This paper describes the morphology of the feet of a population of elite women from the Ming dynasty (1368( -1644 in Shaanxi province. This is a social stratum, time, and place in which foot binding was practiced. Among a group of 31 skeletons exhumed from the cemetery, eight were women with wellpreserved foot bones. Macroscopic examination revealed that half these women (4/8) had clearly altered foot bones: the metatarsal bones, and the few observable phalanges, were gracile and small, while the tarsal bones exhibited a slight reduction in size but no dramatic change in morphology. The other half of the women (4/8) had apparently unmodified metatarsal bones. T-tests comparing linear measurements of the foot bones between the two groups revealed that metatarsal bones were the most affected by binding, and among the tarsal bones, the talar trochlea and calcaneal dimensions were most impacted. This small group of skeletons reveals that some elite women in Shaanxi apparently still did not practice foot binding in the late Ming dynasty, or practiced a much milder form of foot binding, and that there was considerable variation even among those who did practice it.
Yangguanzhai, a Middle Neolithic archaeological site (c. 5500–5000 cal year BP) in the Wei River Valley of China, contains a well‐preserved record of environmental fluctuation, landscape evolution, and human–environment interaction over the Holocene. We examined eight stratigraphic profiles across the site and identified an alternating sequence of sediment and buried soils, indicative of multiple changes in landscape stability. Through this study, we provide a more detailed soil‐stratigraphic framework for the site. Buried soils are well developed, with a subangular blocky structure, high organic matter content, and pedogenic carbonate. There are clear associations between buried soils and the two main archaeological occupations (the Middle Neolithic and a later historic period occupation, c. 600–300 cal year BP). Lower soil horizons contain abundant Middle Neolithic ceramics and archaeological features, and the upper soil horizon contains historic period artifacts and features. Sediment between these soils lacks any artifacts or evidence of occupation, suggesting that Yangguanzhai was abandoned as a residential area for over 3000 years. Heightened sediment deposition and landscape instability contributed to Late Holocene shifts in human land use and settlement patterns at the site. Our work is consistent with previous stratigraphic investigations at the site, while refining descriptions of buried soil horizons.
The Jing-Wei Floodplain, located in Shaanxi, China, has been home to various groups of people over the last 5000 years. Drawing together evidence from archaeology, paleobotany, geomorphology, climate sciences, and history, this paper provides a longue durée study of the local (pre)history of human occupation in this area with a special focus on human adaptation strategies and environmental history. In particular, the study summarizes and evaluates archaeological and geomorphological field research conducted over the last ten years and connects it with often overlooked local historical accounts and recent climate research in the Wei River Valley and observations on recent economic developments and their impact on both the environment and the people living in it. In spite of a rather long hiatus in occupation from the second century BCE to the twelfth century CE, the evidence shows that there are close similarities in human-environment relations and even continuities into the modern period. Though being a highly localized study, this paper can serve as an example for how such longue durée studies may be conducted in other regions, and it provides some suggestions for future field and laboratory research.
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