Genetic stability in the lower Yangtze River basin from Song to Qing Dynasty
He HPapers in this archive, Kong XPapers in this archive, Tao LPapers in this archive, Zhu LPapers in this archive, Wang XPapers in this archive, Xu MPapers in this archive, Chen YPapers in this archive, Zhu KPapers in this archive, Xu YPapers in this archive, Chen HPapers in this archive, Ma HPapers in this archive, Wang RPapers in this archive, Yang XPapers in this archive, Bai TPapers in this archive, Guo JPapers in this archive, Yang YPapers in this archive, Jia XPapers in this archive, Wang CCPapers in this archive
Abstract
Background The lower Yangtze River basin holds a pivotal role in Chinese history. As previous genetic research in this region has primarily focused on modern population datasets, the limited availability of ancient human genomes has hindered our capacity to reconstruct detailed ancient population histories and evaluate the genetic impact of Yellow River-related groups. Results Here, we present the first set of ancient human genomes from the lower Yangtze River basin, comprising eight individuals from the Song to Qing Dynasties (960–1921 CE). We observed a high degree of genetic homogeneity in most samples, suggesting long-term regional genetic stability. Seven individuals were estimated to derive 69.3–100% of their ancestry from ancient Yellow River-related populations, while the remainder can be attributed to a southern East Asian substrate. Contemporary Han Chinese residing in the lower Yangtze basin can be modelled as direct genetic descendants of historical individuals from this area. Notably, one Qing Dynasty sample reveals a genetic link to the Eastern Mediterranean. Conclusions Our findings illustrate enduring genetic continuity in the lower Yangtze River basin throughout historical times. These findings underscore the region’s role as a genetic bridge between northern and southern East Asia, retaining local rice-farming ancestry while being shaped by southward expansions of Yellow River-related ancestry. Supplementary Information The online version contains supplementary material available at 10.1186/s12915-025-02343-3.
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