来自肥沃新月的洞穴记录,涵盖了最后一次降冰,更好地将新石化纳入了背景
Eleonora Regattieri1, Luca Forti2, Russell N Drysdale3
1Istituto di Geoscienze e Georisorse, Pisa 56124, Italy.
概括
这项研究揭示了伊拉克气候的变化.
科学领域:
- 古气候学 古气候学
- 考古学的考古学
- 四分学科学 四分学科学
背景情况:
- 肥沃的新月 (FC) 经历了显著的气候变化在Epipaleolithic-Neolithic过渡期间.
- 了解区域古气候对于对早期人类社会发展的理解至关重要.
研究的目的:
- 从伊拉克库尔德斯坦地区重建高分辨率的古气候.
- 为了将当地水气候变化与格陵兰的温度变化相关联.
- 调查气候在整个FC塑造新石化模式中的作用.
主要方法:
- 多个proxy speleothem分析 (碳和氧同位素,微量元素,同位素).
- 洞穴纪录的高分辨率约会.
- 与区域古气候和考古学数据进行比较.
主要成果:
- 从18.0到7.5卡的详细洞穴记录显示了与格陵兰岛温度相关的降水变化.
- 在Bølling-Allerød (BA) 期间,降雨量增加和水气候变化发生.
- 较年轻的干旱 (YD) 时期的特点是更干燥和更有尘埃的条件,区域差异很大.
结论:
- 伊拉克的当地降雨量与格陵兰岛的温度变化非常相似.
- 在FC经历了大致相似的降水模式,但在BA和YD期间有明显的水气候变化.
- 古老环境记录为了解气候对新石化多样性的影响提供了一个模板.
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