大西洋牙鲆幼鱼肌肉组成与营养需求的探讨

测定了养殖大西洋牙鲆幼鱼肌肉中的蛋白质、脂类、灰分等生化组织,并计算了其比能值,分析了肌肉蛋白质中17种常见氨基酸的含量、脂肪酸组成及含量。结果表明:大西洋牙鲆属高蛋白、低脂肪、低比能值鱼类,肌肉氨基酸含量同其它鲆鲽鱼类相比,属中等水平,必需氨基酸和呈味氨基酸的含量较高;肌肉蛋白中氨基酸的支/芳值为2.794;脂肪酸含量中棕榈酸(16∶0)的含量最高,其次为油酸(18∶1 n)和DHA(22∶6 n-3);其EPA(20∶5 n-3)和DHA(22∶6 n-3)的含量较高,营养丰富且平衡良好,是值得推荐的优良养殖品种和食用鱼类。     

牙鲆鱼白化病因的研究进展

牙鲆鱼(Paralichthys olivaceus)在我国俗称比目鱼、偏口,属于鲽形目,鲽总科,鲆科,牙鲆属。该鱼肉细嫩、口感好、营养高,在我国是一种很受欢迎的经济鱼类。分布于干岛群岛至香港之间,我国的渤海、黄海、东海、日本沿海、朝鲜半岛西岸均有分布。牙鲆是冷水性、底栖、肉食性经济鱼类,也是重要的海水养殖鱼类。在国外,日本最早于50年代就开始进行牙鲆人     

南方池养牙鲆全人工配合饲料饲养试验

采用全人工配合饲料(试验组饲料)与湿颗粒饲料 (对照组饲料 )对南方池养牙鲆进行为期 204d的饲养试验.结果表明,试验组与对照组牙鲆的尾相对增重率分别为 2 304%、2 297%,尾平均日增重差异不大,平均饲料系数分别为 1. 56、2. 58,牙鲆增重 1kg所需饲料成本分别为 10. 92元和 13. 55元,试验组比对照组节省饲料成本2. 63元 /kg鱼增重;试验组与对照组牙鲆平均内脏比 (分别为 6. 50%、6. 38% )、平均丰满度(分别为 1. 09、1. 07)、肌肉粗蛋白含量、粗脂肪含量等差异不显著(p>0. 05),10种必需氨基酸和 5种鲜味氨基酸的含量很接近.由此可见,南方池养牙鲆采用全人工配合饲料饲养是完全可行的.     

海产鱼类中异尖线虫酶消化检测技术的研究与应用

以3种海鱼(牙鲆、狭鳕、鲱鱼)为样本,针对海产品中主要的致病性寄生虫-异尖线虫,开展了酶消化检测技术的研究.根据鱼肉消化前后干物质的质量变化设计了胃蛋白酶消化效率的计算方法,并按照鱼肉:消化液＝1:10 (g/mL)的反应比例,分别确定了酶水解鱼肉的最佳条件为:初始pH值为1.1,温度为37 ℃,酶活力为8 U/mL左右;消化后所得的虫体采用多重PCR方法替代传统的形态学观察进行种属鉴定,从而初步建立了基于酶水解-多重PCR的异尖线虫的酶消化检测体系.实际样本检测表明,该技术可以较为准确、快速地用于海产鱼类中简单异尖线虫(Anisakis simplex)和伪地新线虫(Pseudoterranova decipiens)的确证性检测.     

中国鳜亚科(Sinipercunae)——七种鱼类骨骼形态特征的比较研究

对中国鳜亚科七种鱼类的骨骼进行比较。指出这七种鱼类之间存在着明显的类群差异,提出将鳜亚科分为三个属,即少鳞鳜属Coreoperca)、鳜属(Siniperca)和长身鳜属(Core-osiniperca);广西与福建的斑鳜和大眼鳜不存在种的分化,而福建产暗鳜(S.obscura Nichols)与广西暗鳜在某些骨骼形态特征上存在某些差异。     

东南沿海几种经济鱼类肌肉组织学比较研究

采用石蜡组织切片的方法,对大黄鱼(Pseudosciaena crocea)5个品系以及斜带髭鲷(Hapalogenys nitens)、牙鲆(Paralichthys olivaceus)、青石斑鱼(Epinephelus awoara),尼罗罗非鱼(Tilapia nilotica)和条纹斑竹鲨(Chiloscyllium plagiosum)等鱼类肌肉纤维组织学特性的研究表明:野生大黄鱼与野生养殖品系肌肌肉纤维在组织学上没有明显差异,而雌核发育品系及其杂交后代则相对野生品系表现出显著差异,它们的肌肉纤维更细密;不同种鱼之间肌肌肉纤维在组织学表现出巨大的差异,是与各个种类的遗传特征和生存模式相适应的.     

饲料中添加还原型谷胱甘肽对牙鲆生长和抗氧化能力的影响

以酪蛋白、明胶为主要蛋白源配制精制基础饲料,添加不同浓度梯度的还原型谷胱甘肽(GSH),饲料中GSH的含量分别为0、97.96、189.92、371.84、688.72和1 063.56 mg.kg-1,在流水式养殖系统中分别投喂初始体质量为(9.49±0.22)g的牙鲆(Paralichthys olivaceus)幼鱼,8周后观测各组牙鲆的生长情况及机体的抗氧化状态。结果表明,饲料中添加外源的GSH对牙鲆成活率没有显著影响(P>0.05);牙鲆增重率(WGR)在饲料GSH含量为371.84 mg.kg-1时达到最大值,显著高于其它各组(P<0.05);饲料GSH添加组牙鲆肝脏中GSH的含量显著高于零添加组(P<0.05);各处理组肝脏中丙二醛(MDA)的含量没有显著差异(P>0.05);肝脏中谷胱甘肽还原酶(GR)的活力随饲料中GSH含量的升高呈现先降低后上升的趋势,并在饲料中GSH含量为371.84 mg.kg-1时达到最低值;肝脏中超氧化物歧化酶(SOD)和谷胱甘肽过氧化物酶(GPx)活力没有受到饲料中GSH含量的显著影响(P>0.05);饲料中GSH含量为371.84 mg.kg-1时,肝脏中总抗氧化力(T-AOC)显著高于1 063.56 mg.kg-1组(P<0.05),谷胱甘肽-S-转移酶(GST)活力显著低于其它各组(P<0.05)。根据WGR的实验数据,利用折线模型得到牙鲆幼鱼饲料中GSH的适宜含量为368.92 mg.kg-1,过高或过低都会对生长造成负面影响,抑制机体抗氧化能力,增加机体氧化压力。     

微颗粒饲料中添加谷氨酰胺对大黄鱼稚鱼生长、存活及消化酶活力的影响

以初始体质量为(2.75±0.31)mg的大黄鱼(Pseudosciaena crocea)稚鱼(15日龄)为实验对象,在基础饲料中分别添加0.00%(对照组)、0.60%、1.20%和1.80%的谷氨酰胺,并用甘氨酸调节总蛋白质水平一致,制作而成4种粗蛋白58%左右、粗脂肪16%左右的实验微颗粒饲料,在室内养殖系统中投喂大黄鱼稚鱼30 d,研究饲料谷氨酰胺对大黄鱼稚鱼生长、存活及消化酶活力的影响。实验结果表明,大黄鱼稚鱼的特定生长率和存活率随饲料中谷氨酰胺含量的升高有上升的趋势,但差异未达到显著水平(P0.05)。饲料中谷氨酰胺的添加未对大黄鱼稚鱼肠段、胰段胰蛋白酶活力和淀粉酶活力,肠段氨基肽酶活力和碱性磷酸酶活力产生显著的影响(P0.05)。饲料中添加谷氨酰胺未能对大黄鱼稚鱼的生长、存活和消化酶活力产生显著的影响,可能与基础饲料中鱼粉、鱼肉水解蛋白等蛋白源所含有的谷氨酰胺已经达到或超过稚鱼吸收、利用谷氨酰胺的阈值,额外添加的谷氨酰胺不能被吸收利用而未能表现出促进效果。本实验条件下,大黄鱼稚鱼基础饲料中无需额外添加谷氨酰胺即可满足稚鱼正常生长发育的需要。     

大黄鱼精液的高效超低温保存

采用2 mL的冷存管和程序降温仪高效超低温保存大黄鱼(Pseudosciaena croce)精液。分析比较了5种不同浓度抗冻剂(二甲基亚砜、乙二醇、丙二醇和甘油和甲醇)、3种降温速率(10,20和30℃/min)和2种解冻温度(28℃和43℃)对大黄鱼精液超低温保存效果的影响。实验结果表明,采用Hanks’作为稀释液,10%～20%甘油或10%DMSO作为抗冻剂,20℃/min的降温速率对精液进行超低温保存43℃水浴解冻,冻精激活后获得理想的运动率(76.6%±11.4%～80.0%±12.6%),而且对10%甘油保存的冻精进行人工授精实验获得了与新鲜精液相似的受精率和孵化率。     

天鹅湖长蛸营养成分的分析及评价

对长蛸(Octopus minor)肌肉组织营养成分、营养价值进行了分析评定。结果表明:长蛸肌肉样品中,粗蛋白、粗脂肪、灰分的鲜质量分数和干质量分数分别为14.85%和71.80%、0.41%和2.0%、1.94%和9.36%,水的质量分数为79.30%;测得17种氨基酸,总质量比是651.7 mg/g,必需氨基酸质量比为256.5 mg/g,占氨基酸总量的39.36%;必需氨基酸中色氨酸得分最高为217,所有必需氨基酸均在53分以上,半胱氨酸+蛋氨酸为第一限制性氨基酸;共检测10种主要脂肪酸,其中EPA+DHA的总质量分数为31.23%(雌)、32.10%(雄);富含钠、钾、钙、镁、铁等11种矿物元素,微量矿物元素中锌质量比最高,为111.36 mg/g;维生素A、B含量丰富。     

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.     

Assessing the Validity of Seismo-Acoustic Predictor Equations for Obtaining Seabed and Sub-Surface Sediment Physical Properties

The interdependence between the seismo-acoustic properties of a marine sediment and its geotechnical/physical parameters has been known for many years, and it has been postulated that this should allow the extraction of geotechnical information from seismic data. Though in the literature many correlations have been published for the surficial layer, there is a lack of information for greater sediment depths. In this article, a desktop study on a synthetic seafloor model illustrates how the application of published near-surface prediction equations to subsurface sediments (up to several tens of meters burial depth) can lead to spurious predictions. To test this further, acoustic and geotechnical properties were measured on a number of sediment core samples, some of which were subjected to loading in acoustically-equipped consolidation cells (oedometers) to simulate greater burial depth conditions. For low effective pressures (representing small burial depths extending to around 10 meters subsurface), the general applicability of established relationships was confirmed: the prediction of porosity, bulk density, and mean grain size from acoustic velocity and impedance appears generally possible for the investigated sedimentary environments. As effective pressure increases through, the observed relationships deviate more and more from the established ones for the near-surface area. For the samples tested in this study, in some instances increasing pressure even resulted in decreasing velocities. There are several possible explanations for this abnormal behavior, including the presence of gas, overconsolidation, or bimodal grain size distribution. The results indicate that an appropriate depth correction must be introduced into the published prediction equations in order to obtain reliable estimates of physical sediment properties for greater subsurface depths.     

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.     

Interannual Sea Level Variations and Annual Tides in the Northwestern Pacific

Specific properties of the interannual sea level variations and annual tides in the Northwestern Pacific were studied. Several tide stations were monitored. The monthly mean sea level for the year of 1995 was analyzed at each tide station. A seismic event in 1995, some tectonic activity around the subject area, and the Kuroshio (the oceanic western boundary current) may possibly contaminate results which would have occurred from the astronomical annual tide alone.     

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.     

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.     

Flow Cytometric Analysis of Coastal Lagoon Bacterioplankton and Picophytoplankton: Fixation and Storage Effects

The effect of different fixation and storage protocols on the flow cytometric (FCM) simultaneous analysis of bacterioplankton and phytoplankton in coastal seawater samples (Mediterranean coastal lagoons) was investigated. FCM measurements (cell number, fluorescence and scatter characteristics) were obtained through DAPI staining. Three fixatives [glutaraldehyde (GA), formaldehyde (FA) and paraformaldehyde (PFA)] and two storage (3 months duration) methods (5 °C and −196 °C) were tested. Two dominant populations were detected in studied samples: bacteria and eukaryotic picophytoplankton. Adding fixatives (2% final concentration) appears necessary to obtain FCM exhaustive counts of all the bacteria and phytoplanktonic cells. This was related to the permeation effect of fixatives which allowed a better DAPI staining of the cells. Maximum fluorescence, i.e. optimal staining of the cells was obtained with FA or PFA, and significant lower fluorescences with GA. Fixed samples stored at 5 °C induced rapid cell loss. Only storage in liquid nitrogen of samples fixed with FA or PFA, allows mid-term (≥4 months) preservation of bacteria or picophytoplankton cell numbers, and limited evolution of DAPI-induced fluorescence and scatter characteristics.