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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.
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.
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. Today, this haplogroup is found in northern Han, Mongols, Manchu, Oroqen, Xibe and Hezhe at low frequencies. Other paternal haplogroups identified in the study were C and O3a (O3a3), both of which predominate among the present-day inhabitants of the region.
Nelson et al. 2020 attempts to link the Hongshan culture to a "Transeurasian" (Altaic) linguistic context. According to a study on genetic distance measurements from a large scale genetic study from 2021 titled 'Genomic insights into the formation of human populations in East Asia', hunter-gatherers of Mongolia and the Amur River Basin have ancestry shared by Mongolic and Tungusic language speakers, but they did not carry West Liao River farmer ancestry, contradicting the Transeurasian hypothesis proposed by Martine Robbeets et al. that the expansion of West Liao River farmers spread these proto-languages.
A 2020 study discovered substantial genetic changes in the West Liao River region over time. An increase in the reliance on millet farming between the Middle-to-Late Neolithic is associated with higher genetic affinity to the Yellow River basin (generally associated with speakers of the Sino-Tibetan languages), while a partial switch to pastoralism in the Bronze Age Upper Xiajiadian culture is associated with a decrease in this genetic affinity. After the Late Neolithic, there was a sharp transition from Yellow River to Amur River-related genetic profiles (generally associated with speakers of Tungusic languages) around the West Liao River. This increase in Amur River affinity corresponds with the transition to a pastoral economy during the Bronze Age.
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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.
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.
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. Today, this haplogroup is found in northern Han, Mongols, Manchu, Oroqen, Xibe and Hezhe at low frequencies. Other paternal haplogroups identified in the study were C and O3a (O3a3), both of which predominate among the present-day inhabitants of the region.
Nelson et al. 2020 attempts to link the Hongshan culture to a "Transeurasian" (Altaic) linguistic context. According to a study on genetic distance measurements from a large scale genetic study from 2021 titled 'Genomic insights into the formation of human populations in East Asia', hunter-gatherers of Mongolia and the Amur River Basin have ancestry shared by Mongolic and Tungusic language speakers, but they did not carry West Liao River farmer ancestry, contradicting the Transeurasian hypothesis proposed by Martine Robbeets et al. that the expansion of West Liao River farmers spread these proto-languages.
A 2020 study discovered substantial genetic changes in the West Liao River region over time. An increase in the reliance on millet farming between the Middle-to-Late Neolithic is associated with higher genetic affinity to the Yellow River basin (generally associated with speakers of the Sino-Tibetan languages), while a partial switch to pastoralism in the Bronze Age Upper Xiajiadian culture is associated with a decrease in this genetic affinity. After the Late Neolithic, there was a sharp transition from Yellow River to Amur River-related genetic profiles (generally associated with speakers of Tungusic languages) around the West Liao River. This increase in Amur River affinity corresponds with the transition to a pastoral economy during the Bronze Age.