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四种重金属对鮸状黄姑鱼胚胎和仔鱼的毒性 总被引：23，自引：0，他引：23
本文研究了汞、铜、锌和铬四种重金属对鮸状黄姑鱼（Ｎｉｂｅａ ｍｉ－ ｉｃｈｔｈｉｏｉｄｅｓ）胚胎发育和仔鱼存活的影响。结果表明;在试验浓度范围内,胚胎发育受 阻,受精卵孵化率显著低于对照组,初孵仔鱼出现不同程度的畸形,这些重金属对鮸 状黄姑鱼仔鱼的毒性强弱依次为Ｈｇ~２＋＞Ｃｕ~２＋＞Ｚｎ２＋＞Ｃｒ~６＋。根据实验数据求得四种 重金属对鮸状黄姑鱼仔鱼的２４、４８、７２和９６ｈ ＬＣ_５０值及安全浓度。 相似文献
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温度及体重对鮸鱼幼鱼耗氧率和排氨率的影响 总被引：12，自引：0，他引：12
利用实验生态学方法研究了不同温度及体重对鮸鱼Miichthys miiuy幼鱼的呼吸、排泄的影响。结果表明,不同温度和体重对鮸鱼幼鱼耗氧率、排氨率有显著影响(p<0.05),耗氧率随温度的升高而增大并呈指数相关,相关方程为:RO=0.168e0.035 5T(R2=0.960 71);鮸鱼幼鱼耗氧率和排氨率随体重的增加而下降并呈幂函数相关,相关方程分别为:RO=0.613 9W-0.403 1(R2=0.994 3),RN=25.055W-0.287 7(R2=0.997 8)。O/N比也随着温度升高和体重增加而升高,不同温度下鮸鱼幼鱼平均O/N比值为21.963,呼吸Q10平均是1.415,排泄Q10平均是1.419;不同规格鮸鱼幼鱼平均O/N比值为21.855。10-30℃鮸鱼幼鱼主要以蛋白质为能源,脂肪和碳水化合物其次。随着温度的升高,鮸鱼幼鱼的蛋白质代谢比率降低,而脂肪和碳水化合物的代谢比率增大。 相似文献
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《海洋科学》2010,(1)
作者对鮸鱼(Miichthys miiuy)的早期发育(从受精卵到45日龄幼鱼)形态特征及生态习性进行了描述。鮸鱼的受精卵在水温21.4℃~22.0℃,盐度25.7条件下,经过29 h30 min仔鱼孵出。从受精卵到仔鱼出膜可分为卵裂期、囊胚期、原肠期、胚体形成期等4个主要时期,然后进入胚后发育阶段。孵出后的3日龄仔鱼已能在水体中平游,极少数个体可开口摄食轮虫。4日龄仔鱼全部开口摄食,并对光反应敏感,出现明显的集群现象。22日龄的后期仔鱼各鳍鳍条发育形成,鳞片开始出现,进入到稚鱼期。39日龄后,鮸鱼全身披满细小的鳞片,全部分布于育苗池的底部,开始进入到幼鱼发育阶段。根据仔、稚、幼鱼形态特征和生活习性对鮸鱼的分类进行了探讨。 相似文献
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盐度和pH值对鮸鱼幼鱼耗氧率和氨氮排泄率的影响 总被引：14，自引：0，他引：14
利用实验生态学的方法研究了不同盐度及pH值对鮸鱼幼鱼的呼吸、排泄的影响．结果表明，不同盐度对鮸鱼幼鱼耗氧率、氨氮排泄率有显著影响（P〈0．05），盐度11～26，鮸鱼幼鱼耗氧率逐步上升，26时达到峰值后呈下降趋势；pH值对耗氧率无显著影响（P〉0．05），pH6．5～9．0鮸鱼幼鱼耗氧率变化幅度很小，在此范围内pH值的变化对鮸鱼幼鱼氨氮排泄率有显著影响（P〈0．05）．O：N比值也随着盐度升高而升高，26时达到峰值，随后下降；pH8．0时，O：N比值最低；不同盐度和pH下鮸鱼幼鱼平均O：N分别为24．258，22．378．鮸鱼幼鱼主要以蛋白质为能源，脂肪和碳水化合物其次． 相似文献
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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
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为了解长江口及其邻近海域鮸鱼(Miichthys miiuy)的群体遗传多样性,采用线粒体COⅠ基因测序,对长江口(崇明)及邻近海域(舟山)2个鮸鱼群体的遗传变异进行了分析。结果表明,599 bp的COⅠ序列中包含22个变异位点,其中简约信息位点7个。60个个体中,共定义了20个单倍型,平均单倍型多样性指数(Hd)为0.676 8±0.069,核苷酸多样性指数(Pi)为0.002 29±0.000 37,表现为高单倍型多样性和低核苷酸多样性。分子方差分析(AMOVA)表明99.12%的遗传变异出现在种群内,仅有0.88%出现在种群间。群体间的遗传分化系数为FST=0.008 83(P0.05),2个群体间无显著遗传分化。NJ系统树显示,2个地理来源的单倍型没有明显的地理群聚和谱系结构。中性检验和碱基岐点分布(Mismatch distribution)分析结果表明鮸鱼群体可能发生过种群扩张事件。研究结果可为鮸鱼渔业资源的合理开发和利用提供必要的参考。 相似文献
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为了解模式生物种海水青鳉(Oryzias melastigma)的胚胎发育特征,作者培育30日龄的海水青鳉,收集自然受精卵,在水温26~28℃、盐度27~28条件下,静水孵化。利用奥林巴斯SZ61解剖镜对海水青鳉胚胎发育进行了观察研究。结果表明:海水青鳉受精卵为圆球形端黄卵,多油球,沉性,卵膜上具有绒毛膜和纤维丝。和多数硬骨相似,胚胎发育的过程大致可以分为7个期:胚盘形成期、细胞分裂期、囊胚期、原肠期、器官形成期、肌肉效应期和孵化期。并发现海水青鳉胚胎发育有其特征:早期分裂具有不规则现象;仔鱼以尾部破膜先出的方式孵化;柯氏囊出现在原口关闭前,少数个体具有两个柯氏囊。 相似文献
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大西洋牙鲆胚胎发育的形态观察 总被引：9，自引：0，他引：9
为了掌握大西洋牙鲆早期发育的规律,2005年2月在实验室利用显微镜和显微数码摄像显示系统观察测量拍摄大西洋牙鲆受精卵胚胎发育和初孵仔鱼的形态特征,描述并记录其发育过程和时间。大西洋牙鲆的卵为球形游离的浮性卵,卵径平均977μm,单油球,偶见2或3油球,油球径180μm。在水温19~20.8℃时孵化,大约受精后50 min胚盘形成,5 h30 min进入囊胚期,8 h后进入原肠胚期,21 h左右进入胚体器官分化期,40 h后尾部游离,心跳开始,胚体搐动,51~52 h孵出。实验表明,大西洋牙鲆受精卵的孵化进度与水温相关。孵化时间(Ht)与水温(t/℃)关系方程为Ht=3 154.8t-1.333 6(R2=0.925 4)。 相似文献
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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
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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
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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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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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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
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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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《海洋学报(英文版)》2014,(11):161-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