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栉孔扇贝×虾夷扇贝的杂交技术 总被引：7，自引：0，他引：7
以栉孔扇贝与虾夷扇贝为实验材料,进行了两者之间自交和栉孔扇贝♀×虾夷扇贝♂和虾夷扇贝♀×栉孔扇贝♂的杂交的实验。实验结果表明:两者的杂交是可行的,在幼虫阶段表现出一定的生长优势,幼虫成活率间没有差异,但在幼虫附着变态方面,杂交组低于自交组,两者之间有明显的差异。然后以具有生长优势的栉孔扇贝♀×虾夷扇贝♂组进行了生产性育苗实验,取得明显的经济效益。 相似文献
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本文采用DAPI染色荧光显微方法连续观察了栉孔扇贝♀×海湾扇贝♂的受精细胞学过程,发现海湾扇贝精子可以正常入卵,并能完成后续的发育过程获得杂交后代。同时进行栉孔扇贝♀×海湾扇贝♂杂交组及栉孔扇贝、海湾扇贝自交组3组实验,对各组的受精率、卵裂率、D形幼虫孵化率、幼虫生长速度、幼虫存活率进行统计分析,实验结果表明:杂交组的受精率为92.77%,卵裂率为81.46%,D形幼虫孵化率为51.23%,杂交组幼虫在培育到第7天时全部死亡,栉孔扇贝和海湾扇贝自交组的幼虫可正常发育到眼点幼虫,杂交组幼虫在其存活阶段的生长和2自交组无显著性差异,但成活率差异显著。 相似文献
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两种扇贝杂交和自交家系早期生长及甲基化的比较分析 总被引：1，自引：0，他引：1
运用杂交和自交方法建立虾夷扇贝♂(A)×栉孔扇贝♀(B)、栉孔扇贝♀(B)×栉孔扇贝♂(C)、栉孔扇贝♂(C)×栉孔扇贝♀(D)3 种组合家系, 每个组合3 个平行, 共9 个家系。对各家系卵径大小、胚胎孵化率、幼虫浮游阶段壳长生长速度等生物学参数进行比较, 建立了幼虫浮游期壳长与日龄的线性回归方程; 运用甲基化敏感扩增多态性(MSAP)分析了基因组DNA 胞嘧啶甲基化水平, SPSS 分析了DNA 甲基化与壳长生长的相关性。结果表明, 杂交家系的卵径大小、胚胎孵化率与自交组没有显著差异, 但壳长生长速度显著高于自交组, 这种优势可能主要来自于父本的影响; 家系AB、BC、CD 的平均DNA甲基化率分别为18.672%、22.661%和22.303%, 杂交使后代DNA 甲基化水平降低, 生长速度与DNA甲基化水平相关系数为?0.934, 相关水平极显著(P<0.01), DNA 甲基化与杂种优势具有一定的关系。 相似文献
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为了解栉孔扇贝(Chlamys farreri)、虾夷扇贝(Patinopecten yessoensis)及其杂交子代(F1)的种群遗传多样性和遗传结构,对3个群体的线粒体COI和Cytb基因的部分序列进行了扩增和分析。经比对分别获得781bp和725bp核苷酸片段,74个样本共检测到47个单倍型;F1群体的单倍型数、单倍型多样性指数、核苷酸多样性及平均核苷酸差异数都是最高的,而双亲的较低;F1和栉孔扇贝间的遗传距离最小,其次为栉孔扇贝和虾夷扇贝群体之间,F1和虾夷扇贝群体之间的遗传距离最大;F1和栉孔扇贝之间的遗传分化系数较小而两者间的基因流比较大,F1和栉孔扇贝与虾夷扇贝之间的遗传分化系数较大而基因流较小,说明栉孔扇贝和虾夷扇贝群体群体很早就发生了遗传分化;采用UPGMA法和简化的中介网络法构建的系统树表明,3个群体的所有个体被分为2个族群,栉孔扇贝和F1交叉聚为一类,虾夷扇贝独自聚为一类,2个分支间没有交叉;使用特异性引物分别对3个群体进行PCR扩增检验,结果栉孔扇贝的特异引物能在杂交子代中扩增,而虾夷扇贝的特异引物不能在子代中扩增出条带,说明栉孔扇贝和虾夷扇贝杂交,其子代的线粒体遗传模式为严格的母系遗传。本研究结果表明杂种优势的形成与线粒体遗传多样性的变化有关。 相似文献
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雌性虾夷扇贝与雄性栉孔扇贝杂交子代及其亲本的核型研究 总被引：5，自引：0，他引：5
采用滴片法制片-吉姆萨染色对雌性虾夷扇贝(Patinopecten yessoensis)与雄性栉孔扇贝(Chla-mysfarreri)杂交子代及其双亲的核型进行了研究,报道了在扇贝杂交过程中产生的特殊的细胞遗传学现象,结果表明,栉孔扇贝染色体核型2n=38=6m+10sm+22st;虾夷扇贝染色体核型2n=38=6m+10sm+16st+6t;两者杂交子代染色体数目2n=38,但其染色体组型不符合预期型,不是简单地由两个亲本各自一套染色体组型组合而成,呈现出复杂的形态多态性,端部着丝点染色体明显增多. 相似文献
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栉孔扇贝♀×华贵栉孔扇贝♂受精及早期胚胎发育过程的细胞学荧光显微观察 总被引：4，自引：0，他引：4
为探讨贝类杂交优势 ,利用HOECHST3 3 2 5 8对已固定样品进行染色的方法 ,连续观察了栉孔扇贝♀×华贵栉孔扇贝♂受精的细胞生物学过程 ,初步证明了这 2种远缘扇贝种类之间进行杂交的可行性。结果表明 ,栉孔扇贝的成熟未受精卵子处于第一次减数分裂中前期 ,部分来自华贵栉孔扇贝的异源精子可顺利进入卵子并激发后者完成 2次减数分裂 ,排出第一及第二极体。成熟的雌雄原核形成后完成融合过程 ,形成合子核 ,受精过程结束。大部分杂交受精卵及杂种早期胚胎可以正常发育 ,但其发育进程较种内近交对照组有明显的差别 ,具体表现在延缓性和不同步性 2个方面。 相似文献
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4种养殖扇贝的群体遗传多样性及特异性AFLP标记研究 总被引：29，自引：2，他引：27
应用AFLP技术对我国4种主要养殖扇贝进行了遗传分析.虾夷扇贝、海湾扇贝、华贵栉孔扇贝、栉孔扇贝4种养殖扇贝群体中,种内遗传相似度依次分别为0.841 5,0.786 3,0.719 0和0.673 1,香侬氏指数分别为43.52,58.87,80.16和92.83,栉孔扇贝和华贵栉孔扇贝的遗传多样性水平明显高于海湾扇贝和虾夷扇贝;AFLP标记共享位点分布表明,在4种扇贝中栉孔扇贝与华贵栉孔扇贝之间的共享位点最多,同时4种扇贝的种间遗传相似度也以栉孔扇贝和华贵栉孔扇贝之间为最高(0.769 5),海湾扇贝和虾夷扇贝之间为最低(0.662 6),揭示所研究的几种扇贝中栉孔扇贝和华贵栉孔扇贝的遗传关系最近(遗传距离为0.262 1);找到了21个种内特异性AFLP标记和种间共享标记,可用于种质鉴定和分子辅助分类. 相似文献
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采用单一自由度独立比较的方法,研究了两个栉-华杂交组合HCH(栉孔扇贝长岛群体×华贵栉孔扇贝)和HJH(栉孔扇贝胶南群体×华贵栉孔扇贝)以及栉孔扇贝种内交配组合ZZ的胚胎发生及幼虫生长发育过程。结果表明,栉孔扇贝和华贵栉孔扇贝的种间杂交F1在生长和发育的两个环节上是不一致的,在涉及器官及其功能形成的发育环节上,杂交表现负效应;而在涉及形态变化和增大的生长环节上,杂交表现正效应,存在杂种优势现象。两个杂交组合中,HJH综合效果较好,授精22h平均孵化率达到95.8%,与ZZ基本接近;30日龄平均变态率达61.5%,明显好于组合HCH的42.0%;8日龄幼虫平均大小达143.4μm×123.2μm,表现出更强的生长优势。这些结果为全面评价栉孔扇贝与华贵栉孔扇贝杂交体系应用价值和选配优良杂交组合提供了理论依据。 相似文献
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Arne Schnack-Friedrichsen Angela M. Davis Jim D. Bennell Dei G. Huws 《Marine Georesources & Geotechnology》2001,19(4):221-243
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. 相似文献
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Shigehisa Nakamura 《Marine Geodesy》2000,23(1):55-61
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. 相似文献
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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. 相似文献
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《海洋学报(英文版)》2014,(9):F0003-F0003
<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, 相似文献
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The relationship between the flux of exotic benthic foraminiferal tests (i.e. tests which are supplied from open-sea sources alone) in a tidal inlet and that of bulk sediment was analysed, which can be expressed as two first-order linear equations. According to this relationship, in order to determine net sediment transport directions in the entrance, the test concentration in surficial sediments of the tidal basin can be compared against a ‘ critical level ’. The critical level is determined for the conditions that no net transport of bulk sediment is present within the entrance. If the observed concentration (averaged over the tidal basin) is higher than the simulated critical level, then the net sediment transport is directed to landward. This method is applied to the analysis of net sand transport at Christchurch Harbour, a tidal inlet system located in southern England. In this investigation, concentrations of exotic foraminiferal tests in the surficial sediments of the tidal basin and ebb tidal delta area were obtained from the analysis of sea-bed sediment samples. A series of probable critical levels were calculated based upon the data sets with regard to: (1) sediment discharge from the rivers; (2) magnitude of sediment discharge within the entrance during the ebb; (3) the test concentration outside the harbour; (4) the thickness of the moving layer; and (5) two parameters associated with dispersive processes. The results show that the concentration in the tidal basin sediment is higher than a number of simulated critical concentrations for representative cases. Consequently, the high level of the concentration of exotic benthic foraminiferal tests within the harbour should be explained as a result of landward net transport of sands within the entrance. 相似文献
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Coastal inundation associated with extreme sea levels is the main factor which leads to the loss of life and property whenever a severe tropical cyclonic storm hits the Indian coasts. The Andhra and Orissa coasts are most vulnerable for coastal inundation due to extreme rise in sea levels associated with tropical cyclones. Loss of life may be minimized if extreme sea levels and associated coastal flooding is predicted well in advance. Keeping this in view, location specific coastal inundation models are developed and applied for the Andhra and Orissa coasts of India. Several numerical experiments are carried out using the data of past severe cyclones that struck these regions. The simulated inland inundation distances are found to be in general agreement with the reported flooding. 相似文献
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Hoi-Soo Jung Kap-Sik Jeong Yong-Shik Chu Sung-Hyun Park Ki-Hyune Kim 《Marine Georesources & Geotechnology》2001,19(3):181-195
Grain size and water content in box-core sediments from the Clarion-Clipperton fracture zone (C-C zone) in the northeast equatorial Pacific were analyzed in detail to understand the downcore variations across a hiatus between Quaternary and Tertiary layers. Grain-size distributions in the topmost core sediments show two modes: a coarse mode (peaked at 50 μm) and a fine mode (at 2-25 μm). The coarse mode disappears gradually with depth accompanied by the dissolution of siliceous fossil tests, whereas the fine mode coarsens due to the formation of authigenic minerals. Water content increases abruptly across a color boundary between an upper pale brown layer and a lower dark brown layer that is the hiatus between Quaternary and Tertiary layers. Abundant smectites and microvoid molds, which are created by the prolonged fossil dissolution in the underlying sediment, are attributed for the abrupt downcore variation of water content. Overall variations in grain size and water content in the topmost core sediments in the western C-C zone are possibly constrained by the dissolution of biogenic siliceous fossils. Variations in geotechnical properties related to these changes must be considered in the design of nodule collectors. 相似文献
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Shigehisa Nakamura 《Marine Geodesy》2001,24(1):27-33
This article concerns an interrelation between the sea levels and the western boundary flow near a tectonic boundary in a local zone in the Northwestern Pacific. In this zone, sea level variations at stations located on the coast facing the Pacific are studied to find the interrelation between variations of the Kurosio flow as an index of the distance of the flow axis off a specific coast. The result is discussed after data processing of the monthly means of the sea levels, and a notice is taken of variations caused by active crustal upheavals during a seismic event, a local earthquake. 相似文献