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1.
为研究真鲷(Pagrus major)精子在外源DNA下的生理特性和转染效果,探索真鲷精子介导转基因技术,作者通过计算机辅助分析外源DNA环境下(不同孵育时间、DNA长度、DNA浓度)真鲷精子活率和运动速度的变化,进一步采用PCR和荧光探针的方法检测外源DNA与真鲷精子的结合情况,并通过人工授精来评价外源DNA能否转染精子并传递至F0代。结果表明:外源DNA浓度、孵育时间及DNA长度对精子活率无显著影响。在5μg/106个精子的高浓度10 kb DNA下孵育12 h,真鲷精子仍具有(75.89±5.55)%的精子活率,平均直线速度(70.97±6.37)μm/s,与对照组无显著差异,但精子平均曲线速度显著下降,比对照组低21.85μm/s。真鲷精子与带Fluorescein荧光素的DNA片段共孵育后,部分精子在荧光显微镜下观察到绿光。将DNA孵育后精子进行人工授精表明经过1μg DNA/106个精子孵育后的受精率和孵化率无显著下降,通过PCR法并没有在外源DNA处理的精子和F0代中检测到目的基因,表明外源DNA虽然能够吸附在真鲷精子表面,但并不足以携带进入卵子产生转基因后代。 相似文献
2.
长期超低温保存后真鲷精子的质量变化 总被引：1，自引：0，他引：1
通过对精子运动率、受精率和超微结构的观察,研究了2003~2009年分5批冷冻保存的真鲷(Pagrus major)精子经1~73个月保存后质量变化情况。冷冻精子在40℃水浴中解冻,大约100~110 s转化为液态后取出,用海水激活后观察精子运动率,人工受精6~8 h后观察受精率,同时精子用2.5%戊二醛前固定,经处理后用扫描电镜和透射电镜观察精子超微结构。结果表明,冷冻精子的最高运动率(87.67%±2.52%)和受精率(71.33%±8.84%)都是2009年保存1个月的精子,保存1,13,26个月的精子运动率和受精率差异不显著(P0.05),保存48个月后的精子运动率和受精率显著低于保存1个月的精子(P0.05),2003年保存的精子(73个月)运动率(50.67%±5.31%)和受精率最低(39.56%±0.69%)。精子的超微结构损伤主要包括精子头部损伤,线粒体损伤以及精子质膜的损伤。 相似文献
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花鲈精子生理特性及其精液超低温冷冻保存 总被引：21，自引：0，他引：21
以精子的活率、寿命和运动状态为参数,探讨了花鲈鲜精在不同盐度、酸碱度和离体条件下的生理特性,并对花鲈精液进行超低温冷冻保存研究.结果表明:盐度和酸碱度主要影响精子的寿命,对精子的活率影响不大;精子离休后置于室温(15～17℃)下8h,其活率和寿命随时间的延长而呈下降趋势,运动状态也逐渐减弱;不同组成成分的基础溶液以及抗冻保护剂的种类、浓度和使用方法均影响精液超低温冷冻保存效果;精液冷冻前经30min降温平衡(0～2℃),效果好于直接冷冻;冻精采用水浴快速解冻法(38～40℃)的效果优于室温(15.5～17.5℃)解冻法. 相似文献
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采用两步降温法超低温冷冻保存大黄鱼精子,并用透射电镜技术研究了精子的超微结构损伤.结果表明,大黄鱼冻精的激活率、运动时间及寿命与鲜精相比无显著差异.鲜精中28.5％的精子形态结构异常,冻精中37％的精子形态结构异常.形态结构正常的精子表现为质膜与核膜结构完整、无膨胀现象,袖套、轴丝及中心粒结构正常,线粒体形态完整、嵴较发达;形态结构异常的精子表现为质膜破裂、脱落,质膜膨胀,核膜破裂、脱落,核局部受损伤,线粒体膨胀、嵴退化或消失,线粒体移位或脱落.结果显示,以Cortland溶液为稀释液,10％ DMSO为抗冻剂,对大黄鱼精子具有较好的抗冻保护作用. 相似文献
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大黄鱼精子生理特性及其冷冻保存 总被引：14，自引：0，他引：14
研究了大黄鱼精子的生理特性及其冷冻保存技术。实验结果表明,大黄鱼精液pH值为6.72—7.25。精子平均密度为14.45×109·ml-1。精子离体后在精液中3.5h(25℃)仍有80.5%可以存活。在精子激活液中,不同的盐度和酸碱度对精子的活力、存活时间和运动状况影响很大。精子适宜的盐度为20—35,pH值为6.60—8.50。在海水中精子的直线快速运动仅持续3min。使用筛选出的精液稀释液和抗冻剂组成精子冷冻保存液。采用快速冷冻保存方法在液氮中保存精子。经保存1a,采用室温(21—23.5℃)自然解冻冻精,精子活力可达到89.5%±4.2%。利用冻精进行大黄鱼的人工授精试验,受精率达82.7%±5.5%,孵化率达85.7%±5.8%,与鲜精对照组相近。 相似文献
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采用计算机辅助分析和电子显微镜方法, 对大菱鲆(Scophthalmus maximus)精子生理活性(运动率、运动速度和寿命)和超微结构进行观察, 研究其精子经超低温保存后质量变化情况, 得到了新鲜精子的路径速度[(101.91±9.30)?m/s]、运动率(88.30%±2.62%)和寿命[(368.00±111.50)h], 以及冷冻精子的路径速度[(76.78±8.49)?m/s]、运动率(65.60%±4.76%)和寿命[(120.00±12.00)h]。结果表明, 新鲜精子的生理特性好于冷冻精子。同时通过电镜去进行超微结构分析, 发现大菱鲆精子经过超低温保存后, 40%—60%的精子基本保持正常的形态结构, 其余精子遭受不同程度的机械损伤。其中膜损伤为主要损伤, 损伤精子中60%—70%带有膜损伤。推测大菱鲆精子在冷冻解冻过程中遭受到的机械损伤可能是导致冻精生理活性显著下降的主要原因。 相似文献
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采用分步降温法冷冻保存太平洋鳕(Gadus macrocephalus)精液,并用扫描电镜和透射电镜技术研究了精子的超微结构损伤。分析了添加剂(蛋黄)及五种抗冻剂(PG(丙二醇)、DMSO(二甲基亚砜)、EG(乙二醇)、GLY(甘油)、MeOH(甲醇))不同浓度(8%、10%、12%、14%、16%、18%)对太平洋鳕精子冷冻保存效果的影响。实验结果表明,蛋黄能够显著提高太平洋鳕冷冻保存效果(P0.05);12%PG中添加10%蛋黄保存的冻融精子运动率最高(85.87%±1.6%),显著高于其他冻存组(P0.05)。添加蛋黄的12%浓度的DMSO组解冻后精子运动速率较高,平均直线速度、平均曲线速度、平均路径速度分别达到了(120.39±20.78)μm/s、(120.39±20.78)μm/s、(155.64±12.02)μm/s,与其他各实验组差异显著(P0.05)。通过扫描电镜和透射电镜观察新鲜和冻融后的鳕鱼精子发现,鲜精中75.5%精子形态结构正常、24.5%精子形态结构异常;运动率最高的冻精中67%精子形态结构正常、33%精子形态结构异常。超低温保存对太平洋鳕精子结构产生了显著影响,细胞膜破裂、线粒体肿胀变形,鞭毛脱落、断裂。 相似文献
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点带石斑鱼精子超低温冷冻保存研究 总被引：1，自引：0，他引：1
为建立点带石斑鱼(Epinephelus malabaricus)精子冷冻保存技术,保存点带石斑鱼种质资源,作者通过选用TS-19、TS-2、Hank’s、MPRS、Cortland、0.75%NaCl等作为稀释液及10%~25%二甲亚砜、甘油、甲醇作为抗冻液,对繁殖季节中3个不同时期的点带石斑鱼精液进行超低温冷冻保存研究。研究结果表明:(1)Hank’s溶液为点带石斑鱼精子冷冻保存最适冷冻稀释液;(2)Hank’s溶液与10%~15%DMSO溶液为点带石斑鱼精子保存的最适冷冻保护液组合,可以获得60%以上的冻精成活率,而使用不同浓度的MeOH作为抗冻液时,冻精成活率均为0%;(3)以10%~25%Gly作为抗冻液时,冷冻前未加天然海水时均能激活点带石斑鱼精子正常运动,其效果与天然海水相似,加入天然海水后精子运动效果急剧下降,精子冷冻保存后也存在同样现象;(4)为保证获得更高的冻精成活率,点带石斑鱼精液冷冻保存样品的最佳获取时期是在亲鱼自然繁殖期前进行为宜。 相似文献
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对赤点石斑鱼(Epinephelus akaara)精子的激活特点、超低温冷冻方案筛选、短期保存、受精实验等方面进行了研究。结果表明：水温25℃、比重为1.018的海水对赤点石斑精子具有最佳的激活效果,活力为(82.50±4.18)%;在进行超低温冷冻时,选择距离液氮面7 cm的高度进行降温,获得冻后活力为(65.83±3.76)%,显著高于1、3、15 cm 的处理组(P<0.0001),利用冻存液 B(含30 g/L 海藻糖、10%DMSO 的生理盐水)冻存赤点石斑精子,冻精活力为(67.92±3.96)%,显著高于另外两种冻存液(P<0.05);通过优化的方案(冻存液B,7 cm高度)冻存得到精子可获得较好的受精效果,受精率为(74.55±4.31)%,而相应的鲜精受精率可达(87.42±4.63)%,二者间的差异具有显著性(P=0.017);短期保存的结果表明,赤点石斑鱼精子在4℃环境中保存约两周后活力降低为0。 相似文献
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Chandralata Raghukumar G. Sheelu P. A. Loka Bharathi Shanta Nair C. Mohandass 《Marine Georesources & Geotechnology》2001,19(1):1-16
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. 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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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. 相似文献
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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。 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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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. 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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Phylogenetic diversity and phenotypic characterization of cultivable bacterioplankton isolated from polar oceans 总被引：1，自引：0，他引：1
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. 相似文献