微卫星标记在大菱鲆(Scophthalmus maximus L.)家系系谱印证中的应用研究

用8个微卫星标记对大菱鲆7个人工选育家系进行了系谱鉴别和遗传多样性研究。8个微卫星位点的平均多态信息含量为0.6721,平均杂合度为0.7206。8个微卫星位点在7个家系分析中,共检测到40个等位基因,每个位点的等位基因数在38个之间,每个位点平均有5个等位基因。根据已知亲本及子代基因型,成功的推断出了7个家系中缺失亲本的基因型。在双亲未知的情况下8个微卫星位点累积排除概率是97.07%,已知单亲时累积排除概率达99.63%。用UPG-MA法对7个家系的137个子代个体进行了聚类分析,90.5%同一家系的子代个体能完全聚类到一起,分类结果与系谱来源基本一致。微卫星标记可以为大菱鲆混养家系进行亲权鉴定和系谱构建提供技术支持。     

刺参杂交子代的微卫星和AFLP分析

用微卫星和APLP标记分析了中国刺参(♀)和日本红刺参(♂)杂交子一代的遗传特性。2对微卫星标记对两亲本及其杂交子代的分析结果表明,杂交子代的等位基因均来自两亲本,为真正的杂交种。8对AFLP引物共扩增出375个位点,其中多态位点265个,多态位点比例69.8%;238个位点在子代中发生分离,符合孟德尔分离规律的位点175个,其中母本69个,父本66个;偏离孟德尔分离的位点43个;异常分离位点20个。子一代与母本间的遗传距离为0.0391,小于其与父本之间的遗传距离(0.0999),表明杂交子代在遗传上与母本较近。     

利用微卫星标记的魁蚶混交家系鉴定

本文使用6个具有多态性的微卫星位点,对30个魁蚶亲本及其300个子代(共330个个体)进行家系分析,评估苗种生产中亲本与子代间的遗传变异。研究表明,家系鉴定成功率与模拟结果一致,使用6个微卫星位点可以实现超过99%的鉴定率。魁蚶亲本与子代间等位基因多样性相似,子代群体的期望杂合度显著低于亲本群体(P0.05),观测杂合度和亲本群体相比略有降低,但无显著差异。所有魁蚶父母本都参与了繁殖过程,并具有多重父权和多重母权的现象。研究显示,微卫星作为一种分子标记可以有效应用到家系鉴定中,同时对于养殖魁蚶群体的遗传多样性变化仍需要进一步的监测。本研究为魁蚶人工育苗、养殖生产制定合理的管理方针提供帮助,同时为微卫星作为分子标记进行魁蚶增殖放流溯源提供科学支持。     

大菱鲆亲子鉴定的微卫星多重PCR技术建立及应用

用8个微卫星标记组合建立了2个微卫星多重PCR体系,对大菱鲆7个人工选育家系进行了系谱认证、亲子鉴定和遗传多样性研究。2个多重PCR体系中8个微卫星位点共检测到等位基因49个,每个位点等位基因数为3~8个。根据已知亲本及子代基因型,成功推断出了3个缺失亲本的基因型。在双亲未知的情况下2个多重PCR的8个微卫星位点累积排除概率是96.58%,已知1个亲本时累积排除率为99.71%,亲子鉴定准确率为96.42%。采用70个个体进行双盲验证,利用UPGMA法对7个家系的70个体进行了聚类分析,同一家系95.71%的个体聚类分析结果与系谱来源一致。Cervus 2.0软件亲子鉴定结果表明亲子鉴定准确率为92.86%。2个多重PCR体系的建立为大菱鲆不同家系混养后的亲子鉴定、系谱分析和分子辅助家系管理提供了技术手段。     

大菱鲆亲子鉴定的微卫星多重PCR技术建立及应用

用8个微卫星标记组合建立了2个微卫星多重PCR体系,对大菱鲆7个人工选育家系进行了系谱认证、亲子鉴定和遗传多样性研究.2个多重PCR体系中8个微卫星位点共检测到等位基因49个,每个位点等佗基因数为3～8个.根据已知亲本及子代基因型,成功推断出了3个缺失亲本的基因型.在双亲未知的情况下2个多重PCR的8个微卫星位点累积排除概率是96.58%,已知1个亲本时累积排除率为99.71%,亲子鉴定准确率为96.42%.采用70个个体进行双盲验证,利用UPGMA法对7个家系的70个体进行了聚类分析,同一家系95.71%的个体聚类分析结果与系谱来源一致.Cervus 2.0软件亲子鉴定结果表明亲子鉴定准确率为92.86%.2个多重PCR体系的建立为大菱鲆不同家系混养后的亲子鉴定、系谱分析和分子辅助家系管理提供了技术手段.     

富集文库-菌落原位杂交法筛选仿刺参微卫星标记

应用微卫星富集文库—菌落原位杂交的方法,筛选得到了33个仿刺参的微卫星标记。富集文库中900个重组克隆经过菌落原位杂交后,415个(46.1%)为阳性克隆。随机挑取100个阳性克隆进行测序,结果显示这些克隆都含有微卫星位点。设计了57对特异性PCR引物,33对能扩增出清晰的条带。利用48个野生仿刺参个体对33个微卫星位点进行评价,结果显示位点都具有多态性。33个多态位点共获得222个等位基因,平均每个位点获得6.7个等位基因。观测杂合度(Ho)和期望杂合度(He)的范围分别为0.050 0~1.000 0和0.203 2~0.915 9。结果表明,富集文库—菌落原位杂交法筛选微卫星标记比较高效,获得的微卫星标记可以用于仿刺参的分子遗传学研究。     

刺参(Apostichopus japonicus)EST序列中微卫星分布分析及其标记的筛选

利用微卫星查找软件对现已公布的6632条刺参ESTs的数据库中2—6个碱基重复单元组成的简单序列重复进行筛选,进而对其微卫星的丰度和分布进行比较研究。共发现微卫星序列416个,占整个ESTs数据库的6.48%;其中含双碱基重复序列146个,数量最多,占ESTs数据库中发现微卫星序列总数的65.86%;三、四、五、六碱基重复序列分别占微卫星序列总数的26.68%、1.68%、0.24%、5.53%。对含有SSR位点符合微卫星引物设计的EST序列利用Primer软件结合人工方法设计合成引物21对,其中13对有扩增产物且均为多态位点。扩增产物变性聚丙烯酰胺胶电泳,统计每个微卫星标记等位基因数目,计算等位基因频率、观测杂合度、期望杂合度等统计学指标的评价。结果表明,在13个微卫星位点上,等位基因的数目从3到8不等,等位基因长度从175—382bp,观测杂合度和期望杂合度分别为0.158—0.650和0.198—0.841,所筛选微卫星标记可于遗传分析。     

长牡蛎(Crassostrea gigas)微卫星多重PCR 体系构建及其在家系鉴定中的应用

筛选多态性高、特异性好、片段大小适中的10 个长牡蛎微卫星位点进行优化组合, 根据扩 增片段大小及同一荧光不重叠原则构建了两组五重PCR 体系。运用CERVUS 3.0 软件对0527 组27 个长牡蛎全同胞家系的643 个子代和0612 组27 个全同胞家系382 个子代分别进行亲权鉴定。结果 发现, 用两组微卫星五重PCR 鉴别时, 在0527 组和0612 组的鉴定成功率均为100%; 只用第一组微 卫星五重PCR, 可以将0527 组96%的子代和0612 组96%的子代鉴定到亲本; 只用第二组微卫星五 重PCR, 可以将0527 组97%的子代和0612 组95%的子代鉴定到亲本。本研究中筛选出的两组微卫 星五重PCR 体系在两组家系中的鉴定效率均较高, 可以快速有效地将子代个体鉴定至所属父母本, 在长牡蛎家系鉴定中具有很好的应用价值。     

菊黄东方鲀和双斑东方鲀及其种间杂交子代的ISSR分析

通过对菊黄东方鲀、双斑东方纯及两者的正反杂交子代的ISSR标记分析,研究了2种子代群体之间以及子代群体与共享亲本个体间的遗传关系.使用10个ISSR引物,得到清晰的扩增位点154个,其中多态位点88个,平均多态位点检出率57.14%.分析结果显示:杂交子代个体中具有来自父母本的扩增位点,表明杂交子代确为杂种;杂交子代群体不仅具有较高的遗传多样性,而且在与亲本个体和其他子代群体间的遗传关系上表现出与种内交配子代的明显差异;另外杂交子代与2种亲本的遗传关系上并不对等,表现出明显的倾向性,更加偏向于母本一方.     

多元PCR技术在毛蚶家系鉴定中的应用

为促进毛蚶(Scapharca kagoshimensis)的遗传育种研究及开展其资源的保护工作。本研究用4组微卫星多元PCR体系对5个毛蚶全同胞家系进行了家系鉴定分析。研究表明:4组多元PCR体系中的10个微卫星位点均为高多态性位点,使用1组多元PCR体系的子代模拟鉴定成功率和实际鉴定成功率分别为78%和72%,3组以上多元PCR体系子代的鉴定成功率为100%。研究结果表明,微卫星多元PCR技术能快速、准确地将任意子代鉴定至其所属家系,该技术可用于大批量家系材料分析,具有较好的应用价值。     

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.     

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.     

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,