几种海水鱼人工育苗饵料系列的比较

海水鱼人工育苗的饵料系列一般大致相近,基本为轮虫（或双壳类幼体）一浮游甲壳类一鱼虾贝肉糜。但由于种间的特异性,各育苗饵料系列在饵料品种、投喂时间、使用期限上有所差别（见图１）,现比较、分述如下。１大黄鱼（Ｐｓｅｉｄｐｓｃｏａｅｍａｃｒｏｃｅａ）［１］初孵仔鱼全长３ｍｍ左右,口裂、卵黄囊相应较大,３日龄后仔鱼口径按下颌长计算达４００ｕｍ左右,因此开口饵料用Ｌ型轮虫即可,并添加适量小球藻,进行“绿水”培育。一可以作为轮虫的饵料,既增加轮虫的营养,又增强轮虫的背景反差,易被仔鱼发现,提高摄食率;二可以…     

中国对虾摄食行为的化学感觉生理学研究──Ⅲ.中国对虾幼体及早期仔虾的摄食行为及化学感觉

报道了中国对虾幼体及早期仔虾（ １）对轮虫（活体、死体）和卤虫无节幼体 （活体、死体）的摄食过程及摄食率；（２）对悬浮砂粒的摄食情况；（３）摄食水流的产 生机制、方向及模式；（４）对食物的化学敏感性。结果表明，中国对虾幼体及早期仔 虾化学感觉机能不明显。摄食附肢的协调运动产生摄食水流。摄食水流一方面将 食物带到口器附近，另一方面能促进对虾对食物的机械感受。摄食水流的方向还可 以逆转。幼体及早期仔虾对食物的选择主要依据其大小、形状和运动性，而与食物 的化学组成（味道）关系不大。此阶段的对虾采取了悬浮摄食模式，且主动和被动两 种模式并存。本研究还表明，将幼体和早期仔虾的食性简单地区分为草食或肉食性 值得商榷。     

海水仔稚鱼营养研究动态

海水仔稚鱼营养研究，国外已有相当数量的报道，特别是在ｎ－３高度不饱和脂肪酸（ｎ－３ＨＵＦＡ）方面的研究，取得了显著的进展。但迄今，我国鱼类营养研究，基本集中于幼鱼和成鱼阶段，仔稚鱼阶段的营养研究，尚未见报道。目前，我国养殖的名贵海鱼，如真鲷（Ｐａｇ　ｒｏｓｏｍｕｓｍａｊｏｒ）、黑鲷（Ｓｐａｒｕｓ　ｍａｃｒｏｃｅｐｈａｌｕｓ）、牙鲆（Ｐａｒａｌｉｃｈｔｈｙｓ　ｏｌｉ－ｖａｃｅｕｓ）等，在生产性育苗中，因仔稚鱼阶段的大量死亡，成活率一般低于３０％，从早期仔鱼开始吸收自身卵黄内源营养转变为摄取轮虫、卤…     

真鲷仔鱼早期阶段的摄食能力──发育反应和功能反应

于１９９５年４月￣１９９６年５月在中国水产科学研究院黄海水产研究所小麦岛苗种基地,采用梯度试验方法在不同褶皱臂尾轮虫饵料密度下２￣１２日龄真鲷仔鱼的摄食率和摄食强度,通过拟合发育反应和功能反应模型模型的数据来评价真鲷仔鱼早期阶段的摄食能力。结果表明,从仔鱼开口２日龄至１２日龄,摄食强度从０．３１６μｇ／ｈ提高到１．３７４μｇ／ｈ;摄食成功率从５９％提高到７０％,平均摄食发生率从０．４６９μ ｇ／ｈ     

东山湾鱼类食物网研究

本文分析了东山湾８５种经济鱼类的食物关系，结果表明，东山湾鱼类的食性类型可分为：浮游生物食性；底栖生物食性；游泳动物食性；浮游生物和底栖生物食性；底栖生物和游泳动物食性及浮游生物，底栖生物和游泳动物食性等６种，这些鱼类可分为４个营养级：（１）杂食性鱼类；（２）低级肉食性鱼类；（３）中级肉食性鱼类；（４）高级肉食性鱼类，其中低级肉食性鱼类占优势。东山湾 鱼类食物网的能量流动可简要归纳为６种途径，小公     

中国对虾摄食行为的化学感觉生理学研究──Ⅲ.中国对虾幼体及早期仔虾的摄食行为及化学感觉

报道了中国对虾幼体及早期仔虾（１）对轮虫（活体，死体）和卤虫无节幼体（活体，死体）的摄食过程及摄食率；（２）对悬浮砂粒的摄食情况；（３）摄食水流的产生机制，方向及模式；（４）对食物的化学敏感性，结果表明，中国对虾幼体及早期仔虾化学感觉机能不明显，摄食附肢的协调运动产生摄食水流，摄食水流一方面将食物带到口器附近，另一方面能促进对虾对食物的机械感觉。摄食水流的方向还可以逆转。幼体及早期仔虾对食物的选择     

高密度轮虫对点带石斑鱼早期仔鱼培育影响的研究

本试验在水体为1000dm^3、仔鱼密度为15ind．／dm^3条件下，研究不同轮虫密度(10、25、40、70、100ind．／cm^3)对点带石斑鱼早期仔鱼摄食和生长的影响．至仔鱼12日龄的培育试验结果表明，在点带石斑鱼早期仔鱼的培育过程中，投放轮虫对水质有影响，特别是在2～6日龄间，DO值和pH值都有一降低过程，但随后即回升并相对稳定；轮虫密度越高则pH值越低，pH值最低出现在4～6日龄，4日龄时10ind．／cm^3组的pH值比100ind．／cm^3组高0．32．在10～100ind．／cm^3的轮虫密度范围内，较低的轮虫密度对仔鱼的生长有利，12日龄10ind．／cm。组仔鱼的全长比100ind．／cm^3组高31．83％，但100ind．／cm^3组仔鱼的成活率比10ind．／cm^3组的高出近一倍；不同轮虫密度下仔鱼摄食轮虫数量的差异并不明显；但9日龄以后，过高的轮虫密度100ind．／cm^3下仔鱼生长速度显著降低．     

锯缘青蟹早期幼体的饵料试验

本试验采用不同的饵料投喂青蟹的早期幼体，比较饵料效果，为青蟹人工育苗提供参考。１材料与方法１９９１年７月份在本所清江试验场内进行试验。试验用的青蟹早期幼体～蚤状Ｉ期幼体全部采用清江试验场人工孵化的幼体。文中以Ｚ１青示蚤状１期幼体，Ｚ２为蚤状ＩＩ期幼体。人工饵料为酱油粕（乐清虹桥酿造厂提供）、蛋黄、人工轮虫（美国“ＯｃｅａＳｔａｒＩｎｔｅｒｎａｔｉｏｎａｌ　Ｉｎｃ生产的Ｏ．Ｓ．Ｉ牌人造轮虫）。动物性饵料为褶皱臂尾轮虫（Ｂｒａｃｈｉｏｎｕｓｐｌｉｃａｌｉｌｉｓ）。在室温条件下，将青蟹Ｚ１放在１５００…     

光照对真鲷仔、稚、幼鱼摄食的影响

光照对真鲷（Pagrosomusmojor）仔、稚、幼鱼的摄食有重要影响。摄食的适宜光照度范围为100～102lx，最适光照度范围为101～102lx。103lx强光对仔鱼摄食的影响大于稚、幼鱼；100lx弱光对9d以前的仔鱼和稚、幼鱼的摄食影响较小，对9d以后的仔鱼影响较大。此结果和鱼的感觉器官发育及鱼所摄食的饵料种类有关。     

利用单胞藻培养池进行真鲷育苗技术

１９９３年，于文登市小观海珍品育苗养殖场，在海湾扇贝和对虾育苗结束后，利用其配套的单胞藻培养地进行真鲷育苗，利用对虾育苗池和卤虫孵化池培养轮虫。在不增加任何设备的前提下，育成全长３．０１～６．５０ｃｍ，平均全长３．４４ｃｍ的真鲷商品鱼种１６１１１６尾，从仔鱼培育到商品苗种的成活率达到２４．７２％，平均单位水体出苗量达到２６８５尾，１９９３年７月１９日通过了文登市科委组织的验收。正材料和方法１．１育苗设施亲鱼产卵池（１个）和鱼苗培育池（６个）皆用单胞藻培养池（规格为３．８ｍ×３．７ｍ×０．８ｍ，水…     

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.     

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。     

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.     

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.     

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.     

Phylogenetic diversity and phenotypic characterization of cultivable bacterioplankton isolated from polar oceans

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.     

Deep-Sea Sediment Compression Curves: Some Controlling Factors, Spurious Overconsolidation, Predictions, and Geophysical Reproduction

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.