在最后一次除冰期期间,北大西洋西部的放射性碳变化
Laura F Robinson1, Jess F Adkins, Lloyd D Keigwin
1California Institute of Technology, MS 100-23, 1200 East California Boulevard, Pasadena, CA 91125, USA. laurar@gps.caltech.edu
概括
深海珊瑚的放射性碳记录显示,脱冰过程中水柱发生了显著的变化,影响了大气中的放射性碳水平. 这些发现支持双极摇摆模型,并将深海变化与极地气候变化联系起来.
科学领域:
- 古海洋学是古海洋学.
- 海洋地球化学 海洋地球化学
- 气候科学 气候科学
背景情况:
- 了解过去的海洋循环及其对全球气候的影响至关重要.
- 放射性碳 (14C) 是海洋循环和年龄的关键标记物.
- 深海珊瑚和类珊瑚提供了关于过去海洋条件的宝贵档案.
研究的目的:
- 重建一个详细的放射性碳的历史在深西北大西洋从冰川到全新世时期.
- 研究海洋放射性碳变化,脱冰和大气放射性碳水平之间的关系.
- 用深海古气候记录来测试双极摇摆假说.
主要方法:
- 在深海珊瑚中分析放射性碳.
- 对地和浮游生物相结合的地和浮游生物分析.
- 放射性碳年代测定技术.
主要成果:
- 降冰的特点是放射性碳丰富和贫水之间的转移,造成了大量的水柱梯度.
- 深海放射性碳的变化影响了大气中的放射性碳水平.
- 深海记录支持双极摇摆模型,将北半球变暖与北源深水形成的增加联系起来.
- 在中间/深海中频繁的放射性碳变化与极点的同步变化相关.
结论:
- 深海放射性碳记录为过去的海洋循环动态及其远程连接提供了关键的见解.
- 这项研究加强了深海过程在过渡期间调节全球气候的重要性.
- 有证据支持一种对极地气候动态敏感的海洋-大气系统.
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