日本普通高中教育发展的新走向

通过对日本高中新课程标准、相关法规及报告等新近文献的深入解读。揭示了日本普通高中教育发展的新走向：高中教育目标的法定化、高中性质定位于“国民性中等教育机构”、选修科目成为课程重心、学校经营权限从教育委员会部分转移到学校、导入“学校评议员”制度、加强学生学力评价的综合性与客观性、发展特色化新型高中．     

新历史小说的后现代审美取向

新历史小说在审美取向上与西方后现代主义具有相当的趋同性,尤其体现在历史深度模式削平、主体的退隐或消解、反讽和戏仿的艺术策略等方面。但中国的文化背景决定了新历史小说只能有限地接纳或"误读"西方后现代主义思潮,因此,新历史小说的审美取向只是接受后现代的浅层性特征。     

体验经济与体育旅游的新发展

结合体验经济概念的提出，说明了它与体育旅游新发展的关系；探讨了体育旅游如何与体验经济相结合，加强体验经历，并提出了体验经济时代体育旅游新发展的对策。     

李济深与新桂系的崛起

李济深与新桂系的崛起有着十分密切的关系。他从维护广州革命政府的利益出发 ,为早日实现两广统一 ,完成孙中山北伐的遗愿 ,自 192 3年起就对新桂系采取了军事上援助、政治思想上引导、财政经济上支持的策略 ,使新桂系在 192 5年消灭了旧桂系 ,统一了广西。     

从党的建设的角度解读“三个代表”重要思想

从回顾过去的角度来看,“三个代表”重要思想是中国共产党不断发展壮大的历史经验的深刻总结;从正视现实的角度来看,它是从更高的层面上对中国共产党的性质、宗旨、根本任务和先进性作出的新的科学概括;从展望未来的角度来看,它是解决中国共产党面临的两个历史性课题的战略思考;从“三个代表”重要思想在党建方面的理论创新的角度来看,它提出了六个新的理论观点。     

关于地球生命起源"同源说"

地球上的生命起源问题是一个千古之谜,也是现代科学亟待解决的难题.从20世纪80年代起,笔者就现有主要学说及其引证材料和相关事实进行多学科综合研究,以此提出了地球上的生命起源与地球形成同源的假说,即"生命地球同源说",并不断发展与完善.本文试以生命起源研究或争论中的一些关键和核心问题--如地球生命起源的环境问题、时间问题、有机演化问题以及相关的一些科学问题等为焦点,通过分析讨论阐明"同源说"的基本思想和主要观点,并以此来解释生命起源研究中的某些问题和现象,进而就"同源说"提出的不同于现有生命起源学说的一些观点和论点进行综合分析和阐述.     

钱氏《文选》学研究

<文选>学是钱钟书学术研究的重要组成部分,是终其一生的事业之一.正因为钱公对<文选>学进行了长期的大量的研究,取得了丰硕的成果,把选学推向一个新阶段,可称之为钱氏<文选>学.其内容特点有三:全、深、新.     

重庆开埠与四川社会的近代化进程

重庆开埠刺激和推动了四川社会的近代变迁.传统经济成分逐步缩小,近代经济成分日益增加;社会阶层不断整合与流动;社会组织已较大程度突破血缘与地域关系,开始取向于社会和个人价值实现;近代学堂破土而生,新文化逐步得到传播,观念意识不断趋新解放.由于社会的急剧转型,受制于经济环境、人口和其他社会条件等因素的影响,四川社会的近代化进程体现出相当的艰巨性.     

Deep-water Earliest Oligocene Glacial Maximum （EOGM） in South Atlantic

The most prominent cooling event of the Earth surface during Cenozoic in the long-term transition from a non-glaciated planet, or “green-house world”, to a polar, glaciated planet, or “ice-house world”, is the Earliest Oligocene Glacial Maximum (EOGM) above the Eocene/Oligocene boundary at about 33.7 Ma. Planktonic and benthic foraminiferal oxygen and carbon isotopes, carbonate content, and coarse fraction, along with high-resolution color reflectance and magnetic susceptibility records during 35-30 Ma, from deep-water Sites 1262 and 1265, Ocean Drilling Program (ODP) Leg 208 in South Atlantic, reveal the global cooling event occurring in both surface and deep oceans. The results show that the earliest Oligocene δ^18O values during 33.5-33.1 Ma represent the magnitude of continental ice sheets on east Antarctica and indicate the large decrease in both surface and deep water temperatures of worldwideoceans. The δ^13C records show the large excursion during the period of EOGM event and indicate some types of shift in global carbon reservoir, probably demonstrating the sudden increase in organic carbon burial rates and the changes in the distribution and timing of production. At the same time, lithologic composition, carbonate content, color reflectance, and coarse fraction brought about significant changes close to the Eocene/Oligocene boundary, reflecting the abrupt deepening in the carbonate compensation depth (CCD). Changes in carbonate content were revealed from the color reflectance identify periodicities associated with eccentricity of the Earth‘s orbit (100 and 400 ka), further indicating orbitally forced global climate variations in the Early Oligocene.     

Discovery of a Miaohe-type Biota from the Neoproterozoic Doushantuo Formation in Jiangkou County, Guizhou Province, China

A megascopic algal fossil assemblage was first discovered by Ma Guogan and Chen Meng‘e in the black shales of the Neoproterozoic Doushantuo Formation in Miaohe Town, Zigui County, Hubei Province in 1978. Formal naming of the Miaohe Biota was proposed by Cheng Meng‘e and Xiao Zongzheng in 199112j, and eleven morphological genera have been previously described. including megascopic algae and putative metazoans .Ding et al. greatly expanded the scope of the Miaohe Biota to 9 phyla consisting of 140 genera, including microphytoplanctons, megascopic algae, metazoans, spongesand trace fossils. Xiao et al. further restudied this fossil assemblage, concluding that only about 18 distinct taxa could be recognized and that many Miaohe taxa are poorly defined or svnonvmous.