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2017年9月至2018年1月,在福清东壁岛三联垦区(A、B、C)开展了菲律宾蛤仔垦区人工育苗技术研究,其中A、B垦区用于育苗,C垦区用于饵料培育,并于2017年9月开始分两批次共向A、B垦区投放菲律宾蛤仔亲贝1670 t。结果显示,育苗期间菲律宾蛤仔亲贝共出现4次大规模产卵。亲贝精卵排放率为32.0%~84.0%,孵化率为45.00%~68.54%;浮游幼虫生长速度为4.73~7.14μm/d,变态率为28.37%~59.67%;稚贝壳长生长速度为7.08~25.10μm/d,共培育砂粒苗7580亿粒,育苗成活率为50.23%。因此,采用垦区三联方法可保障菲律宾蛤仔苗种的生物饵料供给,从而提高砂粒苗的生长速度和成活率。 相似文献
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采用光滑河蓝蛤和菲律宾蛤仔两种双壳贝类培养长蛸幼体,分析其生长和存活情况。结果显示,长蛸初孵幼体无外卵黄,体表光滑,第一对腕(最长腕)约为胴长的2.9倍,腕吸盘两列,第1—4对腕平均吸盘数(n=3)分别为66±4.60、55±3.76、43±4.59和41±3.82;1—15d幼体投喂的是光滑河蓝蛤(壳长15.4—20.3mm),之后投喂菲律宾蛤仔(壳长33.2—39.3mm);幼体30d—70d总成活率由80.99%降至54.65%;整个培育过程中,幼体生长率与饵料效率呈极显著线性回归关系(P0.01),y=1.452x-2.731(R2=0.865);1—80d胴长/全长比增幅高于腕长/全长,表明胴体增长快于腕的增长;各腕吸盘数变化不显著;幼体鲜重与培养天数呈指数函数关系,Wt=0.301e0.010t(R2=0.854,P0.01);长蛸幼体最终生长率为122.05%,平均生长率为9.97%/10d。 相似文献
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胶州湾菲律宾蛤仔生长特征研究 总被引：12，自引：0，他引：12
为对胶州湾菲律宾蛤仔增养殖业的可持续发展提供技术支持,2004年5～9月,通过对胶州湾菲律宾蛤仔进行定点采样调查和生物学特性测定,分析研究了菲律宾蛤仔的生长特征.结果表明：近几年胶州湾菲律宾蛤仔的底播增殖,苗种平均体重0.26g、壳长11.1mm;1～3龄期间个体生长速度较快,1～2龄、2～3龄,体重分别增长3.88g和4.02g;1～2龄生物量增长最快,2～3龄由于死亡率提高,使生物量增长缓慢;壳长、壳高、壳宽与体重关系式分别为y=0.000 2x^3.053 3,y=0.000 4x^3.088 6,y=0.005 3x^2.683 4,壳高、壳宽与壳长关系式分别为y=0.667 4x＋0.305 9,y=0.457 5x-0.967 8;1～3龄蛤仔软体部的生长速度快于贝壳,5～6月份是菲律宾蛤仔的肥育期.由个体生长特性分析,3龄为最佳采捕年龄,从生物量上分析,采捕2龄蛤收益最高;6月是最佳的捕获季节. 相似文献
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《中国海洋大学学报(自然科学版)》2016,(7)
为了解和评估胶州湾内菲律宾蛤仔的季节分布和资源状况,于2014年2月(冬季)、5月(春季)、8月(夏季)和11月(冬季)对胶州湾菲律宾蛤仔的季节分布情况与生物资源量进行了全面调查和评估,分析了胶州湾菲律宾蛤仔的壳长、生物量、栖息密度和年龄组成。结果显示,胶州湾2014年的年均栖息密度为409.6ind./m~2,最高栖息密度达2 377.5ind./m~2;年均生物量为625.5g/m~2,最高生物量高达3 445.3g/m~2。胶州湾全年菲律宾蛤仔的年龄组成主要是1、2和3龄蛤,而其中的1和2龄蛤占有明显数量优势。胶州湾菲律宾蛤仔种群年龄结构出现低龄化,1龄蛤占绝对优势,2龄蛤仅次于1龄蛤,3龄以上最少。若以壳长30mm的蛤仔为采捕规格,2014年胶州湾菲律宾蛤仔的年均商品率为6.8%;若以壳长25mm蛤仔为采捕规格,2014年胶州湾菲律宾蛤仔的年均商品率为33.2%。从菲律宾蛤仔的生物量、年龄结构和商品率综合分析,2龄蛤可作为优势的采捕年龄,5月是最佳的采捕时期。 相似文献
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大西洋浪蛤繁殖生物学研究 总被引：2，自引：2，他引：0
于2002年1月至2003年1月 ,在浙江温州对引种养殖的大西洋浪蛤(Spisulasolidissima)的性腺发育、生殖周期、肥满度、胚胎发育、幼虫发育及变态等进行了研究。研究结果表明 ,大西洋浪蛤性腺发育过程分为增殖期、生长期、成熟期、排放期、休止期5个阶段。在浙南沿海的大西洋浪蛤繁殖期在4月下旬至6月上旬 (水温19.5～25℃ ) ,可大量产卵二次 ;肥满度最高出现在5月份,为10.37 % ,最低出现在2月份 ,为4.66 %。个体产卵量为14.1×104～111.1×104粒 ,卵沉性 ,卵径50～60μm ;受精卵在水温19.5～23℃ ,经16～20h孵化成D形幼虫 ;初孵D形幼虫平均大小为75μm×62μm ,浮游幼虫经12～13d培养进入壳顶后期 ,15～16d进入附着变态期 ,壳长为260～290μm ,发育变态为稚贝。 相似文献
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为探究菲律宾蛤仔（Ruditapes philippinarum）筏式养殖模式可行性，在我国黄海北部首次开展了菲律宾蛤仔"斑马蛤2号"新品种的筏式与底播养殖模式对比试验。采用平均壳长为2.37 cm，平均全湿重为2.99 g规格的"斑马蛤2号"苗种为试验材料，对两种养殖方式的"斑马蛤2号"生长、存活、营养成分进行比较分析，结果表明，筏式养殖"斑马蛤2号"夏季（4-7月）壳长、壳宽、壳高、全湿重、软体重的相对生长速率分别比底播养殖"斑马蛤2号"快149.54%、100.61%、116.30%、152.25%、132.58%（P<0.05）。筏式养殖"斑马蛤2号"存活率为90%以上，显著高于底播养殖（P<0.05）。两种养殖方式的"斑马蛤2号"水分、灰分、粗蛋白、糖原、脂肪酸等营养成分季节变化规律基本一致。筏式养殖"斑马蛤2号"冬季糖原、单不饱和脂肪酸含量明显高于底播养殖"斑马蛤2号"（P<0.05）。研究表明，当年10月采用多层聚乙烯网笼按密度为150-200粒/层放养菲律宾蛤仔"斑马蛤2号"大规格苗种（平均壳长为2.37 cm，平均全湿重为2.99 g），可于翌年的4月、7月、10月收获平均壳长为3.03、3.36、3.51 cm的市场规格产品。筏式养殖模式具有存活率高的优点。"斑马蛤2号"筏式养殖模式试验的成功为蛤仔健康养殖提供了新途径。 相似文献
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采用室内受控方法研究了水温(14、16、18、20、22、24、26和28℃)和盐度(22、24、26、28、30、32、34、36、38和40)对皱纹盘鲍变态及变态幼体生长存活的影响。结果表明,水温对变态率、变态幼体存活率和生长率的影响极显著(P0.01)。14~28℃条件下,随着水温的升高,幼体变态率、变态幼体存活率和生长率均呈现先升高后降低的趋势。24℃时变态率最高,为86.05%;18℃时,变态幼体存活率最高,为96.00%;26℃时,投苗6 d内的壳长、壳宽生长率最大,分别为48.49μm/d和43.81μm/d;投苗15 d内的壳长、壳宽生长率最大,分别为68.06μm/d和59.69μm/d。盐度对皱纹盘鲍变态率及变态幼体生长率的影响极显著(P0.01),对幼体存活率却无显著影响(P0.05)。22~40盐度条件下,幼体变态率先升高后降低,于32达最大值,为79.23%;变态的盐度下限为22,该盐度下仅有2.21%的个体能够完成变态。26~40条件下,变态幼体存活率均高达85%以上;随着盐度的升高,变态幼体生长率先升高后降低。投苗6 d内壳长、壳宽生长率均于34达最大值,分别为32.03μm/d和25.20μm/d;投苗15 d内壳长、壳宽生长率分别于34和32达最大值,为43.03μm/d和39.00μm/d。 相似文献
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为查明大神堂浅海菲律宾蛤仔养殖的适宜密度和生长特征,开展了放养密度对不同养殖阶段蛤仔生长与存活的影响试验。幼贝初始规格为壳长5.6±1.3 mm,养殖密度设置为8 000粒/m2、4 000粒/m2;成贝期,养殖密度设置为500粒/m2、1 000粒/m2、2 000粒/m2、4 000粒/m2。经26个月的养殖,结果表明:在幼贝期,当幼贝壳长小于22 mm时,两密度试验组生长速度及存活率无显著差异,当幼贝壳长大于22 mm时,高密度组生长缓慢,差异显著。在成贝养成前期,各密度试验组壳长无显著差异,随着蛤仔的生长,当壳长达到30 mm以上时,4 000粒/m2密度组生长速度显著低于其他组,其他各组间差别不明显;4 000粒/m2密度组蛤仔死亡率高于50%,其他组死亡率在15%~22%之间;另外,4 000粒/m2密度下蛤仔繁殖期的肥满度显著低于其他试验组,而其他组之间无显著差异。因此,2 000粒/m2为该海域蛤仔养殖的适宜密度,适于培育大规格商品贝。 相似文献
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2012年7月,在荣成天鹅湖用自行研制的沉积物捕集器现场测定底内动物菲律宾蛤仔(Ruditapes philippinarum)和底上动物长牡蛎(Crassostrea gigas)的生物沉积速率,以建立潮间带贝类生物沉积的现场测定方法,并评价两种贝类对潮间带生态环境的影响。结果表明:各组内沉积物重量差异不显著,处理组与对照组的沉积物重量差异显著(F=58.047,P=0.000),测得的生物沉积速率与文献具有可比性,因此可以推测新型生物沉积物捕集器适用于浅水区(潮间带),能够准确测定生物沉积速率。在平均水温18.8°C条件下,菲律宾蛤仔和长牡蛎都具有较高的生物沉积速率。壳长(25.0±1.5)mm、软体干重(0.12±0.03)g的菲律宾蛤仔生物沉积速率为(44.92±4.12)mg/(ind·d);壳长(29.8±1.3)mm、软体干重(0.23±0.05)g的菲律宾蛤仔生物沉积速率为(54.84±7.77)mg/(ind·d);壳长(98.8±14.1)mm、软体干重(3.94±0.66)g的长牡蛎生物沉积速率为(1069.01±212.24)mg/(ind·d)。作为天鹅湖海区两种典型贝类,据估算,每平方米面积内的蛤仔和长牡蛎每天分别将29.9g、15.0g的悬浮颗粒物通过滤食和排粪沉积到底层,增强了水层-底栖系统的耦合作用。 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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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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《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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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
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Shigehisa Nakamura 《Marine Geodesy》2001,24(1):27-33
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
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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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Particulate samples were collected from the Changjiang river system during a flood period, in May 1997, and POC, stable isotope and lipids associated with particles were examined. Results showed the decrease (0.84% ～ 1.88%) of organic carbon content from the upper reaches to the estuary.δ13C values of particulate organic carbon was in the range of -24.9×10-3 to -26.6×10-3, which were close to the isotopic signature of continental C3 vegetation. Total particulate n-alkanes concentrations varied from 1.4 to 10.1μg/dm3,or from 23.7 to 107μg/g of total suspended matter. Fatty acids were present in all the samples, from 1.4 to 5.4μg/dm3, with saturated and unsaturated straight-chain and branched compounds in the carbon number range from C12 to C30. Both δ13C and the ratio of carbon content to nitrogen content indicate the predominance of terrestrial inputs (soil organic matter) among the particles. The biomarker approach has been used to identify the relative portion of terrigenous and autochthonous fraction in the particulate samples. The distribution of fatty acids suggests a striking phytoplanktonic and microbial signal in most particle samples. The terrestrial alkanes are used to estimate the contribution of terrestrial inputs along the mainstream. 相似文献