对虾红肢病发病机制的研究

１９９０－１９９３年试验使用副溶血弧菌及溶藻弧菌感染获得成功。在试验过程中发现，环境及对虾体质对驿虾感染死亡率影响甚大，恶劣环境中的死亡率比优良环境中的死亡率出８３．３％；体质差的对虾感染的后的２４ｈ死亡率是正常对虾的２．５－３倍。为此，在对虾虾养殖生产中除应注意消灭病原菌外，还应注意优化养殖环境与增强对虾体质的问题。     

海水养虾池的几种致病弧菌生态

研究了对虾养成期中养殖海水和虾体中弧菌的数量变化、种类组成及其相关因素，初步探讨了弧菌数量与虾病的关系。结果表明，无论养殖水和虾作中弧菌检出率均为100％，养殖水中弧菌测值为2.3×102～4．9×105个／dm3，均值1．78×105个／dm3；虾体中弧菌数是4.4×102～2．9×106个／g，均值为2.9×104个／g。出现于虾体和养殖水中的弧菌有副溶血弧菌（Vibrioparahaemolyticus）、溶藻弧菌（Vibrioalginolyticus）、创伤弧菌（Vibriovulnificus）、河弧菌（Vibriofluvialis）和模拟弧菌（Vibriomimicus）．其中副溶血弧菌和溶藻弧菌是各地的优势种。检测期间，虾池水的生化和理化因素较稳定，对弧菌数量无明显影响。个别虾池出现虾病与弧菌数量较高有关。以分离菌株进行浸染试验的结果表明，副溶血弧菌和溶藻弧菌能使对虾出现与病虾同样的病症。     

厦门同西安柯对虾养殖池的细菌数量动态

本文研究了对虾养成期间养殖池生态系中细菌的数量动态,探讨其变化规律与虾病的关系。结果表明,总细菌、弧菌和发光细菌在水体、底质和虾体中的数量变化各异。在水体各菌数与其环境因子关系中,除了总菌数与ＣＯＤ存在着正相关外,其它的不存在相关性。虾体的总细菌、弧菌和发光细菌的数量（以细胞计）可以用来预报虾病,三者的阀值分别８为１０＾７个ｇ／（湿重）１０＾５个ｇ／（湿重）和１０＾４个ｇ／（湿重）。通过对对虾的细     

不同条件下哈维氏弧菌(Vibrio harvey)对墨吉明对虾(Fenneropenaeus merguiensis)致病性研究

为研究墨吉明对虾弧菌病的防控方法, 本文通过人工注射感染的方式, 研究不同数量哈维 氏弧菌及在不同温度、盐度、pH、不同硝酸氮、亚硝酸氮和氨氮浓度条件下哈维氏弧菌对墨吉明对 虾的致病性的影响。结果表明: 当人工感染哈维氏弧菌数量为3.16×10⁸ CFU 时, 24 h 内对虾累计死 亡率为96.67%; 哈维氏弧菌数量为3.16×10⁶ CFU 以上, 实验结束时, 对虾累计死亡率都超过了 50.00%.在20-32℃ 范围内, 随着温度升高哈维氏弧菌致病力增强, 并且低温组(20℃ 实验组与 26℃ 实验组)对虾累计死亡率显著低于高温组(32℃ 实验组)(P<0.05).在温度为(24±1)℃ 时, 盐度为 20 时对虾累计死亡率处于较低水平; 在温度为(24±1)℃, 盐度为(22±1)时, 96 h, pH 为8.0 时对虾 累计死亡率最低, 并且与另外两个实验组差异显著(P<0.05); 温度为(24±1)℃, 盐度为(22±1), 硝 酸氮对感染哈维氏弧菌的墨吉明对虾有胁迫作用; 在亚硝酸氮浓度(1.0-10.0 mg/L)、氨氮浓度 (0.5-1.5 mg/L)范围内, 哈维氏弧菌对墨吉明对虾的致病性, 随着浓度升高而增强。本实验为墨吉明 对虾弧菌病的防控提供了理论基础。     

四种弧菌对中国对虾的致病性研究

１９９５年８月－１９９６年４月,采用注射感染、浸浴感染、创伤感染和投喂感染比较溶藻弧菌、副溶血弧菌、鳗弧菌、弗尼斯弧菌及其胞外产物对中国对虾的致病性,测定它们的半致死浓度,观察弧菌感染引起的病理组织变化。结果表明,注射感染中,溶藻弧菌、副溶血弧菌、鳗弧菌和弗尼斯弧菌２４小时的半致死浓度（ＬＤ５０）分别是１．２×１０＾６,６．５×１０＾７,４．０×１０＾８,６．８×１０＾９（ＣＦＵ／ｍｌ）;４８小时     

斑节对虾病原菌胞外产物的致病性研究

由养殖濒死病虾体内分离的副溶血弧菌(2019#)、溶藻弧菌(4302#)和嗜水气单胞菌(1003#)培养液中分别提取了胞外产物,测定了酶成分,定量分析了蛋白酶及磷酸酯酶的活性.用细菌胞外产物粗提液对斑节对虾进行致死试验,戊二醛固定致死对虾的肝组织,电镜观察了斑节对虾肝组织的超微病变,初步探讨了三株细菌胞外产物诱发虾病的病理.     

厦门同安西柯对虾养殖池的细菌数量动态

本文研究了对虾养成期间养殖池生态系中细菌的数量动态,探讨其变化规律与虾病的关系。结果表明,总细菌、弧菌和发光细菌在水体、底质和虾体中的数量变化各异。在水体各菌数与其环境因子的关系中,除了总菌数与COD存在着正相关外,其它的不存在相关性。虾体的总细菌、弧菌和发光细菌的数量（以细胞计）可以用来预报虾病,三者的阅值分别为107个　／g（湿重）、105个／g（湿重）和104介／g（湿重）。通过对对虾的细菌学跟踪监测,可以及时采取有效的应急防治措施。     

对虾弧菌制剂试制实验及其在长毛对虾养殖中的应用

本研究进行了实验室弧菌扩大培养方法比较试验，制备成弧菌制剂。实验表明长毛对虾幼虾口服液弧菌制剂或经弧菌制剂浸泡处理，地于预防弧菌感染有一定作用。１９９５年连江大官坂垦区长毛对虾现场养殖实验证明，所采用的一套以弧菌制剂预防虾病的应用方案是可行的，可抑制弧菌引起的并发症，延慢病毒性疾病发生，减少虾病造成的经济损失。     

中国对虾红腿病药物防治应用试验

全身性细菌感染引起的红腿病，是一种重要的弧菌病，主要影响幼虾和成虾，发病率和死亡率都比较高，可以造成整池对虾在较短时间内出现大量死亡，是对虾养成期间危害严重的疾病之一。为了防治对虾红腿病，我们在室内进行了药物饵料筛选试验，在筛选的基础上，研制出复合抗菌药物（ＦＴＬ），在对虾养殖生产中进行了应用试验，获得了较好的防治效果。１材料和方法１．ｌ室内药物筛选试验试验用病虾１９９１年７月采自青岛黄岛区对虾养殖场，病虾体长约６．５ｃｍ，病症表现为游泳足、步足和其它附肢及尾扇变红。病虾取回后放于室内暂养，试验…     

苗期中国对虾幼体异养细菌区系及其变化与病害发生的关系

研究了2个育苗场不同发育期的中国对虾(Penaeus chinensis)幼体的异养菌和弧菌种群变化的动态过程。以典型特征法、BIOLOGGN法和数值分类法对菌株进行鉴定。结果表明，对虾幼体样品中所分离的细菌，大多是革兰氏阴性杆菌。鉴定为假单胞菌属(Pseudomonas)、气单胞菌属(Aeromonas)和弧菌属(Vibrio)。弧菌属主要为溶藻弧菌(Vibrioal-ginozyticus)和哈维氏弧菌(Vibrio harveyi)。在对虾幼体发育早期，假单胞菌(Pseudomonas)和气单胞菌(Aeromonas)占优势，随着对虾幼体的发育，弧菌(Vibrio)渐成为优势，其中溶藻弧菌(Vibrio alginolyticus)和哈维氏弧菌(Vibrio harveyi)优势明显。二者的消长与苗期病害的发生相关，溶藻弧菌总是在虾幼体健康时出现或成为优势，而哈维氏弧菌成为优势时，苗期病害容易发生。     

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.     

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.     

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,     

Estimation of Sediment Properties during Benthic Impact Experiments

Sediment properties, such as water content and density, have been used to estimate the dry and wet weights, as well as the volume of sediment recovered and discharged, during benthic impact experiments conducted in the Pacific and Indian Oceans. The estimates show that the weights of dry (355-1332 t) and wet sediment (1651-4888 t) recovered during the experiments, are not only a function of the total duration and distance covered during the experiment, but also depend on water content and density of the sediment. Estimation of dry sediment and its volumetric ratio in the discharge, are key parameters for calculating the discharged volume. The estimated volume of wet sediment recovered (1427-4049 m 3 ) as well as discharged (2693-6951 m 3 ) during the experiments, provide important inputs to evaluate the sediment resettlement and migration. Using these estimates, the average depth of excavation on the seafloor, can also been calculated. However, the stages of sediment recovery and discharge are expressed differently in some of the experiments. In order to standardize these, different stages have been identified, and definitions of certain terms have been suggested, for use in the future. The methods of calculating different properties, as well as weight and volume of discharged sediment are described in the paper for use in other applications concerning deep-sea discharges.