海水青鳉胚胎发育的观察

为了解模式生物种海水青鳉(Oryzias melastigma)的胚胎发育特征,作者培育30日龄的海水青鳉,收集自然受精卵,在水温26~28℃、盐度27~28条件下,静水孵化。利用奥林巴斯SZ61解剖镜对海水青鳉胚胎发育进行了观察研究。结果表明:海水青鳉受精卵为圆球形端黄卵,多油球,沉性,卵膜上具有绒毛膜和纤维丝。和多数硬骨相似,胚胎发育的过程大致可以分为7个期:胚盘形成期、细胞分裂期、囊胚期、原肠期、器官形成期、肌肉效应期和孵化期。并发现海水青鳉胚胎发育有其特征:早期分裂具有不规则现象;仔鱼以尾部破膜先出的方式孵化;柯氏囊出现在原口关闭前,少数个体具有两个柯氏囊。     

温度、盐度对半滑舌鳎胚胎发育的影响

温度及盐度是鱼类苗种生产当中2个重要的因子。研究了在不同水温、盐度条件下,半滑舌鳎胚胎发育的情况。通过对孵化时间、孵化率、初孵仔鱼畸形率、活力的比较,发现温度对受精卵的孵化影响显著。受精卵在18℃以下及28℃以上均不能孵化出仔鱼,在18~28℃水温条件下,受精卵可以孵化,其适宜的孵化水温为22~23℃,且随着温度升高受精卵孵化时间逐渐缩短。在水温23℃下,受精卵在盐度16以下及48以上均不能孵化出仔鱼,在盐度18~46的范围内,受精卵均可以孵化出仔鱼,盐度38以上均为畸形,且孵化时间不受盐度的影响,其适宜孵化盐度为28~32。     

盐度对牡蛎“华南1号”早期发育与生长的影响

为探究牡蛎"华南1号"早期发育的盐度适应性,本研究以目前北部湾海域的香港牡蛎(Crassostrea hongkongensis)养殖群体为对照组,在水温28～29℃、pH为8.1～8.2条件下,分析了不同盐度(3、8、13、15、18、23、28、33)对牡蛎"华南1号"的胚胎、幼虫发育和稚贝生长的影响。研究显示,不同盐度下牡蛎"华南1号"的受精率和孵化率均高于对照组,差异显著(P0.05),且牡蛎"华南1号"的适宜受精盐度为13～23,对照组的适宜受精盐度为13～18。相同盐度条件下,牡蛎"华南1号"与对照组浮游幼虫期的壳高生长指标差异显著(P0.05),牡蛎"华南1号"不同盐度组间差异显著(P0.05)。不同盐度条件下,牡蛎"华南1号"在幼虫发育阶段和早期稚贝的生长速率和存活率均随着盐度的增加"先升后降",且不同盐度组间差异显著(P0.05),高盐33和低盐3条件下幼虫生长缓慢且存活率较低,牡蛎"华南1号"幼虫的附着率和存活率在盐度13～23时较高。研究结果表明,牡蛎"华南1号"在浮游幼虫和早期稚贝阶段生长速度快于对照组群体(P0.05),且浮游幼虫和稚贝生长的适宜盐度为8～28,最适盐度为13～23;对照组幼虫和稚贝生长的适宜盐度为8～23,最适盐度为13～18。与对照组群体相比,牡蛎"华南1号"适宜盐度较对照组由18提高到23,盐度适应范围广,且具有明显的生长优势。     

黄姑鱼胚胎发育及其与温度和盐度的关系

为研究温度和盐度对黄姑鱼(Nibea albiflora)胚胎发育的影响,作者观察了黄姑鱼受精卵的形态和胚胎发育过程。实验结果表明,温度18~28℃范围内,温度对孵化时间和初孵仔鱼有显著影响,对孵化率影响不大,24~28℃是黄姑鱼胚胎发育的适宜温度范围;盐度低于24时受精卵下沉,26~28内悬浮于水体中,盐度高于34时受精卵浮于水面;黄姑鱼胚胎发育的最适盐度范围26~32,盐度超过或低于其适宜范围时,孵化率明显下降或者幼虫畸形率明显增大。另外,根据其Q10值推算的胚胎发育的适宜水温与实验结果相似。     

盐度对褐毛鲿胚胎发育和早期仔鱼存活率的影响

为了探索褐毛鲿(Megalonibea fusca)胚胎孵化和早期仔鱼生长发育最适宜的盐度条件,作者观察了其胚胎在6个盐度(35、30、25、20、15、10)海水中沉浮性、发育、初孵仔鱼分布状态.结果表明:胚胎在盐度35时完全上浮,盐度低于25完全下沉,在盐度30时处于半悬浮状态;不同盐度对胚胎发育有一定影响:在盐度30~15范围内,胚胎发育较快,孵化时间较为一致,在盐度35和10发育变慢,孵化时间延长2.5 h以上;初孵仔鱼在不同盐度海水中呈不同分布状态:在盐度35时完全上浮表层,盐度25~30分布于中下层至中上层,盐度25大部分仔鱼沉底,盐度低于20,初孵仔鱼全部沉底.观察了10个盐度(35、32、29、26、23、20、17、14、11、8)海水中胚胎孵化率和早期仔鱼存活率,结果表明:褐毛鲿胚胎在盐度35~8范围内孵化率达(76±2)%~(98±2)%,在较低盐度26~11区间,孵化率达(88±0)%~(98±2)%,显示低盐区更高的孵化率,而在较高盐度29~35区间,孵化率在(82±2)%~(84±2)%,并且具有明显趋向性,即盐度大于29,随盐度升高孵化率逐渐下降;盐度对早期仔鱼存活率有明显影响:孵化后40 h 正常仔鱼最高存活率在低盐度26~8区,为(89.4±2.2)%~(97.4±0.1)%,盐度大于29,随着盐度上升仔鱼死亡率骤然升高,在盐度29~35,升至(31.7±0.7)%~(38.1±1.5)%,畸形率升至(7.1±0.2)%~(10.7±0.5)%,正常仔鱼存活率下降至(61.0±1.0)%~(61.9±1.5)%.低盐度区仔鱼有更高的存活率.褐毛鲿胚胎最适孵化盐度在29~32,早期仔鱼最适培育盐度为26.     

虎斑乌贼( Sepia pharaonis )胚胎发育及孵化历期观察

采捕虎斑乌贼野生卵群进行室内培育,采用显微成像系统,观察其胚胎发育过程,并详细描述各发育期的特征。结果显示:虎斑乌贼卵长径(30.7±2.4)mm,短径(13.4±1.3)mm,胚胎发育过程共分为卵裂、囊胚期、原肠期、器官芽原基出现、眼色由无色到黑色等30期,探讨了主要器官(眼、漏斗等)的发生变化过程。在胚体生长期间,胚体长度随时间逐渐增加,而卵黄大小则随之减小。从7—20d,胚体长度由2.5mm增至11.3mm,而卵黄直径由8.9mm减至4.5mm,胚体与卵黄长度比例由0.28增至2.51。在水温(23±0.5)℃,盐度28,pH7.41条件下,孵化高峰期为20—24d,孵化率为85.3%,初孵乌贼幼体平均体长(13.5±0.3)mm,平均胴体长(8.6±0.3)mm,平均体重(0.18±0.02)g。     

黄海大头鳕胚胎发育过程

驯化野生大头鳕(Gadus macrocephalus Tilesius)作为亲鱼,通过自然受精和人工授精两种方法获得受精卵,自然受精卵通过虹吸法收集。受精卵孵化条件为水温6~8℃,盐度32~33,pH7.8~8.2,微充气。在奥林巴斯SZ61解剖镜下对大头鳕的胚胎发育进行了观察,并使用CCD图像传感器拍照,描述了各发育时期的发育时序和形态特征。大头鳕受精卵为圆球形端黄卵,弱黏性,无油球,卵膜上具龟裂结构,卵子直径0.95~1.12mm,n=30,卵黄均匀透明。类似于大部分硬骨鱼类,其胚胎发育可分为胚盘形成期、卵裂期、桑椹期、囊胚期、原肠期、神经胚期、器官发生期、尾芽期、肌肉效应期。在水温6~8℃,盐度32~33的条件下,受精卵历时约336h完成胚胎发育过程,孵化出膜。在大头鳕胚胎发育过程中,具有4个不同于其他硬骨鱼类的地方:(1)发现早期分裂球具有不规则现象;(2)很多胚胎发育过程不出现柯氏囊,有柯氏囊的胚胎仅占10%左右,且出现晚,消失快;(3)胚胎孵化为仔鱼与发育进程关联性不大,孵化的仔鱼有3种主要形态;(4)胚胎各个时期都有较高死亡率,以原肠期最为严重。     

半滑舌鳎胚胎发育及仔鱼生长与盐度的关系

就半滑舌鳎(CynoglossussemilaevisGünther)受精卵和早期仔鱼生长发育与盐度的关系作了初步探讨。受精卵在盐度低于25的海水中全部下沉,在高于29的海水中浮在水面,而当盐度在26～28.5之间时在海水中呈悬浮状态。受精卵孵化的最适盐度为25～35,此盐度范围内孵化率都可达88%以上,盐度低于20或高于40孵化率降低,初孵仔鱼畸形率升高。盐度对仔鱼生长有一定的影响:盐度在25～35时初孵仔鱼存活率最高,盐度32.5时生长最好;盐度30～32.5范围内刚开口仔鱼的存活率较高,生长最快;盐度低于20时变态期仔鱼的存活率与盐度高于25时没有显著差异(P>0.05),但两者体长存在显著差异(P<0.05)。盐度高于40或低于10会延滞胚胎发育速率,孵化时间在盐度低于10时会相对延长。     

环境温度和盐度对墨吉明对虾(Fenneropenaeus merguiensis)胚胎发育的影响

以自然成熟的亲虾为材料,观察并描述了墨吉明对虾(Fenneropenaeus merguiensis)从受精卵到幼体孵化出膜的胚胎发育过程。结果显示,在水温29°C,盐度28的条件下,墨吉明对虾整个胚胎发育过程需要11h左右。水温和盐度对幼体出膜时间和受精卵的孵化率均有显著的影响(P0.05)。孵化水温从32°C下降到23°C时,幼体出膜时间由555min(9.25h)增加到1108min(18.46h)。胚胎发育的最适水温为26—32°C,在此温度范围内,墨吉明对虾的幼体出膜时间与水温呈负相关。胚胎发育的最适盐度25—35,在此范围内,墨吉明对虾的幼体出膜时间和孵化率均无显著差异(P0.05),说明墨吉明对虾的胚胎发育的盐度范围较广。     

鮸状黄姑鱼的早期发育研究

本文对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。绝状黄姑鱼的受精卵为圆球形浮性卵,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18～28C,盐度20～30。仔鱼2日龄稍开口,3～4日龄为混合营养阶段,是仔鱼的主要危险期。     

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。     

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.     

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.     

A Tidal Flow Model for the Gulf of Kachchh, India

A vertically integrated model has been used to study the tidal circulation and currents in the Gulf of Kachchh along the west coast of India. The model is fully nonlinear and uses a semiexplicit finite difference scheme to solve the basic hydrodynamic equations on a staggered grid. The model is forced by prescribing the tides along the open boundary of the model domain. The flow is simulated both with and without the presence of the proposed tidal barrage across the Hansthal Creek in the Gulf of Kachchh. The results show a considerable change in the behavior of the tidal flow in the presence of the barrage.     

利用中国GF-3卫星SAR和HY-2A卫星微波散射计的首次台风联合定量观测

<正>The typhoon,as a mature tropical cyclone that develops in the western part of the North Pacific Ocean with high wind speed and heavy rainfall,is one of the most lethal and costly of natural disasters for the densely populated countries of East Asia.It can be easily detected by space-borne sensors operated at microwave,visible or infrared bands(Liu et al.,2014).Synthetic Aperture Radar(SAR)is     

离子交换—原子吸收光谱法测定海水中痕量铜、铅、锌、镉、铁、锰

本文介绍了用国产D401型螯合树脂分离富集海水中铜、铅、锌、镉、铁、锰等痕量元素,并用原子吸收光谱仪测定其含量的方法。讨论了各元素的分离条件选择及干扰元素的影响,并与溶剂萃取法的结果作了比较。各元素检测的定量下限为:铜0.5μg/L、铅0.1μg/L、锌1.0μg/L、镉0.01μg/L、铁2.0μg/L、锰2.0μg/L。方法精密度在4—8％之间,回收率为90—102％。     

Biogeochemistry of Mangrove Soil Organic Matter: a Comparison BetweenRhizophoraandAvicenniaSoils in South-eastern Brazil

Soil core samples fromRhizophora mangleL. andAvicennia schauerianaStapf & Leech forests from south-eastern Brazil were analysed for their total organic matter content and their sugars, amino acid and amino sugars composition. Organic carbon and nitrogen contents were higher inAvicenniathan inRhizophorasoils. The contribution of sugars and amino acids to the total organic carbon pool was constant with depth inRhizophorasoils whereas inAvicenniasoils it increased. Spectral distribution of sugars and amino acids showed a dominance of Ca-affine monomers, particularly acidic amino acids, and the sugar arabinose. Biogeochemical indicators derived from ratios of individual sugar and amino acid monomers confirm previous studies which showed that organic matter in both soils is mainly of mangrove origin. The results further suggest accumulation of organic matter inRhizophorasoils and a continuing degradation of organic matter inAvicenniasoils. The latter may thus release more nutrients to adjacent ecosystems thanRhizophorasoils.     

A review of orange roughy Hoplostethus atlanticus fisheries,estimation methods,biology and stock structure

Orange roughy Hoplostethus atlanticus are unusual fish. They form dense aggregations that have fuelled lucrative fisheries at great depths (600–1 400 m), especially off Namibia, New Zealand and Australia. They are thought to be very long-lived (>100 years, maturity at 22 – 40 years), and to have exceptionally low natural mortality (M = 0.045–0.064 year^?1) and slow growth rates (K = 0.055–0.070 year^?1). In addition, they spawn large eggs and have low fecundity. These factors combine to make orange roughy highly susceptible to overfishing; most stocks are below 30% of pristine levels. Assessments are obtained from indices of catch rate and trawl, acoustic and egg surveys. Acoustic estimates are the most direct, but are confounded by the species' low target strength (?50 to ?53 dB)–attributable to the wax-filled swim bladder. Extracellular wax esters are stored in abundance and comprise mostly mono-unsaturated fatty acids, with low concentrations of the ω-3 fatty acid family. This unusual composition (resultant from the species' diet) ensures neutral buoyancy. Stock separation has been inferred mainly from biological studies, but genetic studies have also found differences among stocks within New Zealand and Australia. Deep-water habitat may be damaged by trawling operations and may take many years to recover, so in some quarters there is a call for a portion of suitable habitat to be set aside for preservation. Although Namibian orange roughy are shallower, smaller and younger than those in other stocks, the Namibian fishery sustained high catches for only a few years before quotas were reduced, from 12 000 to 1 875 tons. Three management lessons are suggested for developing orange roughy fisheries based on the Namibian experience: (1) imposition of catch limits during exploratory fishing; (2) starting the acoustic surveys earlier in the fishery, if possible; (3) greater reliance on trends in catch rate until a survey series has been established.