苯并异噻唑啉酮类衍生物的制备与生物活性测试

以1,2-苯并异噻唑-2(3H)-酮为原料合成了3-羰基苯并异噻唑-2(3H)-苯甲酸甲酯衍生物,目标化合物的结构经元素分析、<'1>H NMR和质谱确证.化合物对大肠杆菌、金黄色葡萄球菌、溶藻弧菌、嗜水气单胞菌、枯草芽孢杆菌5种海洋菌的抑菌活性结果表明,化合物对上述菌种均有不同程度的抑制作用,其中对大肠杆菌活性最高,...     

2-(N-芳基氨甲基)苯并异噻唑啉酮类化合物对海洋浮游生物的生长抑制活性研究

本文研究了13个2-(N-芳基氨甲基)苯并异噻唑啉-3-酮类化合物对球等鞭金藻Isochrysis galbana、亚心形扁藻Platymonas subcordiformis及舟形藻Navicula的生长抑制性能,并测试了其对藤壶二期无节幼虫的生物活性。结果表明:2-(N-芳基氨甲基)苯并异噻唑啉-3-酮类化合物对球等鞭金藻、亚心形扁藻和舟形藻都有良好的生长抑制活性,其中对球等鞭金藻和亚心形扁藻的抑制作用较强;对藤壶幼虫的生物活性测试表明,化合物最低质量浓度为2.0 mg/L时,除化合物g和l,都具有良好的生长抑制活性。化合物的结构与浮游生物的生长抑制活性关系表现为间位取代优于对位取代。     

取代异噻唑啉酮类化合物抗菌活性的定量构效关系研究

用密度泛函理论(DFT)和逐步回归分析方法对具有抗菌活性的18种新合成的取代异噻唑啉酮类化合物进行了定量构效关系(QSAR)研究。在B3LYP/6-31G(d,p)水平上,对异噻唑啉酮类化合物进行了构型全优化,并提取部分量子化学参数,通过逐步多元回归分析,筛选了影响抗菌活性的主要因素,建立了定量构效关系方程。结果表明,C(5)的亲核电子密度fCN(5)与S(1)-N(2)的键级BS(1)-N(2),是影响异噻唑啉酮类化合物抗大肠杆菌活性的主要因素,所得QSAR模型对该类化合物抗菌活性有较好的预测效果。     

常山酮的合成方法研究

本文对常山酮(halofuginone)的合成方法进行了研究和改进,以2-甲基-3-羟基吡啶为起始原料,其甲基化产物与乙腈加成后经Rh/Al2O3选择性还原得(3-甲氧基-2-哌啶基)-丙酮,再经溴代、N-保护后与6-氯-7-溴-4(3H)-喹唑啉酮偶联,产物经水解脱保护得目标化合物6-氯-7-溴-3-(3-(3-羟基-2-哌啶基)-丙酮基)-4(3H)-喹唑啉酮氢溴酸盐,通过6步反应制得了常山酮,总收率为11.6%,为常山酮的工业化生产提供了可能。目标产物和各步中间体结构经MS1、H NMR和13CNMR确证。     

四种卤代PTP1B抑制剂的化学合成及其活性研究

从松节藻中分离的含卤素化合物表现出显著PTP1B抑制活性。其中BPN效果最佳。为研究BPN侧链基团极性对其抑制活性的影响,本文以香兰素(1)为起始原料,经过溴代、氧化、还原、傅克烷基化以及酯化等反应,成功合成了新化合物2,3-二溴-1-(2-溴-3,4-二甲氧基-6-((4-硝基苯氧基)甲基)苯甲基)-4,5-二甲氧基苯(10)、4-((3-溴-2-(2,3-二溴-4,5-二甲氧基苄基)-4,5-二甲氧基苄基)醚)苯胺(11)、4-((3-溴-2-(2,3-二溴-4,5-二甲氧基苄基)-4,5-二甲氧基苄基)醚)-4-乙酰乙酸(12)和3-溴-2-(2,3-二溴-4,5-二甲氧基苄基)-4,5-二甲氧基苯甲醛肟(14)。通过1 H-NMR,13C-NMR等方法对目标产物进行了结构表征。并对化合物进行了PTP1B酶抑制活性的测定,结果表明化合物侧链极性对PTP1B酶抑制活性有显著影响。     

老鼠簕植物内生真菌Aspergillus terreus (W-8)抗肿瘤活性成分的研究

对红树林植物的枝干、枝叶样品进行微生物分离,以P388细胞为模型进行活性评价得到14株具有抗肿瘤活性的真菌。采用溶剂萃取、柱色谱及半制备HPLC等分离手段对来源于红树林植物老鼠簕Acanthus ilicifolius Linn.的菌株Aspergillus terreus(W-8)发酵产物进行了活性追踪分离,共得到5个化合物。通过理化性质及波谱技术,结合文献,鉴定其结构分别为aspulvinone H1(1)、aspulvinone H(2)b、utyrolactone I(3)t、errein(4)和3-propylbenzene-1,2-diol(5),其中化合物1的核磁数据为首次报道。采用MTT法初步评价了单体化合物的抗肿瘤活性,结果表明化合物4、5对A549、K562和Hela细胞均具有中等强度的细胞毒活性。     

海绵共附生放线菌SH6004菌株中抗肿瘤活性成分的研究

研究共附生微生物,采用活性追踪的方法从1株海绵共附生放线菌SH6004的乙酸乙酯提取物中分离得到7个化合物,根据化合物的光谱特征和理化性质分别鉴定为N-甲基苯甲酰胺(1),2-苯甲酰氧基乙酸(2),对羟基苯乙酰胺(3),N-[2-(4-羟基苯基)乙基]乙酰胺(4),环-(丙-异亮)(5),尿嘧啶-2′-脱氧核苷(6)和胸腺嘧啶-2′-脱氧核苷(7).并利用SRB(丽丝胺罗丹明B)法,对7个单体化合物的体外抗肿瘤活性进行了初步评价,其中化合物3、6和7显示了弱的抗肿瘤活性.     

几种喜树碱-糖缀合物的合成及其抗肿瘤活性研究

以喜树碱为母体,分别以甘氨酸和己二酸为连接臂与喜树碱的20-羟基以酯键缩合,再将其分别与半乳糖、甘露糖、乙酰氨基葡萄糖、乳糖的衍生物缩合定向半合成了3个水溶性(4-6)和1个脂溶性的喜树碱-糖缀合物(7),通过核磁共振氢谱、碳谱和高分辨质谱对化合物结构进行了确证。对已有的α构型喜树碱糖缀合物(1-3)和本文合成的β构型的喜树碱糖缀合物(4-7)的构效关系进行了初步的探讨,体外抗肿瘤实验表明,水溶性糖缀合物(1-6)具有与喜树碱相当的活性,脂溶性糖缀合物(7)的活性有明显下降。     

微波辐射下嘌呤C-2,6位衍生物及“Reversine”的合成

以2,6-二氯嘌呤为原料,微波辐射法合成了"Reversine"[1,2-(4-吗啉苯胺基)-N6-环己基腺嘌呤]的重要中间体2-氯-6-环己胺基嘌呤及其衍生物3b～3f,再以2-氯-6-环己胺基嘌呤为原料,微波辐射下合成了2-苯胺基-6-环己胺基嘌呤及"Reversine"。探索了合适的反应条件及影响因素,产物的结构通过1 H NMR进行了表征。研究表明,微波法可大幅提高合成嘌呤2,6位衍生物收率并缩短反应时间,为嘌呤衍生物及"Reversine"的合成提供了一种绿色、简洁高效的合成方法。     

中国南海短指软珊瑚中化学成分的研究

运用硅胶柱层析、Sephadex LH-20凝胶柱层析和HPLC等技术,采用活性追踪分离的方法,对南海短指软珊瑚Sinularia sp.的化学成分进行了研究.从乙醇提取物中分离获得单体化合物,运用NMR,MS等波谱技术鉴定了8个化合物的结构,分别为:3β-羟基-24-亚甲基胆甾-5-烯-7-酮(1),孕甾烯醇酮(2),cembrene A(3),epoxycembrane A(4),4,8,12-trimethyl-1-(1-methylethenyl)-3,7-cyclotetradecadien-10-one(5),(3E,7E,11E)-11,12-dihydroxy-1-isopropyl-4,8,12-trimethyicyclotetradeca-1,3,7-triene(6),邻苯二甲酸二丁酯(7)和十九烷-2-酮(8).化合物5和8为首次从珊瑚动物中分离得到,6为首次从短指软珊瑚属中分离得到.化合物3和4显示较强的卤虫致死活性.西松烷二萜类化合物是该短指软珊瑚中的重要活性成分.     

Microbial Biomass and Organic Nutrients in the Deep-Sea Sediments of the Central Indian Ocean Basin

In order to assess the impact of deep-sea mining on the in situ benthic life, we measured the microbial standing stock and concentration of organic nutrients in the deep-sea sediments of the Central Indian Ocean Basin in the Indian pioneer area. Sediments were collected using box core and grab samples during September 1996. The total bacterial numbers ranged from 10 10 -10 11 cells per g -1 dry weight sediment. There was a marginal decrease in the number of bacteria from surface to 30 cm depth, though the subsurface section registered a higher number than did the surface. The highest numbers were encountered at depths of 4-8 cm. The retrievable number of bacteria were two orders less in comparison with the direct total counts of bacteria. An almost homogeneous distribution of bacteria, total organic carbon, living biomass, and lipids throughout the depth of cores indicates active microbial and benthic processes in the deep sea sediments. On the other hand, a uniform distribution of total counts of bacteria, carbohydrates, and total organic carbon in all the cores indicates their stable nature and suggests that they can serve as useful parameters for long-term monitoring of the area after the benthic disturbance. Further studies on temporal variability in this region would not only verify the observed norms of distribution of these variables but would also help to understand restabilization processes after the simulated benthic disturbance.     

海上大直径钢管桩打桩过程中桩周土强度弱化研究

海上大直径钢管桩打桩过程中,桩周土体受到强烈扰动而发生强度弱化,掌握桩周土体强度弱化规律对于准确预测打桩过程、保证工程安全具有重要意义。为研究土体强度弱化规律,开展了环剪试验模拟打桩对桩周土体的扰动,测试土体强度随剪切速率的变化规律,建立了描述土体强度弱化规律的拟合公式,引入到打桩分析软件中。研究结果表明：土体的强度折减程度不仅与土体本身的性质有关还受到土体的埋深和剪切速率的影响,埋深越深土体强度折减程度越低,剪切速率越高土体强度折减越高,在打桩分析中可采用这里推荐的线性折减方法来模拟不同深度处土体强度的折减规律。     

Geoacoustic Inversion via Genetic Algorithm and Its Application to Manganese Sediment Identification

An acoustic inversion method using a wide-band signal and two near field receivers is proposed and applied to multiple layered seabed models including a manganese sediment. The inversion problem can be formulated into a probabilistic model comprised of signals, a forward model, and additive noise. The forward model simulates wide-band signals, such as chirp signals, and is chosen to be the source-waveletconvolution plane wave modeling method. The wavelet matching technique, using weighted least-squares fitting, estimates the sediment sound-speed and thickness on which determination of the possible numerical ranges for a priori uniform distribution is based. The genetic algorithm is applied to a global optimization problem to find a maximum a posteriori solution for determined a priori search space. Here the object function is defined by an L 2 norm of the difference between measured and modeled signals. Not only the marginal pdf but also its statistics are calculated by numerical evaluation of integrals using the samples selected during importance sampling process of the genetic algorithm.     

Phylogenetic diversity and phenotypic characterization of cultivable bacterioplankton isolated from polar oceans

A set of 27 marine planktonic bacteria isolated from the polar regions was characterized by 16S rDNA sequencing and physiological and biochemical testing. More than half of these bacteria were positive for caseinase, gelatinase and 13-glucosidase, and could utilize glucose, maltose or malic acid as carbon source for cell growth. Twelve isolates expressed nitrate reduction activities. Except for one antarctic isolate BSwlO175 belonging to Actinobacteria phylum, these isolates were classified as γ-Proteobacteria, suggesting that γ-Proteobacteria dominated in cultivable marine bacterioplankton at both poles. Genus Pseudoalteromonas was the predominant group in the Chukchi Sea and the Bering Sea, and genus ShewaneUa dominated in cultivable bacterioplankton in the Prydz Bay. With sequence similarities above 97%, genus Psychrobacter was found at both poles. These 27 isolates were psychrotolerant, and significant 16S rDNA sequence similarities were found not only between arctic and antarctic marine bacteria （ 〉 99% ）, but also between polar marine bacteria and bacteria from other aquatic environments （ ≥ 98.8% ）, including temperate ocean, deep sea, pond and lake, suggesting that in the polar oceans less temperature-sensitive bacteria may be cosmopolitan and have a bipolar, even global, distribution at the species level.     

Deep-Sea Sediment Compression Curves: Some Controlling Factors, Spurious Overconsolidation, Predictions, and Geophysical Reproduction

Oedometer tests have been carried out on 70 undisturbed surficial clays (at approximately 250 mm below the mudline), mostly collected by free-fall corers from sites widely scattered throughout the deep-sea North Atlantic. Acoustic measurements were also made, initially on contiguous samples and ultimately on the same sample using a geophysically instrumented oedometer which also collected electrical resistivity data. Apart from those quiescent areas below the carbonate compensation depth, such as north of the West Indies where very fine clays exist, most of the samples are silty clays whose geotechnical-geophysical properties are dependent on the type of clay minerals present (and their ability to take in moisture), the sand-size fraction, and the quantity of carbonate present. Thus the pure clays have high compressibilities which decrease on the addition of coarse particles, while the converse is true for the acoustic parameters, these increasing with the sand fraction. Using the notion of the intrinsic compression line for all samples, and comparison to it of the measured compression curves, it is clear that, contrary to some previously held ideas, most deep-sea clays are normally consolidated; the addition of carbonate has the effect of creating an open, stronger sediment skeleton. Interestingly, where information is available, the variation with depth of a sample's acoustic velocity follows the void ratio pressure relationship of the compression curve. This allows the construction of an in-situ sediment compression curve using the in-situ geophysical observations.     

INFORMATION FOR AUTHORS

<正>Acta Oceanologica Sinica(AOS)is a comprehensive academic journal edited by the Editorial Committee of Acta Oceanologica Sinica and is designed to provide a forum for important research papers of the marine scientific community which reflect the information on a worldwide basis.The journal publishes scholarly papers on marine science and technology,including physics,chemistry,biology,     

Estimation of Sediment Properties during Benthic Impact Experiments

Sediment properties, such as water content and density, have been used to estimate the dry and wet weights, as well as the volume of sediment recovered and discharged, during benthic impact experiments conducted in the Pacific and Indian Oceans. The estimates show that the weights of dry (355-1332 t) and wet sediment (1651-4888 t) recovered during the experiments, are not only a function of the total duration and distance covered during the experiment, but also depend on water content and density of the sediment. Estimation of dry sediment and its volumetric ratio in the discharge, are key parameters for calculating the discharged volume. The estimated volume of wet sediment recovered (1427-4049 m 3 ) as well as discharged (2693-6951 m 3 ) during the experiments, provide important inputs to evaluate the sediment resettlement and migration. Using these estimates, the average depth of excavation on the seafloor, can also been calculated. However, the stages of sediment recovery and discharge are expressed differently in some of the experiments. In order to standardize these, different stages have been identified, and definitions of certain terms have been suggested, for use in the future. The methods of calculating different properties, as well as weight and volume of discharged sediment are described in the paper for use in other applications concerning deep-sea discharges.