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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
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花鲈亲鱼人工培育与催产技术研究 总被引：1，自引：0，他引：1
作者研究了花鲈人工培育及促熟催产中的技术措施。采用海捕的天然苗种 ,逐年筛选、精心培育 ,共获得 4～ 6龄的成熟亲鱼 50尾。在外源激素 HCG(70 0～ 150 0 IU/ kg)及 LHRH- A3(2～5μg/ kg)的作用下 (雄鱼减半 ) ,共人工采卵 156 0× 10 4粒 ,卵的平均上浮率为 6 1% ,平均受精率为78% ,平均孵化率为 85.7%。 相似文献
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人工管道诱导大弹涂鱼产卵研究 总被引：12，自引：0，他引：12
报道了人工制作的陶瓷管道诱导大弹涂鱼Boleophthalmus pectinirostris产卵的研究结果，未经激素催熟的亲鱼放入产卵池内7-12d未见产卵，经一次激素注射催熟的亲鱼放入产卵池内第3天开始酱产卵和受精，入池后5d未能产卵雌鱼的卵母细胞开始退化吸收，雌鱼不仅在管道内产卵，而且也将卵产在管道外，池底和池壁，产卵时间集中在下半夜的02：00-04：00，不同产卵池中管道的产卵率差别很大，卵子粘附在管道不同部位的数量和受精率均不相同，强迫配对的亲鱼虽有产卵，但卵子不受精。 相似文献
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为开展黄鳍东方鲀(Fugu xanthopterus)批量全人工育苗、胚胎及仔稚幼鱼发育特征研究, 作者使用地欧酮(DOM)、促黄体释放激素类似物(LRH)及绒毛膜促性腺激素(HCG)对性成熟黄鳍东方鲀进行人工催产。结果表明黄鳍东方鲀亲鱼效应时间为39～60h, 获产率为55.0%～92.5%; 卵受精率为35.5%～84.7%, 3 年产卵7 400 g; 受精卵在海水水温17.0～23.2℃、盐度21～30、pH8.0～8.2 人工条件下孵化, 孵化率为33.6%～91.7%, 孵出仔鱼499 万尾; 2005 年、2006 年经前期培育, 共培育出黄鳍东方鲀后期仔鱼394.5 万尾, 成活率为68.2%～94.3%; 室内水泥池后期培育出平均全长2.6 cm±0.2 cm 幼鱼3100 尾, 成活率为15.5%; 池塘生态培育出平均全长3.7 cm±0.5 cm 幼鱼53.3 万尾, 成活率为11.2%～13.8%。黄鳍东方鲀受精卵为沉性黏性卵, 近椭球形, 乳白色, 卵膜厚且不透明, 卵径0.9～1.0mm,在海水水温18.2～22.2℃条件下, 3 h 分裂为2 细胞; 3 h 20 min 4 细胞; 3 h 45 min 8 细胞; 10 h 10 min 多细胞; 17 h 30 min 囊胚出现; 28 h 原肠期; 57 h 15 min 胚体形成期; 69 h 20 min 心跳出现; 130 h 50 min出膜期; 144 h 孵出仔鱼。初孵仔鱼全长2.2～2.4 mm, 体圆而粗短, 尾部细长、透明; 孵出后第20 天, 胸鳍、臀鳍、背鳍基本形成, 进入稚鱼期; 孵出后第45 天, 上下颌门齿发达, 各鳍发育完整, 小刺基本形成, 进入幼鱼期。 相似文献
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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
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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
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潮间带大弹涂鱼产卵习性和自然受精卵孵化研究 总被引：5，自引：0，他引：5
从环氧树脂模型揭示了福建省福宁湾潮间带滩涂大弹涂鱼Boleophthalmus pectinirostris洞穴的整体结构。多数洞穴略呈Y字形,每个洞穴有主洞口和次洞口之分。春季5—6月大弹涂鱼洞穴的中下部出现1个产卵室,产卵室横切面的上方呈拱形,底部平坦。潮间带滩涂产卵习性实验表明,产卵前性成熟雄鱼建造产卵室,并引诱性成熟雌鱼进入产卵室内交配产卵,受精卵依靠粘着丝粘在产卵室的顶部和周壁。产卵后雄鱼留洞护卵。每个产卵室的受精卵总数为3 595—4 314粒,平均为3 957粒,平均受精率高达99.67%,受精卵密度为58—114粒.cm-2,平均为87粒.cm-2。产卵室顶部和周壁受精卵的粘着丝位于上端,胚体位于下端,呈倒立状态,大多数受精卵的胚体头部朝下,为反向卵(平均占98.07%),易于孵化出仔鱼。将潮间带洞穴内产卵室受精卵取回实验室,模拟洞穴的小生境进行孵化实验。2次模拟孵化实验结果表明,受精卵始终全淹没于海水的平均孵化率(81.19%—82.90%)高于受精卵湿露24h后才全淹没于海水的平均孵化率(76.38%—79.19%)。湿露而不淹没于海水的受精卵不能孵化出仔鱼。 相似文献
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黑鲪苗种培育关键技术的研究 总被引：1，自引：0，他引：1
采用黑鲪[Sebastodes fuscescens(Houttuyn)]野生亲鱼进行了两次工厂化育苗实验。第一次布放仔鱼38.9×104尾,经过56～60 d的培育,共育成全长30.7～32.7 mm的鱼苗2.9×104尾,平均成活率7.5%;第二次布放仔鱼101.7×104尾,经过46～51 d培育,鱼苗全长30.2～35.7mm。项目验收时,鱼苗平均全长45.7mm,平均体质量1.53g,共出苗约32.1×104尾,单位水体出苗量1 529尾/m3,平均成活率31.6%,最高成活率52.1%。实验中研究了黑鲪仔、稚、幼鱼的生长发育与摄食变化,提出了苗种培育阶段的4个"危险期",并探讨了苗种培育的关键技术。 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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This study tests the hypothesis that the in situ void ratio of surficial marine sediments may be predicted from shear wave velocity-depth data with a reliability equal to that of other methods currently available. Shear wave velocity is fundamentally controlled by the number of grain-to-grain contacts per unit volume of material and by the effective stress across those contacts. In this study, three previously established empirical formulae are used to predict void ratio from velocity-depth data. Field data were acquired along a transect off the northern Californian coast across which water depth increased from 35 to 70 m and seafloor sediment type varied from sand to silty-sand, respectively. A towed seafloor sled device was used to collect shear wave refraction data, and a marked, systematic decrease in velocity was observed along the line, ranging from 35-70 m/s for the coarse, near-shore material to 25-40 m/s for the finer, offshore deposits. Void ratios predicted from these velocities were compared with data measured directly from box-core samples. Of the formulae used for prediction, two agree remarkably well with the control data. Both predicted and control values increase from 0.6-0.8 for the sandy material to 1.1-1.5 for the silty-sand. Thus, this study does not disprove the hypothesis set and demonstrates the potential of field shear wave velocity-depth data as a means of delineating spatial variation in void ratio for surficial marine sediments in a remote, nondestructive manner. 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