Initial organic geochemical investigation on Late Neoproterozoic-Early Cambrian sediments in the Yangtze region, China

Totally 19 samples of typical Upper Proterozoic-Lower Cambrian sedimentary rocks were collected and analyzed for an organic geochemical investigation. Almost all these rocks have high TOCs, super-maturities and similar biomarker distribution. As an exception, however, the Sinian Nantuo Tillite shows much lower TOCs and little phytane and pristane in comparison with those in other strata, which implies a very faint photosynthetic process, and a restricted euphotic zone and quite limited sunlight within the sedimentary water column during the Sinian glaciation age in the western Yangtze region providing an evidence for palaeo-oceanic environment of the Neoproterozoic Snowball Earth age.     

从果子狸谈起——从SARS的流行省思人与自然的关系

果子狸是SARS病毒的宿主之一 ,野生动物是人类SARS的毒源。人工驯养野生动物 ,让人造的化学成分进入了大自然本来的生物过程 ,其产生的危害给世人带来了生态性的灾难。人类要善待自然 ,慎用科技 ,让人的自然体在大自然中正常生息才能达致人与自然的和谐。     

Combustion energies and standard molar enthalpies of formation for the complexes of the first-row transitional metal chlorides withL-α-histidine

Seven novel solid complexes of the first-row transitional metal with L-α-histidine were synthesized, and their compositions were determined. The constant-volume combustion energies of the complexes were measured by a precision rotation bomb calorimeter. The standard molar enthalpies of combustion and the standard molar enthalpies of formation were calculated. The results indicated that the plots of the standard enthalpies of formation against the atomic number of the metal show a regularity of zigzag.     

Design and application of 60mer oligonucleotide microarray in SARS coronavirus detection

In April 2003, a novel coronavirus[1,2] which was associated with cases of Severe Acute Respiratory Syn-drome (SARS) was first isolated and sequenced in Canada. The genome of SARS coronavirus (SARS-CoV) is 29727[3] nucleotides in length and has 11 known open reading frames (ORFs). Although the genome organiza-tion of this virus is similar to that of other coronaviruses, phylogenetic analyses and sequence alignment show that SARS-CoV is not closely related to any of the previously ch…     

Temperature variations on the Tibetan Plateau over the last two millennia

The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e.     

Evolution of the South China Sea and monsoon history revealed in deep-sea records

As the third summary report of ODP Leg 184 to the South China Sea (SCS), this paper discusses the evolution of the East Asian monsoon and the SCS basin. A multi-proxy approach, involving geochemistry, micropale-ontology, pollen and other analyses, was adopted for reconstructing the evolutionary history of the East Asian monsoon, which was characterized by a series of paleo-climate events especially at 8, 3.2, 2.2 and 0.4 Ma. The new record indicates similar stages in the development of the East and South Asian monsoons, with an enhanced winter monsoon over East Asia being the major difference. The rich spectrums of monsoon variability from the southern SCS also reveal other characteristic features of the low latitude ocean. Evidence for the evolution of the SCS includes the hemipelagic Oligocene sediments, implying the existence of deep water environments during the early seafloor spreading stage of the SCS basin. The four major unconformities and some remarkabl ediagenetic features in upper Oligocene deposits indicate the strongest tectonic events in the region. From a careful comparison of lithologies and sedimentation rates, we conclude that the prominent differences in sedimentary environments between the southern and northern SCS were established only by ～3 Ma.     

微机在非电量测试系统中的应用

本论述了通过开发一套微机辅助测试系统，利用此系统可进行测试数据的自动采集与分析处理，同时简要地介绍了数据采集与处理软件。     

西门子S7-200与PC实时通讯的实现方法

利用Pcomm Pro软件，在VB6中实现PC与PLC的实时通讯。在探讨PC与PLC的自由口通讯协议、通讯的实现方法以及传输数据的校验、错误的处理等的基础上，编写了实时通讯程序，并应用到跳汰机控制系统中。     

基于离散智能的自重构机器人变形策略

在总结自重构机器人系统结构本质特点的基础上，提出了一种描述模型，对几种典型的同构和非同构系统进行统一的描述．探索了自重构机器人的基本变形方法，给出一种建立在全离散的局部智能基础上的变形策略，使机器人通过模块局部之间的交互产生整体自组织的结果，并且能够减低变形算法的计算复杂度．以一个9模块系统的变形过程为例进行了验证．     

贫燃条件下钙钛矿型催化剂上C_3H_6催化还原NO_x反应的研究

利用柠檬酸络合法制备钙钛矿型复合氧化物 L a0 .8Ce0 .2 Co XFe1- XO3催化剂 ,研究其在贫燃条件下 NOX 的催化还原性能 .实验表明 :在没有水蒸气存在的条件下 ,在 30 0°C时 ,La0 .8Ce0 2 Co O3催化剂上 NOX 的转化率可达 46.8%,这时还原剂丙稀已完全氧化 ;但在水蒸气存在下 ,La0 .8Ce0 2 Co O3催化剂上 NOX的转化率明显下降 ,同时丙稀的完全氧化温度也上升5 0°C～ 1 5 0°C,这主要是由于水蒸气对反应活性中心竞争吸附的缘故 ;而双取代的催化剂La0 .8Ce0 2 Ce0 .2 Fe0 .8O3和 La0 .8Ce0 2 Co0 .8Fe0 .2 O3催化剂具有相当的催化活性和较好抗水蒸气能力 ,这可能是由于 Ce O2 和 Co Fe O3之间的协同作用增加了氧空位 ,从而弥补了由于水蒸气竞争吸附所导致的活性下降