When did prehistoric human beings migrate to the harsh eastern Tibetan Plateau: luminescence and 14C dating results from Qinghai Lake area

2012 ◽  
Vol 279-280 ◽  
pp. 477
Author(s):  
Yongjuan Sun
2020 ◽  
Author(s):  
Naimeng Zhang ◽  
Qinghai Xu ◽  
Dongju Zhang ◽  
Ulrike Herzschuh ◽  
Zhongwei Shen ◽  
...  

<p>Understanding the paleoenvironment (such as climate and landscape) in the area where the early ancient human appears on the Tibetan Plateau is an interesting topic. Based on the results of pollen data on the Yaowuyao loess section of the Qinghai Lake Basin, we used landscape reconstruction algorithms to reconstruct the changes in vegetation cover for 15,000 years. It is shown that the vegetation in the Yaowuyao area changed from temperate steppe (15-7.5 ka) to forest-steppe (7.5-4 ka). Compared with previous studies on the sediment in Qinghai Lake, our study can better reflect the local environment of the Qinghai Lake basin. Furthermore, based on the paleoclimate change data and archeological data from the surrounding areas, it is noticed that while precipitation increases and trees increase, human activities decrease. This may be caused by the substance and strategies of the ancient human beings that have adapted to the steppe. In addition, our results also show that the intensity of ancient human activity has a negative correlation with plant biodiversity, which may be related to human disturbance to the environment. Our paleoecological and environmental study not only shows the paleoenvironment of the early human activities on the Qinghai-Tibet Plateau but also revealed possible early human activity signals.</p>


The Holocene ◽  
2010 ◽  
Vol 21 (2) ◽  
pp. 297-304 ◽  
Author(s):  
Huayu Lu ◽  
Cunfa Zhao ◽  
Joseph Mason ◽  
Shuangwen Yi ◽  
Hua Zhao ◽  
...  

2014 ◽  
Vol 500-501 ◽  
pp. 295-301 ◽  
Author(s):  
Zhenxing Shen ◽  
Junji Cao ◽  
Leiming Zhang ◽  
Zhuzi Zhao ◽  
Jungang Dong ◽  
...  

2021 ◽  
Vol 9 ◽  
Author(s):  
Manping Sun ◽  
Yongjuan Sun ◽  
Haicheng Wei ◽  
Guangliang Hou ◽  
Ji Xianba ◽  
...  

The study of ancient city sites provides valuable evidence for understanding human-land relationships. Qinghai Lake Basin, on the northeastern Tibetan Plateau, was a key location for economic and cultural exchanges between East and West in ancient China and archaeological surveys have identified the remains of many ancient cities. Although there are relatively good historical records for some ancient cities, their absolute ages are still unclear due to a lack of systematic chronological dating. In this study, OSL dating of ceramic and tile remains from three ancient cities in Qinghai Lake Basin, Xihaijun (XHJGC), Beixiangyang (BXYGC), and Fuxi (FSC), was combined with documentary and paleoclimate evidence to investigate historical human-land relationships. Relics from XHJGC and BXYGC were dated to 0–220 AD, in the Han Dynasty, while tiles from FSC were dated to 120–520 AD, largely corresponding to the Wei Jin Southern and Northern Dynasties. Luminescence ages were generally consistent with dates recorded in historical documents, indicating that the OSL method can be reliably used to date buried tiles in ancient cities on the northeastern Tibetan Plateau. Comparing the dates with paleoclimatic records suggests that the warm and humid climate at c. 2 ka was an important driver of immigration to the region that led to the construction of cities in the Qinghai Lake area during the late Western Han Dynasty. During the Wei Jin Southern and Northern Dynasties (220–589 AD), communication between East and the West flourished, and human activities in the area were strong with the continuation of the war in Central China and Hexi Corridor. Fuxi was largely abandoned in the later Wei Jin Southern and Northern Dynasties, although it was still used intermittently until the Ming Dynasty. Pollen records confirm that humans were extensively engaged in agricultural production in the Qinghai Lake area during the Wei Jin Southern and Northern Dynasties.


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