69 resultados para Palissy, Bernard, 1510?-1590.
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β-羧乙基锗倍半氧化物(Ge-132)的无毒广谱抗癌作用以及潜在的治疗艾滋病的功能~[1~3]促进了Ge-132及其衍生物合成及生物活性研究~[4~6],而对锗原子直接与苯环及其衍生物连接的有机锗倍半氧化物的研究则相对较少.我们曾报道了~[7]p-(二甲氨基)苯基锗倍半氧化物的合成、结构及对癌细胞的作用,p-(二乙氨基)苯基锗倍半氧化物的研究尚未见报道.本文采用改进的方法合成了p-(二乙氨基)苯基锗倍半氧化物(Ge-164).通过元素分析、IP、XPS和TG-DTA确定了组成和结构,观察了它对体外培养人乳腺癌细胞有丝分裂的影响.
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Aims: To assess the diversity of antibiotic-resistant bacteria and their resistance genes in typical maricultural environments. Methods nand Results: Multidrug-resistant bacteria and resistance genes from a mariculture farm of China were analysed via cultivation and polymerase chain reaction (PCR) methods. Oxytetracycline (OTC)-resistant bacteria were abundant in both abalone and turbot rearing waters, accounting for 3.7% and 9.9% of the culturable microbes. Multidrug resistance was common, with simultaneous resistance to OTC, chloramphenicol and ampicillin the most common resistance phenotype. 16S rDNA sequence analyses indicate that the typical resistant isolates belonged to marine Vibrio, Pseudoalteromonas or Alteromonas species, with resistance most common in Vibrio splendidus isolates. For OTC resistance, tet(A), tet(B) and tet(M) genes were detected in some multidrug-resistant isolates, with tet(D) being the most common molecular determinant. For chloramphenicol resistance, cat II was common, and floR was also detected, especially in marine Pseudoalteromonas strains. Conclusions: There is the risk of multidrug-resistant bacteria contamination in mariculture environments and marine Vibrio and Pseudoalteromonas species serve as reservoirs of specific antibiotic resistance determinants. Significance and Impact of the Study: This paper and similar findings from Korea and Japan indicate the potential for widespread distribution of antibiotic resistance genes in mariculture environments from the East Asian region of the world.
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AXIS(14)C dating and grain-size analysis for Core DD2, located at the north of the Yangtze River-derived mud off the Zhejiang-Fujian coasts in the inner shelf of the East China Sea, provide us a high-resolution grain-size distribution curve varying with depth and time. Data in the upper mud layer of Core DD2 indicate that there are at least 9 abrupt grain-size increasing in recent 2000 years, with each corresponding very well with the low-temperature events in Chinese history, which might result from the periodical strengthening of the East Asian Winter Monsoon (EAWM), including the first-revealed maximum temperature lowering event at around 990 a BP. At the same time, the finer grain size section in Core DD2 agrees well with the Sui-Tang Warming Period (600-1000 a AD) defined previously by Zhu Kezhen, during which the climate had a warm, cold and warm fluctuation, with a dominated cooling period of 750-850 a AD. The Little Ice Age (LIA) can also be identified in the core. It starts around 1450 a AD and was followed by a subsequent cooling events at 1510, 1670 and 1840 a AD. Timing of these cold events revealed here still needs to be further verified owing to some current uncertainty of dating we used in this study.
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该文对中国黄海和东海的蓝细菌在春、秋两季的生态分布特点进行了研究和比较,对黄海蓝细胞从10月至次年6月的生态分布进行了研究.1.东黄海海区:在秋季(2000年10月19日至11月29日)和春季(2001年3月26日至4月24日)两个季节中蓝细菌丰度在0.19~7.84×10<'4>cell/ml之间,生物量在0.56~13.74μgC/L之间,整体水平上春季比秋季高(蓝细菌的丰充与生物量平均值春季分析为4.83×10<'4>cell/ml和7.25μgC/L;秋季分别为1.72×10<'4>cell/ml和5.07μgC/L),东海比黄海高(蓝细菌生物量平均值春季黄海和东海分别为4.42μgC/L和5.52μgC/L;秋季黄海和东海分别为7.02μgC/L和7.45μgC/L).2.黄海海区:黄海蓝细菌丰度与生物量随时间变化趋势为10月至12月降低(蓝细菌丰度分别为15×10<'4>cell/ml和1.19×10<'4>cell/ml,生物量分别为4.41μgC/L和3.49×10<'4>cell/ml),4月(蓝细菌丰度与生物量分别为4.68×10<'4>cell/ml和7.02μgC/L)与12月相比有明显增高,蓝细菌丰度4月是12月的3.93倍,生物量4月是12月的2.01倍,4月至6月蓝细菌生物量大致稳定,略有增加(5月和6月蓝细菌丰度分别为5.23×10<'4>cell/ml和5.25×10<'4>cell/ml,生物量分别为7.85μgC/L和7.88μgC/L).研究发现蓝细菌在水体中的垂直分布与温度变化比较一致.
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本论文报道从海洋中分离到的一株聚磷菌的分离、鉴定、在系统发育中的地位、除磷特性、菌体内多磷酸盐颗粒的研究、D-海因酶和核苷二磷酸激酶基因的克隆及序列分析,为海水系统的生物除磷提供部分基础资料。 从黄海海域分离到聚磷菌Halomonas sp. YSR-3,菌体呈杆状,大小为3.5 μm×1 μm,革兰氏阴性,好氧生长,能运动。透射电镜观察发现,菌体内有致密颗粒。经DAPI染色确定该致密颗粒是多磷酸盐,亦可称为异染粒、迂回体。16S rDNA鉴定结果表明,YSR-3与Halomonas属中的marine bacterium B5-7有较高的同源性,相似值99%。YSR-3的生理生化特性:对氯霉素和卡那霉素敏感;淀粉水解呈阳性;反硝化和几丁质降解呈阴性;能将葡萄糖作为唯一碳源和能源。 对YSR-3的培养条件进行优化。以海水2216培养基、24 ℃、180 rpm、pH 6.5的条件培养,更利于菌体生长和菌体内多磷酸盐的形成。 对YSR-3的除磷特性进行研究。无磷培养时,菌体不能生长;用磷酸钾盐作为磷源时,菌体生长较好,形成多磷酸盐的菌体比例较高;较适合YSR-3菌体生长和多磷酸盐形成的磷源是KH2PO4,较适磷浓度为1.5 mmol/L。pH的变化影响菌株的生长、多磷酸盐形成和除磷效果。pH值为5时,菌体的数量几乎不增加,体内多磷酸盐和培养基中磷含量变化不大;pH值为6、7和8时,菌体生长良好,95%以上的菌体内形成多磷酸盐,培养基中磷含量明显下降。YSR-3在不同培养基中除磷量和除磷率不同。在高磷培养基中除磷量为0.7 mmol/L(磷含量由1.84 mmol/L降到1.14 mmol/L),除磷率为37.5%;在低磷培养基中除磷量为0.02 mmol/L(磷含量由0.028 mmol/L降到0.008 mmol/L),除磷率为72.2%。 以海洋聚磷菌Halomonas sp. YSR-3的总DNA为模板,用PCR法扩增D-海因酶基因和核苷二磷酸激酶基因,将扩增片段克隆到pGM-T载体,转化E.coli TOP10菌株,经蓝白斑筛选、菌落PCR得到阳性克隆,测序后对序列进行Blast比对分析。得到的D-海因酶基因序列长度为1510 bp,与Pseudomonas entomophila L48的海因酶基因序列的相似性为77%。翻译后的序列与Pseudomonas fluorescens Pf-5,Marinomonas sp. MED121,Burkholderia vietnamiensis G4的海因酶蛋白序列相似性分别为75%,73%,70%。得到的核苷二磷酸激酶基因序列长度为420bp,翻译后的序列与Loktanella vestfoldensis SKA53,Jannaschia sp. CCS1,Roseobacter sp. CCS2的核苷二磷酸激酶蛋白序列相似性分别为89%,86%,85%。 聚磷菌能将外界环境中的磷吸收到体内,并以多磷酸盐的形式储存。多磷酸盐对于细胞的生存和生长有很重要的作用,但目前对于多磷酸盐的形成过程以及过程调控还不是很清楚。在今后可以通过构建高效表达的重组菌,提高与除磷相关的酶的纯度及活性。同时可以将相关酶的基因进行突变,对基因表达的调控以及酶的代谢以及功能结构等多方面进行基础研究,使聚磷菌在生物除磷中得到广泛应用。
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在中国,孔石莼应用于医药方面已有几千年的历史,其煎剂常被当地居民用来治疗中暑和泌尿方面的疾病。实验室以前所做的工作表明,孔石莼的水溶多糖具有很好的抗高血脂活性,本论文在此研究的基础上主要就多糖的长期毒性、一般药理、多糖的衍生化、不同分子量孔石莼多糖的抗氧化活性、衍生物的抗氧化活性和动物调血脂活性进行了研究。 水提醇沉制备多糖,多糖主要由糖醛酸、鼠李糖、木糖、葡萄糖和硫酸根组成,还含有微量的半乳糖、甘露糖和阿拉伯糖。多糖中主要的二糖重复单位为[β-D-Glcp A-(1->4)- α-L-Rhap 3S] 和 [α-L-Idop A-(1->4)- α-L-Rhap 3S]。急性毒性实验表明,KM小鼠对孔石莼多糖的最大耐受量(MTD)大于4000 mg/kg,其腹腔注射雌性小鼠的半致死量(LD50)为408.7 mg/kg,雄性动物为432.7 mg/kg。长期毒性(6个月)实验表明孔石莼多糖无毒反应剂量为1.2 g/kg。一般药理研究表明孔石莼多糖对小鼠中枢神经系统无明显影响,对麻醉犬心血管系统和呼吸系统均无明显影响。 采用过氧化氢降解的方法制备了不同分子量的孔石莼多糖,并且测定了体外抗氧化活性;制备了高硫酸根含量的孔石莼多糖、乙酰化和苯甲酰化孔石莼多糖衍生物,测定了体外抗氧化活性和动物调血脂试验。结果表明,不同分子量的孔石莼多糖其抗氧化活性是不同的,分子量低的孔石莼多糖表现出了较强的抗氧化活性。孔石莼多糖的衍生物其抗氧化活性要优于孔石莼多糖。调血脂动物试验表明,孔石莼多糖以及其衍生物都具有很好的调血脂效果。高硫酸根含量孔石莼多糖的中、低剂量组的调血脂活性要优于高剂量组(低剂量组降低低密度脂蛋白的能力要稍弱于原料),而且,中剂量组与原料组相比,小鼠血清TG明显降低(P<0.05),LDL-C 明显降低(P<0.01)。低剂量组乙酰化衍生物降低甘油三酯(TG)和低密度脂蛋白(LDL-C)的能力要优于中高剂量组。对于孔石莼多糖以及衍生物调血脂的机制还需进一步的研究。
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The formation and evolution of magedunes and lakes in Badain Jaran desert is focused by scholars for a long time. In this paper, detailed investigation was made with the Remote Sensing, Geographic Information Systems, climatological data of research region to study the evolution of magedunes, vegetation and lakes. The main conclusions are presented as follows: (1) The magedunes are mainly located in south and northeast of the desert. The density of magedunes decreases from south to north, east to west, and greatest in southeast of the desert. Most of magedunes strike NE30°~60°, and which are NE-SW and NNE-SSW directions. The distribution of magedunes’ strikes indicates that the paleowind of the desert is northwest and west wind. (2) The vegetation cover is low in the Badain Jaran Desert, but there are some well-vegetated areas in the desert, and the value of NDVI is 0.6107. In southeast of the desert, the vegetation degradated seriously from 1987 to 2000. (3) At about 2000, the total area of permanent lakes was 2231.64 hm2 (±5.9%) in southeast of Badain Jaran Desert. From 1960 to about 2000, the lakes changed as followings: in the early 30 years, the area of lakes increased, but after 1990 it decreased. When lakes were large, the toral area of lakes is 20648 hm2 in Badain Jaran Desert, much larger than that of present lakes. (4) From 1961 to 2001, the mean annual evaporation of lakes was 1039.8mm (±10%) in Badain Jaran Desert, and the difference between years was large. The monthly evaporation of lakes was mainly affected by rainfall, temperature. And it was largest in June, 140.9mm(±10%). (5) Based on water balance calculation of present lakes and old lakes in southeast of Badain Jaran Desert, the total precipitation is more than the total evaporation in this area. So it is probable that the precipitation in the lake area supplies water to the lakes, and also to groundwater in west and north part of the desert.
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Manganese-modified mesoporous MCM-41 molecular sieves were synthesized at the absence of alkaline metal ions under mild alkaline condition using cetylpyridinium bromide surfactant as a template, and characterized with X-ray diffraction, N-2 adsorption, transmission electron microscopy, electron spin resonance (ESR), and nuclear magnetic resonance (NMR) spectroscopies. The synthesized MnMCM-41 has a high pore volume of 1.30 cm(3) g(-1) with a corresponding surface area of 1510 m(2) g(-1). The ESR and Si-29 MAS NMR spectra revealed the presence of framework manganese ions in either the as-synthesized or calcined forms. (C) 2002 Elsevier Science B.V. All rights reserved.