Rice Domesticated 10,000 Years Ago

Phytoliths can occlude some organic carbon during their deposition, which is captured through photosynthesis from atmospheric CO2 during plant growth. Carbon occluded in phytoliths can thus directly reflect the age of organic sources exploited by humans. Under the guidance of Prof. LU Houyuan, Post-doctoral Researcher ZUO Xinxin carried out phytolith carbon-14 studies on three archaeological sites associated with Shangshan culture. The results show that the phytolith dates are consistent with their paired charcoal or seed dates.

Two phytoliths dating from the early (upper layer of the eighth cultural stratum) and late stages (upper layer of the fifth cultural stratum) of the site range from 9,417-9,134 calibrated years before the present (“cal yr BP”) to 8,175-8,012 cal yr BP. This suggests that the initial occupation of Shangshan may have occurred around 9,400 cal yr BP, or perhaps somewhat earlier, i.e., around 10,000 cal yr BP, since the phytolith sample SH-8 is derived from between the seventh and eighth cultural strata of the site.

Detailed studies of the rice’s bulliform phytolith morphological characteristics show that approximately 36 percent had more than nine fish scales in the early occupation stages of Shangshan and Hehuashan (ca. 10,000 to 9000 cal yr BP), less than the approximately 60 percent counted from the late stages of Hehuashan and Huxi (ca. 9000-8500 cal yr BP).

However, there was a significantly larger amount of rice bulliforms, with more than nine fish scales in the early stages, compared to modern wild rice (17.5 ± 8.3 percent), thus suggesting that the process of rice domestication had begun at this site during the beginning of the Holocene.

Image by Lu Houyuan

Such an age for the origin of rice cultivation and domestication would agree with the parallel roots of agriculture in other regions of the world, during a period of profound environmental change when the Pleistocene was transitioning into the Holocene. In East Asia, a significant strengthening monsoon at about 9500 yr BP is consistent with the initial occupation of Shangshan. Climatic amelioration during these transitional periods may thus serve as a key factor in the early process of rice domestication.

This research was performed in collaboration with the Zhejiang Provincial Institute of Relics and Archaeology and the Institute of Geographic Sciences and Natural Resources Research of the Chinese Academy of Sciences.

This work was funded jointly by the 973 Program, the National Natural Science Foundation of China, and the China Postdoctoral Science Foundation.

Lu Houyuan

Citation: Dating rice remains through phytolith carbon-14 study reveals domestication at the beginning of the Holocene