红树林海洋细菌PLM4抑制肿瘤细胞生长活性多糖的纯化及结构分析

红树林海洋短小芽孢杆菌Bacillus pumilus（PLM4）的发酵液对人喉癌细胞Hep-2、肝癌细胞BEL-7404和舌癌细胞TCA8123的生长抑制活性分别为63．6％、59．2％和61．5％。PLM4发酵液经乙醇沉淀和凝胶柱层析纯化可得到多糖纯品。采用高效凝胶渗透色谱法测定其分子量和纯度,硫酸-咔唑法、2,4-二硝基苯肼比色法、氯化钡明胶比色法、茚三酮反应和气相色谱法等测定其组分。采用红外光谱分析、高碘酸氧化和Smith降解等方法研究其结构。结果表明,该多糖分子量为116kd,由己糖醛酸、甘露糖、葡萄糖和丙酮酸组成,其摩尔比为31：19：6：1,不含硫酸、乙酸和蛋白质。平均每100个己糖基中含有约42个1→3糖苷键、42个1→6糖苷键和／或非还原末端基、13．5个1→2糖苷键和2．5个1→4糖苷键。     

GC-MS联合二维核磁对文蛤多糖Fr.2A组分结构的解析

采用GC-MS联合二维核磁的方法,对文蛤均多糖结构进行解析。运用双酶辅助水提的方法,提取文蛤粗多糖(MMPX),分离纯化得到文蛤均多糖,并通过气质联用技术(GC-MS)和核磁共振波谱(1D,2D NMR),对文蛤均多糖的结构进行了分析。结果表明,从文蛤中提取得到文蛤粗多糖(MMPX),经分离纯化得到高纯度文蛤均多糖Fr.2A,其单糖组成为葡萄糖(Glc)。GC-MS分析发现,Fr.2A存在三种残基单元1,4-Glcp、T-Glcp和1,4,6-Glcp,摩尔比为5.58︰1.26︰1.0;核磁共振波谱分析表明,Fr.2A是以α-(1→4)与少量α-(1→6)连接为主链,并存在少量的α-(1→6)和β-(1→4)支链的新型水溶性D型吡喃葡聚糖。     

自养小球藻硫酸多糖的红外光谱分析

利用二乙胺基乙基琼脂糖凝胶柱层析纯化自养小球藻(Chlorella autotropica)粗多糖,得到3个硫酸多糖组分(A,B,C);利用高效液相色谱仪和熔点仪测定了3个多糖的分子质量和熔点;利用BaCl2浊度法测定了硫酸多糖中硫酸根的质量分数;利用傅立叶变换红外光谱分析了海水自养小球藻3个硫酸多糖组分的环状结构、半缩醛羟基构型及取代基类型。结果显示,3个硫酸多糖组分的硫酸根的质量分数分别为0.77%,8.46%,2.69%,3个组分均含有硫酸基、酰氨基,葡萄糖是3个硫酸多糖组分的主要组成单糖;3个硫酸多糖组分组成单糖的环构型均是吡喃环,成苷的半缩醛羟基构型有一定差异,A是α构型,B、C是α、β两种半缩醛羟基构型并存。为深入研究自养小球藻硫酸多糖的结构及抗癌活性提供基础。     

褐藻多糖硫酸酯的结构与生物活性研究

褐藻多糖硫酸酯（fucoidan,FPS）是所有褐藻中所固有的细胞间多糖,存在于细胞壁基质中。生长于潮间带、长时间与空气接触的褐藻种类中,如多年生的墨角藻（Fucus vesiculosus）类,其褐藻多糖硫酸酯的含量可高达20%;生长在较深处的海带（Saccharina japonica）类中含量较低,约为1%~2%。褐藻多糖硫酸酯是一类独特的结合有硫酸基的水溶性杂聚糖,其化学组成和结构非常复杂,以岩藻糖和硫酸基为主,随着褐藻的种类不同还含有半乳糖、木糖、糖醛酸等其他成分。褐藻多糖硫酸酯具有多种生物活性,目前针对墨角藻、泡叶藻（Ascophyllum nodosum）、鼠尾藻（Sargassum thunbergii）等褐藻中的褐藻多糖硫酸酯研究较多,发现其具有免疫调节、抗病毒、抗肿瘤、抗凝血、抗氧化等生物活性。本文主要就褐藻多糖硫酸酯的提取、纯化、结构及生物活性等方面研究进行综述。     

用13C-NMR光谱法研究几种红藻含硫半乳聚糖的结构特征

于１９８９年８月对采自青岛地区的５种红藻用冷水和热水分步提取或直接加热提取方法制备含硫半乳聚糖，对其多糖进行的＾１３Ｃ－光谱分析结果表明，扁江蓠多糖主要由琼胶糖和６－硫酸基－琼胶糖组分构成，海萝和多管藻多糖主要由６－硫酸基－琼胶糖组成，并含微量琼胶糖前体，６－ＯＣＨ３－琼胶糖组分，此两种藻的热水提取物中还含有微量２－ＯＣＨ３－琼胶糖，三叉仙菜的热水提取多糖主要由琼胶糖的前体组成；从海膜多糖谱图的信     

南海红树林内生真菌1356＃代谢产物的研究

从南海红树林内生真菌1356＃分离出两种鞘胺醇（A，B）和三种环二肽（C，D，E）。它们的结构通过IR，MS，1D NMR和2D NMR谱推导出来，（3'E,4E)-1-(-D-吡喃葡萄糖基－3－羟基－2－（2'-羟基十八碳酰基）氨基－10－甲－3',4,9-十八碳三烯（A）是一种新的鞘胺醇甙。     

厚藤共生真菌(Fusarium oxysporum Y24-2)胞外多糖的化学组成和结构研究

从厚藤共生真菌(Fusarium oxysporum Y24-2)发酵液中提取得到胞外多糖,以Q-Sepharose Fast Flow阴离子交换柱和Superdex S-75凝胶色谱柱对其进行分离纯化,得到纯度高的多糖组分F1S。采用HPGPC和HPLC对F1S的分子量及单糖组成进行分析,结果表明F1S主要由Man、Glc和Gal组成,其摩尔比为1.0∶1.9∶2.1,分子量为37.3kD。F1S的GC-MS和1D,2D-NMR分析表明,该多糖是以→6)-β-Galf(1→为主链,以→2)-α-Glcp(1→,α-Glcp(1→和β-Manp(1→为支链的杂多糖,支链取代于→6)-β-Galf(1→的O-2位。该厚藤共生真菌的胞外多糖为富含呋喃型半乳糖的结构新颖的具有多分支结构的中性杂聚多糖。     

三种绿藻多糖的提取及理化性质和活性比较

采用80℃水浴8h、乙醇沉淀、Sevage法去除蛋白质的方法提取湛江裂片石莼、肠浒苔和总状蕨藻多糖，并用Molish反应、Fehling反应鉴定多糖的化学性质，用苯酚-硫酸法测定多糖的总糖含量，用Dodgson法测定多糖的硫酸基含量，用Folin-酚法测定多糖的蛋白质含量．结果表明：3种绿藻的多糖提取率和多糖总糖含量以裂片石莼最高，分别为3．0％和72．6％，总状蕨藻最低分别为1．65％和38．6％；3种绿藻的硫酸基含量相差不大．总状蕨藻的蛋白质含量最高，为14．5％．3种多糖溶液作用于体外白血病细胞结果以总状蕨藻的抑制效果最明显，浓度为12mg／dm^3的总状蕨藻多糖溶液作用72h的抑瘤率达66％．     

浒苔多糖的分级纯化及保湿活性研究

用DEAE-Sepharose FF离子交换凝胶层析柱对浒苔(Enteromorpha)多糖进行分级纯化,利用HPLC色谱分析了单糖组成,并以甘油和透明质酸为对照,研究其吸湿和保湿活性。结果表明,浒苔多糖主要为葡萄糖醛酸-鼠李糖-木糖-甘露糖聚合物;浒苔多糖主要由两种组分组成,其一组分木糖和鼠李糖含量摩尔比为1.11:1,另一组分木糖和鼠李糖含量比为1:3.28;浒苔多糖具有与透明质酸相似的吸湿和保湿能力。     

一种灰树花菌丝体多糖GF4F1的结构特征及其抗肿瘤活性

以灰树花发酵菌丝体为原料，经过提取分离纯化得到1种水溶性多糖GF4F1，经高碘酸氧化、Smith降解、甲基化、红外光谱（IR）以及核磁共振波谱（NMR）等分析表明，该多糖是1种β-1, 3／1，6-葡聚糖，且小鼠体内实验结果表明其具有良好的抗肿瘤活性。在1mg／kg时，对小鼠抑制率为67.3％。     

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,     

Evaluation of the Risk of Marine Slope Instability: A Pseudo-3D Approach for Application to Large Areas

This article presents a methodology developed to evaluate the instability of submarine slopes that extend over a large area. Special attention was paid to (1) the complex geometry (bathymetry) and the expanse of the slope, (2) the heterogeneity of the sediment, and (3) the distribution of the pore pressure. The safety factor was considered as a spatially varying quantity. The General Formulation (GLE, Fredlund and Krahn 1977), which fully satisfies equilibrium conditions, was used for evaluating the stability of the marine slope. The submarine slope failure, which occurred on 16 October 1979 during the construction of the new Nice airport, was studied in order to test the developed model. Geotechnical parameters were taken from experimental tests carried out by IFREMER on 19 cores extracted at different depths (from 27 m to 1300 m) (Cochonat, Bourillet, and Savoye, 1993; Mulder et al., 1994). Many scenarios were proposed in order to explain the cause of the Nice slope failure (Habib, 1994). In this article, two of those scenarios were tested. Simulation results are presented and discussed.