古代目录中史部故事类到政书类的演变

故事本意系指旧事,司马迁继承其父遗愿时曾表示:"请悉论先人所次旧闻,弗敢阙."以后又曰:"余所谓述故事,整齐其世传,非所谓作也."①从对旧事的引录叙述,渐指旧日事例及前朝的典章制度,《汉书·楚元王传附刘向传》:"是时,宣王循武帝故事,招名儒俊材置左右."又《汉书·苏武传》:"卫将军张安世荐(苏)武明习故事,奉使不辱使命."故事意指典章制度,史志中一直沿用至明代.     

秦代墓研究的几个问题

秦人墓,指的是属于“秦族”或秦国人在关中及其它地区死亡后所埋葬的遗迹。它既存于秦统一以前,也存在于秦统一以后,大约在西汉中晚期秦人文化完全汉化后,秦人的墓基本不复存在。     

清代帝陵的哑巴院和月牙城

本文论述清代帝陵中的哑巴院和月牙城的建置与功用,进而探讨其规制的起源问题。指出关外的福陵与昭陵系参照北京明代后期的帝陵及清孝陵兴建,而南京明孝陵的规制已见哑巴院的雏形,其发展演变脉络清晰,故而哑巴院和月牙城并非明清两代帝陵规制最显著的差别。     

穿越开罗千年老城

作为“世界之母”的开罗吸引着大批的外国人。19世纪和20世纪初,欧美各国的人把这里当作气候温和的冬季运动场。现在海湾地区的阿拉伯人为了远离沙特阿拉伯和科威特的炎热,每年夏天都到这里避暑。对于他们来说,开罗是阿拉伯的好莱坞和“大苹果城” (美国纽约市的绰号)。     

战争话语下的草根文化——论抗战时期山西革命根据地的民间小戏

民间小戏,作为草根文化的代表,其产生、发展、兴盛与乡村社会有着直接而紧密的联系,较真实地反映了社会生活的多元图景。抗战爆发后,政治的强大力量渗透到乡村社会,对乡村戏剧的改造就是其中之一。处于战争话语下的民间小戏在结构和内容方面都随之发生了深刻变化,娱乐功能的主导地位被政治教化功能所取代。政治开始以一种前所未有的方式介入到民间文艺中,融入到乡村生活中。本文以抗战时期山西革命根据地的民间小戏为考察对象,分析了战争话语下草根文化在内容、形式和功能方面的转变及其与政治在乡村社会的结合。     

和谐社会视野中的青海民族宗教问题

青海是多民族多宗教的地区,大多数少数民族群众信仰宗教,民族问题和宗教问题相互交织、相互影响,民族宗教工作在全省工作大局中有着十分重要的地位。只有坚持从青海实际出发,认真贯彻落实党的民族与宗教政策,不断加强对宗教事务的依法管理,积极引导宗教与社会主义社会相适应,巩固和发展党的爱国统一战线,坚决抵制敌对势力的分裂渗透活动,不断加强民族团结,才能切实做好青海的民族宗教工作。     

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"。     

福泽谕吉与“脱亚论”的理论与实践

福泽谕吉既是一位近代启蒙思想家,也是一个征韩侵华论的积极倡导者。这种“矛盾”性,取决于他要着力完成的两大任务：一是建立主权独立的近代化国家;二是以武威“大东亚秩序”来取代札教“华夷秩序”。前者诱因于西方“条约体系”下的“民族国家”理念;后者催生于颠覆东亚“朝贡体系”进而取中国而代之的百年夙愿。两大任务的显隐交替和互为前提,解释了《文明论之概略》与《脱亚论》之间的表层矛盾和内在关联。     

徐兆奎先生的生平及其历史地理学贡献

徐兆奎是一位在历史地理学、地名学、地理学史及地理教育上做出重要贡献的历史地理学家。本文梳理了徐兆奎的生平,分析了其在上述领域的主要贡献,希冀引起学界的重视,以此缅怀这位前辈知名学者。     

Conodonts and tabulate corals from the Upper Ordovician Angullong Formation of central New South Wales,Australia

Zhen, Y.Y., Wang, G.X. &; Percival, I.G., August 2016. Conodonts and tabulate corals from the Upper Ordovician Angullong Formation of central New South Wales, Australia. Alcheringa 41, xxx–xxx. ISSN 0311-5518.

The Angullong Formation is the youngest Ordovician unit exposed in the Cliefden Caves area of central New South Wales. Its maximum age is constrained by a Styracograptus uncinatus graptolite Biozone fauna at the very top of the underlying Malongulli Formation, but the few fossils previously reported from higher in the Angullong Formation are either long-ranging or poorly known. From allochthonous limestone clasts in the middle part of the formation, we document a conodont fauna comprising Aphelognathus grandis, A. solidum, Aphelognathus sp., Aphelognathus? sp., Belodina confluens, Drepanoistodus suberectus, Panderodus gracilis, Panderodus sp., Phragmodus undatus, Pseudobelodina inclinata and Pseudobelodina? sp. aff. P. obtusa, which supports correlation with the Aphelognathus grandis Biozone (late Katian) of the North American Midcontinent succession. The species concepts of Aphelognathus and Pseudobelodina are reviewed in detail. Associated corals are exclusively tabulates, dominated by agetolitids, including Agetolites angullongensis sp. nov., Heliolites orientalis, Hemiagetolites breviseptatus, Hemiagetolites sp. cf. H. spinimarginatus, Navoites sp. cf. N. circumflexa, Plasmoporella bacilliforma, P. marginata, Quepora sp. cf. Q. calamus and Sarcinula sp. Affinities of the coral fauna from the Angullong Formation are closer to faunas from northern NSW and northern Queensland than to the locally recognized Fauna III of late Eastonian age in central NSW. We propose a subdivision of Fauna III to account for this difference, with the late Katian Fauna IIIB characterized by the incoming of agetolitid corals. The currently known distribution of representatives of this group with adequate age constraints suggests that agetolitids possibly originated in North China, subsequently migrating to Tarim, South China and adjacent peri-Gondwanan terranes while also spreading eastward to northern Gondwana, where they progressively moved through eastern Australia to reach the central NSW region by the early Bolindian.

Yong Yi Zhen* (yong-yi.zhen@industry.nsw.gov.au) and Ian G. Percival (ian.percival@industry.nsw.gov.au), Geological Survey of New South Wales, W.B. Clarke Geoscience Centre, 947–953 Londonderry Road, Londonderry, NSW 2753, Australia; Guangxu Wang (gxwang@nigpas.ac.cn), State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, 39 East Beijing Road Nanjing 210008 PR China.