4.Evolution of cultivated rice during the neolithic age in the lower Yangtze basin
        Linghua Tang1, Jiaxiang Sun1, Min Zhang2 and Mingchang Li2 1) Jiangsu Academy of Agric. Sciences. Nanjing. 210014 China
2) Institute of Archaeology. Nanjing Museum. Nanjing
    The ancient site of Nongqiu village in Gaoyou town lies on the east bank of the great
canal connecting Beijing and Hangzhou, and 60 km north of the Yangtze river. In 1993-94,
the archaeologists of Nanjing Museum conducted excavation of the ancient site. The soils
deposited over the site were divided into eight layers, and the 4th to 8th were determined to
belong to the new stone (neolithic) age, the 8th being the oldest. From all these layers except
for the 5th, carbonized rice grains and husks were obtained. We measured these ancient
materials and analyzed the data.

    We found that: 1) The carbonized grain differed in size according to layers, as shown in Table 1.
The grain from the 4th layer were significantly longer than those from other layers. They also had
larger mean values of width and thickness. This was due to an addition of large grains to the
population increasing interplant variations.

    The 8th to 4th layers showed at increasing trend of coefficient of variation for grain thickness.
In grain length and width, grains from the 4th layer showed larger variability than those from the
8th layer, although the 6th and 7th layers in the middle had almost the same variability (Table 1).
This suggests that the rice grains in the oldest age were relatively uniform, and variability increased
later, particularly in the latest neolithic age.

2) The dimensions of carbonized grain were compared with those of present local varieties grown
in Nanjing area. In length/width ratio, the ancient rice generally had greater values than the present
varieties. The volume of grain as estimated by (length x width)^ 1/2 and (length X width X thickness)
1/3 was smaller than corresponding values for the present local varieties (Table 2). The grain from
the 4th layer showed comparable values with some of present varieties.
 

Table 1. Mean value, standard d deviation and coefficient of variation for dimensions of carbonized rice excavated at a vestige site of Gaoyou
Layer: 4 6 7 8
Number of grains sampled: 118 48 65 14
.Length           Mean (mm) 5.8 4.6 4.7 4.8
                         S.d. 0.89 0.51 0.58 0.47
                      Coef. variation (%) 11.9 11.1 11.9 9.7
Width                   Mean (mm) 2.6 2.3 2.3 2.2
                               S.d. 0.45 0.30 0.31 0.23
                      Coef. variation (%) 17.9 13.1 13.6 10.2
Thickness           Mean (mm) 1.78 1.65 1.69 1.65
                              S.d. 0.41 0.29 0.23 0.21
                        Coef. variation (%) 23.0 17.6 13.7 12.7

Table 2. Dimensions of carbonized grain as compared with present local varieties
 

L-length W-width T-thickness
Material L/W (L-W)½ (L-W-T) 1/3
Carbonized

grain

4th layer 2.31 3.85 2.97
6th layer 2.03 3.22 2.57
7th layer 2.07 3.29 2.64
8th layer 2.19 3.28 2.61
Present

Local

variety

Ai Huang Zhong 1.94 3.96 3.00
Chang Jing Uu Nuo 1.82 3.78 3.01
Hei Zhong 1.78 3.91 3.06
Huang Zhong 1.96 3.88 2.98
Carbonized 2.07 3.91 2.88

    The silica bodies or plant opals were examined in the soil samples. The beta type
representing the Japonica grains were found in all layers except for the 8th layer (cf. Sato
et al. 1990).

    It may be inferred that with the initiation of rice cultivation, the variability within populations
increased. The development of rice culture was slow in the early stages, but was faster in the
later period, say. 6300 to 5500 years before present. Conscious artificial selection would have
been practiced in this period. According to the shape of plant opal in the ancient site, the earliest
cultivars seem to be of Japonica type.

Reference

Sato, Y. I., H. Fujiwara and T. Udatsu. 1990. Morphological differences in silica body derived
        from motor cells of indica and japonica rice. Japan. J. Breed. 40: 495-504.