在美国西南部的晚期Holocene气候和文化变化
1Department of Earth and Planetary Sciences, University of New Mexico, 200 Yale Boulevard, Albuquerque, NM 87131, USA. polyak@unm.edu
概括
来自瓜达卢佩山脉石岩的4000年气候记录显示,美国西南部有明显的潮湿和干旱时期. 这些气候变化与土著人民的文化活动和定居模式的变化有关.
科学领域:
- 古气候学 古气候学
- 四季地质地质学四季地质地质学
- 美国西南部气候历史
背景情况:
- 柱状石提供了过去气候条件的年度解决档案.
- 美国西南部的晚期Holocene气候尚未完全理解.
- 了解过去的气候变化对于解释生态和文化变化至关重要.
研究的目的:
- 为了重建美国西南部每年解决的4000年的气候历史.
- 为了将古气候数据与土著人民的考古记录联系起来.
- 调查气候变化对人类定居点和文化活动的影响.
主要方法:
- 来自瓜达卢佩山脉的柱状岩的分析.
- 使用年度带和间歇时间来进行时间分辨.
- 高精度的系列测年法用于准确的年龄限制.
主要成果:
- 从4000年前到3000年前,在一个更干燥的中期全新纪之后,存在着与今天类似的气候.
- 一个较冷,较潮湿的时期发生在3000年至800年前.
- 恢复了与今天相似的条件,短暂的湿间隔从440年到290年前.
结论:
- 斯塔拉格米特气候重建提供了美国西南部气候变化的详细历史.
- 重建的气候历史显示,与土著文化活动的转变有很强的相关性.
- 气候变化可能影响了该地区的住房废弃和人口重新分配.
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