"虚拟"先人与十九世纪新加坡华人社会--兼论海外华人的"亲属"概念

在东南亚殖民地时代,"虚拟血缘"的组织原则对于华人移民社会的重组重建及其运作,具有重要的意义.本文以19世纪的新加坡为个案,考察华人移民如何透过埋葬先人的坟山组织建构"社群共祖"以整合华人社会,讨论东南亚华人虚拟的"先人"或"祖先"概念,进而思考海外华人的亲属研究问题.本文也讨论与比较了"虚拟血缘"组织原则在明代华南宗族"联宗"形态、台湾汉人社会发展早期的"合约式"宗族和东南亚华人坟山组织的不同运用.     

商代马车及其相关问题研究

殷墟发掘以来 ,曾多次发现商代车马坑。但在解放前 ,因受当时发掘条件所限 ,都未能将坑中的木质车子的遗迹清理出来。19 5 0年在河南辉县琉璃阁战国墓地 ,夏鼐先生带领数名技工 ,通过精心操作 ,剥剔出十几辆已朽为尘土的木车遗迹。后来 ,随着发掘经验的积累和发掘技术的提高 ,新中国考古工作者先后在大司空村、孝民屯南地、白家坟西地、郭家庄西南、刘家庄北地、梅园庄东南等处的商代车马坑的发掘中 ,经过精心细致剥剔清理 ,将数十辆殷代车子发掘出来 ,为复原商代车子提供了可靠的依据 ,也为研究商代车制及其相关问题提供了珍贵的科学资料。…     

政治与法律的良性互动——英国法治道路成功的根本原因

政治和法律既相辅相成,又相反相克。二者关系结构的不同,直接影响着甚至决定着一个国家的法治文明进程。英国的法治道路是一条较为顺畅的成功之路,其成功的根本原因在于政治与法律之间建立和保持了一种良性互动关系。16世纪以前,适度强大的政治权威促成了英国法治传统的生成以及自治型、制度化普通法体系的建立和衡平法的产生。16～17世纪,借助于普通法制度积极有效的制衡作用,英国有幸绕过了绝对专制统治的历史弯路,先于其他各国跨入了现代法治社会。认真总结英国法治经验,对于当前我国的法治建设事业无疑是大有裨益的。     

重庆晒网坝一座蜀汉墓发掘简报

2001年在重庆万州晒网坝遗址发掘的编号为CWTM10的墓葬被确定为蜀汉时期墓葬,这是该遗址中唯一一座可确定的蜀汉墓。该墓出土的30件陶器和陶俑成为遗址断代的重要依据。     

襄樊长虹南路墓地第二次发掘简报

本文简要介绍了在襄樊市长虹南路墓地发掘的13座墓葬,其中东汉墓2座、隋墓2座、唐墓9座。均为砖室墓,随葬器物有陶、硬陶、瓷、铜、铁、铅锡、金、银器等。它们的发掘丰富了本地区汉唐时期墓葬资料,尤其是M16画像石门的结构填补了东汉墓葬发掘的空白。     

Hydrothermal dolomitization,mixing corrosion and deep burial porosity formation: numerical results from 1‐D reactive transport models

Major corrosion has been found at depth in carbonate hydrocarbon reservoirs from different geologic provinces. Fluid inclusion microthermometry and stable isotopic compositions of carbonate cements, predating major corrosion, constrain the interpretation of the evolution of parental fluids during progressive burial and prior to the major corrosion event. Post‐major corrosion mineral paragenesis includes pyrite (‐marcasite), anhydrite, kaolinite (dickite) and fluorite. Although the post‐corrosion mineral paragenesis represents minor volumes of rock, it may provide valuable insights into the post‐corrosion brine chemistry. Using reactive transport numerical models, the roles of cooling and/or mixing of brines on corrosion have been evaluated as controls for dolomitization, deep burial corrosion and precipitation of the post‐corrosion mineral paragenesis. Modelling results show that cooling of deep‐seated fluids moving upward along a fracture may cause minor calcite dissolution and porosity generation. Significant dolomitization along a fracture zone and nearby host‐rock only occurs when deep‐seated fluids have high salinities (4 mol Cl kg^?1 of solution) and Darcian flow rates are relatively high (1 m³ m^?2 year^?1). Only minor volumes of quartz and fluorite precipitate in the newly formed porosity. Moreover, modelling results cannot reproduce the authigenic precipitation of kaolinite (dickite at high temperatures) by cooling. As an alternative to cooling as a cause of corrosion, mixing between two brines of different compositions and salinities is represented by two main cases. One case consists of the flow up along a fracture of deep‐seated fluids with higher salinities than the fluid in the wall rock. Dolomite does not precipitate at a fracture zone. Nevertheless, minor volumes of dolomite are formed away from the fracture. The post‐corrosion mineral paragenesis can be partly reproduced, and the results are comparable to those obtained from cooling calculations. Minor volumes of quartz and fluorite are formed, and kaolinite‐dickite does not precipitate. The major outputs of this scenario are calcite dissolution and slight net increase in porosity. A second case corresponds to the mixing of low salinity deep‐seated fluids, flowing up along fractures, with high salinity brines within the wall rock. Calculations predict major dissolution of calcite and precipitation of dolomite. The post‐corrosion mineral paragenesis can be reproduced. High volumes of quartz, fluorite and kaolinite‐dickite precipitate and may even completely occlude newly formed porosity.     

论黄河流域先秦时期腰坑墓葬俗文化——兼说与长江流域同类墓葬俗的关系

腰坑墓流行于黄河流域中原地区的墓葬中,学者们多把对其研究的焦点集中在对这一葬俗文化起源问题的讨论上,并较一致地认为该葬俗最早起源于河南地区。本文对发现的有关材料进行梳理,围绕中原地区先秦时期腰坑墓的起源、用途、性质、发展演变等进行了分析,以澄清过去研究中存在的一些模糊认识。认为,腰坑墓的葬俗最早可以追溯到新石器时代,而其起源亦非河南地区。     

宋代的石藏葬制

宋代石藏葬制的发端一般被认为是治平四年(1067)英宗永厚陵,仔细查考文献可知,此时实以石椁作为变通形式。真正在皇堂内设置地下石藏,始自元丰三年(1080)慈圣光献皇后陵。而在此之前,熙宁八年(1075)韩琦墓已首次特诏构筑石藏。此后,又有少数与皇帝关系特别密切的王爵及对朝政起重要作用的宰臣得以使用。通过排比北宋后期帝陵、后陵、特制亲王宰臣墓、亲王墓资料,发现在墓室尺寸、石藏尺寸、石门有无等方面都构成了比较明显的等级差别。在考虑宋代墓葬等级问题时,除了地上设施诸因素需要纳入考察视野外,对于特制墓例地下形制的独特之处也要给予充分的注意。     

Kyordyughen Site,Ymyiakhtakh Culture,Yakutia: An Interpretation of Burial Rite

A series of radiocarbon dates for the Late Neolithic burial at Kyordyughen, Yakutia, support its association with the Ymyiakhtakh culture. The article proposes a new interpretation of the burial rite in the context of the site. Possible reasons for the disruption of the burial are presented. The presence of the dismembered remains of another body may indicate the practice of human sacrifice. The emergence of warriors as a social group is discussed, and the question is raised as to whether such a group might have been present in the Late Neolithic societies of northeast Asia on the basis of evidence favoring social differentiation with regard to military status.     

The Fauna from Ele Bor: Evidence for the Persistence of Foragers into the Later Holocene of Arid North Kenya

This paper reports on the results of zooarchaeological analysis of fauna from two stratified rockshelters at Ele Bor, 200 km east of Lake Turkana, Kenya. Ele Bor Site A, with radiocarbon determinations from 7000 to 1000 B P, yielded around 4000 identifiable bone specimens. The other site, Ele Bor M, yielded only a hundred bone specimens and will be discussed less extensively in this paper. Fauna from the EBA, although heavily modified by various taphonomic agents, testify to the strong continuity of a broad-based foraging pattern into the first millennium AD, the long stability of human use of a broad range of wild vertebrate species and to a stone-working tradition, augmented but not substantially modified by the introduction of ceramics and grinding equipment during the sixth to third millennium BC.Cette article présent des résultats de 1'analyses zooarquéologiques du faune de deux abris stratifiés à Ele Bor, situé 200 km à 1'est du Lac Turkana dans Kenya. Ele Bor Site A, avec datations du radiocarbon du 7000–1000 ans B.P., provient dans 1'environ de 4000 pièces identifiqués, et le de Ele Bor M, 100 pièces identifiques. Le faune de Ele Bor A, bien que modifiés par diverses processes taphonomiques, testifié à un continuité assez fort de subsistence bassé des especies vertébres indigènes, typiques d'environnements secs. Il n'ya pas d'évidences de adoptation de especies domestique, ni des plantes ni des animaux, jusqu'a 1'ultime millenaire avant présent.