人类学学报 ›› 2022, Vol. 41 ›› Issue (03): 514-522.doi: 10.16359/j.1000-3193/AAS.2021.0055cstr: 32091.14.j.1000-3193/AAS.2021.0055
收稿日期:
2020-12-11
修回日期:
2021-04-15
出版日期:
2022-06-15
发布日期:
2022-06-16
作者简介:
李文成,博士,主要从事旧石器时代考古学研究。Email: 基金资助:
Received:
2020-12-11
Revised:
2021-04-15
Online:
2022-06-15
Published:
2022-06-16
摘要:
盘状石核以两面交互打击、向心剥片为主要特征,在中国旧石器文化发展中具有重要地位。本文针对华北石片石器中盘状石核与非定型石核长期共存这一文化现象,展开剥片实验,分析了这两种剥片策略所获得的石片之间的差异。研究发现,石片的台面类型、背面片疤方向、保留石核台面边缘特征石片比例这三个指标可以有效区分这两种剥片策略,石片的技术分析对于理解华北石片石器工业的剥片策略同样具有重要价值。
中图分类号:
李文成. 盘状石核剥片实验及对华北石片石器研究的启示[J]. 人类学学报, 2022, 41(03): 514-522.
LI Wencheng. Experimental analysis on flaking of discoidal cores and its application in understanding the flake tool industry in North China[J]. Acta Anthropologica Sinica, 2022, 41(03): 514-522.
类型Type | 编号No. | 毛坯 Blank | 石核 Core | 剥片数量 n of flaking | ||||
---|---|---|---|---|---|---|---|---|
长L(mm) | 宽b(mm) | 厚d(mm) | 长L(mm) | 宽b(mm) | 厚d(mm) | |||
盘状石核Discoidal core | 19XLL:3 | 72 | 95.6 | 47.4 | 20.5 | 50.4 | 37 | 20 |
19XLL:5 | 116.4 | 141.7 | 56.8 | 26.2 | 51.5 | 42.1 | 36 | |
19XLL:6 | 76.4 | 90.9 | 32.3 | 22.4 | 43.6 | 38 | 24 | |
19XLL:7 | 96.4 | 142.3 | 44.7 | 39.7 | 70.3 | 64.6 | 19 | |
19XLL:8 | 58.6 | 91.8 | 40.1 | 31 | 50.7 | 44.8 | 18 | |
非定型石核剥片Amorphous core | 19XLL:9 | 72.2 | 83.4 | 52 | 47 | 55.3 | 31.8 | 13 |
19XLL:10 | 87.6 | 93.5 | 50.9 | 28 | 50.9 | 34.4 | 27 | |
19XLL:11 | 94.8 | 107.9 | 45.4 | 89.7 | 55.7 | 41.8 | 23 | |
19XLL:12 | 52.8 | 82.7 | 26.9 | 40.1 | 44.5 | 21 | 15 | |
19XLL:13 | 88.8 | 134 | 43.4 | 67 | 71.8 | 49.9 | 32 |
表1 实验标本剥片前后尺寸对比
Tab. 1 Dimensions of blanks and cores in experimental study
类型Type | 编号No. | 毛坯 Blank | 石核 Core | 剥片数量 n of flaking | ||||
---|---|---|---|---|---|---|---|---|
长L(mm) | 宽b(mm) | 厚d(mm) | 长L(mm) | 宽b(mm) | 厚d(mm) | |||
盘状石核Discoidal core | 19XLL:3 | 72 | 95.6 | 47.4 | 20.5 | 50.4 | 37 | 20 |
19XLL:5 | 116.4 | 141.7 | 56.8 | 26.2 | 51.5 | 42.1 | 36 | |
19XLL:6 | 76.4 | 90.9 | 32.3 | 22.4 | 43.6 | 38 | 24 | |
19XLL:7 | 96.4 | 142.3 | 44.7 | 39.7 | 70.3 | 64.6 | 19 | |
19XLL:8 | 58.6 | 91.8 | 40.1 | 31 | 50.7 | 44.8 | 18 | |
非定型石核剥片Amorphous core | 19XLL:9 | 72.2 | 83.4 | 52 | 47 | 55.3 | 31.8 | 13 |
19XLL:10 | 87.6 | 93.5 | 50.9 | 28 | 50.9 | 34.4 | 27 | |
19XLL:11 | 94.8 | 107.9 | 45.4 | 89.7 | 55.7 | 41.8 | 23 | |
19XLL:12 | 52.8 | 82.7 | 26.9 | 40.1 | 44.5 | 21 | 15 | |
19XLL:13 | 88.8 | 134 | 43.4 | 67 | 71.8 | 49.9 | 32 |
图1 标本19XLL:5不同剥片阶段形态变化 a.毛坯形态Morphology of the blank;b.成功剥取20件完整石片后石核形态Morphology of the core after 20 flake removals;c.成功剥取36件完整石片后剥片行为终止时石核形态Morphology of the core at the end of reduction, 36 flakes removals
Fig. 1 Morphological change of 19XLL:5 in different reductional stages
台面类型Type of platform | 盘状 Discoidal | 非定型 Amorphous | ||
---|---|---|---|---|
数量n | 百分比% | 数量n | 百分比% | |
自然面Cortical | 4 | 3.4% | 0 | 0 |
自然面+石片疤Cortical + Scar | 5 | 4.3% | 0 | 0 |
素台面Plain | 39 | 33.3% | 94 | 85.5% |
节理面+石片疤Joint surface + Scar | 2 | 1.7% | 0 | 0 |
有疤(≥2个片疤)Dihedral + Faceted | 44 | 37.6% | 10 | 9.1% |
线状Linear | 6 | 5.1% | 3 | 2.7% |
点状Punctiform | 12 | 10.3% | 3 | 2.7% |
脊状Ridge | 5 | 4.3% | 0 | 0 |
总计Total | 117 | 100% | 110 | 100% |
表2 盘状石核与非定型石核石片台面性质
Tab. 2 Platform type of flakes produced by discoidal and amorphous cores
台面类型Type of platform | 盘状 Discoidal | 非定型 Amorphous | ||
---|---|---|---|---|
数量n | 百分比% | 数量n | 百分比% | |
自然面Cortical | 4 | 3.4% | 0 | 0 |
自然面+石片疤Cortical + Scar | 5 | 4.3% | 0 | 0 |
素台面Plain | 39 | 33.3% | 94 | 85.5% |
节理面+石片疤Joint surface + Scar | 2 | 1.7% | 0 | 0 |
有疤(≥2个片疤)Dihedral + Faceted | 44 | 37.6% | 10 | 9.1% |
线状Linear | 6 | 5.1% | 3 | 2.7% |
点状Punctiform | 12 | 10.3% | 3 | 2.7% |
脊状Ridge | 5 | 4.3% | 0 | 0 |
总计Total | 117 | 100% | 110 | 100% |
图4 保留石核台面边缘特征的石片 a. A类Type A;b. B1类Type B1;c. B2类Type B2;d. C类Type C其中灰色箭头指示打击方向与打击点位置Grey arrows show the striking direction and location of striking point
Fig. 4 Different types of flakes retaining the edge of the core’s platform
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