圆斑星鲽连续性鳃细胞系的建立

为建立圆斑星鲽(Verasper variegatus)鳃细胞系,本文采用胰蛋白酶消化法启动了圆斑星鲽鳃组织的体外培养,并通过对培养液配方和培养条件的优化成功地进行了圆斑星鲽鳃细胞的原代培养和继代培养。结果显示,圆斑星鲽鳃细胞的最适培养液为含有20%胎牛血清(FBS)的DMEM/F-12培养液,培养液最适pH值为7.2,最适培养温度为22℃;通过向20%FBS-DMEM/F-12培养液(pH=7.2)中添加N-乙酰葡萄糖盐酸盐、羧甲基壳寡糖、碱性成纤维细胞生长因子(bFGF)及I型胰岛素样生长因子(IGF-I),在22℃成功启动了圆斑星鲽鳃细胞的原代培养,细胞的贴壁、生长和分裂状态良好,为典型的成纤维样细胞形态,30 d即可形成汇合的细胞单层;经连续继代培养后,已成功建立了连续性圆斑星鲽鳃细胞系,现已继代培养至第76代;该细胞系细胞经液氮冻存复苏后仍保持其原有的成纤维样细胞形态,其贴壁生长状态和增殖速度也与冻存前无差异;生长特性鉴定结果显示,第60代圆斑星鲽鳃细胞系细胞的群体倍增时间为43.6 h,表明细胞的生长分裂依然十分旺盛。染色体分析结果显示,圆斑星鲽鳃细胞系细胞虽然出现了染色体的非整倍性,但其特征性染色体数目仍为46条,并具有其典型的二倍体核型特征(46 t),表明所建立的细胞系确为圆斑星鲽鳃细胞系。该细胞系的建立对于病毒与宿主相互作用机理的研究及病毒疫苗的开发具有重要的理论和应用价值。     

褐点石斑鱼三种组织细胞系的建立

为建立褐点石斑鱼鳍、心脏和鳔组织细胞系,本文利用不同培养液和培养温度对褐点石斑鱼鳍、心脏和鳔组织细胞进行了原代培养和传代培养。实验结果显示,在24℃培养于含有羧甲基壳寡糖、碱性成纤维样生长因子、I型胰岛素样生长因子及20%胎牛血清的DMEM/F12培养液(pH=7.2)中的3种细胞,均为成纤维样细胞,其生长分裂状态最佳,可以持续稳定传代。第60代褐点石斑鱼鳍、心脏和鳔细胞的群体倍增时间分别为50.6 h、40.3 h和43.3 h,其特征性染色体数目均为48条。目前鳍、心脏和鳔细胞已分别传至第90代、第70代和第75代,已成功建立了3种细胞的连续性细胞系,为鱼类病毒与宿主细胞相互作用机制等鱼类病毒学基础研究,以及鱼类病毒的分离、鉴定、繁殖及病毒疫苗研制等奠定了基础。     

大黄鱼鳍细胞系的建立及久效磷对其毒性作用的研究

为了建市大黄鱼(Pseudosciaena crocea)鳍细胞系,为其细胞毒理学、病毒学与细胞工程等研究奠定基础,本文采用酶消化法使用含有20%胎牛血清(FBS)的DMEM/F12、Leibovitz L-15和DMEM培养液(pH7.2)在22～28℃分别启动了大黄鱼鳍组织的体外培养,通过添加促细胞贴壁和分裂的物质在最适堵养条件下对大黄鱼鳍细胞进行了原代培养和继代培养,并研究了久效磷对大黄鱼细胞系鳍细胞的毒性作用.体外培养结果显示,大黄鱼鳍细胞的最适培养液为20%FBS-DMEM/F12,最适培养温度为25℃,体外培养鳍细胞的形态主要为成纤维细胞样,22 d后便可形成汇合细胞单层,经过连续继代培养成功建立了大黄鱼的连续性鳍细胞系,目前已传至第112代;对第60代大黄鱼鳍细胞系细胞的鉴定结果显示,其群体倍增时间为50.96 h,分裂状态十分旺盛,虽然出现了染色体的非整倍性,但其特征性染色体数目仍为48条,并具有正常的6m+6sm+36t二倍体核型,证明所建立的细胞系确为大黄鱼鳍细胞系.不同浓度久效磷处理的检测结果显示,大黄鱼鳍细胞对久效磷敏感,20～160 μg/mL久效磷可引起鳍细胞乙酰胆碱酯酶活性的持续性显著降低,引起超氧化物歧化酶和谷胱甘肽-S-转移酶活性的显著升高并随着浓度的升高而逐渐降低,久效磷对该细胞系细胞的48 h半抑制浓度(IC50)为43.05 μg/mL,,证实久效磷对大黄鱼鳍细胞具有显著的毒性作用.     

锦鲤组织细胞体外培养的初步研究

为建立来源于锦鲤的细胞系,本文采用组织块法,对来源于锦鲤(Cyprinus carpio)鳍条、吻端、肌肉、心脏、鳔、肠道、卵巢等组织的细胞进行原代培养和传代培养.在25℃下,添加20％胎牛血清、0.2μg/mL表皮生长因子(EGF)和25ng/mL成纤维生长因子(FGF)的L-15培养基中进行培养.结果显示,鳍条、心脏、鳔、吻端、肌肉、肠道、卵巢分别在原代培养第3、6、12、13、15、3、3天,有细胞从组织块迁出;对长至单层的鳍条、心脏、肌肉细胞进行传代培养,鳍条细胞已传至第39代,心脏和肌肉细胞分别传到第2代和第4代;鳍条、心脏和肌肉细胞分别呈现上皮细胞样、上皮细胞样和上皮细胞样与成纤维状混合型.第6代锦鲤鳍细胞的染色体计数,结果显示,细胞染色体数目分布范围为55～154条,2n=100.病毒敏感性实验,发现锦鲤鳍条细胞对草鱼出血病病毒(GCRV)和鲤春病毒血症病毒(SVCV)都敏感,且在24h内出现细胞病变(CPE);但对斑点叉尾鮰病毒(CCV)不敏感.锦鲤鳍条细胞系的建立为后期建立更多的锦鲤细胞系和鱼类病毒研究奠定了基础.     

宽纹虎鲨软骨细胞体外培养的启动

以活体宽纹虎鲨(Heterodortus japonicus)的鳃软骨和鳍软骨组织为材料,利用透明质酸酶(hyaluronidase)、Ⅱ型胶原酶(type Ⅱ collagenase)和胰蛋白酶(trypsin)进行消化获得游离软骨细胞,对所得游离细胞连同软骨组织分别用含20％小牛血清的MEM培养液进行体外培养。对软骨细胞体外培养条件的优化结果显示,宽纹虎鲨鳍软骨细胞体外培养的最适pH为7．2～7．6、最佳温度为24℃,成纤维细胞生长因子(bFGF,basic fibroblast growth factor)对软骨细胞作用不显著。培养于pH7．2～7．6的MEM培养液(含20％小牛血清)中的宽纹虎鲨鳍软骨组织,在24℃启动培养3d后便有软骨细胞开始陆续从组织中迁出,新迁出细胞的形态多为圆形,随着培养时间的延长,部分细胞形态逐渐转变成上皮样。     

大菱鲆红体病虹彩病毒体外增殖条件的研究

探讨大菱鲆病毒疫苗的研制,以牙鲆鳃细胞(FG细胞)为增殖体系,利用细胞病变效应(CPE)为判断指标,对大菱鲆红体病虹彩病毒(Turbot reddish body iridovirus,TRBIV)的体外最适增殖条件等进行了研究。结果表明,病毒接种量、病毒吸附时间、细胞培养条件对TRBIV的体外增殖均有明显的影响,以0.2 mL病毒液接种FG细胞、吸附2 h、用含10%胎牛血清的MEM培养液于22℃培养时,病毒的增殖速度最快。研究还发现,病毒的收获时间和病毒液冻融次数对所得病毒的感染力均有显著影响,在最佳增殖条件下,病毒在FG细胞中增殖至第4天时进行收获,且只冻融1次,其感染活性最强,反复冻融后病毒的感染活性会显著降低。     

利用牙鲆鳃细胞系分离和培养淋巴囊肿病毒

本文利用牙鲆鳃细胞系进行了养殖牙鲆淋巴囊肿病毒的分离及培养 ,并通过电镜对培养细胞中淋巴囊肿病毒的形态及感染循环进行了初步研究。将病鱼的淋巴囊肿组织无菌滤液接种牙鲆细胞系 ,细胞出现了明显的细胞病变 ( Cytopathic effect,CPE)。电镜观察在培养细胞的胞质中有病毒的包涵体 ,胞质中散在 6角形、5角形或圆形的病毒粒子 ,大小为 10 0～ 140 nm之间。在感染细胞的线粒体中也存在大量的病毒颗粒。     

凡纳滨对虾血淋巴、类淋巴细胞培养

以 ×L-15 培养基为基础,添加不同比例的胎牛血清和对虾肌肉提取液配制成不同的培养液,当 22×L-15培养基、胎牛血清和对虾肌肉提取液的比例分别为 60 %、20 %、20 %时,培养效果较好。培养液 pH 维持在7.0 ~ 7.2时血淋巴和类淋巴细胞生长最好,且类淋巴细胞迁出迅速。绝大部分血淋巴细胞贴壁迅速并伸展成多角样或披针形,一般存活 7 ~ 9 d,少部分呈悬浮状态的血淋巴细胞存活达 60 d 以上。培养中如未及时去除对虾血清,血淋巴细胞迅速衰老并死亡。类淋巴组织细胞 6 d可形成单层,迁出细胞主要有两种形态: 多角样和成纤维样,细胞可存活 16 d以上。     

姬松茸提取物组分体外抗病毒感染活性的研究

为了探明姬松茸提取物的体外抗病毒感染活性及其作用方式,进而为水产养殖鱼类高效抗淋巴囊肿病毒(lymphocystis disease virus,LCDV)感染活性物质的开发和鲆蝶类淋巴囊肿病的防治奠定基础,利用热水浸提和酒精沉淀法得到了5种姬松茸提取物组分(E1～5),并利用MTT、细胞病变程度观察等方法研究了5种组分对LCDV感染体外培养大菱鲆鳍细胞(turbot fin cells,TF细胞)的影响作用.细胞毒性实验结果显示,5种组分对体外培养TF细胞均无毒性.细胞病变程度结果表明,本文所得5种姬松茸提取物组分尤其是E5组分具有显著的抗LCDV感染TF细胞的活性.不同方式感染的实验结果进一步显示,5种姬松茸提取物组分抗LCDV感染TF细胞的作用可能主要是通过直接灭活病毒和/或阻断病毒吸附细胞来实现的.     

云纹石斑针淋巴囊肿病病变过程的超微研究

于１９８９１－９９０年，对海水网箱养殖的云纹石斑鱼自然感染和人工感染的淋巴囊肿病进行电镜观察。观察结果表明，自然感染和人工感染的淋巴囊肿细胞之间并无区别，经们均含有许多包涵体和病毒颗粒；主要描述用患淋巴囊肿病鱼的皮肤结节匀浆对实验鱼 下注射而感染的淋巴囊肿病的超微病理过程，包括病毒颗粒在成纤维细胞胞膜上的附着和成纤维细胞及其内含物的形态变化等过程；此外，病鱼心脏、肝脏、脾脏、肾脏和肠上皮也有不同程     

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.