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1.
双斑东方Tun人工繁殖及育苗技术 总被引：1，自引：0，他引：1
本文报道了福建省水产研究所2001年双斑东方Tun人工繁殖及育苗过程与结果。在春季当海水水温达到16℃以上时，用DOM、LRH－A3或HCG进行催产，混和或单一使用，剂量视亲鱼性腺成熟度而定。受精卵在水温18．0－22．4℃、盐度22．2－28．6条件下，经117－156h孵化。用250万尾开口仔鱼培育出平均全长为37mm，平均体重为1．3g的鱼苗52．35万尾，成活率25．5％。此外，对亲鱼的暂养、催产、受精卵的孵化、仔鱼的前期培育和后期培育等关键环节进行了探讨。 相似文献
2.
报道了2004～2005年菊黄东方鲀(Fugu flavidus)人工繁殖及育苗实验结果.在春季当水温达到20℃以上时,用地欧酮(DOM)、促黄体素释放激素类似物(LHRH)或绒毛膜促性腺激素(HCG)进行催产,混和或单一使用,剂量视亲鱼性腺成熟度而定.受精卵在海水盐度20.0～30.0,水温20.0～25.0℃条件下,经144～156 h孵化.608万尾仔鱼培育出平均全长4.43 cm、平均体质量1.98 g的幼鱼168.5万尾,成活率27.7%.对亲鱼的暂养、催产、孵化、仔鱼的前期培育和仔鱼的后期培育等关键技术进行了探讨. 相似文献
3.
利用人工培育的亲鱼所获得的受精卵 ,孵化出仔鱼 30 0万尾 ,在水温 18～ 2 0℃、微充气的培育条件下 ,使用海水小球藻、轮虫、卤虫无节幼体和不同规格的微颗粒配合饲料进行饲喂 ,经 58d培育出平均全长 2 .3cm的苗种 132万尾 ,育苗成活率高达 64.1% ,单位水体最高出苗量达 1.33万尾 / m3;另外 ,还有 1.3～ 1.9cm的苗种 68万尾 相似文献
4.
花尾胡椒鲷人工繁殖及育苗技术研究 总被引：1，自引：0，他引：1
海水网箱饲养的3龄花尾胡椒鲷，催产前2个月进行培育，用绒毛膜促性腺激素（HCG）和LRH－A3激素进行催产，混合或单一使用，剂量视亲鱼性腺的成熟度而定，受精卵在盐度为31，PH为80－8．4，水温20－23℃的海水中，经35－36h完成胚 发育，破膜卵孵出成仔鱼。室内水泥池，在盐度为25－26，PH为8．0－8．4，水温24－26℃的海水中，仔鱼经36d培育，态进行幼鱼期；室土肥有苗，在海水盐度为22－31．1，PH为8．0－8．4，水温19－24℃时，仔鱼经30d培育，完成变态进入幼鱼期。 相似文献
5.
双棘黄姑鱼人工育苗技术的研究 总被引：8，自引：1，他引：7
对双棘黄姑鱼【Nibeadiacanthus(Lacepede)】催产孵化和育苗技术进行了试验研究,并从形态学方面对其近似种和易混种进行了比较。结果显示,双棘黄姑鱼性腺发育至Ⅳ期经人工催产都能产卵受精．效应时间为20～40h。胚胎发育适宜水温为22～26℃．适宜盐度为30～35,孵化率为80％～90％。在育苗水温27～29℃,盐度28～30,150万初孵仔鱼经20d培育,共育出全长1．4～2．3cm的稚鱼95．3万尾,育成率62．3％;其中32．2万稚鱼分池继续培育至36天,育出全长3．1～5．2cm的幼鱼18．4万尾。本试验说明对双棘黄姑鱼进行人工催产孵化育苗,能够培育出达到商品规格的鱼种。 相似文献
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7.
美洲鲥的人工繁殖及胚胎发育的研究 总被引：10，自引：0，他引：10
2007～2009年,利用深井水及设有钢架保温大棚的土池成功进行了美洲鲥(Alosa sapidissima)的亲鱼培育与人工繁殖的研究,同时观察了美洲鲥的胚胎发育过程.结果表明:2龄美洲鲥在池塘中经专池培育并采用激素+不饱和脂肪酸+维生素E投喂、水流刺激等培育措施使雌雄鱼的性腺成熟率达60％～80％.性腺成熟的亲鱼经生态调控促使产卵或人工催产繁殖,生态调控促使产卵中水温保持在16～23℃,池水始终保持流动状态,50对美洲鲥亲鱼自4月中下旬至5月底陆续产卵,共收集鱼卵9.0万粒,平均受精率10％,孵化率70％～80％;人工催产试验中,采用LHRH-A2+鱼类催产助剂、LHRH-A2+HCG+DOM+鱼类催产助剂和LHRH-A2+HCG+鱼类催产助剂3种催产剂配伍,背鳍基部两针注射法,催产率20％～100％,获卵10.57万粒,受精率0～21.5％,孵化率0～70％.美洲鲥受精卵呈卵圆形,卵膜径为(4.03±0.25)mm,根据胚胎的外形与内部主要特征,胚胎发育分为7个生理阶段30个具体发育时期,在水温(20±1)℃下,历时约71 h40 min完成整个胚胎发育过程. 相似文献
8.
利用人工培育的2龄四指马鲅(Eleutheronema tetradactylum)亲鱼自然产卵受精而获得的受精卵在实验室中孵化和培育,对受精卵胚胎发育到仔鱼孵出的全过程进行详细的观察记录.结果表明:四指马鲅受精卵呈圆球形,卵膜光滑,单油球.平均卵径675.78μm,油球平均直径258.46μm.在水温为31~33℃,盐度为27.50~28.00,p H值为8.2条件下,胚胎发育用时13 h 52 min,可分为卵裂、囊胚、原肠胚、胚体形成、器官分化和孵化6个阶段,初孵仔鱼全长1.46±0.25 mm,3DAH仔鱼全长2.42±0.18 mm,口和肛门张开,仔鱼开口摄食. 相似文献
9.
大泷六线鱼全人工繁育技术研究 总被引：7，自引：0，他引：7
2012年~2014年,作者在山东省海洋生物研究院鳌山卫中试基地进行了大泷六线鱼(Hexagrammos otakii)全人工繁育研究,通过人工促熟、激素诱导,培育F1代全人工亲鱼558尾(雄鱼231尾,雌鱼327尾),获得受精卵33.0万粒,孵化F2代仔鱼30.0万尾,受精率98%,孵化率91%。在水温16~17℃、盐度31、p H 7.8~8.1、溶解氧6 mg/L条件下,历时110 d,培育平均全长6.2 cm F2代苗种11.7万尾,苗种成活率39%。作者在国内外首次开展了大泷六线鱼全人工繁育技术研究,丰富了大泷六线鱼养殖基础资料,为大泷六线鱼产业的发展奠定基础。 相似文献
10.
台湾海峡野生牙鲆人工繁殖和育苗技术研究 总被引：4，自引：0，他引：4
2003年12月至2004年5月对台湾海峡的野生牙鲆进行了亲鱼的驯养、促熟产卵及人工育苗技术研究.结果表明,活的鲻鱼苗可用于牙鲆亲鱼的诱食;当水温达到16.2~19.5℃时,牙鲆可自然产卵,产卵盛期为3月中旬至4月上旬.4月份受精率高达86%.在驯养过程中亲鱼未发生死亡.本实验共用受精卵约153万粒,孵出仔鱼140.8万尾,孵化率达92%.经63d培育,育出全长3.8~5.5cm幼鱼53.4万尾,成活率37.9%.育苗水温为20~24℃,海水盐度为26~31. 相似文献
11.
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
12.
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
13.
Derek V. Ellis 《Marine Georesources & Geotechnology》2001,19(1):51-63
This article reviews information recently available from existing marine and coastal mining for responses to environmental issues affecting marine mining at different depths. It is particularly but not exclusively concerned with those issues affecting seabed biodiversity impact and recovery. Much information has been gathered in the past 10 years from shallow mining operations for construction aggregate, diamonds, and gold, from coastal mines discharging tailings to shallow and deep water, and from experimental deep mining tests. The responses to issues identified are summarized in a series of eight tables intended to facilitate site-specific consideration. Since impacts can spread widely in the surface mixing layer SML, and can affect the biologically productive euphotic zone, the main issues considered arise from the depth of mining relative to the SML of the sea. Where mining is below the SML, the issue is whether it is environmentally better to bring the extraction products to the surface vessel for processing (and waste discharge), or to process the extraction products as much as possible on the seabed. Responses to the issues need to be sitespecific, and dependent on adequate preoperational environmental impact and recovery prediction. For deep tailings disposal from a surface vessel, there are four important environmental unknowns: (1) the possible growth of "marine snow" (bacterial flocs) utilizing the enormous quantities of fine tailings particles (hundreds or thousands of metric tons per day) as nuclei for growth, (2) the possibility that local keystone plankton and nekton species may migrate diurnally down to and beyond the depth of deep discharge and hence be subjected to tailings impact at depth, (3) the burrow-up capability of deep benthos and their ability to survive high rates of tailings deposition, and (4) the pattern and rate of dispersion of a tailings density current through the deep water column from discharge point to seabed. Actions to obtain relevant information in general and site-specifically are suggested. 相似文献
14.
G. Parthiban 《Marine Georesources & Geotechnology》2000,18(3):223-235
Particle fluxes were measured 7 m above the sea bottom during the predisturbance, disturbance, and postdisturbance periods by using time series sediment traps attached to seven deep-sea moorings deployed in the INDEX experiment site in the Central Indian Basin. The predisturbance particle fluxes varied between 22.3 to 55.1 mg m -2 day -1 . Increased and variable particle fluxes were recorded by the sediment traps during the disturbance period. The increase observed was 0.5 to 4 times more than the background predisturbance fluxes. The increases in particle fluxes (~4 times) recorded by the sediment trap located in the southwestern direction (DMS-1) were the greatest, which could be the result of preferential movement of resuspended particles generated during the deep-sea benthic disturbance along the general current direction prevailing in this area during the experimental period. Also, the traps located closer to the disturbance area recorded greater fluxes than did the traps far away, across the Deep Sea Sediment Resuspension System path. This variability in recorded particle fluxes by the traps around the disturbance area clearly indicates that physical characteristics such as grain size and density of the resuspended particles produced during the disturbance had an important effect on particle movement. The postdisturbance measurements during ~5 days showed a reduction in particle fluxes of ~50%, indicating rapid particle settlement. 相似文献
15.
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
16.
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
17.
The advanced piston corer (APC) has been used by the Ocean Drilling Program since 1985 for recovering soft sediments from the ocean floor. The pullout force measured on extracting the core barrel from the sediment is shown to correlate with the average shear strength of the sediment core measured in the ship's laboratory. A simple rule of thumb is derived relating the shear strength of the sediment to the pullout force. Multiple APC holes at individual sites allow the consistency of the pullout measurements to be assessed. The effects of different operational procedures during APC coring are also explored. Although generally applicable, the correlation between pullout force and laboratory measurements of shear strength breaks down for some APC holes, possibly because of the disturbance of some sediment types during the APC coring process. A better understanding of the physical process of APC coring, and its effect on the properties of the sediment both inside and immediately outside the core barrel, would indicate what confidence can be put on the measurement of pullout force as a way of evaluating the in situ shear strength of deep sea sediments. 相似文献
18.
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
19.
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
20.