动态的氧化还原促进的铁和营养循环驱动了石灰岩在奥尔多维克斯-西卢里亚斯过渡时期的演变
Zhen Qiu1, Caineng Zou1, Jiaqiang Zhang2,3
1Research Institute of Petroleum Exploration & Development, China National Petroleum Corporation, Beijing, China.
Science advances
|January 21, 2026
概括
在奥尔多维纪晚期的大规模灭绝期间,海洋氧化还原变化影响了石墨岩物种. 铁 (Fe) 和 (P) 循环变化解释了石墨矿石的消失和随后的辐射.
科学领域:
- 古海洋学是古海洋学.
- 古生物学的古生物学
- 生物地质化学生物地质化学
背景情况:
- 石灰岩石是丰富的早期古老纪动物浮游生物.
- 在奥尔多维纪晚期的大规模灭绝期间发生了显著的物种变化.
研究的目的:
- 评估鱼生态系统在灭绝过程中重塑的驱动因素.
- 研究海洋氧化还原,铁同位素和循环的作用.
主要方法:
- 对海洋氧化还原,铁同位素 (δ56Fe) 和相分割的分析.
- 检查架和深海沉积物记录的检查.
主要成果:
- 货架上的负 δ56Fe 移动与与铁吸收和 euxinia 相关的 mesopelagic 石灰岩的减少相关.
- 深海和货架沉积物中的积极δ56Fe转移表明广泛的铁去除和增强的回收.
- 这些变化加剧了状石灰岩的辐射.
结论:
- 与氧化还原状态和循环相关的海洋铁循环变化推动了石墨矿石的灭绝和多样化.
- 广泛传播的eocinia和随后的释放是重塑早期古老生态时期海生态系统的关键因素.
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