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中国近代考古学建立之初,不免材料不足并有先天局限,但随着考古学的发展和壮大,其对中国上古史之重建的作用日益显现。以顾颉刚为代表的古史辨派对旧古史系统进行了摧毁性的批判,傅斯年、李济等人继之而起,开辟了重建之路。傅斯年为重建中国古史提供了体制保证并指明方向,李济则在理论和方法上提出了系统的方案。然而,李济等人限于当时条件,具体实践工作并不理想,而中国大陆考古学者们则做出了切实的贡献。经过60年的发展,中国田野考古学取得极大的成就,苏秉琦等学者据此提出考古学文化"区系类型理论"和中国文明"多元一体格局说",中国上古史重建已进入切实展开的时期。  相似文献   
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During the long-lasting cultural sequences of the Shurābeh and Sialk archeological mounds (6200–550 BC) the inhabitants encountered numerous diversified crises along a narrow fertile passageway at the edge of the Central Iranian Plateau Great Desert. Some of the threats may be attributed to earthquakes, drastic climatic changes, and man-made environmental deterioration, which possibly led to the settlement withdrawing at different stages toward a more suitable location. Our study identified the occurrence of a large-magnitude earthquake around 3800 BC along the Kāshān fault, which is well-documented by various lines of circumstantial evidence, including: (i) numerous contemporaneous smashed skeletons and artifacts underneath collapsed walls and ceiling debris in several different areas; (ii) tilted and collapsed walls; (iii) nearly N–S oriented fallen large storage jars; and (iv) nearly vertical deep ground fractures cutting walls and floors of the Sialk III5 South Mound settlement. Archeological data also shows additional stratigraphic discontinuities and damages that may be attributed to earthquakes. However, damage features in limited exposed trenches are less conclusive and require additional careful excavations. Apparent ancient paleo-architectural innovative attempts to enhance the coherency/elasticity of the structures and minimize earthquake damage to buildings were also noted, suggesting the indigenous earthquake hazard mitigation endeavor. There seems to be a correlation between some site abandonment dates and possible drastic regional draught/cooling events. The natural and anthropogenic impacts addressed in this study constituted major threats to the sensitive archeological settlements at the fringe of the desert and the vicinity of the Kāshān active fault since antiquity.  相似文献   
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卡若遗址是发现于西藏昌都县的一处新石器时代遗址,于1978年经西藏自治区文管会和四川大学历史系考古专业发掘,两个单位联合撰写的发掘报告中主要介绍了建筑遗存和生产生活用具。发掘报告中统计完整、记录详细的房址柱洞资料引起了笔者关注,因此尝试用定量分析方法对以房址柱洞为主的建筑遗存进行探讨。通过统计分析,柱洞资料反映出了卡若文化在约1000年的发展过程中发展壮大,然后又由盛转衰的历史进程。从技术分析的角度印证了卡若聚落居民在史前生活中经历的生产生活方式的转变。  相似文献   
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高句骊是我国古代少数民族之一。高句骊政权存在705年。该文认为中国学者的高句骊研究肇始于好太王碑的发现,经历19世纪80年代至1949年的研究初始阶段、1949年至20世纪70年代的研究冷落期、20世纪80年代以降的研究勃发期。该文简要地评析了上述3个时期的研究方向、特点及研究成果与不足。  相似文献   
5.
A variety of phytoliths, together with prolific microcharcoal particles, sponge spicules and diatoms were extracted and identified in four cultural layers from an archeological site at Jinluojia, Macheng, Hubei Province, Central China. The warmth (Iw) and aridity (Iph) indices calculated from grass phytoliths reveal warm and wet periods during the West Zhou, early East Zhou, Tang and Song Dynasties whilst cool and dry periods occurred during the late East Zhou, Ming and Qing Dynasties. The paleoclimate conditions reconstructed on the basis of grass phytoliths extracted from archeological sediments are in agreement with those from natural sediments in the Middle Yangtze region. In contrast, the woody phytoliths show a positive correlation with microcharcoal particles, suggesting an anthropogenic contribution to the woody phytoliths from the use of woody plants for fuel during cooking and heating. Two episodes of the enhanced abundance of woody phytoliths and microcharcoal particles were found to occur at East Zhou Dynasty and from Ming and Qing Dynasties to the Present, proposed to be a consequence of the population expansion and/or the frequent wars.  相似文献   
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东方考古学协会述论   总被引:1,自引:0,他引:1  
北京大学国学门考古学研究室 ,是中国乃至东亚最早的专门考古学独立机构。 192 6年 ,国学门考古学会与日本东西两京帝大合组的东亚考古学会结成东方考古学协会 ,计划以联合发掘、交流成果、互派留学等方式 ,共同推进东方考古事业。可惜双方对于如何利用这一机缘并发挥各自的作用 ,利益和想法不一致。结果北大在考古发掘方面更形困顿 ,无法在重建古史的活动中占据重要位置 ,不得不将在这一领域的应有地位拱手让人。  相似文献   
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