Hongshan culture

The Hongshan culture (simplified Chinese: 红山文化; traditional Chinese: 紅山文化; pinyin: Hóngshān wénhuà) was a Neolithic culture in the West Liao river basin in northeast China. Hongshan sites have been found in an area stretching from Inner Mongolia to Liaoning, and dated from about 4700 to 2900 BC.

The culture is named after Hongshanhou (simplified Chinese: 红山后; traditional Chinese: 紅山後; pinyin: Hóngshān hòu), a site in Hongshan District, Chifeng. The Hongshanhou site was discovered by the Japanese archaeologist Torii Ryūzō in 1908 and extensively excavated in 1935 by Kōsaku Hamada and Mizuno Seiichi.

Historical context

In northeast China, Hongshan culture was preceded by Xinglongwa culture (6200–5400 BC), Xinle culture (5300–4800 BC), and Zhaobaogou culture, which may be contemporary with Xinle and a little later.

The Yangshao culture of the Yellow River existed contemporaneously with the Hongshan culture (see map). These two cultures interacted with each other.

Hongshan culture was succeeded by the Lower Xiajiadian culture (2200–1600 BC), which was replaced by a different Upper Xiajiadian culture (1000-600 BC) with a shift from farming to pastoral nomadism, likely due to climate change. In the historical period, the West Liao basin was mainly populated by nomads.

Genetics and linguistic identity

A genetic study by Yinqiu Cui et al. from 2013 analyzed the Y-chromosome DNA haplogroup based N subclade; it found that DNA samples from 63% of the combined samples from various Hongshan archaeological sites belonged to the subclade N1 (xN1a, N1c) of the paternal haplogroup N-M231 and calculated N to have been the predominant haplogroup in the region in the Neolithic period at 89%, with its share gradually declining over time.