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持续的北大西洋变暖导致异常强烈的MIS 11c冰川间时期
Hsun-Ming Hu1,2,3, Gianluca Marino4, Carlos Pérez-Mejías5
1High-Precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University, Taipei, 10617, ROC, Taiwan. hsunming.hu@gmail.com.
Nature communications
|July 15, 2024
概括
海洋同位素阶段11c显示了强烈的气候变化,尽管太阳的强迫力很弱. 这项研究使用了洞穴动物数据,揭示了一个延迟的全球峰值间冰期,由极向热传输驱动.
科学领域:
- 古气候学 古气候学
- 气候科学 气候科学
- 地质时间学 (Geochronology)
背景情况:
- 海洋同位素阶段 (MIS) 11c 间冰川及其冰川终点表现出气候对弱阳光强迫的强烈反应.
- 缺乏放射年龄控制,这阻碍了在这一时期对阳光照射与气候关系的评估.
研究的目的:
- 为MIS 11c期提供新的放射年龄控制.
- 评估MIS 11c.期间的阳光照射-气候关系.
- 为了比较意大利和北大西洋地区的古气候记录.
主要方法:
- - (230Th) 约会来自意大利北部的洞穴.
- 与北大西洋地区现有的古气候记录进行比较.
主要成果:
- 间冰期条件开始于亚热带到中度的423.1 ± 1.3万年前 (kyr BP) 在一个弱的阳光照射最大期间.
- 北方高度地区仍然被冰川覆盖,海平面比现在低约40米.
- 在亚热带开始后,尽管阳光强迫力较弱,但在全球范围内达到了14.5 ± 2.8 kyr的峰值间冰期条件,海平面比现在高6-13米.
结论:
- 在MIS 11c期间的强烈气候反应归因于长期 (~15 kyr) 的极向热流传输.
- 这一发现为太阳化强迫和地球气候系统在冰川间时期之间的复杂相互作用提供了关键的见解.
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