首页 | 本学科首页   官方微博 | 高级检索  
相似文献
 共查询到20条相似文献,搜索用时 421 毫秒
1.
本文以熊本牡蛎为材料,在高温季节,通过强化亲贝营养和26℃以上高温促熟培育,使熊本牡蛎亲贝快速成熟,利用阴干流水刺激方法诱导产卵,并进行了不同盐度下受精卵孵化实验;通过合理控制幼虫密度、投喂新鲜无污染的单胞藻、及时分级筛选等系列技术措施,克服了熊本牡蛎育苗成功率低的技术难题;开展了栉孔扇贝壳、长牡蛎壳和栉江珧壳三种附着基的采苗试验,结果显示牡蛎壳是理想的附着基,可使稚贝的附着变态率达到60%以上,促进稚贝的生长和成活,提高稚贝产量,壳长2mm以上的稚贝单位水体出苗量超过10×10~4粒/m~3。  相似文献   

2.
本文研究了小刀蛏(Cultellus attenuatus)室内人工育苗技术。在繁殖季节选择壳长7.5 cm亲贝,采用铺泥沙蓄养培育,以阴干+维生素浸泡刺激法获得精、卵,幼虫培育中人工控制幼虫密度,D形幼虫到壳顶幼虫前期为5~6个/mL,壳顶幼虫后期为1~2个/mL。进行了不同运输方式和不同底质亲贝蓄养比较试验、不同底质附着基采苗方法试验以及稚贝无底质上升流培育和不同盐度培育试验。研究表明,采用铺细沙加冰的运输方法亲贝成活率最高,干露9 h成活率可达90%;以纯海泥底质蓄养的亲贝肥满度和成活率最高;无底质采苗和铺泥采苗对幼虫变态率的影响没有差异;无底质采苗的稚贝,其生长速度明显慢于铺泥采苗;小刀蛏稚贝不宜用上升流进行培育,宜采用铺泥培育的方法;盐度为15时,稚贝培养效果最好,生长速度快、成活率高,盐度为35时培养效果最差。采用上述技术,成功培育出3 mm以上的商品苗2 000万粒,育苗效果显著。  相似文献   

3.
以大竹蛏(Solen grandis Dunker)为材料,选择一定规格且处于繁殖期的亲贝采用铺砂蓄养培育,以阴干流水刺激法获得精卵,合理控制密度培育幼虫,前期6~8/mL,后期1~2/mL.育苗管理方面,严把饵料质量关,投喂新鲜无污染的饵料,科学换水与充气,使育苗生产顺利进行.不同密度下洗卵与不洗卵的孵化比较试验、无底质采苗和铺砂附着基投放的采苗等试验的结果为:在洗卵的条件下,孵化密度为30/mL时,孵化率可达80%;无底质采苗变态率较铺砂采苗高,但生长速度慢于铺砂采苗。  相似文献   

4.
栉江珧人工育苗初步研究   总被引:5,自引:0,他引:5  
作者1982年在广东汕尾室内水泥池开始进行栉江珧(Pinna Pectinata)人工育苗研究,1984年成功地育出稚贝。本文介绍了作者在研究中采用阴干和升温刺激等方法,可使亲贝自行排放精、卵,并进一步受精、孵化成幼虫,幼虫经多次变态发育,结束浮游期而进入底栖附着期。附着后的稚贝,新壳生长迅速,只要条件适宜,很快便能倒立插起。在一定条件下将稚贝移至海区浮台吊养,生长快,两个半月即成小贝,最大个体为68×30×8.9mm,重6.2g。本文还对栉江珧人工育苗不同于其它双壳类的有关问题进行了讨论。  相似文献   

5.
研究了脉红螺(Rapana venosa(Valenciennes)在室内人工投喂条件下的亲螺交配、卵袋产出、孵化、幼虫培育、采苗。结果为:亲螺促熟培育的适宜饵料是四角蛤蜊,在人工促熟条件下每只雌螺产卵量44.57万粒,胚胎孵化率平均为87.4%;在育苗期间,幼虫前期密度为0.2个/mL,后期0.1个/mL,投喂金藻、小球藻、角毛藻,当平均壳高达到1200μm以上时,投放附有底栖硅藻的聚乙烯波纹板采苗效果最好。本文在稚螺培育中主要研究了脉红螺稚螺食性转换和变态过程中的适宜动物性饵料,以及不同处理方法的附着基对稚螺附着的影响,结果表明:经亲螺爬过和附有底栖硅藻的波纹板,附苗效果好;刚附着变态后稚螺除了投喂牡蛎肉糜外,定期向池内投放活的牡蛎受精卵,可以促进稚螺变态和食性顺利转化,成功培育出壳高1.0cm以上苗种。  相似文献   

6.
本文以长牡蛎海大1号新品种为材料,通过强化亲贝单胞藻投喂量和人工升温促熟培育,使海大1号长牡蛎新品种亲贝成熟,利用阴干升温刺激方法诱导产卵,并进行了受精卵洗卵和不洗卵的孵化实验;通过控制幼虫密度、投喂新鲜无污染的单胞藻以及科学投喂等技术措施,幼虫快速生长发育到眼点幼虫,投放栉孔扇贝壳进行采苗,眼点幼虫的附着变态率达到45%以上,成功培育出壳高0.5mm以上的稚贝9.67亿粒,单位水体出苗量达到32.4×10~4粒/m~3。取得长牡蛎海大1号新品种规模化育苗生产的成功。  相似文献   

7.
本实验开展了疣荔枝螺(Thais clavigera Kuster)室内全人工繁育技术研究;具体包括亲螺人工促熟蓄养、卵囊采集、孵化、幼虫培育、变态和采苗等技术研究,同时,还开展了后期面盘幼虫对不同附着基的喜好选择性实验,以及不同饵料和光照对幼虫附着的影响研究。研究表明:雌螺分批产卵,单个雌螺平均每次产出受精卵为61 750粒;在水温27~29℃时,面盘幼虫经过20 d左右的生长发育,壳长达到约600 μm,此时开始附着变态,由浮游生活转变为底栖生活;附着后10 d左右变态为稚螺。后期面盘幼虫对附着基的选择性实验表明,固着牡蛎苗的栉孔扇贝壳和附有底栖硅藻的波纹板,是稚螺理想的附着基。不同饵料和光照对幼虫附着影响实验结果表明:在附着变态期间,自然光照有利于幼虫附着变态;同时,连续投喂糠虾肉糜可显著提高幼虫变态率和稚螺成活率。本研究结果为今后疣荔枝螺产业化繁育提供了重要的理论和技术支持。  相似文献   

8.
栉江珧人工育苗试验   总被引:3,自引:0,他引:3  
报道了栉江珧(Pinna(Alrina)peclinala Linncaus)人工育苗的试验结果。结果表明采用变温刺激法、阴干流水刺激法及阴干流水升温刺激法催产亲贝效果较好。在水温20.6~24.7℃,密度1.018~1.023水体申经50d培育后幼虫附着变态成稚贝,变态率10%-20%,10d后最大幼贝长达6mm。  相似文献   

9.
孙小真  刘志刚 《海洋科学》2010,34(10):62-67
对马氏珠母贝人工育苗换水、投附着基和饵料等关键环节进行了研究。结果表明:(1)不换水组的D形幼虫及壳顶幼虫的存活率,稚贝育成率以及D形幼虫、壳顶幼虫及稚贝壳长日生长率比换水组分别提高了15.3%、259.6%、186.5%、33.3%、34.2%、12.4%,且差异显著;(2)第1、2次投附着板组的稚贝壳长日生长率均比一次性投附着板组快,第3次投附着板组的壳长日生长率比其他所有组均慢,且差异均显著。多次投附着板组的同一批次稚贝均匀度均比一次性投附着板组好,且多次投附着板组比一次性投附着板组的稚贝育成率提高了32.5%,稚贝存活率提高了19.3%,采苗量提高了35%;(3)投喂虾塘水组稚贝存活率、育成率及壳长日生长率比投喂50%自溶酵母+50%小球藻组分别提高了28.1%、47.2%、35.9%,而投喂这两种不同饵料的稚贝阴干后的存活率差异不显著。研究表明,通过封闭不换水育苗、多次投附着板及投喂虾塘水中的生态饵料的方法可以高效地培育出健康的马氏珠母贝种苗。  相似文献   

10.
珠母贝人工繁育优化技术的研究   总被引:1,自引:0,他引:1       下载免费PDF全文
在室内水泥池分别进行了移池培育、不同种类附着器、光照强度、水流和冲洗对珠母贝附着幼虫变态和稚贝存活的研究,结果表明:附着密度为2.18个/cm~2±0.50个/cm~2时,移池培育,其变态幼虫密度为0.95个/cm~2±0.13个/cm~2,20 d稚贝存活密度0.41个/~2±0.08个/cm~2,移池培育显著提高附着幼虫变态和稚贝存活;附着板、附着绳、网片、小石块变态幼虫密度分别为0.70个/cm~2±0.08个/cm~2、1.38个/cm~2±0.15个/cm~2、0.97个/cm~2±0.12个/cm~2、1.04个/cm~2±0.28个/cm~2,稚贝存活密度分别为0.36个/cm~2±0.06个/cm~2、0.62个/cm~2±0.07个/cm~2、0.45个/cm~2±0.07个/cm~2、0.60个/cm~2±0.08个/cm~2,附着绳显著提高附着幼虫变态和稚贝存活;光照强度为300~600 lx时变态幼虫密度为0.87个/cm~2±0.07个/cm~2,20 d稚贝存活密度0.45个/cm~2±0.08个/cm~2,强光不利于幼虫的变态和稚贝存活;水流速为2.3 cm/s时变态幼虫密度为1.08个/cm~2±0.07个/cm~2,20 d稚贝存活密度0.87个/cm~2±0.07个/cm~2,冲洗的变态幼虫密度为1.64个/cm~2±0.19个/cm~2,20 d稚贝存活密度1.00个/cm~2±0.12个/cm~2,水流或冲洗显著提高附着幼虫变态和稚贝存活.  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   

14.
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.
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   

18.
19.
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   

20.
This article concerns an interrelation between the sea levels and the western boundary flow near a tectonic boundary in a local zone in the Northwestern Pacific. In this zone, sea level variations at stations located on the coast facing the Pacific are studied to find the interrelation between variations of the Kurosio flow as an index of the distance of the flow axis off a specific coast. The result is discussed after data processing of the monthly means of the sea levels, and a notice is taken of variations caused by active crustal upheavals during a seismic event, a local earthquake.  相似文献   

设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号