U-Pb日期的流石限制了南非早期人类记录的干旱气候阶段
Robyn Pickering1,2, Andy I R Herries3,4, Jon D Woodhead5
1Department of Geological Sciences, University of Cape Town, Cape Town, South Africa. robyn.pickering@uct.ac.za.
Nature
|November 23, 2018
概括
南非的流石
科学领域:
- 古人类学
- 地质时间学
- 古气候学
背景情况:
- 人类摇篮的化石记录对于理解人类进化至关重要.
- 这一地区的原始人化石的年代是具有挑战性的, 阻碍了进化研究.
- 流石提供了一个可靠的年代表方法.
研究的目的:
- 为了建立一个可靠的时间表, 在人类的摇篮.
- 将化石保存与古环境条件联系起来.
- 在南非重建过去的气候变化.
主要方法:
- 来自八个洞穴的流石层的- (U-Pb) 年龄测定.
- 核密度估计将29个U-Pb年龄组合到成长间隔记录中.
- 解释流石生长为湿阶段和化石沉积为干燥阶段.
主要成果:
- 流石可以追溯到320万至130万年前的六个不同的时间间隔.
- 确定了主要的潮湿阶段 (流石生长) 和干燥阶段 (化石积累).
- 化石的保存仅限于干燥的时间间隔,
结论:
- 流石U-Pb测年为人类的摇篮提供了坚实的时间表.
- 人类化石记录倾向于干旱时期, 影响我们对它们进化的理解.
- 流石提供了对过去非洲气候变化及其对人类息地的洞察力.
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