在由气候变化和碳酸盐埋葬调节的橄世 - 苗世碳循环中的奇心节奏
Fenghao Liu1, Enqing Huang1, Jinlong Du1
1State Key Laboratory of Marine Geology, Tongji University, Shanghai, China.
Science advances
|January 30, 2026
概括
地球的纪冰河时代在海洋同位素和冰体积上发生了同步变化. 新的研究揭示了轨道周期如何影响海洋碳酸盐化学和埋葬,影响全球碳循环.
科学领域:
- 古海洋学是古海洋学.
- 气候科学 气候科学
- 地质化学 地质化学
背景情况:
- 凯诺时代的冰河时代在轨道时间尺度上出现了同步的谷氧和碳同位素转移.
- 推动海洋温度,冰体积和碳循环之间的这种关系的基本机制仍然不完全理解.
研究的目的:
- 为了研究链接轨道循环的机制,海洋碳酸盐化学,和碳循环动态在米奥生时期.
- 重建深海碳酸盐离子和度的高分辨率记录及其与气候代理的关系.
主要方法:
- 高分辨率的重建本土形基和的比率.
- 在本土藻中分析氧气和碳同位素.
- 整合气候模型模拟.
主要成果:
- 深海碳酸盐离子和的偏心波动与同位素记录和海底碳酸盐沉积相关.
- 轨道强迫和离心率最大的温暖放大了季风降雨和化学气候变化.
- 碳和性的陆地到海运输增加导致碳酸盐埋葬的重新分配,从深盆地到货架.
结论:
- 轨道配置和温度影响低度水文循环,影响海洋碳酸盐化学.
- 碳酸盐埋葬的重新分配显著影响了海水碳酸盐离子度和碳同位素.
- 低度的水文循环在温暖的气候下,在调节碳循环方面发挥着至关重要的作用.
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