The Femoral Midshaft Index as Evidence of a Transition in Mobility Patterns in the Chalcolithic and Bronze Age Populations of Anatolia

Belkıs Abufaur, Henna Bhramdrat
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Abstract

Several studies have demonstrated mechanical loading to be associated with activity patterns such as human subsistence strategies and to generate an adaptive response in bone. The femoral midshaft index (FMI), also known as the pilasteric index, is used to infer functional loading effects on the femur to indicative of bone strength as a product of physiological loading. FMI is calculated by dividing the femoral midshaft anteroposterior (AP) diameter by its mediolateral (ML) diameter; measurements are taken from the periosteal surface. This research examines FMI in Chalcolithic and Bronze Age populations across Anatolian regions to observe changes in midshaft geometry and test correlations with spatiotemporal and sociocultural transformations. The FMI data were sourced from published literature containing post-cranial measurements of anatomically modern humans from the populations of interest. Overall, FMI in the Anatolian region declined over time, with the exception of Central Anatolian sites where FMI increased through the Chalcolithic to Early Bronze Ages before decreasing during the Middle Bronze Age. Fluctuations in FMI during the transition from the Chalcolithic and Bronze Ages correlate to the gradual lifestyle changes in the region, with sociocultural transformations being linked to the development of new activities. The observed overall decline in FMI correlates to the archaeological evidence, which depicts a local decline in pastoral communities and development of complex export-driven villages
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股骨中轴指数是安纳托利亚旧石器时代和青铜时代人口流动模式转变的证据
多项研究表明,机械负荷与人类生存策略等活动模式有关,并在骨骼中产生适应性反应。股骨中轴指数(FMI)又称壁柱指数,用于推断功能性负荷对股骨的影响,以指示作为生理负荷产物的骨强度。FMI 的计算方法是用股骨中轴的前胸(AP)直径除以其内侧(ML)直径;测量从骨膜表面进行。这项研究考察了安纳托利亚地区旧石器时代和青铜时代人群的股骨头坏死指数(FMI),以观察中轴几何形状的变化,并检验其与时空和社会文化变迁的相关性。FMI数据来源于已发表的文献,这些文献包含对相关人群中解剖学意义上的现代人的颅骨后测量数据。总体而言,安纳托利亚地区的颅骨指数随着时间的推移而下降,但中安纳托利亚遗址除外,这些遗址的颅骨指数在旧石器时代到青铜时代早期有所上升,在青铜时代中期则有所下降。在从旧石器时代向青铜时代过渡期间,FMI 的波动与该地区生活方式的逐渐变化有关,社会文化的转变与新活动的发展有关。观察到的 FMI 整体下降与考古证据相关,考古证据显示当地牧业社区的衰落和复杂的出口驱动型村庄的发展。
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