高生产率和多层循环在晚白时期的北冰洋
Shan Liu1,2, David Van Rooij3, Meiting Chen4
1School of Marine Sciences, Sun Yat-sen University, 519082 Zhuhai, China.
Science advances
|March 6, 2026
概括
晚白时期的北极海洋有强烈的深水循环和碳酸盐生产,挑战了以前的观点. 这种动态系统在温室条件下影响了全球气候,然后在白纪-古纪的边界崩.
科学领域:
- 古海洋学是古海洋学.
- 气候科学 气候科学
- 地质地质地质地质地质地
背景情况:
- 北冰洋在全球气候中的作用至关重要,但在温室时期的流通情况尚不清楚.
- 之前的模型建议一个缓慢的,表面占主导地位的晚白纪北极.
- 了解过去的北极循环,可以了解当前的气候动态.
研究的目的:
- 重建坎帕尼亚-马斯特里希特纪 (约80-66万年前) 期间北冰洋的循环和环境条件.
- 调查古代北极地区深水形成和碳酸盐生产的驱动因素.
- 评估全球事件对北冰洋循环的影响.
主要方法:
- 分析了来自楚克奇大陆架的地震,沉积物和钻探数据.
- 地质特征的年代,包括轮岩漂移和碳酸盐丘.
- 解释古环境指标以推断海洋学条件.
主要成果:
- 发现了大型轮岩漂移和浴碳酸盐堆,可以追溯到坎帕尼亚-马斯特里希特时期.
- 证据表明持续的底流和高生产率,表明一个北极深水质量.
- 由潮混合,上游和海洋无氧事件后的氧气条件支持的土丘发展 3.
结论:
- 晚白时期的北极海洋支持了大量的深水形成和碳酸盐生产.
- 一个充满活力的循环系统,可能受到海冰形成的影响,存在于古代北极.
- 由于全球变化,这个系统在白纪-古纪的边界崩,影响了高度气候动态.
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