人类学学报 ›› 2026, Vol. 45 ›› Issue (02): 280-295.doi: 10.16359/j.1000-3193/AAS.2025.0058
收稿日期:2024-09-30
修回日期:2025-01-07
出版日期:2026-04-15
发布日期:2026-04-17
通讯作者:
张双权,研究员,主要研究脊椎动物埋藏学与旧石器时代动物考古学。E-mail: zhshq@ivpp.ac.cn
作者简介:侯沂杉,硕士研究生,主要研究旧石器时代动物考古学和埋藏学。E-mail: houyishan@ivpp.ac.cn
基金资助:
HOU yishan1,2(
), ZHANG Yue3, ZHANG Shuangquan1,2(
)
Received:2024-09-30
Revised:2025-01-07
Online:2026-04-15
Published:2026-04-17
摘要:
骨角制品是考古遗址中发现的重要动物遗存,可能蕴含着有关过去社会文化和技术能力的重要信息。过去对于骨角制品功能的研究主要是根据形态来对功能进行推测,缺乏具体直观的证据。另外,多数骨角制品的材料来源难以通过外观鉴定,影响对古人类行为信息的判断。目前,国外有学者将组织学方法与显微CT技术应用到考古研究中。显微CT技术结合组织学方法可以在不破坏标本的情况下获取骨骼内部信息。在表面没有明显破裂或使用痕迹时,骨骼内部的微裂纹可能会揭示其使用期间所受应力类型,为研究骨角制品制作和使用方法带来更多的信息。另外,通过对骨角制品的组织学观察,可以探究古人类对于骨骼材料选择的规律性,反映出对特定动物的偏爱程度。本文将对两种技术方法的研究成果进行详细梳理,系统介绍骨骼内部微裂纹与所受应力的关系以及组织学属种鉴定的方法,进而探讨新方法在考古学研究中的适用性和发展潜力。
中图分类号:
侯沂杉, 张乐, 张双权. 显微CT技术和骨组织学观察在动物考古学研究中的应用[J]. 人类学学报, 2026, 45(02): 280-295.
HOU yishan, ZHANG Yue, ZHANG Shuangquan. Micro-CT techniques and bone histology in zooarchaeology[J]. Acta Anthropologica Sinica, 2026, 45(02): 280-295.
图2 骨单位中微裂纹的分类[41] 1.骨基质中的微裂纹 microcracks in the interstitial bone matrix;2.基质和黏合线之间的微裂纹 microcracks extending between the matrix and the cement line;3.沿黏合线延伸的微裂纹 microcracks along the cement line;4.层间微裂纹 interlamellar microcracks;5.接近但未到达黏合线的微裂纹 microcracks within the osteon approaching but not reaching the cement line;6.终止于黏合线的微裂纹 microcracks within the osteon terminating at the cement line;7.穿过黏合线的微裂纹 microcracks crossing the cement line.
Fig.2 Classification of micro-cracks in Haversian bone
图3 CT扫描几种实验下微裂纹示意图[9] A.疲劳试验前后CT扫描图像,左侧(a)为未处理的对照组,右侧(b)为增加载荷直至骨骼断裂的实验组 CT scan images before and after fatigue testing: the left side (a) represents the untreated group, while the right side (b) shows the experimental group subjected to increasing load until bone fracture;B.兽皮穿刺实验 hide piercing experiment;C.模拟动物踩踏实验 trampling experiment;D.风化状态 weathering experiment。
Fig.3 CT scan images of microfractures from various experiments
图4 狩猎实验(标本1,2,3,5)和加热实验后的骨箭头(标本7)内部显微结构[48] 箭头指向微裂纹的具体位置;数字表示实验过程中的箭头序号The arrows indicate the specific locations of microfractures, while the numbers correspond to the arrows used in the experimental process。F.前面front;R.右面right
Fig.4 Microfracture morphology of bone arrowheads after hunting experiments (specimens 1, 2, 3, 5) and heating experiments (specimen 7)
图5 比较人类和非人类长骨(胫骨)的组织学差异[69,71] A.人:高亮部分表示黏合线,标志着新旧骨单位的叠压关系 Human: The highlighted areas indicate cement lines, marking the overlapping relationship between new and old osteons;B.牛:骨单位形状近似椭圆形,中央管形状不规则 Cattle: Osteons are approximately oval-shaped, with irregularly shaped central canals;C.猫:单位面积骨单位分布密度高,中央管直径较小 Cat: High-density distribution of osteons per unit area, with smaller central canal diameters;D.狗:较高密度中等大小的骨单位 Dog: Moderately sized osteons with relatively high density;E.鸡:高密度分布的较小的骨单位 Chicken: Small osteons densely distributed;F.猪:骨单位形状不规则,周围有吸收腔隙 Pig: Irregularly shaped osteons with resorption cavities surrounding them.
Fig.5 Comparison of the histological differences between human and non-human bones
图6 不同个体的骨组织结构对比[78-80] A. 4天大婴儿股骨的骨组织结构 Bone tissue structure of a 4-day-old infant femur;B. 4岁半儿童肱骨的骨组织结构 Bone tissue structure of a 4.5-year-old child’s humerus;C.幼年猪桡骨的骨组织结构 Bone tissue structure of a juvenile pig’s radius;D.马骨中以层状成分为主的纤维板层骨 Fibrolamellar bone in horse bone, primarily composed of lamellar components;E.牛骨中以纤维成分为主的纤维板层骨 Fibrolamellar bone in cattle bone, primarily composed of fibrous components;F.偶蹄类 Artiodactyla;G.奇蹄类 Perissodactyla。fa.纤维成分 fibrous component;la.层状成分 lamellar component;cr.热裂纹 heat-induced cracking;HM.过度矿化 hyper-mineralisation;DD.成岩溶蚀作用 digenetic dissolution。
Fig.6 Comparison of bone tissue structures among different individuals
图7 骨骼化石在成岩过程中产生的几种微裂纹[91] A.早期成岩作用产生的径向微裂纹Radial microfractures caused by early diagenesis;B.新鲜状态下的哈弗氏骨Haversian bone in a fresh state;C. 在水生条件下,由于骨胶原蛋白吸水膨胀产生的微裂纹Under aquatic conditions radial microcracks appear due to water uptake and swelling of the bone collagen in secondary osteons;D.在干燥条件下,由于骨胶原蛋白收缩而产生的由中央管向外放射的微裂纹Under dry conditions shrinkage of the bone collagen in secondary osteons due to desiccation produces radial cracks from the Haversian canal outwards;E.干燥环境维持较长时间的情况下,周向裂纹将骨单位与周围分离,周缘出现微小的裂纹If desiccation is prolonged, circumferential cracks can isolate osteons from adjacent structures; small peripheral cracks occur, which start at the osteon boundary but do not spread beyond it
Fig.7 The types of microfractures occurring in bone fossils during the diagenetic process
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