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1.
凡纳滨对虾的遗传育种研究现状   总被引:1,自引:0,他引:1       下载免费PDF全文
凡纳滨对虾(Litopenaeus vannamei Boone),由于其生长快,抗环境变化能力强,对饵料的要求低,肉味鲜美、出肉率高,成为世界上公认的优良养殖对虾品种之一.凡纳滨对虾自1998年从美国夏威夷再次引进到中国华南,并相继突破集约化防病养殖和全人工繁育技术以来[1],已成为中国海水养殖动物中发展最快的一个种类,其养殖产量已达到中国养殖对虾产量的80%~90%.然而目前中国凡纳滨对虾亲虾多数直接从虾塘挑选,造成品质参差不齐,抗病力下降,生产周期延长,严重制约了中国凡纳滨对虾养殖业持续健康发展.凡纳滨对虾亟需形成稳定优良的养殖品系.  相似文献   

2.
循环水养殖系统在凡纳滨对虾种虾养殖中应用较少,本研究应用循环水养殖系统养殖凡纳滨对虾种虾,设定4个不同的养殖密度(30、40、50、65尾/m2),初始体重:(0.102±0.008)g,研究凡纳滨对虾种虾在循环水养殖系统中的生长情况。养殖期间定时对对虾体重和水体指标(氨氮、亚硝酸氮、pH、水温、微生物)进行分析测定。通过对各项数据分析表明:低密度组(30、40、50尾/m2)凡纳滨对虾体重增长较快,各组特定生长率分别为(3.83±0.03)%、(3.87±0.01)%、(3.81±0.03)%,绝对增重率分别为(0.201±0.009)、(0.214±0.004)、(0.194±0.009)g/d,但均无显著性差异(P0.05);高密度组(65尾/m2)的凡纳滨对虾体重增长较慢,特定生长率和绝对增重率分别为(3.41±0.02)%和(0.107±0.004)g/d,该结果与低密度组间存在显著性差异(P0.05)。低密度组中凡纳滨对虾养殖水体的水质指标要优于高密度组,4个密度组中氨氮、亚硝酸氮、绿菌均维持在安全浓度范围内,仅仅黄菌数量略高。综合分析,采用该养殖系统养殖凡纳滨对虾的最优密度为50尾/m2。因此,本研究可为循环水养殖系统养殖凡纳滨对虾种虾提供参考。  相似文献   

3.
研究了低盐度条件下,二溴海因和碳水化合物水平对凡纳滨对虾(Litopenaeus vannamei)生长和免疫的影响,共3个实验。实验1研究了二溴海因对凡纳滨对虾存活的影响,发现在0.2、5和20三个盐度水平,随着二溴海因浓度的升高,凡纳滨对虾存活率呈下降趋势;二溴海因对凡纳滨对虾的安全浓度随盐度的增加呈上升趋势。实验2和实验3研究了盐度、二溴海因浓度和饲料中碳水化合物水平对凡纳滨对虾生长和免疫的影响,结果表明:在低盐度养殖条件下,凡纳滨对虾长期生活于二溴海因环境中,可导致对虾处于应激状态,需要消耗体内较多的免疫因子,血清酚氧化酶和超氧化物歧化酶活性降低,生长速度下降,而在饲料中适量增加碳水化合物不仅可促进对虾生长又可起到饲料蛋白质节约作用。  相似文献   

4.
2003年在乳山养殖场采用两种围栏养殖模式养殖了凡纳滨对虾,并对其防白斑综合征病毒(WSSV)效果进行了比较。结果表明,凡纳滨对虾在养殖过程中WSSV阳性率有下降趋势,浮游动物WSSV阳性率较低,布围隔的防病毒效果好于网围隔。  相似文献   

5.
集约式养殖凡纳滨对虾体长与体重的关系   总被引:9,自引:0,他引:9  
研究了集约化养殖凡纳滨对虾Litopenaeus vannamei体长与体重的关系,通过全过程采样测试并经回归分析得到不同生长阶段的体长、体重关系式。研究发现当体长大于12.5cm时相同体长的雌虾要明显重于雄虾(p〈0.01)。比较地膜养殖池与沙底养殖池对凡纳滨对虾生长的影响,结果表明当养殖天数大于90d时,地膜养殖池对虾的生长明显优于沙底养殖池对虾(p〈0.05)。  相似文献   

6.
凡纳滨对虾是当今世界公认的重要对虾养殖品种之一,然而良种选育研究仍相对落后,亟需采用分子遗传学手段加以解决.本文以凡纳滨对虾为材料,对预扩增体系、选择性扩增体系中的稀释倍数、dNTP浓度、Taq浓度、Mg2+浓度、引物浓度进行比较,结果表明,300 ng基因组DNA采用5U PstI和5UMseI双酶切4 h,16℃连接过夜,连接产物稀释10倍进行预扩增,预扩增产物稀释50倍进行选择性扩增,能够得到稳定丰富的条带,最终建立了适用于凡纳滨对虾的AFLP反应体系.本研究又进一步应用优化后的AFLP反应体系,从64对选择性扩增引物组合中筛选出12对多态性高的引物组合,便于对凡纳滨对虾基因多态性位点进行分析,从而为凡纳滨对虾的遗传多样性研究奠定基础.  相似文献   

7.
研究了3种凡纳滨对虾池塘养殖模式环境因子变化情况和对养殖效益的分析。实验分为3种不同的养殖模式:对虾单养组、鱼虾混养A组、鱼虾混养B组。结果表明:pH变化范围在8.40~9.06之间,其中对虾单养组pH较之两组鱼虾混养组略高,最高值达9.06;COD变化范围在101~211之间,其中对虾单养组COD较之两组鱼虾混养组略高,范围在132~211之间;氨氮和亚硝酸盐氮浓度为对虾单养组鱼虾混养A组鱼虾混养B组;异养菌数目和弧菌数目,随着养殖的进行呈现逐渐增加的趋势,最大值分别为对虾单养组1.1×106 CFU/mL、2.0×103 CFU/mL,鱼虾混养A组1.45×106 CFU/mL、1.80×103 CFU/mL,鱼虾混养B组1.20×106 CFU/mL、1.56×103 CFU/mL;养殖效益上,总产值、纯利润、亩利润、投入产出比均呈现出鱼虾混养B组鱼虾混养A组对虾单养组。由此可见,凡纳滨对虾和鱼类混养,可以在保证水质的前提下,提高凡纳滨对虾养殖规格,提高投入产出比,增加养殖效益,是一种相较于凡纳滨对虾单独养殖优越的养殖模式;而不同规格和数量的鱼类和不同数量凡纳滨对虾的混养,又会产生不同的养殖效益。  相似文献   

8.
为了研究我国海南地区某凡纳滨对虾(Litopenaeus vannamei)繁育群体的种质资源多样性,选取14个比利时野生对虾的EST微卫星标记,以240个中国人工选育的凡纳滨对虾个体为研究对象,检测这些标记在该养殖群体遗传多样性评估中的可行性,结果表明,有7个引物可扩增出清晰条带,其中5个引物(CNM-MG 345,...  相似文献   

9.
高位池养殖对虾携带白斑综合症病毒变化   总被引:3,自引:0,他引:3  
采用实时荧光定量 PCR 技术研究6口高位池塘斑节对虾和凡纳滨对虾携带WSSV变化,结果表明:养殖过程中凡纳滨对虾WSSV携带量最高为9.7×105拷贝/g;斑节对虾最高携带量为9.5×105拷贝/g.凡纳滨对虾WSSV感染率分别为:苗种没有携带WSSV;30d为80.0%;60 d为90.O%;90 d为90.0%;120 d为93.3%,斑节对虾潜伏感染率分别为:苗种没有携带WSSV;30d为73.3%;60d为83.3%;90d为90.O%:120d为96.7%.  相似文献   

10.
本研究以凡纳滨对虾(Litopenaeus vannamei)为对象,通过琼脂扩散法、荧光染色法与分光光度法筛选出对凡纳滨对虾致病菌有抑制作用、对对虾肠黏液有黏附作用且对盐度有耐受性的3株菌(YRL45、KTP(C-2)、QL),经16S rDNA测序比对发现此3株菌均为植物乳杆菌。将其混合饲喂凡纳滨对虾4周,通过高通量测序研究虾肠道菌群变化。研究表明,混合植物乳杆菌的饲喂对凡纳滨对虾肠道菌群的α多样性无显著性影响,变形菌门和拟杆菌门为凡纳滨对虾肠道优势菌门,植物乳杆菌对凡纳滨对虾肠道中放线菌门的丰度有一定的提高。通过LEfSe分析,发现植物乳杆菌处理组中潜在致病菌发光杆菌属减少,而属于光合细菌的赤杆菌属有所增加。研究结果为益生菌在凡纳滨对虾的应用提供了一定的理论指导。  相似文献   

11.
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   

12.
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   

13.
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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15.
《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   

16.
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   

17.
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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19.
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   

20.
Observations on seafloor features from subbottom profiling and seabed photography data show that the undisturbed and natural conditions before the benthic disturbance undergo a substantial change after operation of the disturber. The effects can be seen in the form of deep trenches and grooves, formed by the action of the sleds and the pumping of the sediment along its path, as well as sediment piles on either side of the track. Biological traces such as fecal coils, casts, tubes, burrows, and trails get obliterated in the areas of disturbance and resedimentation. The smooth, uniform nature of the seafloor observed in predisturbance phase shows microtopographic changes in and around the disturbed area as a result of sediment excavation and resettlement. Vertical mixing as well as lateral transport of sediment alter the geological, biological, physical, and chemical conditions on the seafloor, which need to be monitored over time to assess the process and the time taken for restoration of environmental conditions.  相似文献   

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