三角帆蚌不同部位外套膜的比较研究

本文比较了三角帆蚌不同部位外套膜的细胞和组织,并用不同部位外套膜进行育珠生产试验,其结果是,由于采用不同部位外套膜细胞小片育珠、珍珠质量和产量有差异。同一横切面中外套膜三个褶比较,外褶最大,中褶最小。同一个体蚌的外褶比较,以中部外褶最大,出水管的外褶最小,同一个体内褶比较,出水管内褶最大,体后部内褶最小。从外套膜的厚薄来看,蚌的外套膜以中部及中后部较厚,中褶内外侧上皮细胞形态,细胞中高尔基体的分布和结缔组织的结构有很大的不同,说明两者发生上可能来源不同。     

中国北方沿海“褶牡蛎”的分类和订名

中国牡蛎的种类繁多,多样性极为丰富,由于其形态变异大,已报道的中国牡蛎物种组成及分布争议甚大,中国北方沿海常见"褶牡蛎"的分类也一直存在很大的争议,这严重阻碍了其他相关研究的进行.作者系统综述了中国北方沿海"褶牡蛎"的分类历史和研究现状,并对中国北方沿海"褶牡蛎"进行了系统的分类研究,取得了最新研究成果.确立了中国北方沿海"褶牡蛎"的分类地位,改变其分类长期混乱的局面,这对于"褶牡蛎"的养殖和其他相关研究均具有重要的意义.     

细尾属吸虫—新种

从大头狗母鱼Trachinocephalusmyops的消化道内检获细尾属1新种：厦门细尾吸虫，新种Eriepturusxiamenensissp.nov.。新种与狗母色细尾吸虫E.trachinocephaliYamaguti，1970和带鱼细尾吸虫E．trichiuriGuetShen，1978相似，但它们可以从虫体大小和虫卵大小以及其他形态特征相区别。     

中国海洋吸虫纲物种多样性的研究

在国家908专项调查和成果集成工作的基础上,结合对海洋吸虫文献资料的收集,分析研究了中国海洋吸虫的物种多样性.其结果表明中国海洋吸虫有1 184种,其中单殖目吸虫410种,复殖目吸虫774种.单殖目的宿主都是硬骨鱼.复殖目物种成虫的宿主主要是鱼,也有爬行纲和兽纲.吸虫感染宿主有些具有专一性,但也有些具有普遍性.宿主的食性、地理分布和季节分布与吸虫感染密切相关.不同于以往70多年来主要进行的分类研究,本文主要探讨海洋吸虫的生活史及与其宿主的关系,这将为水生生物病虫害的防治和海洋物种多样性的研究提供基础资料,具有重要生物学和生态学的意义.     

鱼居叉盘吸虫的再描述及其地理新记录

在我国首次从南海的金钱鱼Scatophagusargus(Linnaeus)消化道里检获鱼居叉盘吸虫Waretrema piscicola Srivastava，1939，并对其形态结构进行重新描述和绘图。比较了来自不同宿主的鱼居叉盘吸虫的大小及形态结构。     

南沙群岛多毛类背褶沙蚕属一新种

于１９８８年，中国科学院南海海洋研究所在南沙群岛进行综合考察，在采集到的多毛类标本中，发现了背褶沙蚕Ｔａｍｂａｌａｇａｍｉａ的一新种，其与代表种背褶沙蚕Ｔ．ｆａｕｖｅｌｉ和东方背褶沙蚕Ｔ．ｏｒｉｅｎｔａｌｉｓ在眼、双背须出现的刚节数以及背须的形状等有明显的区别，故定名为中华背褶沙蚕Ｔａｍｂａｌａｇａｍｉａ ｓｉｎｉｃａ，模式标本保存于中国科学院南海海洋研究所。     

外栉绕宫吸虫种群生态研究

外栉绕宫吸虫在不同体长组的褐菖鲉肠道内的感染率变动范围在12.50%-31.25%之间;感染强度和种群平均密度呈现不规则的变动;在体长为80mm≤L〈140mm的宿主中,外栉绕宫吸虫种群的感染率是随宿主体长的增加而逐渐增加的.不同月份中外栉绕宫吸虫在宿主肠道内的感染率、感染强度和种群平均密度没有明显的变化规律.吸虫种群在不同月份和不同体长组宿主中的分布类型属于聚集分布,而且聚集强度随种群密度增加而增强.     

东海鱼类的囊双科吸虫

囊双科Didymozoidae Poche,1907吸虫为鱼类专性寄生虫之一,其体形多变,寄生部位广泛,侵袭宿主体内与体外各种组织与器官,因而引起人们的注意,国外不断有该科的研究报道。我国关于该科的研究,顾昌栋在1965,1983年曾有文章发表,但其中有关东海的种类不多。1975,1976,1979年作者在东海采集鱼类寄生虫,整理后共得囊双科吸虫11种。其中除双枝囊双吸虫Didymosoon biramous Ku et Shen,1965,大眼鲷囊双吸虫Didymozoon priacanthi Ku et Shen,1965;海南合体双吸虫Syncorpozoum hainanensis Ku et Shen,1965鲐囊双吸虫Didymozoon Pneumatophori Gu et Shen,1983和线形线双吸虫Nematobothrium filiforme Yamaguti,1934在我国已作报道外,共发现1新属3新种及3个新记录。本文为新种和新记录描述。测量一律用毫米,卵子用微米。模式(副模式)标本存放于中园科学院海洋研究所。     

东海陆架外缘隆褶带的形成与构造演化

东海陆架外缘隆褶带是菲律宾海板块俯冲带陆侧弧后裂陷盆地(陆架盆地与冲绳海槽)之间的水下残留火山弧.其地球物理特征、地层组成、岩浆活动及地质构造等均具有“东西分带、南北分块”之特征.本隆褶带的形成始于第三纪初,当时为陆缘弧;中新世末以后,由于琉球弧后冲绳海槽的张裂作用,遂成为古琉球弧的残留弧.其形成机理受东海构造格局控制,与菲律宾海板块的俯冲作用及俯冲带的东向迁移有关,东海隆褶带的形成和构造演化大致经历了四个阶段:(1)断隆火山弧(E₁₊₂)、(2)褶隆火山弧(E₃)、(3)褶隆残留弧(N₁)和(4)消亡残留弧(N₂～Q).最后一个阶段隆褶带与陆架盆地整体沉降,接受了厚约1500m的上新世-第四纪浅海相沉积.     

双尾亚科一新种（吸虫纲：半尾科）

本文报道芽腺属吸虫一新种，即矶鲈芽腺吸虫，新种LecithocladiumparapristipomatissP．nov.，虫体大小1.24～1．74×0．25～0．45mm；虫卵18～22×9～12μm。     

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.     

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.     

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.     

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.