使用原版英文教材进行分子生物学双语教学的实践与思考

双语教学不仅是我国高等院校教育改革的一项重要内容,而且也对我国21世纪的人才培养提出了更高的要求.本文结合分子生物学双语教学实践及其教学效果调查,针对对师范院校开展双语教学提存在的问题提出了一些可行的建议.     

一株具抗肿瘤活性的北极细菌的筛选及分子鉴定

在中国首次北极科学考察期间，从北极海域采集了水体，沉积物等样品，从中分离得到一批嗜冷细菌，采用MTT法对这些北极海洋细菌进行了细胞毒活性物质的筛选，得到一株具有细胞毒活性的菌株。采用16SrDNA序列分析及系统发育分析方法对该株菌株进行了分子鉴定。     

船舶电站实时仿真

在船舶电站仿真研究中，引入节点电压法的建模方法和节点撕裂法的并行算法，设计了自动生成模型的数学支持系统。这些方法提高了仿真的速度。针对船舶电站的特点，设计了仿真算法和并行计算程序。这些方法可以很好地满足实时性和准确性的要求。     

生物学网络信号教学模式的构建

通过对理论依据、制作方法、教学程序、教学评价、注意事项等方面的阐述，介绍一种以心理学教学论知识为基础，充分体现学生自主学习，融科学性、逻辑性、直观性、趣味性为一体的生物学教学模式。     

Timing and history of marine hydrocarbon accumulation in Tarim craton

<正> Based on the analyses of hydrocarbon inclu-sions, K-Ar dating of authigenic illites and oil/gas-watercontact retrospection as well as other methods, the marineprimary reservoirs in the cratonic region of the Tarim Basinare found to have been formed in the late Caledonian toearly Hercynian, late Hercynian, and Himalayan, and oil andgas adjusted and redistributed in the Yanshanian (Jurassic toCretaceous) and Himalayan (Tertiary). The analyses alsoshow that the remaining primary oil accumulations aremostly formed in the late Hercynian, and the secondary oilreservoirs resulted from the adjustment and redistribution ofthe earlier accumulations during the Yanshanian and Hima-layan (especially late Himalayan), of which the Himalayan isalso the major stage of gas accumulation. The primary oilreservoirs formed in the late Hercynian mostly occur withinthe Paleozoic formation, whereas the secondary reservoirsformed in the Himalayan in the Mesozoic. The late adjust-ment and redistribution of reservoirs in the craton region ofthe Tarim Basin is ubiquitous because of the intensified tec-tonic movements since the Mesozoic, especially Cenozoic andintrusion of the high- to over-mature gas. Furthermore, thelower amplitude of reservoirs in the craton region also makesthem easier to be adjusted and redistributed. Therefore, theremaining paleo-uplift and palaeo-slope developed in rela-tively stable tectonic regions are the main potential areas forthe middle-large marine reservoirs in the Tarim Basin.     

人类结构基因功能研究与应用

对人类结构基因功能的核心问题:基因的多样性、基因的表达、模式生物基因及疾病相关基因研究及应用等方面进行了概述.     

公婆泉铜矿岛弧型含矿斑岩地质地球化学特征

目前发现的斑岩型铜矿的含矿斑岩均产于陆相环境，公婆泉铜矿斑岩是目前为止发现的惟一产于海相环境的含矿斑岩，围岩沉积环境，岩石化学和地球化学研究表明，含矿次英安斑岩和花岗闪长斑岩产于海相环境，形成于水下500－1000m，是中一晚志留纪哈萨克斯坦板块向（南）塔里木－中朝板块俯促时公婆泉－东七一山岛弧岩浆晚期分异的产物。     

闽江口晚第四纪海侵地层的研究

大量钴孔岩芯的岩性特征,微体古生物硅藻和有孔虫化石组合,以及~(14)C测年结果揭示,闽江河口区发育两期海侵地层。表明本区在晚第四纪期间至少经历了两次海侵事件,发生于距今44000～22000a的玉木亚间冰期海侵相对较弱,其范围仅达福州市区一带,另一次海侵发生于距今12000a以来的冰后期,该次海侵较为广泛,其范围可达闽侯的甘蔗一带。     

Ecology and physiology of phototrophic bacteria and sulfate-reducing bacteria in marine salterns

Marine salterns are habitats for a large variety of halophilic bacteria. In the anoxic zones, halophilic sulfur bacteria develop mainly at the sediment surface, but only a few of them have so far been isolated from such environments. Among the phototrophic sulfur bacteria that sometimes form purple layers underneath the green cyanobacterial layers, members of the generaEctothiodhodospira, Chromatium (C. salexigens), Thiocapsa (T. halophila) were isolated. They grow by using sulfide as an electron donor. In the marine salterns, sulfide originates from active sulfate reduction. Among the halophilic sulfate-reducing bacteria, onlyDesulfovibrio halophilus andDesulfohalobium retbaense have so far been isolated. The ecology and physiology of both kinds of bacteria are discussed in this paper.     

Extraordinary levels of cadmium and zinc in a marine sponge,Tedania charcoti Topsent: inorganic chemical defense agents

The Antarctic marine spongeTedania charcoti has been shown to contain extraordinarily high natural concentrations of cadmium and zinc, which have in turn been correlated to the ability of the crude ethanol extract to modulate protein phosphorylation in chicken forebrain and to inhibit the growth of several test bacteria.