过去1.65亿年的海洋循环稳定性
Linda V Godfrey1, Anne Willem Omta2, Eli Tziperman3
1Department of Earth and Planetary Sciences, Rutgers University, Piscataway, NJ, USA. linda.godfrey@rutgers.edu.
Nature communications
|October 9, 2025
概括
海洋的生产力受到和的限制. 过去的海洋沉积物同位素揭示了大陆漂移和海岸线的方向如何影响了超过1.65亿年的循环和海洋生产力.
科学领域:
- 海洋地质学 海洋地质学
- 生物地质化学生物地质化学
- 古海洋学是古海洋学.
背景情况:
- (N) 和 (P) 是限制生物生产力的关键海洋宏观营养素.
- 虽然P的供应是地质的,N是大气的,但可以通过铁等微量营养素来限制.
- 了解N周期与生产率的反对于海洋生态系统至关重要.
研究的目的:
- 重建过去1.65亿年 (Ma) 的 (N) 和碳 (C) 同位素记录.
- 研究海洋N循环和生物生产力之间的反.
- 探索古地理和气候对N-同位素的影响.
主要方法:
- 在165万年前的海洋沉积物中分析N和C同位素.
- 使用同位素盒模型.
- 采用相结合的气候模型.
主要成果:
- 在过去的165万年里,海洋沉积物的N同位素平均为+3.2‰,变化 (-2至+9‰).
- 由于垂直混合有限,在遥远的海洋地区观察到较高的δ15N值.
- 由大陆漂移和海岸线方向驱动的风引起的上升变化影响了δ15N.
结论:
- 古地理变化,特别是大陆和海岸线的方向,显著影响了海洋上游和N周期动态.
- 东西泰提亚海岸线促进了低δ15N,而南北海岸线由于脱而导致高δ15N.
- 这些发现突出了地球地质,气候和海洋生物地球化学循环之间的长期相互作用.
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