抗战时期陕甘宁边区的国民教育

陕甘宁边区的教育经历了曲折的探索过程,从旧教育模式到创立自己的教育模式,由强迫教育到尊重群众的自愿与需要,由包办到民办公助,形成了具有鲜明时代特色的教育体制。、国民教育培养出的毕业生成为社会的有用之才,提高了陕甘宁边区文化程度,培养了大量专门人才。抗战时期陕甘宁边区的教育从抗战的环境和边区的实际出发,坚持教育同抗战、同社会、同生产劳动相结合的方针,为抗战培养人才,消除了群众中的文盲、迷信、不卫生的习惯,解决了群众生产和生活中的实际问题,既推动了边区教育事业的发展,也但排了边区经济、社会的进步,为抗战作出了重要贡献。     

中国文化自然遗产管理评价的指标体系初探

化和自然遗产管理的研究引起学术界重视。目前献集中于研究转型期遗产管理的组织结构的调整,但缺少在管理机制的设计和操作层面上开展研究。本试图从遗产管理绩效评估入手开始对遗产管理激励机制的探索。初步构建了以遗产保护为基本目标和以社区发展、游客管理和经营开发为贡献目标的遗产管理评价指标体系,并对评价的原则和关键指标确定等进行思考。     

同文馆与晚清留英教育

晚清留英教育在船政学生留英之前已经开始,同治五年(1866年),清政府就派遣了同文馆学生赴欧洲游学。之后,历届驻英公使都带有同文馆学生充任使馆随员或翻译学生,在处理外交及使馆事务之外,这些同文馆学生还负有学习的任务,可以入英国学校学习。19世纪90年代总理衙门还制订章程,派遣了两次同文馆留英生。20世纪初,京师同文馆归并京师大学堂改称译学馆后,再次派遣学生赴英留学。同文馆学生留英在整个晚清虽然不多,但也自成一系,是晚清留英教育中重要的一支。     

2002年度香港西贡沙下遗址C02区和DⅡ02区考古发掘简报

20 0 2年 ,香港古物古迹办事处和河南省文物考古研究所联合在香港发掘西贡沙下遗址 ,发掘面积达 70 0平方米。发现有新石器时代晚期、青铜时代和宋元代的遗存。遗迹中属新石器时代晚期有房址、灰坑等 ,青铜时代有房址、灰坑、石器制造场、灰沟等 ,宋元代有灰坑。遗物中有不同时代的石器、陶器、硬陶器、瓷器、釉陶器等。     

An inter-site comparison of enamel hypoplasia in bison: implications for paleoecology and modeling Late Plains Archaic subsistence

Bison bison mandibular molars from the Late Plains Archaic kill/butchery sites of Buffalo Creek (Wyoming) and Kaplan-Hoover (Colorado) exhibit significant frequencies of dental enamel hypoplasia (DEH), a defect believed to reflect information about physiological status of individual animals. This study provides a methodology to estimate the ontogenetic and seasonal timing of DEH formation in bison dentition. Integration of these estimates with data from bison life history and grassland ecology allows inferences on age- and season-specific factors exacerbating periodic physiological declines that were recorded in the form of enamel hypoplasias. Differences between assemblages indicate regional variability in grassland conditions, with data from Buffalo Creek pointing to recurrent drought that reduced forage capacity and contributed to physiological stress in bison over two consecutive years. Seasons of physiological stress reflected in the DEH correspond to each of the three kill events at the locality, suggesting that predictability of bison behavior in this location was a critical factor in influencing the seasonal timing and location of repeated hunting episodes. Unlike Buffalo Creek, timings of stress episodes are not consistent with season of death in the Kaplan-Hoover bison assemblage, suggesting that favorable grassland conditions were the primary factor influencing timing of this large single-kill event in order to provision for the upcoming winter. DEH analysis represents a developing approach in the construction of models addressing key aspects of local grassland and bison ecology as well as offers unique insights into the hunting strategies and subsistence decisions of Late Plains Archaic foragers.     

试论作为长城"原型"的北方早期石城带

在新石器时代和青铜时代早期,长城沿线的内蒙古中南部、陕北、内蒙古东南部、辽西等地分布有若干石城带,这些石城带基本上都位于当时农业、半农业文化区的北缘,受到气候环境变迁的影响而南北略有移动,其重要功能之一是为了防御北方民族的南侵。由于这些特点与长城有可比之处,故可称其为长城的"原型"。     

论马家浜文化之前太湖地区的地理埋藏环境

近年来,地处东部沿海的浙江和山东地区陆续发现了距今11000～7000年间新石器时代中期和早期遗址,因此探讨江苏地区马家浜文化之前的地理埋藏问题也是必要的。本文重点探讨了长江下游太湖地区更新世晚期和早全新世时期的地理埋藏环境,并认为本区也应该存在新石器时代早中期的遗址。     

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。     

Siberia at the Last Glacial Maximum: Environment and Archaeology

This article focuses on the presence of humans in Siberia and the Russian Far East at the coldest time of the Late Pleistocene, called the Last Glacial Maximum (LGM) and dated to c. 20,000–18,000 rcbp. Reconstruction of the LGM environment of Siberia, based on the latest models and compilations, provides a background for human existence in this region. Most of Siberia and the Russian Far East at c. 20,000–18,000 rcbp was covered by tundra and cool steppe, with some forest formations in the river valleys. Climate was much colder and drier than it is today. Eighteen Upper Paleolithic sites in Siberia are radiocarbon dated strictly to the LGM, and at least six of them, located in southern parts of western and eastern Siberia and the Russian Far East, have solid evidence of occupation during that time span. It seems clear that southern Siberia was populated by humans even at the height of the LGM, and that there was no dramatic decline or complete disappearance of humans in Siberia at that time. The degree of human adaptation to periglacial landscapes in the mid-Upper Paleolithic of northern Eurasia was quite high; humans coped with the cold and dry environmental conditions using microblade technology, artificial shelters, tailored clothes, and megafaunal bones as fuel. An erratum to this article can be found at     

Multiregional Perspectives on the Archaeology of the Andes During the Late Intermediate Period (c. A.D. 1000–1400)

During the Late Intermediate period (LIP, c. A.D. 1000–1400), the central Andes experienced the decline of the Wari and Tiwanaku states, as well as processes of state formation, regional population growth, and competition culminating in the imperial expansion of the Chimú and Inka polities. The LIP holds the potential to link the archaeological features of early Andean states with the material signatures of the later ones, providing a critical means of contextualizing the intergenerational continuities and breaks in state structures and imperial strategies. The recent proliferation of LIP research and the completion of a number of regional studies permit the overview of six LIP regions and the comparison of highland and lowland patterns of political and economic organization, social complexity, and group identity.