黄姑鱼(Nibea albiflora)雌核发育的人工诱导及鉴定

采用紫外线(UV)灭活的同源精子通过冷休克抑制第二极体排放诱导黄姑鱼(Nibea albiflora)的雌核发育。结果表明,黄姑鱼精子最适的灭活剂量为420mJ/cm2,紫外照射剂量与黄姑鱼精子和卵子授精后的受精率及孵化率之间表现出明显的Hertwig效应。多次试验筛选的黄姑鱼雌核发育的最适条件为授精后2min于3℃处理8min。雌核发育仔鱼经形态学和流式细胞仪鉴定为二倍体。进一步利用10对微卫星分析了遗传物质在亲本和子代中的传递情况,结果表明雌核发育后代的等位基因完全来自于母本,没有父本基因参与;雌核发育后代在5个微卫星位点具有较高的重组率,使其与母本保持了高度同质性。     

条石鲷(Oplegnathus fasciatus)雌核发育的人工诱导与鉴定

条石鲷(Oplegnathus fasciatus)是我国重要的经济鱼类,具有复性染色体性别决定型(X₁X₁X₂X₂/X₁X₂Y)。利用紫外线(UV)灭活的同源精子通过冷休克方法诱导了条石鲷的雌核发育,筛选精子紫外灭活剂量并优化冷休克相关参数。结果表明:条石鲷精子最适的灭活剂量为80 mJ/cm2雌核发育的最适条件为授精后2 min在3～4°C水温下处理10 min。条石鲷雌核发育子代经形态学和流式细胞仪鉴定为二倍体,进一步利用微卫星分析表明雌核发育后代的等位基因完全来自于母本没有父本基因参与。对子代的性比和生长进行了比较,结果表明条石鲷雌核发育后代均为雌性,15月龄后雌核发育后代比普通条石鲷具有更快的生长速度。研究结果为条石鲷单性苗种的培育及其性别决定机制的深入研究提供基础。     

大黄鱼雌核发育二倍体的人工诱导

采用紫外线照射对大黄鱼(Pseudosciaena crocea Richardson)精子遗传物质进行完全灭活,灭活后精子与卵子受精获得雌核发育单倍体受精卵,再通过冷休克对单倍体受精卵进行倍性恢复,成功诱导出大黄鱼雌核发育二倍体。实验结果表明:(1)在紫外照射过程中照射剂量与大黄鱼精子和卵子受精后其成活率和孵化率呈现出明显的Hertwig效应,紫外照射时间超过2 min(剂量>2 400 ergs/mm2),可使大黄鱼精子遗传物质完全灭活。大黄鱼雌核发育诱导中精子遗传灭活的最适紫外照射时间为2.5 min(剂量为3 000 ergs/mm2);(2)冷休克法可成功抑制大黄鱼受精卵第二极体排放,诱导效果受处理时刻、处理时间和处理温度三因素的影响。综合雌核发育二倍体的诱导率、处理后受精卵早期胚胎存活率和仔鱼孵化率等因素,较适合的染色体加倍条件为23℃培育水温下授精后2 min,在3-4℃海水中处理10 min。     

刺参雌核发育二倍体的诱导及其早期生长发育

紫外线照射使精子遗传物质失活,用细胞松弛素B(CB)处理受精卵抑制第二极体释放,诱导刺参(Apostichopusjaponicus)雌核发育二倍体。用强度为2561μW/(cm2.s)的紫外线(254 nm)照射不同时间的精子与正常卵子受精。结果发现随照射时间的增加,卵裂率、早期胚胎存活率和小耳幼虫发生率逐渐降低,照射30 s时小耳幼虫发生率降为0。受精后35 min,显微镜下观察到有20%~30%受精卵排出第1极体时,用浓度0.5μg/mL的CB持续处理受精卵20 min,诱导出刺参第二极体抑制型雌核发育二倍体,雌核发育二倍体发育速度低于正常二倍体。微卫星分析表明,雌核发育二倍体诱导成功率为93.3%。     

紫贻贝雌核发育二倍体的人工诱导研究

采用紫外线照射的方式使精子遗传物质失活,通过细胞松弛素B(CB)的处理来抑制受精卵第二极体的释放,人工诱导紫贻贝(Mytilus gallopovincialis)雌核发育二倍体。将精子在强度为2561μW/(cm~2·s)的紫外线(254 nm)下进行时间梯度的照射,之后与正常的卵子受精,实验发现随照射时间的增加,卵裂率、早期胚胎存活率和D形幼虫发生率总体呈下降趋势,在照射55 s时D形幼虫发生率降为0。受精后25 min,用浓度0.5μg/mL的细胞松弛素B(CB)持续处理受精卵20 min,诱导出紫贻贝第二极体抑制型雌核发育二倍体。通过微卫星分析鉴定所得的子代个体均为雌核发育二倍体。     

人工诱导香港巨牡蛎雌核发育单倍体的研究

研究利用紫外线诱导香港巨牡蛎Crassostrea hongkongensis雌核发育的条件.结果表明,在强度为1820μW · (cm2·s)-1的紫外线(254nm)下分别照射精子0,5,10,15,20,25,30,35,40,45,50,55,60,70,80和90s后,照射30s的实验组能够保持较高的受精率(61.6%),该组的D形幼虫发生率为0,出现"Hertwig效应".研究表明,在强度为1 820 μW·(cm2·s)-1的紫外线下照射精子30s是获得香港巨牡蛎雌核发育单倍体的适宜条件.研究还表明受精率和D形幼虫发生率随照射时间的增加而下降,遗传失活的精子与正常卵子受精后其胚胎发育至D形幼虫前期停止.经紫外线照射的精子授精后所产生的单倍体胚胎发育速度慢于正常受精所产生的二倍体胚胎,各照射组均出现非整倍体.     

《中国海洋湖沼学报》(英文版,SCI-E收录)Chinese Journal of Oceanology and Limnology 2010年第4期论文导读

<正>Artificial induction of mito-gynogenetic diploids in large yellow croaker(Pseudosciaena crocea)by hydrostatic pressure蔡明夷,王志勇等:研究了人工诱导大黄鱼(Pseudosciaena crocea)有丝分裂雌核发育的条件。研究结果表明,处理持续时间为3 min时,静水压抑制大黄鱼雌核发育卵第一次有丝分裂适宜的压力强度为40 Mpa,与抑制第二次减数分裂相当。作用起始时间存在一个时间窗口,25.0±1.0°C下为授精后36.1~38.1 min,在此窗口中正常仔鱼的得率没有显著性差异。其中,在授精后38.1 min开始施压,正常仔鱼得率最高,达9.36%±2.97%。     

夏牙鲆(♂)与牙鲆(♀)人工杂交的细胞遗传学初步研究

于2004年11～12月在青岛薛家岛养鱼场采用夏牙鲆(Paralichthysdentatus)的精子与牙鲆(Paralichthysolivaceus)的卵子实施了多次人工杂交实验,并进行了父本母本鱼类个体、子代的染色体制片观察和细胞中DNA相对含量的流式细胞仪检测。结果表明,夏牙鲆染色体数为48,核型为2n=48t、臂数NF=48;子代的染色体数和核型与父母本的一样,也为2n=48t;子代的细胞中DNA的相对含量也表明其为二倍体。因此,可以明确其为杂交的后代,而不是雌核发育。     

人工诱导栉孔扇贝雌核发育胚胎的SNP标记分析

利用紫外线照射灭活的同源精子,激活栉孔扇贝(Chlamys farreri)卵子分裂,获得雌核发育胚胎,流式细胞仪检测胚胎细胞平均单倍体率为82.5%。对获得的胚胎进行全基因组扩增,获得足量的基因分型模板,利用高分辨率溶解曲线(HRM)技术对其进行96个单核苷酸多态性(SNP)位点分型。结果显示,诱导雌核发育胚胎的位点检出率为96.27%,其中99.06%的位点分型结果与相应雌性亲本相符;单个胚胎中只表现一种等位形式的位点占91.67%~96.88%,平均为94.81%,较雌性亲本的纯合位点比例(64.25%)明显提高。本研究利用灭活同源精子诱导获得栉孔扇贝雌核发育胚胎,并利用单个胚胎的全基因组扩增产物进行基因位点分析,为扇贝人工诱导雌核发育个体的早期多基因位点检测和评价提供参考。     

同源和异源精子诱导大黄鱼(Pseudosciaena crocea)雌核发育的胚胎发育比较及子代 SSR 遗传标记分析

以紫外灭活的同源(大黄鱼)精子和未灭活的异源(鮸鱼)精子为激活源, 采用冷休克处理的方法诱导了大黄鱼雌核发育二倍体, 进行胚胎发育和 SSR 标记分析的比较研究。结果表明, 异源组的受精率和孵化率高于同源组, 但存活率低于同源组; 两组中经冷休克处理未能恢复倍性的胚胎发育畸形而陆续死亡, 恢复倍性的胚胎在发育程序上均与普通大黄鱼相同, 但各阶段出现时间较对照组滞后; SSR 分析显示同源组子代中有 16.7%出现父本条带, 异源组子代均未出现父本条带。以灭活的同源(大黄鱼)精子和未经灭活的     

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.     

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.     

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.     

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,     

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.