期特里亚斯生物复苏的理解很少.
- 海洋化学显著影响海洋生态系统的恢复.
- 湖地区为研究这一时期提供了一个关键地点.
研究的目的:
- 评估海洋化学对湖地区早期三叠纪生物恢复的影响.
- 为了重建早期三叠纪时期的古海洋学条件.
- 确定驱动或抑制海洋生物恢复的环境因素.
主要方法:
- 对酸盐含量,δ13Corg,以及酸盐的S同位素组成进行分析.
- 使用地球化学代理的海洋无氧和氧状况的重建.
- 地化学数据与生物回收事件的相关性.
主要成果:
- 经常性和长期的海洋无氧是查胡地区的特征.
- 在最早和最晚的斯帕提亚时代发生了两次明显的氧气状况.
- 在史密斯/斯帕提斯边界的积极的 δ13 C 转移和 δ34 S 游览与生物恢复和氧气条件一致.
结论:
- 在气候冷却期间,全球海洋循环可能增强的氧气条件,有助于生物恢复.
- 频繁的环境干扰和持续的海洋无氧最终阻止了在三叠纪早期的持续生物复苏.
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