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.