桑托里尼火山爆发的放射性碳年代为公元前1627年至1600年
Walter L Friedrich1, Bernd Kromer, Michael Friedrich
1Department of Earth Sciences, University of Aarhus, DK-8000 Aarhus, C.F. Moellers Allé 1120, Denmark. walter@geo.au.dk
概括
桑托里尼橄树的放射性碳波动匹配精确地将米诺伊火山爆发定于公元前1627年至1600年. 这一发现挑战了传统的埃及铜器时代时间表.
科学领域:
- 考古学科学 考古学科学
- 登德罗年代学 登德罗年代学
- 通过放射性碳测年法进行测年.
背景情况:
- 桑托里尼 (Thera) 的米诺伊火山喷发是青铜时代的全球关键标志.
- 这一事件的确切日期对于理解地中海史前史至关重要.
- 以前的约会努力依赖于不那么直接的方法,并产生了不同的结果.
研究的目的:
- 通过使用独特的考古发现,精确地确定圣托里尼米诺火山爆发的日期.
- 为了建立一个可靠的时间标记全球青铜时代.
- 为了协调科学和历史记录之间的不同时间数据.
主要方法:
- 放射性碳波动匹配应用到一系列碳-14测量从树环.
- 对一棵保存极好的橄树的分析,该橄树被发现被火山石埋藏在地.
主要成果:
- 米诺亚火山爆发的年代是公元前1627年至1600年. 有95.4%的概率.
- 这为事件提供了直接和精确的日期.
- 新的日期比埃及年代表所建议的日期早大约一个世纪.
结论:
- 这项研究确定了米诺火山爆发的更准确日期.
- 这一修订的时间表对了解青铜时代历史和相互联系具有重大意义.
- 可能需要进一步的研究,以充分整合这一发现与现有的历史记录.
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