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选用高毒性微小亚历山大藻台湾株和菲律宾蛤仔为研究对象,研究了不同毒藻投喂量对贝类累积和排出麻痹性贝毒(PSP)的影响.实验分为累积和排出2个部分,累积实验设计了4个投喂梯度(A组:2.0×107cell/d、B组:7.0×107cell/d、C组:1.1×108cell/d和D组:2.0×108cell/d),在排出毒素阶段,每实验组又分成投喂无毒饵料藻组和饥饿组并进行比较.结果显示不同投喂梯度组间PSP毒素累积存在明显差异.随着毒藻投喂量的增加,PSP毒性增加,但毒素累积率下降,这说明在一定范围内毒藻投喂量的大小对蛤仔的毒素累积有影响.A组、B组、C组的最高累积量依次为6.5,82.9,113.9μgSTXeq/100g,D组达到本实验的最高累积量154.1μgSTXeq/(100g),但累积率却随着投喂量的增加而递减,分别为1.79%,0.92%,0.42%和0.39%.停止投喂毒藻后蛤仔体内的PSP毒性迅速下降,在排出阶段,对投喂饵料组和饥饿组的比较结果用单因素方差分析(ANOVA)得出P＜0.05,结果差异显著,饥饿组的毒性均高于投喂饵料藻组,说明投喂无毒饵料有助于菲律宾蛤仔体内的毒素排出.其中D饵料组和饥饿组间排出速率差异最明显,饵料组的排出速率为13.2 μgSTXeq/(100g·d),饥饿组的仅为8.3μgSTXeq/(100g·d),因此将菲律宾蛤仔归属于快速排毒者. 相似文献
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《海洋科学进展》2010,(2)
选用高毒性微小亚历山大藻台湾株和菲律宾蛤仔为研究对象,研究了不同毒藻投喂量对贝类累积和排出麻痹性贝毒(PSP)的影响。实验分为累积和排出2个部分,累积实验设计了4个投喂梯度(A组:2.0×107cell/d、B组:7.0×107cell/d、C组:1.1×108cell/d和D组:2.0×108cell/d),在排出毒素阶段,每实验组又分成投喂无毒饵料藻组和饥饿组并进行比较。结果显示不同投喂梯度组间PSP毒素累积存在明显差异。随着毒藻投喂量的增加,PSP毒性增加,但毒素累积率下降,这说明在一定范围内毒藻投喂量的大小对蛤仔的毒素累积有影响。A组、B组、C组的最高累积量依次为6.5,82.9,113.9μgSTXeq/100g,D组达到本实验的最高累积量154.1μgSTXeq/(100g),但累积率却随着投喂量的增加而递减,分别为1.79%,0.92%,0.42%和0.39%。停止投喂毒藻后蛤仔体内的PSP毒性迅速下降,在排出阶段,对投喂饵料组和饥饿组的比较结果用单因素方差分析(ANOVA)得出P0.05,结果差异显著,饥饿组的毒性均高于投喂饵料藻组,说明投喂无毒饵料有助于菲律宾蛤仔体内的毒素排出。其中D饵料组和饥饿组间排出速率差异最明显,饵料组的排出速率为13.2μgSTXeq/(100g.d),饥饿组的仅为8.3μgSTXeq/(100g.d),因此将菲律宾蛤仔归属于快速排毒者。 相似文献
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为研究链状裸甲藻所产麻痹性贝类毒素(paralytic shellfish toxins, PST)在翡翠贻贝体内的累积、转化和排出规律,设置试验组和对照组,采用链状裸甲藻和中肋骨条藻投喂翡翠贻贝,开展短期累积(12 h)、长期累积(10 d)和排出(28 d)试验。结果表明:翡翠贻贝具有较强的毒素累积能力,内脏团是PST累积的主要部位, PST含量与产毒藻密度呈显著正相关关系。当链状裸甲藻密度为1.0×106cells/L时,贻贝内脏团PST含量累积2 h已接近食用贝类毒素安全标准,累积8 h超标。当产毒藻密度为5.0×105 cells/L时,贻贝内脏团PST含量累积2 d超标,累积8 d达到峰值(3 590.4±545.7)μg/kg。贻贝对PST具有累积快排出慢的特点,内脏团PST含量在排出16 d达标,排出速率先快后慢。内脏团对PST的累积和排出速率显著高于闭壳肌和其他组织,闭壳肌和其他组织则无显著差异。PST进入贻贝体内后发生了代谢转化,贻贝可能将产毒藻中膝沟藻毒素GTX3转化为GTX2, N-磺酰氨甲酰基膝沟藻毒素C2转化为C1,部分C1转化为脱氨甲酰基膝沟藻毒素2(dc... 相似文献
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以缢蛏(Sinonovacula constricta)(A)、菲律宾蛤(Venerupis Philippinaram)仔(B)及自制配合饲料(C)作为饵料,分别研究了上述3种饵料对二龄管角螺(Hemifusus tuba Gmelin)生长、肝脏消化酶活性以及软体部营养成分的影响。结果表明：(1)鲜活饵料的投喂更有利于管角螺的生长和营养物质的累积,配合饲料的摄食效果较差,还需进一步的优化和完善;其特定生长率大小为：缢蛏组＞菲律宾蛤仔组＞配合饲料组,组间差异显著(P＜0.05);(2)不同饵料的投喂对其肝脏消化酶活性的影响差异显著,在整个实验区间的胰蛋白酶活力的大小为：缢蛏组＞菲律宾蛤仔组＞配合饲料组,组间差异显著(P＜0.05);配合饲料组的淀粉酶活力和脂肪酶活力先降后升,鲜活饵料组则较稳定;45 d 后配合饲料组的淀粉酶活力和脂肪酶活力皆显著高于鲜活饵料组的(P＜0.05);表明管角螺在饥饿时,消化酶可能存在补偿性分泌,优先利用糖原和脂肪作为能源物质;(3)不同饵料对管角螺软体部的灰分和水分没有显著影响(P＞0.05),鲜活饵料组的粗蛋白和粗脂肪含量皆显著高于配合饲料组(P＜0.05)。 相似文献
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三疣梭子蟹对饵料鱼和蛤摄食参数的研究 总被引：1，自引：0，他引：1
研究体重为(9.20±1.50)g的三疣梭子蟹在分别投喂饵料鱼和兰蛤及有无沙底质条件下的昼夜摄食节律、摄食率和昼夜摄食量的差异.结果表明:投喂兰蛤组的三疣梭子蟹摄食高峰在20:00左右,投喂饵料鱼组三疣梭子蟹的摄食高峰在02:00左右;沙底质条件下三疣梭子蟹的夜晚摄食量占全天摄食量的94.34%,而无底质组为75%,表明在潜底环境条件下三疣梭子蟹具有更明显的昼夜摄食节律;投喂兰蛤组三疣梭子蟹黑夜摄食量比值显著高于白天,分别为75%和25%,而投喂鱼组黑夜摄食量比值仅略高于白天,分别为59.21%和40.79%.此外,投喂鱼组白昼摄食率可达80%,显著高于投喂兰蛤组的10%,表明投喂鱼饵料有利于三疣梭子蟹的白昼进食.根据昼夜摄食量对比分析,建议采用白昼投喂占总投喂量20%～30%的鱼肉以降低蜕皮残食,夜晚投喂70%～80%的兰蛤的投喂策略促其生长,并减少梭子蟹的残食. 相似文献
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通过室内摄食实验,研究了栉孔扇贝(Chlamys farreri)对麻痹性贝毒(PSP)产毒藻的敏感性及其累积和排出毒素的特征.有毒微小亚历山大藻(Alexandrium minutum)在短时间内可对栉孔扇贝的摄食有一定的抑制作用,且投喂毒藻的浓度越大,对摄食作用的抑制越明显.栉孔扇贝对PSP贝毒的累积能力很强,实验中,48 h后内脏累积毒素就高达5000μg STXeq100g-1,但其毒素排出速率较慢,在24d解毒阶段后内脏中的毒素还没有下降至国际贝毒食用安全标准水平的80μg STXeq 100g-1.各毒素组成比在整个累积与排除过程中有较大变化,GTX1,GTX4在累积阶段比例下降,同时GTX2,GTX3比例上升;内脏中GTX2:GTX3的比值逐渐增加.毒藻中PSP贝毒毒素组成和贝体中PSP贝毒毒素组成之间的主要差别是GTX4含量的减少和GTX1含量的升高;而扇贝粪便中的毒素组成却与对数生长期的毒藻极为接近. 相似文献
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为探讨不同饵料对青蛤(Cyclina sinensis)与文蛤(Meretrix meretrix)生长和存活的影响,本实验选用紫菜(Pyropia)、浒苔(Enteromorpha prolifera)、海带(Laminaria japonica)、小球藻(Chlorella vulgaris)和人工配合饲料5种饵料,采用单一饵料投喂方式进行饲养.结果表明:小球藻组中特定生长率、存活率及饲料转换率与各饵料组均有显著性差异(P<0.05),青蛤的增质量率显著低于紫菜组、海带组及人工配合饲料组(P>0.05).在人工配合饲料组中青蛤与文蛤的特定生长率与各饵料组均有显著性差异(P<0.05),青蛤的增质量率与各饵料组无显著性差异(P>0.05),文蛤的增质量率显著高于紫菜组、浒苔组及人工配合饲料组(P<0.05).在3组大型藻中,海带组中青蛤的特定生长率为0.07％,增质量率为4.59％,饵料转换率为7.09％,存活率为74％;文蛤的特定生长率0.13％,增质量率为8.36％,饵料转换率为1.41％,存活率为55.6％.综上,小球藻和人工配合饲料有利于青蛤和文蛤的生长,在3组大型藻中,投喂海带有利于文蛤和青蛤的生长和存活. 相似文献
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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
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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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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
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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
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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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Oedometer tests have been carried out on 70 undisturbed surficial clays (at approximately 250 mm below the mudline), mostly collected by free-fall corers from sites widely scattered throughout the deep-sea North Atlantic. Acoustic measurements were also made, initially on contiguous samples and ultimately on the same sample using a geophysically instrumented oedometer which also collected electrical resistivity data. Apart from those quiescent areas below the carbonate compensation depth, such as north of the West Indies where very fine clays exist, most of the samples are silty clays whose geotechnical-geophysical properties are dependent on the type of clay minerals present (and their ability to take in moisture), the sand-size fraction, and the quantity of carbonate present. Thus the pure clays have high compressibilities which decrease on the addition of coarse particles, while the converse is true for the acoustic parameters, these increasing with the sand fraction. Using the notion of the intrinsic compression line for all samples, and comparison to it of the measured compression curves, it is clear that, contrary to some previously held ideas, most deep-sea clays are normally consolidated; the addition of carbonate has the effect of creating an open, stronger sediment skeleton. Interestingly, where information is available, the variation with depth of a sample's acoustic velocity follows the void ratio pressure relationship of the compression curve. This allows the construction of an in-situ sediment compression curve using the in-situ geophysical observations. 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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Phylogenetic diversity and phenotypic characterization of cultivable bacterioplankton isolated from polar oceans 总被引：1，自引：0，他引：1
A set of 27 marine planktonic bacteria isolated from the polar regions was characterized by 16S rDNA sequencing and physiological and biochemical testing. More than half of these bacteria were positive for caseinase, gelatinase and 13-glucosidase, and could utilize glucose, maltose or malic acid as carbon source for cell growth. Twelve isolates expressed nitrate reduction activities. Except for one antarctic isolate BSwlO175 belonging to Actinobacteria phylum, these isolates were classified as γ-Proteobacteria, suggesting that γ-Proteobacteria dominated in cultivable marine bacterioplankton at both poles. Genus Pseudoalteromonas was the predominant group in the Chukchi Sea and the Bering Sea, and genus ShewaneUa dominated in cultivable bacterioplankton in the Prydz Bay. With sequence similarities above 97%, genus Psychrobacter was found at both poles. These 27 isolates were psychrotolerant, and significant 16S rDNA sequence similarities were found not only between arctic and antarctic marine bacteria （ 〉 99% ）, but also between polar marine bacteria and bacteria from other aquatic environments （ ≥ 98.8% ）, including temperate ocean, deep sea, pond and lake, suggesting that in the polar oceans less temperature-sensitive bacteria may be cosmopolitan and have a bipolar, even global, distribution at the species level. 相似文献