在撒哈拉的气候控制的全新世纪占领:非洲进化的引擎
Rudolph Kuper1, Stefan Kröpelin
1Collaborative Research Center 389 (ACACIA), University of Cologne, Institute of Prehistoric Archaeology, Africa Research Unit, Jennerstrasse 8, 50823 Köln, Germany.
概括
史前撒哈拉地区的人口在潮湿时期壮成长,随着气候在12000多年内干燥而迁徙. 这些气候变化影响了早期的非洲文明和牧民.
科学领域:
- 古气候学 古气候学
- 考古学的考古学
- 非洲史前史 非洲史前史
背景情况:
- 研究气候变化和东撒哈拉人类定居点之间的关系.
- 利用来自埃及,苏丹,利比亚和得的150个考古遗址的放射性碳测年方法.
- 分析了12000年的史前占领模式.
研究的目的:
- 调查气候变化和东撒哈拉史前人类定居点之间的关系.
- 重建人类占领和流亡的时间表,以应对过去12千年气候变化.
主要方法:
- 来自埃及,苏丹,利比亚和得150个考古发掘的放射性碳数据的分析.
- 利用主要时间段的综合多指标视图来分析气候占用动态.
主要成果:
- 在过去的12,000年里,在气候变化和史前占领模式之间建立了密切的联系.
- 在公元前8500年左右的潮湿条件下,有记录的初始定居点. 在公元前5300年以后,由于干旱而导致的流离失所.
- 证明了沙漠边缘在气候变化影响下向南移动.
结论:
- 撒哈拉的气候变化是史前人类迁徙和定居模式的主要驱动因素.
- 这些气候驱动的迁徙影响了法老文明的出现和牧民在非洲的传播.
- 撒哈拉气候动态的长期影响继续影响撒哈拉以南非洲.
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