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11.
During the first few decades of the twentieth century, legal theory on both sides of the Atlantic was characterized by a tremendous amount of skepticism toward the private law concepts of property and contract. In the United States and France, Oliver Wendell Holmes and François Gény led the charge with withering critiques of the abuse of deduction, exposing their forebears’ supposedly gapless system of private law rules for what it was, a house of cards built on the ideological foundations of laissez faire capitalism. The goal was to make the United States Constitution and the French civil code more responsive to the realities of industrialization. Unlike the other participants in this transatlantic critique, François Gény simultaneously insisted on the immutability of justice and social utility. His “ineluctable minimum of natural law” would guide judges and jurists toward the proper social ends, replacing deduction with teleology. The problem was that nearly all of Gény's contemporaries were perplexed by his conception of natural law, which lacked the substance of the natural rights tradition of the eighteenth and nineteenth centuries and the historicist impulse of the early twentieth. No one was more perplexed than Oliver Wendell Holmes, whose more thoroughgoing skepticism led him to see judicial restraint as the only solution to the abuse of deduction. The ultimate framework for this debate was World War I, in which both Holmes and Gény thought they had found vindication for their views. Events on the battlefield reaffirmed Gény's commitment to justice just as they reignited Holmes’ existential embrace of the unknown. In a sense, the limits of their skepticism would be forged in the trenches of the Great War.  相似文献   
12.
We propose a reassessment of Neandertal mobility strategies by crossing technological and zooarchaeological data. A broad comparative approach to the Middle Paleolithic series from western France shows that the Levallois and laminar flaking systems, the Mousterian of Acheulian Tradition (MTA) shaping system and the Quina and discoidal-denticulate flaking systems, vary significantly in terms of duration of reduction sequences, blank versatility and tool maintenance. These technological systems, which prevail in this context over different time periods, reflect distinct mobility strategies as a response to differing hunting practices. This new approach to Middle Paleolithic technologies and related mobility patterns gives new insights into Mousterian diversity. It also highlights the determinant role played by large game hunting strategies in the organization of late Neandertal societies.  相似文献   
13.
六朝石刻辟邪是六朝时期文化和艺术的载体。六朝石刻辟邪的艺术图像的构型要素以狮形头、张口露舌、体侧刻划羽翼等为主要特色。通过对这些艺术要素源头的追溯,笔者认为:六朝石刻辟邪是中西经济文化交流及中国传统丧葬礼俗的产物。  相似文献   
14.
Excavations at the site of Bosutswe on the eastern edge of the Kalahari Desert in Botswana have uncovered over 4 m of deposit ranging in age from CE 700 to 1700. Our research has produced quantitative and qualitative measures of the material and ecological dimensions that structured the everyday actions and behaviors through which social identities were constituted, maintained, and transformed during the period when the polities of Toutswe, Mapungubwe, Great Zimbabwe and Khami rose to power. By examining the material dimensions that underlay shifting relations of production, exchange, and social stratification we are able to contextualize the social judgments that ascribed value to material goods and food ways, while specifying the ways these were used to create and naturalize social relationships and power differentials. Stable isotope analyses, combined with evidence of vitrified dung, further enable us to suggest changes in herd management strategies used by the inhabitants of the site to compensate for ecological changes brought about by long-term occupation, while at the same time enabling them to economically tie subordinates to them as social divisions became more rigidly defined after CE 1300. The cultural and economic changes that took place at Bosutswe thus directly impact our understanding of the social transformations that immediately preceded contemporary configurations of ethnicity in Botswana.  相似文献   
15.
广州南越国宫署遗址东晋南朝的铁甲和皮甲   总被引:1,自引:0,他引:1  
2004~2006年,广州市文物考古研究所、中国社会科学院考古研究所和南越王宫博物馆筹建处组成的考古队在南越国宫署遗址的两口水井内清理出东晋南朝时期的铁甲和皮甲各1件,铁甲有53片形状不同的甲片,皮甲应为马甲上的胸甲。这类铠甲的出土在岭南属首次发现,同时也填补了这一时期铠甲资料的欠缺。  相似文献   
16.
The Trèves zinc–lead deposit is one of several Mississippi Valley‐type (MVT) deposits in the Cévennes region of southern France. Fluid inclusion studies show that the ore was deposited at temperatures between approximately 80 and 150°C from a brine that derived its salinity mainly from the evaporation of seawater past halite saturation. Lead isotope studies suggest that the metals were extracted from local basement rocks. Sulfur isotope data and studies of organic matter indicate that the reduced sulfur in the ores was derived from the reduction of Mesozoic marine sulfate by thermochemical sulfate reduction or bacterially mediated processes at a different time or place from ore deposition. The large range of δ34S values determined for the minerals in the deposit (12.2–19.2‰ for barite, 3.8–13.8‰ for sphalerite and galena, and 8.7 to ?21.2‰ for pyrite), are best explained by the mixing of fluids containing different sources of sulfur. Geochemical reaction path calculations, based on quantitative fluid inclusion data and constrained by field observations, were used to evaluate possible precipitation mechanisms. The most important precipitation mechanism was probably the mixing of fluids containing different metal and reduced sulfur contents. Cooling, dilution, and changes in pH of the ore fluid probably played a minor role in the precipitation of ores. The optimum results that produced the most metal sulfide deposition with the least amount of fluid was the mixing of a fluid containing low amounts of reduced sulfur with a sulfur‐rich, metal poor fluid. In this scenario, large amounts of sphalerite and galena are precipitated, together with smaller quantities of pyrite precipitated and dolomite dissolved. The relative amounts of metal precipitated and dolomite dissolved in this scenario agree with field observations that show only minor dolomite dissolution during ore deposition. The modeling results demonstrate the important control of the reduced sulfur concentration on the Zn and Pb transport capacity of the ore fluid and the volumes of fluid required to form the deposit. The studies of the Trèves ores provide insights into the ore‐forming processes of a typical MVT deposit in the Cévennes region. However, the extent to which these processes can be extrapolated to other MVT deposits in the Cévennes region is problematic. Nevertheless, the evidence for the extensive migration of fluids in the basement and sedimentary cover rocks in the Cévennes region suggests that the ore forming processes for the Trèves deposit must be considered equally viable possibilities for the numerous fault‐controlled and mineralogically similar MVT deposits in the Cévennes region.  相似文献   
17.
20世纪 60年代 ,我国出现了第二次外交高潮 ,1 965年我国政府向以法国为代表的西欧地区派出了第二批留学生。作者以亲身经历回忆了这批留学生的人员组成情况、在法国的生活学习状况以及“文化大革命”开始后留学生的思想变化。这批留学生回国后 ,周总理在繁忙的工作中 ,对他们进行了周到细致地安排 ,并着手培养外交干部。本文从一个侧面展现了当时一段鲜为人知的历史  相似文献   
18.
南宋官窑源于越窑,其制品特点、工艺技术、窑炉设备与同期的越窑系窑场一脉相承。  相似文献   
19.
南唐方镇在许多方面都发生了重要变化,这些变化引发了方镇体制军事特质的丧失,因此南唐方镇的体制实际上已不再是原先的军政体制,而是一种新的民政体制。决定南唐方镇体制崩解的根本因素是安定战略。五代十国时期是一个特别值得重视的在政治体制方面发生变化的关键时期。  相似文献   
20.
The Bromme culture belongs to the Lateglacial, the period when people settled in the recently deglaciated Southern Scandinavia. Until now there have been only a few imprecise fix-points relating to the chronological position of this archaeological culture. This situation can now be improved with the aid of research results from a Bromme culture settlement at Trollesgave in SE Denmark. Using pollen and plant macrofossil data, Lateglacial lacustrine deposits containing waste material from the settlement can be assigned to the end of the climatically mild Allerød period. A series of 14C dates establishes the age of the settlement as c. 10 826 ± 49 14C years BP (12 871–12 590 cal yr BP). By correlation with climate data from the Greenland ice cores, the occupation can be assigned to the early part of the cold climatic zone GS-1, thus demonstrating that the global ice-core climate zones are not absolutely synchronous with the regional division into biozones.  相似文献   
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