黄鳍鲷不同组织同工酶的研究

运用聚丙烯酰胺垂直梯度凝胶电泳法对黄鳍鲷的7种组织(心肌、肝脏、肾脏、肌肉、性腺、脾脏、脑)进行了4种同工酶(EST,LDH,MDH,ME)的初步研究,并对几种酶的同工酶位点及酶谱表型进行了分析。结果表明：黄鳍鲷的4种同工酶系统具有明显的组织特异性。同时还分析了聚丙烯酰胺垂直梯度凝胶电泳法对同工酶电泳的分离效果,认为该种方法对同工酶系统的分辨率高,分离效果好,可得到更精确的结果。     

克氏原螯虾LDH同工酶的组织特异性研究

以克氏原螯虾为材料,采用聚丙烯酰胺凝胶电泳方法,分析了肌肉、眼球、肝胰腺和心脏4种组织和器官中乳酸脱氢酶（LDH）同工酶的表达情况。结果发现,眼球中出现Ldh-5和Ldh-62条酶带,肌肉中出现Ldh-1、Ldh-2、Ldh-3、Ldh-4、Ldh-5共5条酶带．肝胰腺中只出现Ldh-61条酶带,心脏中出现Ldh-3和Ldh-5共2条带。在这些检测到的酶带中,肌肉中Ldh-5活性最强,染色最深。实验结果表明,不同组织中LDH的同工酶的表达存在差异。表现出明显的组织特异性。     

口虾蛄(Oratosquilla oratoria)同工酶的组织特异性及生化遗传分析

采用聚丙烯酰胺凝胶垂直平板电泳方法，研究分析了口虾蛄(Oratosquilla oratoria)肌肉、眼球、腹鳃、心脏和肝胰腺5种器官或组织中LDH、ADH、MDH、SDH、MEP、POD、AMY、GDH、SCD、EST、GLDH和SOD共12种同工酶的表达情况。结果表明，口虾蛄同工酶的表达具有明显的组织特异性。对12种同工酶进行生化遗传分析，获得了基本酶谱。12种同工酶共记录出35个基因座位，其中11个基因座位Ldh-3、Adh-1、Sdh-2、Est-1、Est-2、Est-3、Mdh、Mep-7、Gldh-1、Gldh-2和Scd-1为多态，其多态座位比例为31.43％。     

中国对虾两个种群的F_1的LDH和MDH同功酶初步分析

采用不连续聚丙烯酰胺凝胶垂直平板电泳法，分析了黄、渤海南移和珠江口北移的中国对虾Ｐｅｎａｅｕｓｏｒｉｅｎｔａｌｉｓ及其杂交于一代的乳酸脱氢酶（ＬＤＨ）和苹果酸脱氨酶（ＭＤＨ）同工酶。结果表明：这两种同工酶具明显的组织特异性，均只在尾部肌肉表达。ＬＤＨ同工酶表现为紧密相邻的两条带。ＭＤＨ的表达谱式与其它物种类似，表现为趋向阳极的上清液型和趋向阴极的线粒体型。本研究分析的两种同工酶未见两种来源的中国对虾及其杂交子一代的差异。文中对此进行了讨论。     

鲈鱼群体生化遗传学研究 Ⅰ.同工酶的生化遗传分析

于1994年9月－1995年12月，在青岛近海采集37尾鲈鱼的生化样品，采用淀粉胶和聚丙烯酰胺凝胶2种电泳分析，分析了LDH、MDH、MEP、IDHP、PGM、G3PDH、AK、CK、ADH、SDH、G6PDH、GDH、PGDH、CAT、MPI、EST、SOD等同工酶在鲈鱼眼睛、肌肉、心脏、肝脏、肾脏、鳃、胸鳍等7种组织或器官中的表达情况，并对同工酶表型进行了生化遗传分析，以期为其种质资源保护和开发，以及遗传育种等方面的研究提供基础资料。结果表明，17种同工酶由31个基因座位编码，其中Mep-1,Pgm-1,Sdh,Gdh,Pgdh,Mpi,Est-1,Est-4等8个基因座位为多态。多态座位比例为25．8％。     

鲈鱼群体生化遗传学研究 Ⅰ.同工酶的生化遗传分析

于1994年9月—1995年12月，在青岛近海采集37尾鲈鱼的生化样品，采用淀粉胶和聚丙烯酰胺凝胶2种电泳方法，分析了LDH、MDH、MEP、IDHP、PGM、G3PDH、AK、CK、ADH、SDH、G6PDH、GDH、PGDH、CAT、MPI、EST、SOD等同工酶在鲈鱼眼睛、肌肉、心脏、肝脏、肾脏、鳃、胸鳍等7种组织或器官中的表达情况，并对同工酶表型进行了生化遗传分析，以期为其种质资源保护和开发，以及遗传育种等方面的研究提供基础资料。结果表明，17种同工酶由31个基因座位编码，其中Mep-1、Pgm-1、Sdh、Gdh、Pgdh、Mpi、Est-1、Est-4等8个基因座位为多态。多态座位比例为25 8%。     

休眼与非休眠期中华鳖乳酸脱氢酶同工酶的比较分析

本文用聚丙烯酰胺凝胶电泳的方法，分析了休眠与非休眠期中华鳖10种组织的乳酸脱氢酶同工酶，同时测定了休眠与非休眠期乳酸脱氢酶的总活性。结果表明，某些组织的电泳图谱显示出一定差异；多数组织冬眠期LDH同工酶的总活性有所降低。     

中华绒螯蟹不同组织LDH同工酶凝胶电泳分析

采用高pH不连续系统聚丙烯酰胺垂直板凝胶电泳,特异性组织化学染色对中华绒螯蟹(Eriocheir sinensis)的血清、肌肉、鳃、心脏、肝胰腺、精巢和精子等组织的乳酸脱氢酶(LDH)同工酶酶谱进行了研究。同时,利用2种底物(乳酸钠和α-羟基丁酸钠)进行了特异性反应,并对其精子特异性乳酸脱氢酶进行了研究。结果表明:以乳酸钠为底物时,中华绒螯蟹的肌肉、鳃、血清和心脏有2条谱带,而精巢和精子有3条谱带,但在肝胰腺中未发现谱带;以α-羟基丁酸钠为底物时,只在血清、精巢和精子发现有1条谱带。从而说明,中华绒螯蟹乳酸脱氢酶同工酶存在组织特异性;精子存在特异性乳酸脱氢酶。     

褐点石斑鱼不同组织4种同工酶的研究

运用聚丙烯酰胺垂直梯度凝胶电泳法对褐点石斑鱼7种组织(眼睛、肌肉、心脏、肝脏、肾脏、尾鳍、脾脏)的4种同工酶(EST、SOD、LDH、MDH)进行了初步研究。结果表明:褐点石斑鱼的4种同工酶系统具有不同程度的组织特异性。EST由4个基因位点编码,具有多态性现象;肌肉SOD与其它组织SOD有明显差异;眼睛LDH酶谱酶带最多;MDH具有线粒体型(m-MDH)和上清液型(s-MDH)两种类型。     

口虾蛄超氧化物歧化酶同工酶的组织特异性研究

以口虾蛄为材料进行研究，用聚丙烯酰胺凝胶电泳法，对其肌肉、心脏、腹鳃、肝胰腺及眼球5种组织器官进行超氧化物歧化酶(SOD)同工酶的研究分析。结果表明：不同组织中超氧化物歧化酶(SOD)的同工酶谱带存在差异，具有明显的组织特异性。眼球、腹鳃、肝胰腺和心脏中有2条酶带，肌肉中几乎不表达，心脏中SOD2和肝胰腺中SODl谱带表达最浓，而腹鳃中的酶带表达最弱。     

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.     

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.     

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。     

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.     

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.     

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,     

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.