Mian状黄姑鱼的早期发育研究

本文对Ｍｉａｎ状黄姑鱼的胚胎和仔、稚鱼各发育阶段的形态特征进行了描述。Ｍｉａｎ状黄姑鱼的爱精卵的为圆球形浮性卵,无色透明。在水温２０￣２３℃,盐度２６￣３０的条件下,经２４ｈ３５ｍｉｎ陆续孵出仔鱼。胚胎发育分为２６期。初孵仔鱼至孵化后４日龄为仔鱼前期;孵化后５￣２２日龄为仔鱼后期;孵化后２３￣３２日龄为雅鱼期;孵化后３３日龄进入幼鱼早期。仔、稚鱼培育水温１８￣２８℃,盐度２０￣３０。仔鱼２日龄稍开     

黄姑鱼(Nibea albiflora Richardson)早期生长发育研究

为研究黄姑鱼胚胎发育特征和胚后发育的仔、稚、幼鱼发育阶段的形态学,2010-06-08在实验室利用显微镜和显微镜数码摄像显示系统对黄姑鱼胚胎发育过程进行连续观察拍摄,描述并记录其发育过程和时间。结果表明,黄姑鱼卵为圆球形的端黄卵,盘状分裂,中央有一个油球,卵径为(0.89±0.028)mm,油球直径为0.25mm;在水温为24℃、S为27条件下经22.5h完成孵化,胚胎发育可分为24期。胚后发育阶段,1～3日龄为卵黄囊期仔鱼;4日龄仔鱼开口,卵黄囊完全消失,此时仔鱼处于混合营养阶段,进入前弯曲期;6日龄仔鱼油球完全消失,进入外源性营养阶段;16日龄仔鱼尾鳍担鳍骨形成,脊椎末端上曲,进入弯曲期;21日龄仔鱼尾下骨后缘与尾索垂直,鳍条数不断增加,同时背鳍、臀鳍和腹鳍原基出现,进入后弯曲期;26日龄鱼苗全身被菊花状黑色素细胞,尾柄处开始被鳞,进入稚鱼期;31日龄以后,鱼苗全身被鳞,进入幼鱼期。在水温为25～27℃,S为26～28的条件下,仔、稚、幼鱼全长与日龄具有显著的正相关性。研究表明,黄姑鱼进入稚鱼期之后,其生长速率明显增大,为减少自残,应及时分池和投足饵料。     

漠斑牙鲆仔、稚、幼鱼的形态发育研究

2006年12月至2007年2月,在福建省漳州市东山县华涛水产综合养殖场,对漠斑牙鲆(Paralichthys lethostigma)仔、稚、幼鱼各发育阶段的形态特征进行了观察和描述.初孵仔鱼平均全长2.73±0.211mm.在培育水温18.1～23.0℃和盐度为33～34条件下,初孵仔鱼至孵化后7日龄为前期仔鱼,6日龄仔鱼开口;孵化后8日龄至30日龄为后期仔鱼;孵化后31日龄至45日龄为稚鱼期;孵化后46日龄进入幼鱼期.冠状幼鳍的消长、右眼的移位以及体色的左右不对称是漠斑牙鲆早期发育过程中最明显的外部形态变化.     

斜带石斑鱼仔、稚、幼鱼的形态发育研究

2005年10～12月,在集美大学水产学院水产试验场,对人工培育的斜带石斑鱼仔、稚、幼鱼各发育阶段的形态特征进行了观察和描述.根据卵黄囊、鳍膜、鳞片以及背鳍长棘和腹鳍长棘的变化,将斜带石斑鱼的胚后发育划分为仔鱼期、稚鱼期和幼鱼期3个时期.初孵仔鱼平均全长1.68mm(1.60～1.78mm).在培育水温为21.0～28.5℃,盐度为24.8～28.3条件下,初孵仔鱼至孵化后5日龄为前期仔鱼,3日龄仔鱼开口;孵化后6日龄至31日龄为后期仔鱼;孵化后32日龄至68日龄为稚鱼期;孵化后69日龄进入幼鱼期.背鳍第二鳍棘和腹鳍鳍棘的长出与收缩是斜带石斑鱼前期发育过程中最明显的变化.此外,本文探讨了斜带石斑鱼与青石斑鱼、点带石斑鱼和赤点石斑鱼仔、稚、幼鱼期发育的异同.     

(鱼免)状黄姑鱼早期发育特征及对温盐度的适应性

1996年3~6月采用人工注射LRH-A和HCG诱导状黄姑鱼自然产卵受精,观察6批次胚胎发育的结构特征和1~16日龄仔鱼形态变化及温度、盐度对状黄姑鱼早期发育和存活的影响,为状黄姑鱼大规模人工繁殖和苗种培育提供科学依据。根据其外部形态和胚胎行为的出现将状黄姑鱼胚胎发育划分为17期,3日龄开口;状黄姑鱼受精卵孵化的温度范围为16.3~30℃,最适孵化温度为22~24℃;孵化盐度范围为13.7~53,最适孵化盐度范围为26.9~40.7,其中盐度为7.2时受精卵无法孵化,盐度在40.7以上的受精卵全部为浮性,盐度为26.9以下全部呈沉性;状黄姑鱼仔鱼存活的适合盐度为20.2~33.4,随着仔鱼的生长,对耐盐的适应性也逐渐增强。     

双棘黄姑鱼人工育苗技术的研究

对双棘黄姑鱼【Nibeadiacanthus(Lacepede)】催产孵化和育苗技术进行了试验研究,并从形态学方面对其近似种和易混种进行了比较。结果显示,双棘黄姑鱼性腺发育至Ⅳ期经人工催产都能产卵受精．效应时间为20～40h。胚胎发育适宜水温为22～26℃．适宜盐度为30～35,孵化率为80％～90％。在育苗水温27～29℃,盐度28～30,150万初孵仔鱼经20d培育,共育出全长1．4～2．3cm的稚鱼95．3万尾,育成率62．3％;其中32．2万稚鱼分池继续培育至36天,育出全长3．1～5．2cm的幼鱼18．4万尾。本试验说明对双棘黄姑鱼进行人工催产孵化育苗,能够培育出达到商品规格的鱼种。     

光唇鱼( Acrossocheilus fasciatus) 胚胎及仔、稚鱼的发育

采用干法授精方法获得受精卵,在人工培育条件下观察了光唇鱼胚胎及仔、稚鱼发育过程。结果表明,光唇鱼受精卵呈圆球形,沉性、弱粘性。在水温23—25℃下,胚胎发育历时46h45min,经历了胚盘形成、卵裂、囊胚、原肠胚、神经胚、器官形成和孵化等阶段。在水温24—27℃下,仔、稚鱼发育历时22d,初孵仔鱼具有较大的卵黄囊,胸鳍原基及肛门原基形成;4日龄仔鱼开口摄食,进入混合营养期;7日龄仔鱼卵黄囊消失,营外源性营养,体侧8条横斑形成,各鳍均已出现,进入晚期仔鱼阶段;14日龄仔鱼各鳍鳍条发育基本完成;16日龄仔鱼鳞片开始出现,进入稚鱼期;22日龄稚鱼全身被鳞,进入幼鱼期。     

犬齿牙鲆胚胎及仔、稚、幼鱼形态发育观察

犬齿牙鲆(Paralichthys dentatus)卵为端黄卵,受精卵浮性,卵径950~1100μm,油球径200~225μm.在水温20.5~22.0℃,盐度33条件下培育,受精后1 h 20 min 进入卵裂期,6 h 10 min 进入囊胚期,11 h 20 min 进入原肠胚期,19 h 10 min 发育到胚孔封闭期,胚体形成,26 h 50 min 尾芽出现,33 h 35 min心跳开始,48 h 10 min 开始孵化出仔鱼.初孵仔鱼平均全长2.59 mm±0.02 mm,在培育水温为17.0~21.0℃,盐度24~34条件下,胚后发育时序为:1日龄~9日龄为仔鱼前期,10日龄平均全长5.52 mm±0.05 mm,卵黄囊和油球完全吸收进入仔鱼后期;40日龄平均全长20.82 mm±0.67 mm,各鳍鳍条发育形成进入稚鱼期;65日龄平均全长41.13 mm±0.88 mm,全身鳞被完整进入幼鱼早期     

星斑川鲽仔、稚、幼鱼的形态发育与生长

为了摸清星斑川鲽仔、稚、幼鱼各期形态发育特征,2006年4-7月在实验室利用显微数码摄像系统,通过电脑显示屏观察、测量、拍摄记录星斑川鲽胚后发育形态变化.培育水温14.0～19.5 ℃,S 27～31,光照度500 lx左右,饵料依次为经过强化的轮虫、卤虫无节幼体和配合饲料.星斑川鲽初孵仔鱼全长1.80～2.08 mm, 1日龄仔鱼平均全长2.89 mm;3日龄开始摄食;5日龄卵黄囊吸收完毕进入后仔鱼期;15～16日龄全长8.84 mm,开始伏底变态进入稚鱼期;20日龄全长10.12 mm,稚鱼右眼完全迁移至左侧,变态完成营底栖生活进入幼鱼期.星斑川鲽仔鱼变态发生日龄与培育水温有关,在12～15 ℃需24～27 d;15～16 ℃需18～20 d;17～19 ℃需15 d.开始变态仔鱼全长9 mm,变态完成时全长11 mm.幼鱼期鳞被形成,基本具有成鱼的外部形态和习性.     

鮸状黄姑鱼胚胎和仔鱼发育的实验生态

本实验研究了温度、盐度、 ｐＨ对鮸状黄姑鱼胚胎发育和前期仔鱼存活的影响。结果表明,鮸状黄姑鱼受精卵孵化的温度范围为１５～３０℃,最适孵化温度为２５～３０℃;孵化盐度范围为１５～４５,最适孵化公度范围为１５～２５;ｐＨ值在５．００～８．９９范围内,受精卵孵化率没有显著的差异。鮸状黄姑鱼前期仔鱼存活的适合温度为１５～３０℃,最适温度为２５℃;适合盐度为１５～３５;适合ｐＨ值为５．９９～１０．０１。     

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.     

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.     

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.     

Flow Cytometric Analysis of Coastal Lagoon Bacterioplankton and Picophytoplankton: Fixation and Storage Effects

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.     

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

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INFORMATION FOR AUTHORS

<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,