Table 1. Shizitan 29, layer 8 and 7: The lithic sample.
Layers | Raw material | Cores | Blades | Flakes | Other | Total | Sampling regime |
---|---|---|---|---|---|---|---|
7 Top | BF | 33 | 106 | 77 | 16 | 232 | All cores and all retouched flakes. All blades, and all recorded flakes from the selected area |
RF | 27 | 112 | 57 | 7 | 203 | ||
Q | 7 | 2 | 39 | 5 | 53 | ||
O | 0 | 10 | 2 | 4 | 16 | ||
67 | 230 | 175 | 32 | 504 | |||
7 Base | BF | 9 | 0 | 43 | 6 | 58 | Entire collection from the selected area |
RF | 1 | 1 | 10 | 3 | 15 | ||
Q | 3 | 0 | 45 | 6 | 54 | ||
O | 0 | 0 | 3 | 1 | 4 | ||
13 | 1 | 101 | 16 | 131 | |||
8 | BF | 9 | 0 | 60 | 13 | 82 | Entire collection |
RF | 2 | 0 | 5 | 1 | 8 | ||
Q | 3 | 0 | 32 | 5 | 40 | ||
O | 0 | 0 | 1 | 0 | 1 | ||
14 | 0 | 98 | 19 | 131 | |||
Total | 142 | 287 | 473 | 82 | 984 |
Quantitative data for the lithics from the three analyzed stratigraphic units from Shizitan 29, Layer 8, and 7 (Base and Top), and their sampling regimes: (BF) Black flint; (RF) River flint; (Q) quartz/quartzite; (O) other materials). The blade fragment found within layer 7 Base probably resulted from a limited post-depositional process repositioning it.