莱切尔火山爆发的确切时间与年轻的德里亚斯同步
Frederick Reinig1, Lukas Wacker2, Olaf Jöris3,4,5
1Department of Geography, Johannes Gutenberg University, Mainz, Germany. reinig@geo.uni-mainz.de.
Nature
|July 1, 2021
概括
拉切尔海喷发 (LSE) 发生的时间比以前想象的要早一个世纪,可追溯到公元前13006年±9年. 这一修订的时间将年轻的干旱开始转移到12807±12年以后.
科学领域:
- 火山学
- 古气候学
- 地质时间学
背景情况:
- 拉切尔湖喷发 (LSE) 是欧洲上流纪的一次重大火山事件.
- 来自LSE的特弗拉沉积物对于同步古气候档案至关重要,但其确切年龄尚不确定.
- 之前对LSE年龄的估计缺乏准确性,影响了气候事件的时间表.
研究的目的:
- 准确地确定使用树枝年代和放射性碳方法的Laacher See喷发的年龄.
- 重新评估与LSE相关的年轻干旱的时间.
- 研究LSE,北大西洋气候和海洋循环之间的关系.
主要方法:
- 在LSE火沉积物中埋藏的亚化石树木的 dendrochronological分析.
- 这些亚化石树的放射性碳测年.
- 修订后的LSE时间表与欧洲湖记录和格陵兰冰芯数据的比较.
主要成果:
- 在LSE的日期是13006±9年 BP,比以前接受的早一个世纪.
- 年轻的Dryas的开始被修改为12807±12年 BP.
- 经过修订的时间表同步了整个北大西洋-欧洲地区的年轻德里亚斯开始.
结论:
- 格陵兰风暴并没有直接引发年轻的干旱 (格陵兰 Stadial-1).
- 一个共同的机制,在变暖的条件下,大西洋南部翻转循环的减弱,影响了这两种事件.
- 这项研究为后期冰河到早期全新纪的过渡提供了更强大的时间框架.
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