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热带太平洋的1200万年温度历史
Yi Ge Zhang1, Mark Pagani, Zhonghui Liu
1Department of Geology and Geophysics, Yale University, New Haven, CT 06511, USA.
概括
在300万年前之前永久的厄尔尼诺状况没有得到新的海面温度 (SST) 数据的支持. 我们的发现揭示了1200万年前更温暖的太平洋暖池,挑战了之前的气候重建.
科学领域:
- 古代海洋学 古代海洋学 古代海洋学
- 气候科学 气候科学
- 海洋地球化学 海洋地球化学
背景情况:
- 以前的研究表明,永久的厄尔尼诺状况存在于300万年前.
- 这些结论是基于有限的海面温度 (SST) 记录,这些记录可能会受到调节和校准问题的影响.
研究的目的:
- 为了重建更可靠的SST记录从太平洋.
- 重新评估新生代中是否存在永久的类似厄尔尼诺现象的情况.
主要方法:
- 建立了新的基于生物标志物的SST记录.
- 分析了太平洋温暖池和冷舌温的变化.
- 随着时间的推移量化的赤道区域温度梯度.
主要成果:
- 太平洋温暖的水池在1200万年前比现在大约4°C温暖.
- 温暖的水池和冷的舌头都逐渐冷却到现代温度.
- 稳定的区域温度梯度为~3°C,在米奥森晚期保持稳定,在普利奥-普莱斯托时代增加.
结论:
- 这些发现与之前的重建相矛盾,这表明永久的厄尔尼诺状况.
- 新一代太平洋气候逐渐演变,不以不变的厄尔尼诺状况为特征.
- 新的SST数据提供了对过去太平洋气候动态的更准确的了解.
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