Histological observation of eye ontogeny in rock bream larvae （Oplegnathus fasciatus ）

应用石蜡切片技术和显微测量法,对条石鲷（Oplegnathusfasciatus）视觉器官的早期发生、分化和形成过程进行了连续观察。结果显示：在水温24℃±1．0℃的条件下,受精后10．5h,视杯出现;受精后15．5h,晶状体形成;受精后22h,在脉络膜裂口处出现角膜;2日龄,巩膜和脉络膜形成;3日龄,虹膜出现：6日龄,视网膜分化完全,由色素层、视锥视杆层、外界膜、外核层、外网状层、内核层、内网状层、神经节细胞层、神经纤维层和内界膜组成;13日龄,角膜分化完全,由外向内依次为复层扁平上皮、前弹性膜、纤维层、后弹性膜和肉皮层;21日龄,虹膜完全分化,由内向外依次为色素层、后缘层、基质层、前缘层和内皮层。此时条石鲷眼的各个部分（巩膜、脉络膜、视网膜、晶状体、虹膜、角膜）均发育完善。     

条石鲷鳔器官早期发育的组织学观察

应用石蜡切片技术和显微测量法,对条石鲷(Oplegnathus fasciatus)鳔的早期发生、分化和形成过程进行了连续观察。结果显示:条石鲷为闭鳔鱼类,在水温为23.5℃±0.5℃的条件下,鳔的形成过程可分为鳔原基出现、鳔管形成、鳔腔充气、鳔管退化及气腺形成4个时期。1日龄(孵化后第2天)仔鱼,在食道与肠的交界处分化出鳔原基;4日龄,鳔管原基出现;5日龄,气腺原基出现;6日龄,迷网出现;8日龄,鳔管形成;10日龄,鳔开始充气;17日龄,鳔充气完毕,鳔管开始退化;20日龄左右,鳔管从幽门处完全脱离;25日龄,气腺迷网发育完全;30日龄,鳔管完全消失,鳔的发育基本完善。在条石鲷的苗种培育过程中,鳔器官的发育影响到条石鲷仔鱼的成活率。     

红鳍笛鲷(Lutjanus erythopterus)胚胎发育的形态学研究

通过显微直接观察法对红鳍笛鲷胚胎发生的形态学进行了研究,以期为红鳍笛鲷人工繁殖、育苗提供参考资料。红鳍笛鲷胚胎的形态发生过程可分为受精卵、卵裂、囊胚、原肠胚、神经胚、器官形成等6个阶段,24个时期。红鳍笛鲷受精卵为浮性卵,透明而呈圆球形,内有一大油球,在水温28℃、海水盐度32.2的条件下,受精后15 min原生质隆起形成胚盘;受精后30 min进行第1次卵裂,为盘状卵裂;受精后3 h,胚胎进入高囊胚期;受精后6 h 27 min,胚胎发育至原肠期;受精后9 h 36 min形成神经板,继而神经板前端分化出前脑泡、中脑泡和后脑泡;脑泡分化后,视囊、听囊、晶状体等相继形成;受精后15 h 32 min尾芽形成;受精后约20 h,仔鱼出膜。其发育过程与黄鲷、金头鲷、点带石斑等其他海水鱼相似。     

条石鲷( Oplegnathus fasciatus) 心脏早期发育的组织学观察

应用石蜡切片技术和显微测量法,对条石鲷心脏的早期发生、分化和形成过程进行了连续观察。结果表明,在水温(24±1.0)℃的条件下,心脏原基在受精后13h30min出现于中部脑的腹面,其外部由卵黄多核层包围,内部则为扁平细胞所填充;受精后20h30min,心脏开始搏动,可见血细胞;初孵仔鱼心脏呈直管状,位于体腔前端;2日龄(daysafterhatching,DAH),心脏分化成静脉窦、心耳(心房)、心室和动脉球四个部分;3日龄,耳室瓣和半月瓣形成;6日龄,窦耳瓣和心小室形成;12日龄,心脏内血细胞的数量急剧增加,血流量显著加大;27日龄,心耳内形成小梁结构,心脏发育完善。     

条石鲷早期发育的形态特征

条石鲷(Oplegnathus fasciatusTemminck et Schlegel 1844)的受精卵为球形浮性卵,卵径为0.79~0.90 mm,无色透明,油球一个,卵黄靠近动物极有龟裂结构。在22℃±0.5℃,盐度为30的条件下,卵子授精后31 h仔鱼孵出。初孵仔鱼全长1.66~2.20 mm,在背鳍膜的前边缘上有4~5个星状黑色素;1日龄仔鱼全长1.83~2.32 mm,背鳍膜上黑色素异常明显;2日龄仔鱼,胸鳍原基出现,尾部鳍膜中间开始出现放射丝;3日龄仔鱼,背鳍膜上黑色素消失,上下颌开启,部分仔鱼开口摄食;4日龄仔鱼,卵黄囊吸收殆尽,鳔原基出现;5日龄仔鱼,胸鳍可垂直向外伸展,上下颌开启频繁;12日龄仔鱼,具有集群和趋光性;20日龄仔鱼,体前部呈黑色,在水中分散均匀,摄食旺盛。25日龄稚鱼,全长6.55~8.42 mm,体前部开始出现黑色条带痕迹;30日龄稚鱼,头部眼的上缘由一横带,鱼体体侧出现3条黑褐色的横条带。40日龄幼鱼,全长15.50~35.55 mm,鱼体体型与成鱼相似,体侧有6~7条黑褐色的横条带。通过对条石鲷早期发育的形态学观察,了解其卵胚及仔稚的发育规律和种属的特异性,不仅可以丰富我们对鱼类早期生活史的认识,而且对进一步进行条石鲷的生产育苗起到积极的推进作用。     

条石鲷消化道发育的组织学观察

对人工养殖的条石鲷（Oplegnathus fasciatus）仔、幼稚鱼消化道及消化腺的发育过程进行了系统的组织学观察。研究表明： 初孵仔鱼 （体长1.66～2.20 mm）的消化道完全处于未分化状态。1 日龄仔鱼全长1.83～2.32 mm, 消化道中部开始形成空腔, 为初始的消化道腔。2 日龄仔鱼全长2.61～2...     

中国近海条石鲷(Oplegnathus fasciatus)群体遗传多样性线粒体DNA序列分析

采用线粒体(mtDNA)DNACOI和Cytb基因片段序列分析方法,进行了中国近海条石鲷(Oplegnathus fasciatus)舟山和胶南群体遗传多样性及其遗传结构现状研究。结果表明,基于mtDNACOI分子标记揭示条石鲷舟山群体遗传多样性水平(h=0.814±0.060,π=0.009±0.005,k=5.653±2.789)显著高于胶南群体(h=0.742±0.116,π=0.003±0.002,k=1.970±1.196);MST分析、NJ系统分析和核苷酸不配对分布分析结果皆显示两群体内存在三个显著分化的单倍型类群,支系间的遗传距离为0.018—0.025;遗传分化指数结果(Fst=0.331,P=0.000)和确切P检验结果显示(P=0.000)两群体间存在显著遗传分化。基于mtDNACytb分子标记显示条石鲷群体遗传多样性总体上呈现较低水平(h=0.874±0.023,π=0.006±0.003,k=2.761±1.492),舟山群体核苷酸多样度水平显著高于胶南群体;NJ系统发育和群体遗传分化研究结果显示,条石鲷群体间未检测到显著的遗传分化。     

条石鲷(Oplegnathus fasciatus)养殖群体与野生群体线粒体控制区序列遗传变异研究

采用线粒体(mtDNA)控制区序列分析方法,进行了条石鲷养殖群体(F1代和F2代)与野生群体的遗传变异比较研究.结果表明:在长度为484bp的mtDNA控制区片段中,条石鲷养殖群体F1代单倍型多样度水平(h=0.955±0.047)略低于野生群体(h=1.000±0.034),却显著高于养殖F2代群体(h=0.797±0.070);条石鲷野生群体(π=0.021±0.012)、养殖群体F1代(π=0.018士0.010)和养殖群体F2代(π=0.014±0.008)的核苷酸多样度水平呈现明显的递减趋势;核苷酸不配对分布和两两序列相比较碱基差异结果显示条石鲷野生群体、养殖群体F1代和养殖群体F2代也呈现明显的递减趋势.分子方差分析(AMOVA)、两两群体相比较的ΦsT和确切P检验结果皆显示条石鲷养殖群体F1代和F2代与野生群体存在显著的遗传分化.单倍型最小跨度分析和NJ系统分析结果均未检测到显著的谱系结构.     

温度对条石鲷幼鱼代谢率、排泄率及窒息点的影响

采用静水密闭式呼吸仪,分别测定了13,18,23,28和33℃5个水温梯度下条石鲷Oplegnat-hus fasciatus幼鱼的代谢率、排泄率及窒息点。结果表明:(1)不同温度条件下,条石鲷幼鱼的代谢率和排泄率差异显著(p<0.05);当温度由13℃升高至28℃时,条石鲷幼鱼的代谢率和排泄率均随之升高;当水温为28℃时,其代谢率和排泄率达最大值,分别为(16.33±0.45)J/(g·h)和(1.03±0.04)J/(g·h),是13℃实验组的6.69倍和5.15倍;与28℃实验组相比,33℃实验组的代谢率和排泄率分别降低了19.04%和15.53%,33℃已超出了条石鲷幼鱼生长的最高适温。(2)实验温度下,条石鲷幼鱼的蛋白质供能比值为37.94%～72.24%,蛋白质是其主要能源物质。(3)条石鲷幼鱼的窒息点为(3.17～3.64)mg/L,并随水温升高而升高。(4)Q10值和蛋白质供能比值的变化特征表明,18～28℃是条石鲷幼鱼的适宜生长温度。     

条石鲷mPRα基因的cDNA克隆和表达模式分析

采用同源性克隆和末端快速扩增(RACE)方法,首次获得全长为1222bp的条石鲷膜孕激素受体α(mPRα)的cDNA序列。其开放阅读框为1060bp,编码了含353个氨基酸的蛋白,N端前16个氨基酸为信号肽。氨基酸序列比较分析发现其存在7个跨膜区域。其预测的蛋白质三级结构中存在着多个蛋白结合位点。同源性比较和进化分析表明,条石鲷mPRα与鲈形目鱼类mPRα聚为一支,进化关系较近,相似度达到95%以上。实时荧光定量PCR方法检测mPRα mRNA表达情况:发现mPRα mRNA在性成熟雌性条石鲷各组织均有表达,并在脑、垂体和卵巢组织中的表达较丰富。在条石鲷繁殖周期的脑和垂体组织中,mPRα mRNA的表达水平在卵巢发育的Ⅳ期达到最大值;在繁殖周期的卵巢组织中,mPRα mRNA的表达水平从卵巢发育Ⅲ期到Ⅴ期持续升高并且在Ⅴ期达到最大值(P0.05)。条石鲷雌鱼血清中雌二醇激素的含量变化在整个繁殖周期中差异显著(P0.05),在性腺发育Ⅲ期含量迅速升高并在Ⅳ期达到峰值。本研究为条石鲷卵巢成熟调控机制研究提供了基础参考资料。     

Microbial Biomass and Organic Nutrients in the Deep-Sea Sediments of the Central Indian Ocean Basin

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.     

A Review of Some Environmental Issues Affecting Marine Mining

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.     

Increased Particle Fluxes at the INDEX Site Attributable to Simulated Benthic Disturbance

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.     

Assessing the Validity of Seismo-Acoustic Predictor Equations for Obtaining Seabed and Sub-Surface Sediment Physical Properties

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.     

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.     

海上大直径钢管桩打桩过程中桩周土强度弱化研究

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。     

Determination of In Situ Sediment Shear Strength from Advanced Piston Corer Pullout Forces

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.     

Interannual Sea Level Variations and Annual Tides in the Northwestern Pacific

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.     

《Acta Oceanologica Sinica》Vol. 33(2014) contents

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