概括
怀俄明州米奥森晚期湖泊沉积物的花粉分析揭示了类似于现代的植物群和交替的潮湿/干燥气候. 这种高分辨率记录显示了气候变化,类似于三叠纪晚期和四叠纪晚期的海洋记录.
科学领域:
- 古植物学是古植物学.
- 气候科学 气候科学
- 在平流图学中,平流图学.
背景情况:
- 陆地三级沉积物往往缺乏植物和气候历史的高时间分辨率.
- 湖层提供了详细的古老环境重建的潜力.
研究的目的:
- 通过花粉层学分析中新世纪晚期的植被和气候历史.
- 为了实现比以前报告的陆地三级沉积物更高的时间分辨率.
主要方法:
- 来自怀俄明州杰克逊霍尔的Teewinot形成的湖层的花粉分析.
- 晚期米奥森期沉积物的平流图分析.
主要成果:
- 发现的植物基本上是现代的.
- 六个连续的花粉组合表明交替干燥和潮湿的气候条件.
- 气候变化的频率与海洋同位素记录相当.
结论:
- 来自湖泊沉积物的花粉层学提供了对米奥森晚期植被和气候的高分辨率洞察力.
- 末期米奥森时期经历了频繁的气候波动,类似于后来的地质时期.
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