人类学学报 ›› 2019, Vol. 38 ›› Issue (01): 1-18.doi: 10.16359/j.cnki.cn11-1963/q.2019.0010
• • 下一篇
收稿日期:
2018-09-20
修回日期:
2018-11-12
出版日期:
2019-02-15
发布日期:
2020-09-11
作者简介:
裴树文(1968-),男,河南兰考县人,研究员,主要从事旧石器时代考古学研究。E-mail: 基金资助:
Received:
2018-09-20
Revised:
2018-11-12
Online:
2019-02-15
Published:
2020-09-11
摘要:
遗址形成过程(或成因)研究是以地质考古学的研究手段为出发点,解读古人类遗址的形成和埋藏过程,其研究结果对正确解读遗址完整性和早期人类生存行为具有重要意义。该研究方向在中国尚未引起足够重视,这在一定程度上降低了我国古人类学和旧石器时代考古学学术研究的国际影响力。鉴于旷野遗址在保存早期人类化石及遗物方面的特殊地位,本文以地质考古学为出发点,系统分析有关旷野遗址形成过程研究所涉及的科学问题,对Glynn Isaac在东非创立的一套系统解读旷野遗址形成过程研究所涉及的指标进行梳理。此外,作者以古人类活动遗物的埋藏和空间分布特征为切入点,详细介绍目前从事旷野遗址成因研究所涉及的关键指标及学术意义,并对中国境内有关遗址成因研究以及旷野遗址形成过程研究的历史与现状进行讨论。
中图分类号:
裴树文. 旧石器时代旷野遗址形成过程研究综述[J]. 人类学学报, 2019, 38(01): 1-18.
PEI Shuwen. A general study review of site formation processes for Paleolithic open-air sites[J]. Acta Anthropologica Sinica, 2019, 38(01): 1-18.
图1 水洞沟第7地点[45]、飞梁TOK地点[46]和马岭2号地点[47]剥片类和废片类石制品统计图
Fig. 1 Ratios of flaked pieces/detached pieces of lithic artifacts from SDG7[45], FL-TOK[46], and ML2A[47] sites
图2 水洞沟第7地点[45]、飞梁TOK地点[46]和马岭2号地点[47]石制品废片尺寸大小区间统计图
Fig.2 Debitage size distributions of lithic artifacts from SDG7[45], FL-TOK[46], and ML2A[47] sites
图3 水洞沟第7地点和马岭2号地点石制品分布的数字等高模型图
Fig.3 Digital elevation model (DEM) figures of lithic artifacts from SDG7 and ML2A site A) 水洞沟第7地点/SDG7 site;B) 马岭2号地点/ML2A site
图4 水洞沟第7地点[45]、飞梁TOK地点[46]和马岭2号地点[47]石制品走向和倾向玫瑰花图
Fig.4 Rose diagrams showing the orientation and dip patterns on the lithic artifacts from SDG7[45], FL-TOK[46] and ML2A[47] sites A)水洞沟第7地点石制品走向/Orientation pattern of SDG7 lithic artifacts(n=998); B)飞梁TOK地点石制品走向/Orientation pattern of FL-TOK lithic artifacts(n=447); C)马岭2号地点石制品走向/Orientation pattern of ML2A lithic artifacts(n=343); D)水洞沟第7地点石制品倾向/Dip pattern of SDG7 lithic artifacts(n=611); E)飞梁TOK地点石制品倾向/Dip pattern of FK-TOK lithic artifacts(n=126); F)马岭2号地点石制品倾向/Dip pattern of ML2A lithic artifacts (n=377)
遗址成因模型→ 古人类活动信息↓ | 生活面模型 (living floor)[ | 快速堆积模型 (rapid-accumulation palimpsest)[ | 缓慢堆积模型 (slow-accumulation palimpsest)[ |
---|---|---|---|
古人类活动频次 | 一次单一的活动事件 | 少量活动事件伴随后期再沉积改造的遗址形成过程,但活动期次可辨 | 多个活动事件,活动期次边界被后期改造变得难以识别 |
古人类活动时间 | 短暂且单一的人类活动行为 | 人类活动和地质形成过程交替发生 | 长时间人类活动,但仅有地质形成过程可以识别 |
考古层位属性 | 文化层厚度多在10cm以下,水平延伸和顶底边界清楚 | 文化层厚度多在10cm以上,水平延伸不稳定 | 文化层大大超过10cm,且水平延伸不稳定,垂向边界不清 |
标本空间分布特点 | 空间分布不规律,多个分散的人类活动区域可辨 | 活动集中区由于后期的地质改造而变得模糊 | 无法分辨古人类活动的具体区域 |
石制品保存状况 | 古人类遗存均为同时期形成,石制品保存新鲜无磨蚀 | 大部分石制品的外表新鲜 | 不同保存状况的石制品混杂一起 |
表1 遗址成因模型与古人类活动信息
Tab.1 Accumulation models and corresponding archaeological signatures
遗址成因模型→ 古人类活动信息↓ | 生活面模型 (living floor)[ | 快速堆积模型 (rapid-accumulation palimpsest)[ | 缓慢堆积模型 (slow-accumulation palimpsest)[ |
---|---|---|---|
古人类活动频次 | 一次单一的活动事件 | 少量活动事件伴随后期再沉积改造的遗址形成过程,但活动期次可辨 | 多个活动事件,活动期次边界被后期改造变得难以识别 |
古人类活动时间 | 短暂且单一的人类活动行为 | 人类活动和地质形成过程交替发生 | 长时间人类活动,但仅有地质形成过程可以识别 |
考古层位属性 | 文化层厚度多在10cm以下,水平延伸和顶底边界清楚 | 文化层厚度多在10cm以上,水平延伸不稳定 | 文化层大大超过10cm,且水平延伸不稳定,垂向边界不清 |
标本空间分布特点 | 空间分布不规律,多个分散的人类活动区域可辨 | 活动集中区由于后期的地质改造而变得模糊 | 无法分辨古人类活动的具体区域 |
石制品保存状况 | 古人类遗存均为同时期形成,石制品保存新鲜无磨蚀 | 大部分石制品的外表新鲜 | 不同保存状况的石制品混杂一起 |
图5 东非奥杜威峡谷EF-HR遗址T2探方文化层地面水系解析和标本分布密度解析图[51]
Fig.5 Main streams networks of the bottom of the archaeological layers and artifacts density of the artifacts of T2 main trench of EF-HR site from Olduvai Gorge, East Africa[51] A)文化层底面水系解析图/Main stream networks of channels (identified through field observations), B)标本空间分布密度图/Probability surface of T2-Main Trench: a log-linear regression model based on elevation, slope, flow direction, and flow accumulation. Intensity of artifacts is represented by colors from blue (minimum) to yellow (maximum)
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