九孔鲍和杂色鲍等位酶的生化遗传分析

应用聚丙烯酰胺凝胶电泳技术,对九孔鲍(Haliotis diversicolor supertexta)的养殖群体和杂色鲍(H．diversicolor diversicolor)的自然群体进行了10种等位酶的电泳检测和谱带遗传分析,在研究九孔鲍的18个等位酶位点和27个等位基因中,单态位点有Ldh-1、Adh-1、Sod-1、Sod-2、Sod-3、Est-1、Mdh-2、Me-1、Idh-1、Sdh-1、Sdh-2、Amy-2、Amy-3,在这些位点只有一个等位基因(Sdh-2除外)：有5个位点是多态的,它们是Est-2、Est-3、Mdh-1、Aat-1、Amy-1(P0.99标准),多态位点的百分数为27．78％,在这些位点有2～4个等位基因。在研究杂色鲍的18个等位酶位点和26个等位基因中,单态位点有Ldh-1、Adh-1、Sod-1、Sod-2、Sod-3、Est-1、Mdh-2、Idh-1、Sdh-1、Sdh-2、Amy-2、Amy-3,在这些位点只有一个等位基因;有6个位点是多态的,它们是Est-2、Est-3、Mdh-1、Me-1、Aat-1、Amy-1(P0.99标准),多态位点的百分数为33.33％,在这些位点有2～4个等位基因。九孔鲍和杂色鲍在所有位点中共享大多数常见等位基因,因此在生化遗传上它们非常相似。本研究揭示了九孔鲍和杂色鲍群体等位酶位点及其等位基因谱带的变异式样,为九孔鲍和杂色鲍的遗传结构及遗传育种的研究提供了一批等位酶位点及其等位基因的参考图谱。     

盘鲍和皱纹盘鲍等位酶的生化遗传分析

应用聚丙烯酰胺凝胶电泳技术,对盘鲍(Haliotis discus discus)和皱纹盘鲍(Haliotis discus hannai)的养殖群体进行了10种等位酶的电泳检测和谱带遗传分析。确定了盘鲍的18个等位酶位点及21个等位基因,单态位点有15个;仅有3个位点是多态的,它们是Sod-1,Est-3,Mdh-1(P0.99标准),多态位点的百分数为16．67％,这些多态位点分析到2个等位基因。确定了皱纹盘鲍的18个等位酶位点及20个等位基因,单态位点有16个;仅有2个位点是多态的,它们是Sod-1,Est-3(P0.99标准),多态位点的百分数为11．11％,这些多态位点中也分析到2个等位基因。盘鲍和皱纹盘鲍在所有位点中共享大多数常见等位基因,因此在生化遗传上它们非常相似。该研究揭示了盘鲍和皱纹盘鲍养殖群体等位酶位点及其等位基因带谱的变异式样,为盘鲍和皱纹盘鲍的遗传结构及遗传育种的研究提供了一批等位酶位点及其等位基因的参考图谱。     

大竹蛏同工酶组织特异性与多态性初步研究

用不连续垂直聚丙烯酰胺凝胶电泳对大竹蛏(Solen grandis Dunker)外套膜、鳃、性腺、消化腺、斧足5种组织6种同工酶(LDH、ADH、EST、MDH、ACP、SOD)进行组织特异性分析,并对吕四渔场海域大竹蛏自然种群生化遗传多样性进行了初步研究.结果表明:大竹蛏同工酶的活性及酶谱特征具有明显的组织特异性,6种酶在消化腺中的活性最强,LDH、EST、MDH和SOD酶谱具有明显的组织特异性;6种酶在消化腺和斧足中共检测到12个基因位点,其中Ldh-1、Ldh-2、Adh-1、Est-1、Mdh-1、Mdh-2、Mdh-3、Sod-2等8个基因位点为多态,多态位点比例为66.67%,平均每个位点的等位基因数N<,a>为2.5,有效等位基因数(N<,e>)为1.9,预期杂合度(H<,c>)为O.373 7,实际杂合度(H<,o>)为0.333 3,香农信息指数(I)为0.624 2.     

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％。     

西施舌3 个自然群体杂合性的研究

采用聚丙烯酰胺凝胶电泳技术,对广西北海、福建漳港和江苏启东3个西施舌(Coelomactra antiquata (Spengler))自然群体杂合性进行了研究.共检测分析了7个酶,获得12个位点,25个等位基因.其中4个位点是多态的,分别是Sod-1、Mdh-1、Est-1、Est-3,这些位点分别有1～7个等位基因.结果表明,福建漳港群体的Sod-1和Est-1位点、广西北海群体的勋Sod-1位点符合Hardy-weinberg平衡(P>0.05);江苏启东群体的多态位点中所有位点、福建漳港群体的Mdh-1、Est-3位点,广西北海群体的Mdh-1、Est-1、Est-3位点均非常显著偏离Hardy-weinberg平衡(P<0.01).另外,除了江苏启东和福建漳港群体的Est-1位点表现出杂合子缺失(F>0)外,各群体中每个位点均表现出杂合子过量(F<0).结合各群体中每个多态位点的观察杂合度和期望杂合度,认为中国东南沿海西施舌的种质资源状况良好.     

厦门文昌鱼(Branchiostoma belcheri Gray)种群杂合性研究

应用聚丙烯凝胶电泳技术,研究了厦门海域四个野生文昌鱼种群的杂合度缺乏和过量情况.在测定的7个酶系统中,共有14个等位酶基因位点,分别为Aat-1、Amy-1、Amy-2、Amy-3、Amy-4、Me-1、Me-2、Mdh-1、Mdh-2、Sod-1、Sod-2、Est-1、Est-2、Per-1.多态位点有8个,分别为Sod-1、Aat-1、Me-1、Me-2、Mdh-1、Mdh-2、Est-2、Amy-2.结果表明,在大嶝岛种群、南线至十八线东端种群、南线至十八线西端种群及黄厝种群中,多态位点Sod-1、Mdh-2、Me-2、Aat-1显著偏离H-W平衡标准(P<0.05),而位点Me-1、Mdh-1、Est-2符合H-W平衡标准(P>0.05).多态位点Amy-2除南线至十八线东端种群显著偏离H.W平衡标准(P<0.05)外,其它三个种群的多态位点Amy-2均符合H-W平衡标准(P>0.05).在所有的8个多态位点中,只有大嶝岛和黄厝两个种群的Amy-2位点表现为杂合子缺失(F>0),其它种群的多态位点均表现为杂合子过量(F<0).造成杂合体缺失的主要原因可能是自然选择、近交、哑等位基因等.杂合体的缺失会导致某些基因从该物种的基因库中消失,从而降低了物种的遗传多样性,同时也使物种对环境的适应能力降低.     

硬壳蛤同工酶的组织特异性研究

采用垂直板聚丙烯酰胺凝胶电泳技术,对硬壳蛤5种组织(足、外套膜、闭壳肌、鳃和肝)的酯酶(EST)、苹果酸脱氢酶(M DH)和乳酸脱氢酶(LDH)同工酶进行了比较研究,并对酶谱表型及位点表达进行了分析。结果表明,硬壳蛤上述组织的EST和M DH同工酶存在不同程度的组织特异性,而LDH没有组织特异性。在EST酶谱中,肝组织染色最深,说明其EST活性最高,这与肝脏为重要的消化腺和解毒器官相适应。在M DH酶谱中发现了s-M DH和m-M DH所形成的谱带,闭壳肌的M DH谱带染色很深,这与肌肉需要由三羧酸循环提供大量ATP相适应。     

罗氏沼虾肌肉8种同工酶的研究

利用聚丙烯酰胺凝胶电泳技术,对罗氏沼虾(Macrobrachium rosenbergii)肌肉中的ADH,LDH,G6PDH,SOD,GDH,EST,AKP,ACP等8种同工酶进行分析,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,8种同工酶由17个基因位点所编码,其中G6pdh-1,Gdh-1和Est-3等3个基因位点具有多态现象.多态位点比例为17.6%.     

卤虫等位酶的遗传控制

应用聚丙烯酰胺凝胶电泳技术分析了孤雌生殖卤虫产生的罕见雄体、两性卤虫及其杂交后代 (F1)的酯酶 (EST)、超氧物歧化酶 (SOD)、过氧化物酶 (PRX)、碱性磷酸酶 (AL P)、四唑氧化酶(TO)和乳酸脱氢酶 (L DH)的同工酶酶谱表型。对编码 5种酶的 19个位点、35个等位基因的表达进行了遗传分析。结果表明 ,在 EST、PRX和 TO酶谱中既有共显性等位基因 ,又有沉默等位基因的表达 ;卤虫 PRX、AL P和 SOD为单体酶 ,在 EST和 TO酶谱中还存在着二聚体同工酶 ;除 LDH为单态外 ,其余 5种同工酶为多态酶。     

岱衢洋与官井洋大黄鱼养殖群体遗传多样性的AFLP分析

应用扩增片段长度多态性技术(AFLP),比较研究了岱衢洋大黄鱼养殖群体和官井洋大黄鱼养殖群体的遗传多样性。9对选择性引物组合,在2个群体的40个个体中共扩增出381个位点,其中多态位点为288个。2个养殖群体的多态位点比例、Nei′s基因多样性指数、Shannon多样性指数分别为65.01%和57.50%,0.162 3和0.1175,0.254 7和0.185 6,显示岱衢洋大黄鱼F2代养殖群体的遗传多样性高于官井洋大黄鱼繁育多代养殖群体的遗传多样性。UPGMA聚类分析图显示2个群体各自聚成一支。遗传分化系数Gst及AMOVA分析表明,2个群体的遗传变异主要来源于群体内个体间,但群体间已有一定程度的遗传分化。     

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。     

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.     

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.     

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.