同位素的证据表明,在早古时代扩大了海洋的潜层
Emma R Kast1, Daniel A Stolper2,3, Alexandra Auderset4,5
1Department of Geosciences, Princeton University, Princeton, NJ 08540, USA. ekast@princeton.edu.
概括
海洋循环在数百万年的变化是不清楚的. 在5700万年前的高同位素比率 (δ15N) 表明存在广泛的亚盒,随后与亚洲和印度的碰撞相关的下降.
科学领域:
- 古代海洋学
- 地质化学
- 海洋循环
背景情况:
- 海洋循环的长期变化仍然不太清楚.
- 体中的同位素比率 (δ15N) 是重建过去海洋条件的关键代理.
研究的目的:
- 研究海洋循环的百万年变化.
- 了解地质时间尺度上的亚体变化和脱变化的驱动因素.
主要方法:
- 在甲生物结合的有机物中分析15N/14N比率 (δ15N).
- 使用三个沉积物核来重建过去的海洋条件.
主要成果:
- 在5700万年前高的δ15N值表明水柱扩张的亚和脱.
- 在全球冷却之前,δ15N的下降与早期的亚洲-印度碰撞相吻合,可能是由于泰提斯海的影响.
- 较低的 δ15N 值在 50 到 35 Ma 之间表明大陆架有广泛的脱.
- 在35万年前的δ15N上升与冰盖的增长,海平面的下降和大陆架的收窄有关.
结论:
- 海洋循环经历了数百万年的重大变化,受地质事件和气候变化的影响.
- 海洋学和构造学因素,如亚洲 - 印度碰撞和泰提斯海的演变,在调节循环和海洋氧化中发挥了关键作用.
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