医患通平台在经皮冠状动脉介入治疗术后患者中的应用

目的：探讨医患通平台对经皮冠状动脉介入治疗（PCI）术后患者进行护理的临床效应。方法：选取54例冠心痛行PCI治疗术后患者,随机分为对照组和试验组,各27例。对照组采用常规护理,试验组在对照组的基础上采用医患通平台进行护理干预,比较两组患者血压、血脂、血糖的控制情况,主要不良心脏事件（MACE）的发生情况,并采用汉密尔顿焦虑量表（HAMA）及汉密尔顿抑郁量表（HAMD）对两组患者进行心理状况调查。结果：实施干预后,试验组血压、血脂、血糖的控制率优于对照组（P〈0．05）,MACE的发生率低于对照组（P〈0．05）;两组患者两组干预前HAMA、HAMD评分比较无明显差异（P〉0．05）,干预后试验组患者HAMA评分、HAMD评分有所下降,与干预前及对照组比较差异显著（P〈O．01）,对照组干预前后无变化（P〉0．05）。结论：医患通平台能有效地让PCI术后患者对危险因素进行控制,降低MACE的发生,改善患者的负性情绪,是较好的健康教育方式．     

平台化学品短链支链脂肪酸和短链支链醇的微生物代谢工程

短链支链脂肪酸和短链支链醇均为重要的平台化学品,是合成多种高附加值产品的前体物质,市场需求巨大。目前两者的生产主要是利用基于石化原料的化学合成法。化学合成法存在着严重依赖化石燃料、反应效率低以及极易造成环境污染等缺点。微生物代谢工程的快速发展为这些平台化学品的生产提供了一条极具潜力的生物合成路线。利用微生物代谢工程技术构建生产这些平台化学品的微生物细胞工厂具有绿色清洁、可持续发展和经济效益好等独特优势。本文系统综述了近年来微生物代谢工程技术在短链支链脂肪酸和短链支链醇合成方面的研究进展,包括所涉及的宿主菌株、关键酶、代谢途径及其改造等,并探讨了未来的发展前景。     

基因表达谱信息分析软件IDEA与WebGEA

基因芯片具有高通量快速并行检测基因表达水平的功能,是功能基因组研究的有力工具。针对基因芯片常规的信息分析需要,我们初步设计开发了基因表达谱的信息学分析平台,包括基于单机的软件IDKA(Information Digger for Experiments of microArray)与网络应用程序WebGEA(WEB GeneChip Expression Analysis),分别支持用户运行独立程序与在因特网上提交数据运行服务器程序来完成数据采掘分析任务。该平台得到良好的应用,是解决基因芯片常规的信息分析问题的一个方便工具。     

Middle–Late Ordovician chitinozoans from Songliang of Qiaojia,western South China,and their biostratigraphic implications

Ordovician chitinozoans are as yet inadequately documented from the western Yangtze Platform, South China. Here we present a systematic study on chitinozoans from a Middle–Upper Ordovician succession at Songliang of Qiaojia, northestern Yunnan, southwestern China. Altogether 34 species of 12 genera are identified from the upper Hungshihyen and the Huadan formations. The top of the Hungshihyen Formation yields typical Early and Middle Ordovician forms, for instance, Lagenochitina obeligis and Belonechitina chenjiawuensis, with the latter only known from the lower Darriwilian in South China, thus suggesting an early Darriwilian age for this interval. The chitinozoans recovered from the Huadan Formation include Lagenochitina prussica and Spinachitina fossensis, both are mainly confined in Katian and sometimes ranging into younger strata. This indicates an age younger than the middle to late Darriwilian previously determined for the Huadan Formation. However, conflicts exist in age assignment of the Huadan Formation based on chitinozoan and other evidence, and further work is required.     

Taxonomy and distribution of the Ordovician conodontDrepanodus arcuatus Pander, 1856, and related species

PalZ - Drepanodus arcuatusPander, 1856, is one of the geographically most widely distributed conodont species in the Ordovician, and has been reported to range practically throughout the entire...     

Parafurnishius,an Induan (Lower Triassic) conodont new genus from northeastern Sichuan Province,southwest China and its evolutionary implications

A fundamental aspect of taxonomy at the generic level, critical to understand Early Triassic conodont evolution, is the composition of the multielement apparatus. In this paper, we document a platform-bearing new conodont genus, Parafurnishius n. gen., as well as its multielement apparatus from the Griesbachian Feixianguan Formation (Lower Triassic) in Xuanhan County, northeastern Sichuan Province, southwest China. The new conodont genus is characterized by numerous robust and irregularly distributed conical denticles with variable platform morphology that has a possible affinity with the P₁ elements of Furnishius. These genera have apparatuses similar to those of Ellisonia and are classified with the family Ellisoniidae. The strong intraspecific variation of P₁ elements and the growth series within the entire sample population suggest that Parafurnishius may have evolved from the Griesbachian Isarcicella by developing random denticle positioning away from the platform centre, and then possibly evolved into younger Triassic Furnishius by developing a stable blade configuration. This preferred interpretation implies an ellisonid apparatus for Isarcicella. Alternatively, Parafurnishius may have evolved from Ellisonia and developed a homeomorphic P₁ element with Isarcicella. This new taxon has strong intraspecific variation of denticle growth orientation during the Early Triassic.     

Nonmarine ostracodes at the Permian–Triassic boundary of the central part of the East European Platform

Extensive geological and paleontological materials from the upper Permian and the Lower Triassic of the East European Platform had been accumulated by the end of the 20th century. Recently obtained new data indicate the stratigraphic continuity of the East European Permian–Triassic succession. The Permian–Triassic boundary is in many sections associated with the boundary between the Zhukovian and Vokhmian regional stages. New stratigraphic data have led to the revision of the temporal distribution of Zhukovian and Vokhmian ostracodes. In contrast to previous ideas, the rapid development of genus Gerdalia already began in the Zhukovian time rather than in the Vokhmian. At the same time, the first Darwinula of the Triassic type also appeared in the Zhukovian. A proportion of the Permian species were found to cross the boundary between Zhukovian and Vokhmian. The degree of similarity between the Permian and Triassic ostracode assemblages turns out to be much higher than previously recognized.     

Multidisciplinary study of the Mechetlino Quarry section (Southern Urals,Russia) — The GSSP candidate for the base of the Kungurian Stage (Lower Permian)

The Mechetlino Quarry section is a potential candidate for the Global Section Stratotype and Point (GSSP) for the base of the Global Kungurian Stage on the International Stratigraphic Chart. In 2017, the Mechetlino Quarry section became the part of the First Geopark in Russia, therefore excavation work was carried out to clear it, a road was laid, and infrastructure was developed. Recent evidence to justify the base Kungurian boundary in the Mechetlino section was obtained. Additional conodonts confirmed the data of V.V. Chernykh on the Artinskian–Kungurian transition. Besides Neostreptognathodus pnevi Kozur and Movshovitsch, the second marker (N. lectulus Chernykh) of the base-Kungurian was established. The Artinskian–Kungurian transition of the Mechetlino Quarry section is characterized by the richest associations of small foraminifers, ammonoids, and other groups. The occurrence of mass Clausiuraloceras above the Kungurian boundary, which changed the representative Artinskian association, was identified. Small foraminifers of the Artinskian–Kungurian transition are numerous and include sufficient species to provide a correlation with Western Tethys, Svalbard and Australia. Data on isotopic ratios of δ¹³C and δ¹⁸O, δ¹³C_org values and the magnetic susceptibility were obtained for the first time.