长毛对虾精子的发生过程

于１９８９－１９９４年每年４－５月,在福建省漳浦县海区采集长毛对虾,以雄虾精巢为材料,应用光镜和电镜技术研究长毛对虾的精子发生情况。结果表明,长毛对虾精子的发生可划分为精原细胞、初级精母细胞、次级精母细胞、精子细胞及精子５个阶段。精原细胞染色质呈团块状分布在核内膜,孢质电子密度低,呈嗜酸性,细胞紧密排列在一起;初级精母细胞核糖体密度高,胞质呈现嗜酸性;次级精母细胞经历减数分裂变化;精子在细胞变态过     

三倍体鲶鱼的性腺发育研究

于１９９６年５月１０月在黑龙江省肇东市东发渔场两次对１９９５年５月用静水压休克法人工诱导并在池塘养殖的三倍体鲶鱼以及对照组二体鲶鱼随机取样进行性腺组织解剖和显微观察。结果表明,雄性三倍体鲶鱼的精巢发育与对照组二倍体鲶鱼基本保持在相同的发育水平上,均能完成从精原细胞、初级精母细胞经减数分裂形成精子细胞的过程,但是,三倍体鱼精 壶腹腔中精子细胞手成熟精子都明显少于二倍体鲶鱼,而且尚能见到少量畸形精子。     

孔鳐雄性生殖系统解剖学与组织学观察

本研究对成年雄性孔鳐(Okamejei kenojei)的生殖系统进行解剖学和组织学观察,结果表明,孔鳐的生殖系统主要由精巢、附睾、输精管、储精囊、间质腺、鳍脚腺和鳍脚组成。其中孔鳐的精巢中的精小囊,按照成熟度依次由中心向小叶外周辐射状排列,其精子发育成熟过程根据精巢支持细胞的位置、精小囊的大小和精小囊中的生精细胞所处的状态可划分为7个时期:精巢支持细胞未迁移期、精巢支持细胞迁移期、精巢支持细胞定植早期、精巢支持细胞定植晚期、精子变形期、精子迁移期、精子聚拢期。变态成熟的精子最终每59~64根精子组成精子束进入附睾。精子束在附睾中经历“游离-聚拢-游离”3个过程后,最终储存在储精囊中。鳍脚是孔鳐的外生殖器,主要有鳍扇、扇盾等结构组成,它与储精囊相连,是将精液输送至体外的器官。     

细角螺的生殖系统组织学研究

应用组织切片技术对细角螺Hemifusus ternatanus性腺发育及生殖细胞发生进行研究.结果表明,细角螺为雌雄异体.精巢为多分枝管状腺,由生精小管和输精小管组成;精巢发育可分为4个时期,即增殖期、生长期、成熟期和休止期.精原细胞紧靠生精小管的基膜,由基膜向管腔依次排列着不同发育时期的生精细胞:初级精母细胞、次级精母细胞、精子细胞和精子.精巢发育显示为多次性成熟、多次排精的方式.根据细胞的大小和所含卵黄颗粒的大小,卵母细胞发育过程分为繁殖期、生长期和成熟期;根据滤泡大小、结构、内含物的变化将卵巢的发育分成5个时期:增殖期、生长期、成熟期、排放期和休止期.最后对细角螺特殊个体的出现进行初步讨论.     

企鹅珍珠贝Dmrt2基因的克隆及表达分析

本研究利用RACE-PCR技术获得企鹅珍珠贝(Pteria penguin)一个Dmrt2基因cDNA的全长序列,通过荧光定量PCR分析Dmrt2基因在各组织中的表达特征,以及在早期卵巢、成熟期卵巢、早期精巢、成熟期精巢和排放期精巢中的表达变化。结果表明,Dmrt2基因全长1 257bp,其中开放阅读框(open reading frame,ORF)为951 bp,编码316个氨基酸,5′非编码区(untranslated region,UTR)为52 bp,3′UTR为254 bp,第20位到第73位氨基酸为DM结构域。预测其分子质量为36.61ku,等电点为9.80。氨基酸序列比对显示该企鹅珍珠贝Dmrt2基因与黑蝶真珠蛤(Pinctada margaritifera)和马氏珠母贝(Pinctada martensii)的Dmrt2基因同源性(identity)最高,分别为46.0%和45.7%。其中在DM结构域高度同源。荧光定量PCR分析组织表达特征显示,Dmrt2在企鹅珍珠贝的外套膜、鳃、消化盲囊、足、精巢和卵巢均有表达,其中在精巢中表达量最高(P0.05),足为其次,在闭壳肌中没有检测到Dmrt2表达。对性腺发育不同时期的表达量分析发现,Dmrt2在发育早期和成熟期卵巢中表达量都很低,在发育早期精巢中表达量较高,在成熟期精巢检测到最大表达量(P0.05),到精巢排放期表达显著下降,推测Dmrt2可能与企鹅珍珠贝精巢的发育有关,可能参与了企鹅珍珠贝雄性性别分化和性腺发育这一生理过程。     

鲻鱼精子发生和形成的超微结构研究

用透射电子显微镜研究了鲻鱼精子发生和精子形成过程.结果表明,鲻鱼早期精巢有两种类型的精原细胞,即A型和B型,在B型精原细胞可见核旁有类核周体(nuage),可视为精原细胞向初级精母细胞发育分化的一个重要标志.初级精母细胞减数分裂早期同源染色体配对明显可见,精子细胞之间存在着间桥联系.鲻鱼成熟精子的特点是细胞核呈马蹄形,核凹较浅,核前端无顶体,核内染色质呈粗颗粒状,核膜与质膜之间有较大的空隙.中段较短,近端中心粒和远端中心粒互相垂直.精子尾部细长,横切面为典型的“9+2”双联微管结构,两侧有侧鳍     

半滑舌鳎精子发生的组织学研究

本文应用组织学方法对半滑舌鳎雄鱼精巢结构和精子发生过程进行了详细地研究．观察结果表明,它的精巢结构特点是随着精巢的发育可见它的精巢外面有一条管状贮精囊与输出管相连,在精巢发育成熟过程中,贮精囊中逐渐充满精子,这个特点有助于了解半滑舌鳎的受精生物学的复杂性．另外,从半滑舌鳎精子发生过程分析,它的精巢属于小叶型,精巢发育分为6期．精子发生经历精原细胞、精母细胞、精子细胞及精子．最后,文中还讨论了半滑舌鳎精巢中非生殖细胞（间质细胞和Sertoli细胞）的分布及其可能的生理作用．     

闽南近海尖头斜齿鲨的精巢结构及精子发育

尖头斜齿鲨是闽南近海的常见板鳃类。本文研究了其精巢的结构及精子的发育。尖头斜齿鲨的精巢属于放射型,其基本单位是圆形或圆形的壶腹,生精区位于精巢的一侧,生精壶腹由此区向精巢对壁发育,每一壶腹中的细胞处于同一发育时期。在精巢靠近成熟壶腹一侧有精子输出管。精子的发生可分为３个时期精原细胞增殖期、精母细胞期、精子形成期。尖头斜齿鲨的精子细长、呈流线形,头部钝圆,其形成期约为７个月。粗巢的结构随体长和季节的     

线纹海马(Hippocampus erectus)性腺特异性结构与生殖细胞发育特征研究 *

海马属(Hippocampus)鱼类具有独特的雄性育儿繁殖方式, 其卵巢和精巢结构也极其独特。本研究系统阐明了线纹海马(Hippocampus erectus)的性腺及生殖细胞的发育特征, 根据组织学结构和细胞形态学变化特征, 将线纹海马的精巢和卵巢发育过程均分为6个时期。其中, 卵巢发育方式为不同步成熟型, Ⅰ期卵巢只包含第Ⅰ时相卵母细胞, 包括卵原细胞和早期初级卵母细胞(d<20μm); Ⅱ期卵巢开始出现第Ⅱ时相卵母细胞(d=20~140μm); Ⅲ期卵巢卵母细胞数量显著增多, 体积增大, 并开始出现第Ⅲ时相卵母细胞(d=140~260μm), 此时细胞内开始出现皮质小泡、卵黄颗粒和卵黄膜; Ⅳ期卵巢开始出现第 Ⅳ时相卵母细胞(d=260~1100μm), 卵黄颗粒充满整个细胞质, 形成过渡期的卵黄球; Ⅴ期卵巢出现大量第Ⅴ时相成熟卵母细胞(d=1100~2000μm), 细胞内形成流动性卵黄囊; Ⅵ期卵巢为排卵不久后的卵巢, 卵母细胞数量显著减少。线纹海马精巢属于非限制型小叶精巢, Ⅰ期精巢主要含精原细胞, 核大, 含一到多个核仁; Ⅱ期精巢开始形成精小囊, 囊内出现初级精母细胞; Ⅲ期精巢呈乳白色, 开始出现次级精母细胞; Ⅳ期精巢体积较 Ⅲ期时显著增大, 开始出现精子细胞, 并逐渐移向中央生精腔; Ⅴ期精巢内含大量的成熟精子, 随时准备释放。精子释放后精巢进入Ⅵ期, 残留少量精细胞在生精腔中。组织化学反应结果显示, 氨基酸、蛋白质和脂肪的信号在卵母细胞的细胞质、卵黄囊中呈阳性, 且随着卵母细胞的发育而增强。本研究结果为进一步探索海马属鱼类雄性繁殖策略提供了重要的基础数据。     

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.     

Size-fractionated uranium isotopes in surface waters in the Jiulong Estuary in China

Surface water was collected from the Jiulong Estuary for determination of activity concentrations of uranium isotopes in different size fractions, namely, greater than 53, 10 -53, 2 - 10, 0.4 -2 μm, 10 000 u -0.4 μm and less than 10 000 u fractions by microfihration and cross-flow uhrafiltration technologies. Results indicated that most of the dissolved uranium （ 〈 0.4 μm） exis- ted in the low molecular mass fraction （ 〈 10 000 u）, and the colloidal uranium-238 （10 000 u -0.4 μm） only contributed less than 1% of the dissolved uranium-238. The fractions of colloidal uranium in the dissolved phases decreased with the increasing sa- linity. A positive linear relationship between uranium-238 activities and salinities was observed for the dissolved, colloidal and low molecular mass fractions, indicating a conservative behavior of uranium in the Jiulong Estuary. In the particulate phases （ 〉 0.4 μm）, the partitioning of uranium isotopes among different size fractions was controlled by the partitioning of particle concentrations. In the regions with salinities below 20, the partitioning of uranium-238 among different size fractions was as follows： 10 - 53 μm 〉 2 - 10 μm 〉 0.4 - 2 μm greater than above 53 μm. However, the order at the offshore station with salinities above 30 changed as follows ： 0.4 - 2 μm 〉 10 - 53 μm 〉 2 - 10 μm greater than above 53 μm. The fraction of the 0.4 - 2 μm particles increased at the offshore station, suggesting the increased contribution of the authigenic uranium. The activity ratio of uranium-234 to uranium-238 in the dissolved phases, including the low molecular mass fraction and the colloidal fraction, was larger than unity, showing the occurrence of excess uranium-234. In contrast, the activity ratio of uranium-234 to uranium-238 in all size fractions of the particulate phase was close to the equilibrium value （1.0）. The observed different values of the activity ratio of uranium-234 to uranium-238 in the dissolved phase and the partic     

夏季珠江口沉积物中营养盐剖面分布和界面交换通量

通过对夏季珠江口区域沉积物间隙水营养盐剖面分析,调查了营养盐含量分布和特征,探讨了有机物的降解特性、营养盐的底部通量估算和作用.结果表明,珠江口沉积物间隙水中营养盐以高含量铵盐为主要的存在形式,沉积物中有机物的降解反应主要在厌氧状态下进行,底部水体铵盐的增加来源于底部沉积物有机质的降解释放,而且对水体的营养盐循环有较大的贡献.     

Recent progress in submarine geosciences in China

In China submarine geosciences represents a newly established discipline of oceanography, focusing on the oceanic lithosphere, and its interface with the hydrosphere and biosphere. Recently, supported by the National High Technology Research and Development Program and other high-tech development projects, significant progress has been made in the development of advanced technologies and equipment. This en- ables the scientists in China to carry out explorations of the international seabed area in the Pacific Ocean and on the Southwest Indian Ridge. In addition, they have been active in the research activities associated the mid-ocean ridges and western Pacific marginal seas. It is anticipated that this research field will continue to be highly fruitful in the near future.     

湄洲湾夏季的初级生产力

湄洲湾１９９２年夏季的叶绿素ａ，三磷酸腺苷，碳比积累速率，初级生产力的变化范围和均值分别为０．４５－４．７２，１．４９ｍｇ／ｍ＾３；０．１２－１．０７，０．３１μｇ／ｄｍ＾３；０．０６－０．５８，０．３４ｄ＾－１；０．０７－０．３４，０．２１ｍ／（ｍ＾２．ｄ）。叶绿素ａ与三磷酸腺苷之间。初级生产力与碳比积累速率之间均呈正相关关系。叶绿素ａ三磷本能腺苷的比值为４．８，湄洲湾夏季浮游植物的生长受氮不足     

Seasonality in nutrient concentrations in Galveston Bay

In order to investigate factors controlling nutrient cycling in the shallow and turbid coastal ecosystem of Galveston Bay, data from: (1) the Texas Water Commission (TWC) database 1980–1989, and (2) salinity transects in 1989 and 1993 are presented and analyzed. Statistical regression and time-series analysis were carried out on data acquired by TWC between 1980 and 1989, in an attempt to establish seasonally of nutrient and chlorophyll-a (chl.-a.) concentrations in the bay and to determine factors which regulate these concentrations.A strong seasonality was found for phosphorus and chl.-a. in the upper and mid-bay stations. A recurring maximum for phosphate occurred in September and a chl.-a. maximum occurred regularly in March–April. It is hypothesized that benthic regeneration of phosphorus at the end of summer is responsible for the phosphate maximum. The inverse correlation of the partition coefficient (K_d) for phosphate with the concentration of suspended particulate matter (SPM), coupled to a strong enrichment of phosphate in suspended particles at low SPM concentrations, indicates additional control by geochemical and physical processes such as particle sorting and/or particle-colloid interactions. Nitrate is inversely correlated with salinity at the upper and mid-bay stations, indicating the Trinity River is a major source.Nutrient concentrations in the lower bay (East and West Bay stations) are considerably lower and less predictable, as they are not correlated with salinity or temperature. Data from the 1989 and 1993 transects confirm the yearly maximum in phosphate concentration in late summer months, with peak concentrations in the upper Trinity Bay. It is concluded that despite possible phosphate buffering by physical and geochemical mechanisms, relatively large concentration maxima recur regularly every year during the summer, possibly caused by a benthic source of phosphate.     

Mesozooplankton in the Arctic Ocean in summer

The biomass, species and chemical composition of the mesozooplankton and their impact on lower food levels were estimated along a transect across the Arctic Ocean. Mesozooplankton biomass in the upper 200 m of the water column was significantly higher (19–42 mg DW m^-3) than has previously been reported for the Arctic Ocean, and it reached a maximum at ca. 87°N in the Amundsen Basin. The lowest values were recorded in the Chukchi Sea and Nansen Basin, where ice cover was lower (50–80%) than in the central Arctic Ocean. In the deeper strata (200–500 m) of the Canadian and Eurasian Basins, the biomass was always much lower (4.35–16.44 mg DW m^-3). The C/N (g/g) ratio for the mesozooplankton population was high (6.5–8.5) but within the documented range. These high values (when compared to 4.5 at lower latitudes) may be explained by the high lipid content. Mesozooplankton accounted for approximately 40% of the total particulate organic carbon in the upper 100 m of the water column. Mesozooplankton species composition was homogeneous along the transect, consisting mainly of copepods (70–90% of the total number). It was dominated by four large copepod species (Calanus hyperboreus, C. glacialis, C. finmarchicus and Metridia longa), which together accounted for more than 80% of the total biomass. According to measurements of gut pigment and gut turnover rates, the mesozooplankton on average ingested between 6 and 30% of their body carbon per day as phytoplankton. Microzooplankton may have provided an additional source of energy for the mesozooplankton community. These data emphasize the importance of mesozooplankton in the arctic food web and reinforce the idea that the Arctic Ocean should no longer be considered to be a “biological desert”.     

微生物对土壤中镉的固定作用

镉是一种重要的环境污染物,它通过沉淀作用、磷酸肥料的使用等排放到农田中。由于镉具有较高的蒸气压,因此,人为排放的镉大部分来自工业的挥发。排放到大气中的镉通过沉积作用转移到植物、土壤及水体中。在污染的土壤中镉被植物吸收并且在植物体内富集,通过这种机制镉进入了食物链。镉是一种诱导有机体突变的物质,能对动物和人类产生有害影响,并能够抑制植物的光合作用,因此,环境中镉的存在一直被人们所关注。     

海水双壳类受精生物学研究进展

1 研究概况,在海水双壳类中开展的大量受精生物学研究表明,绝大部分的海水双壳类为卵生型,雌雄配子被排放到海水中完成受精。排放的卵子处于第一次减数分裂前期(生发泡期)或中期。精子入卵后,受精卵恢复减数分裂,先后排放出两个极体,形成雌雄原核并最终启动卵裂。     

海水黄色物质研究进展

叙述了海水黄色物质的研究历史、研究动态和研究方法,并且指出黄色物质荧光性质研究的重要性.海水中黄色物质在海洋生态系统、光学遥感和海洋碳循环等方面具有广阔的应用前景.