The Hemudu culture (河姆渡文化) (5000 BC to 4500 BC) was a Neolithic culture that flourished just south of the Hangzhou Bay in Jiangnan in modern Yuyao, Zhejiang, China. The site at Hemudu, 22 km north-west of Ningbo, was discovered in 1973. Hemudu sites were also discovered on the islands of Zhoushan.
The Hemudu culture co-existed with the Majiabang culture as two separate and distinct cultures, with cultural transmissions between the two. Two major floods caused the nearby Yaojiang River to change its course and inundated the soil with salt, forcing the people of Hemudu to abandon its settlements. The Hemudu people lived in long, stilt houses.
The Hemudu culture was one of the earliest cultures to cultivate rice. Recent excavations at the Hemudu period site of Tianluoshan has demonstrated rice was undergoing evolutionary changes recognized as domestication. Most of the artifacts discovered at Hemudu consist of animal bones, exemplified by hoes made of shoulder bones used for cultivating rice.
The culture also produced lacquer wood. The remains of various plants, including water caltrop, Nelumbo nucifera, acorns, melon, wild kiwifruit, blackberries, peach, the foxnut or Gorgon euryale and bottle gourd, were found at Hemudu and Tianluoshan. The Hemudu people likely domesticated pigs, and dogs but practiced extensive hunting of deer and some wild water buffalo. Fishing was also carried out on a large scale, with a particular focus on crucian carp. The practices of fishing and hunting are evidenced by the remains of bone harpoons and bows and arrowheads. Music instruments, such as bone whistles and wooden drums, were also found at Hemudu.
The culture produced a thick, porous pottery. The distinct pottery was typically black and made with charcoal powder. Plant and geometric designs were commonly painted onto the pottery; the pottery was sometimes also cord-marked. The culture also produced carved jade ornaments, carved ivory artifacts and small, clay figurines.
Fossilized amoeboids and pollen suggests Hemudu culture emerged and developed in the middle of the Holocene Climatic Optimum. A study of a sea-level highstand in the Ningshao Plain from 7000 – 5000 BP shows that there may have been stabilized lower sea levels at this time followed by, from 5000 to 3900 BP, frequent flooding.
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- Fuller, Dorian Q, Ling Qin, Yunfei Zheng, Zhijun Zhao, Xugao Chen, Leo Aoi Hosoya, and Guo-ping Sun (2009) "The Domestication Process and Domestication Rate in Rice: Spikelet bases from the Lower Yangtze". Science 323: 1607–1610 doi:10.1126/science.1166605
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