卵胎生硬骨鱼褐菖精子发生的超微结构研究

研究了卵胎生硬骨鱼褐菖 Sebastiscus marmoratus精子发生的过程.褐菖的精子发生经历了初级精原细胞、次级精原细胞、初级精母细胞、次级精母细胞、精子细胞等阶段,最终形成精子.在初级精原细胞和次级精原细胞阶段,细胞核中释放出拟染色体.拟染色体分布于精原细胞和前期Ⅰ的初级精母细胞的细胞质中.在前期Ⅰ以后的初级精母细胞、次级精母细胞和精子细胞中,拟染色体已消失.在初级精母细胞阶段,前期Ⅰ至末期Ⅰ的细胞形态变化明显.在前期Ⅰ的偶线期,同源染色体开始配对并形成联会复合体;在粗线期,联会复合体完全形成;在双线期,联会复合体开始解体.     

卵胎生硬骨鱼褐菖You精子发生的超微结构研究

研究了卵胎生硬盘鱼褐草YouSebastiscus marmoratus精子发生的过程。褐菖You的精子发生经历了初级精原细胞、次级精原细胞、初级精母细胞、次级精母细胞、精子细胞等阶段，最终形成精子。在初级精原细胞和次数精原细胞阶段，细胞核中释放出拟染色体。拟染色体分布于精原细胞和前期I的初级精母细胞的细胞质中。在前期I以后的初级精母细胞、次级精母细胞和精子细胞中，拟染色体已消失。在初级精母细胞阶段，前期I至末期I的细胞形态变化明显。在前期I偶线期，同源染色体开始配对并形成联会复合体；在粗线期，联会复合体完成形成；在双线期，联会复合体开始解体。     

我国海域耳鲍(Haliotis asinisne)精子发生的超微结构研究

应用透射电子显微镜技术研究了我国海域耳鲍精子发生的全过程。结果表明,耳鲍精原细胞呈近椭圆形,染色质分布较均匀,线粒体较少;初级精母细胞较大,染色质凝聚成小块状,线粒体增多;次级精母细胞较初级精母细胞小,线粒体较多,部分线粒体发生融合,呈扁囊状。分化早期精细胞染色质凝聚成团块状,多数贴附于核膜内面,胞质中出现前顶体颗粒。分化中期精细胞染色质继续凝聚成较大的团块,线粒体在核的一端融合,形成数量少、体积大的线粒体,前顶体颗粒形成圆形外膜明显的前顶体。分化后期精核由近圆形变成长桶状,核内染色质凝聚并均质化,前顶体泡化发育成顶体,鞭毛形成,精细胞分化成精子。成熟精子为鞭毛型精子,由头部、中段和尾部(鞭毛)3部分组成。     

鲻鱼精子发生的组织学研究

本文报道用组织学方法研究了不同季节鲻鱼的精巢结构和精子发生过程。结果表明，鲻鱼精巢属于叶状结构。根据精子发生的特点，分为5个时期：精原细胞增殖期、初级精母细胞期、次级精母细胞期、精子形成期和精子成熟期。依雄性鲻鱼精子发育和成熟的季节来看，厦门鲻鱼繁殖季节为每年11－12月，系一次性排精类型。文中详细描述各级生精细胞的特征，并讨论了Sertoli细胞在精子发生中的生理作用。     

斗嫁蜮精子发生及雄性性腺组织学研究

采用石蜡切片法,对分布于粤西沿海的斗嫁蜮Cellana grata(Gould)的精子发生和雄性性腺的组织结构进行了研究。斗嫁蜮精子发生经历雄性性细胞的增殖、生长、成熟、变态等阶段.依据精子发生过程中生精细胞形态的变化,精子发生过程可分为精原细胞期、初级精母细胞期、次级精母细胞期、精细胞期和精子形成期等5期。雄性性腺组织主要由滤泡构成,滤泡为生殖细胞增殖、生长、成熟、变态的场所,滤泡腔中的精子经生殖输送管向外输送。显微观察与分析表明:(1)精子发生中,生长期不明显,初级精母细胞较精原细胞小;(2)生精细胞及核的大小随发育逐渐变小,核嗜碱性逐渐增强;(3)精子发生过程中的变态期长,易观察到变态过程中的不同形态的精细胞;(4)成熟精子为鞭毛型,头部短杆状,约0.5×(3~4)μm,尾部细长呈鞭毛状;(5)生长-成熟期的雄性性腺由形态较规则的(多边形)滤泡构成,滤泡界限清晰;(6)雄性滤泡壁由不同发育时期的生精细胞依次排列,较原始的生精细胞呈嗜酸性,靠近滤泡膜分布,而发育晚期的生精细胞呈嗜碱性,渐离滤泡膜分布,成熟精子群集并呈涡旋状分布于腔中;(7)成熟雄性性腺可伸入足部或肝组织中;在肝组织切片中,可观察到结构不同的4个级别的生殖输送管;8)斗嫁蜮雌雄异体,但存在雌雄同体、性转化现象。还对斗嫁蜮精子发生与成熟过程及雌雄同体的有关问题进行了探讨。     

凡纳滨对虾精子发生的超微结构研究

对凡纳滨对虾Litopenaeus vannamei精子发生的过程进行了透射电镜的观察.结果表明,成熟凡纳滨对虾精巢为指状,分16叶.凡纳滨对虾精子发生分为精原细胞、初级精母细胞、次级精母细胞、精子细胞和精子5个时期.染色质经历了从以异染色质为主变为高度凝聚状态,再经解聚为弥散絮状的变化过程.核膜由完整转变为不完整.凡纳滨对虾精子发生过程中仅见线粒体、内质网、核糖体细胞器的参与,未见有典型的高尔基体结构的出现.顶体由内质网囊泡团和线粒体囊泡共同转变而来.精子的棘突以及亚顶体区需在输精管的中后端形成,而非在精巢中形成.纳精囊内精子比储精囊内精子的棘突细长.     

秀丽白虾早期生精细胞结构特征的研究

用透射电镜技术研究了秀丽白虾精子发生过程中早期生精细胞的结构特征。结果表明：精原细胞可分为原始型和发育型两种。原始型精原细胞体积较小，形状不规则，整个细胞呈现极高的电子密度，胞质中线粒体多。早期发育型精原细胞度过非繁殖期后开始生长，内质网、线粒体增多。初级精母细胞胞质中细胞器结构典型，数量达到最多。次级精母细胞期，线粒体开始解体并相互融合；高尔基体、内质网形态不典型，胞质中充满了不规则的囊泡。     

糙海参精子的发生及超微形态结构

为了解糙海参(Holothuria scabra)精子发生的过程及其形态结构,作者于2013年11月~2014年4月每月采集2头海南岛的野生雄性糙海参,取精巢组织固定后分别制作投射电镜、扫描电镜切片和石蜡包埋切片,在电镜和光镜下连续观察。观察结果表明,糙海参精子发生经历了精原细胞、初级精母细胞、次级精母细胞、精细胞和成熟精子5个阶段。精细胞分化过程可分为3个时期,早期:细胞核前端出现前顶体囊;中期:顶体腔内出现围顶体物质;后期:胞质往尾部方向收缩,形成精子中部。糙海参成熟精子全长约60μm,由头部、中部和尾部3部分组成,为典型的鞭毛型精子。精子头部呈球形,精子核中顶体形态为"U"型内陷囊状体,围顶体物质呈"月牙"形,核染色质凝集成团块状。精子中部由一个巨大的线粒体和中心粒复合体融合而成。精子尾部鞭毛横切面为典型的"9+2"微管结构。本研究可为糙海参的繁殖生物学和人工育苗提供理论参考。     

黑鱾精子发生过程中的超微结构变化

利用透射电镜对黑鱾Girella leonina精子发生过程中的各个阶段细胞以及精子的超微结构变化进行了观察.结果表明:1)黑鱾的精子发生过程主要经历了初级精原细胞、次级精原细胞、初级精母细胞、次级精母细胞、精子细胞和精子6个阶段.由精子细胞形成成熟精子还需经过前、中、后期的一系列变态过程.2)各阶段生精细胞以初级精原细胞体积最大,大小约为10.00μm×6.40μm,核大小约为8.801μm×5.80μm,而精子细胞体积最小,大小约为3.20μm×2.60μm,核约为2.80μm×2.50μm;随着生精细胞不断分裂和成熟,细胞的体积逐渐减小,核的位置、核仁、线粒体等发生相应的变化,核内染色质趋于浓缩,电子密度增加,染色程度也逐步加深.3)线粒体是各期细胞内的最主要细胞器之一,在精子发生过程中,它的数量逐渐减少,至成熟精子形成时,核内仅存4个线粒体,但体积却不断增加,内嵴变得长而明显.4)与大多数硬骨鱼类精子特点相似,黑纪的成熟精子不具顶体,核后窝深,精子的鞭毛细长,两旁具侧鳍.尾部为典型的"9+2"型结构.     

文昌鱼的精子发生及释精过程

本文较详细地描述了文昌鱼精巢重新形成过程中,精原细胞的增殖和分化。本工作首次观察到原始精原细胞的形态特点,初级精母细胞的成熟分裂、精子形成以及精子释放的过程。我们的研究结果表明,精原细胞至少经三次有丝分裂后才进入初级精母细胞,但未观察到文昌鱼精巢中有类固醇激素生成细胞。我们还观察到文昌鱼释精的另一途径,即精子先在鳃裂和内柱周围聚集。后经咽至口排出。     

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,     

Evaluation of the Risk of Marine Slope Instability: A Pseudo-3D Approach for Application to Large Areas

This article presents a methodology developed to evaluate the instability of submarine slopes that extend over a large area. Special attention was paid to (1) the complex geometry (bathymetry) and the expanse of the slope, (2) the heterogeneity of the sediment, and (3) the distribution of the pore pressure. The safety factor was considered as a spatially varying quantity. The General Formulation (GLE, Fredlund and Krahn 1977), which fully satisfies equilibrium conditions, was used for evaluating the stability of the marine slope. The submarine slope failure, which occurred on 16 October 1979 during the construction of the new Nice airport, was studied in order to test the developed model. Geotechnical parameters were taken from experimental tests carried out by IFREMER on 19 cores extracted at different depths (from 27 m to 1300 m) (Cochonat, Bourillet, and Savoye, 1993; Mulder et al., 1994). Many scenarios were proposed in order to explain the cause of the Nice slope failure (Habib, 1994). In this article, two of those scenarios were tested. Simulation results are presented and discussed.