论南朝序体文的撰作风貌

南朝序体文数量颇多,篇幅长短不一,题材内容丰富多彩,创作意图各异。从内容上来看,诸作或为帝王歌功颂德,或诠释文学批评观,或褒扬某些作家的为人为文,或自述志趣好尚等。从形式上来看,这些序体文以骈、散两体并行于文苑,骈体序文讲究形式技巧,藻采纷呈,用典繁密,音律协畅,对偶精工;散体序文句式灵活多样,言志抒情明确深刻。     

西安南五台色球藻科蓝藻类的研究

本文报道了西安南五台山的色球藻科蓝藻30种(其中包括变种),并对这些种在不同生态环境和不同林带的生态分布作了初步研讨.     

Radiolarian record to paleoecological environment change events over the past 1.2 MaBP in the southern South China Sea

This note studies the Radiolarian fossil groups since 1.2 MaBP in ODP leg 184 site 1143, the southern South China Sea (SCS). The result shows that radiolarian abundance experienced a significant variation: before 0.9 MaBP it remained at the extremely low level, but increased with low extent between 0.9–0.65 Ma, which corresponded to the Mid-Pleistocene Transition stage, and it increased rapidly after 0.65 MaBP. During the whole process, the average abundance became higher and higher in each stage, and showed regularly periodic fluctuations. The obvious increase after 0.65 MaBP is inferred to result from the enhanced upwelling in this region, which was induced by the intensified monsoon circulation after the “Mid-Pleistocene Transition”. An outstanding result of the spectral analyses is that a long oscillation of ∼ 0.2 Ma cycle was found in the records of radiolarian abundance and complex diversity, which corresponds well to the result of other paleoceanographic indexes. This probably indicated a special cycle characteristic of paleoecological environment evolution in this area. In addition, all of the radiolarian indexes show an obvious boundary in about 0.47 MaBP, indicating the abrupt variation of the community structure and radiolarian abundance level before and after 0.47 MaBP. So we suppose that there existed a distinct change event of oceanic ecology environment during that period.     

Carbon isotopic record of foraminifers in surface sediments from the South China Sea and its significance

Since the 1990s, the papers and data involved withthe South China Sea (SCS) have been emerging in largenumbers in the world as people pay more attention to thepaleoceanography of the SCS. There have been more than100 cores mentioned in papers containing p…     

Original component of grain size index in core sediment from southwestern slope of the South China Sea and its paleoenvironmental implication

Traditional grain size analysis was basically used to discriminate sediment type based on its particle dimension for sedimentary naming[1,2] and to analyze the dynamic feature of transport medium, including water current and wind strength[3―5]. Recently, some patency advances havebeen made by using different methods to separate different grain sizes in various original composition from sediments for searching a new way of paleoenvironmental study[6―8]. Grain size analysis is even playing an …     

Barrier layer in the northeastern South China Sea and its formation mechanism

A VERTICALLY UNIFORM LAYER OF TEMPERATURE(ISOTHERMAL LAYER),SALINITY(ISOHALINE LAYER)AND DENSITY(MIXED LAYER)IS USUALLY FORMED IN THE UPPER OCEAN DUE TO THE WIND STIRRING.UNDERNEATH IS THE LAYER WITH RELATIVELY STRONG VERTICAL GRADIENT AS THE THERMOCLINE,…     

论两宋时期的历史教育

两宋时期,历史教育受到了统治阶级的高度重视。历史教育形式多样,内容丰富,既有针对统治者而开展的以资政、资治为目的的历史教育,又有系统传授历史知识、以培德育人为目的的学校历史教育,同时还有面向普通民众的社会历史教育,极大地促进了两宋历史教育的大众化和通俗化,推动了历史教育的不断发展。