西藏高原中期的丹尼索瓦人下
Fahu Chen1,2, Frido Welker3,4,5, Chuan-Chou Shen6,7
1Key Laboratory of Alpine Ecology (LAE), CAS Center for Excellence in Tibetan Plateau Earth Sciences and Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China. fhchen@itpcas.ac.cn.
Nature
|May 3, 2019
概括
在西藏高原发现的丹尼索瓦下提供了西伯利亚以外古人类的直接证据. 这种化石揭示了丹尼索瓦人在16万年前适应了高海拔.
科学领域:
- 古人类学
- 古代DNA分析
- 人类的进化
背景情况:
- 丹尼索瓦人是从西伯利亚的有限化石和亚洲种群的遗传证据中知道的.
- 形态上不同的丹尼索瓦化石很少,阻碍了对它们的地理范围和进化关系的理解.
- 丹尼索瓦基因与现代人类的高海拔适应性有关.
研究的目的:
- 在阿尔泰山脉以外的丹尼索瓦化石的鉴定和描述.
- 调查丹尼索瓦人适应高海拔环境.
- 了解西藏高原早期人类的存在.
主要方法:
- 古代蛋白质分析以识别人类物种.
- 一个碳酸盐矩阵的U系列约会来确定化石的年龄.
- 下和牙形态的分析.
主要成果:
- 一个丹尼索瓦下被发现在西藏高原的岩洞.
- 这个下至少可以追溯到16万年前.
- 该标本提供了关于丹尼索瓦人形态的见解, 以及他们在中纪的高海拔地区的存在.
结论:
- 古代人类,包括丹尼索瓦人,在中纪居住在西藏高原.
- 在现代人类到达该地区很久之前, 丹尼索瓦人已经适应了高海拔的低氧环境.
- 这一发现扩大了丹尼索瓦人已知的地理范围及其适应能力.
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