锯缘青蟹染色体核型的分析研究

十足目甲壳动物染色体的研究,从上个世纪Carnoy1885年开始,至今已有100多年的历史。截止1987年,共报道了26科68种十足目动物的二倍体染色体数目,之后,又报道了18种,其中短尾类37种,占半数弱。这些种的二倍体染色体数目从64到376不等（平均125）,且每个染色体很小,一般不超过4μm。染色体数目多且每个染色体小是十足目动物染     

锯缘青蟹胸神经团的免疫细胞化学定位研究

采用兔抗哺乳类抗血清，应用链霉菌抗生物素蛋白-过氧化物酶免疫细胞化学技术，研究了锯缘青蟹（Scylla serrata）胸神经团中5-羟色胺（5-HT）、胰高血糖素（Glu）和神经肽Y（NPY）的分布。其分布的主要特征为：5-HT免疫阳性细胞在每对步足神经节都呈对称排列；GLU免疫阳性最强，胸神经节的阳性细胞排列成两条环境胸动脉孔分布的细胞带，神经髓质中免疫阳性物质呈斑块状分布；NPY阳性细胞主要分布于食道下神经节。这3种免疫阳性物质的特定分布模式可为腹神经链的系统演化和参与神经活动提供形态学证据。     

东方扁虾卵巢和滤泡结构的研究

卵巢包括4种形态的组分:(1)卵巢壁,(2)生殖上皮,(3)卵母细胞(早期卵巢还包括卵原细胞)一滤泡细胞层,(4)卵巢壁内突.卵巢壁及壁内突均含有血管、血窦、肌细胞等成分,卵巢壁内突延伸至每个滤泡的外层基膜处.滤泡由内至外由卵母细胞、卵周隙、滤泡细胞及基膜等4部分组成.卵母细胞膜表面向卵周隙内伸出许多微绒毛,并具有许多微吞饮凹.随着滤泡的发育,卵周隙内含物电子密度越来越大,成熟滤泡的卵周隙内含物演变为卵壳.卵壳由两部分构成:外层较薄,而内层较厚且含电子致密的颗粒物质.滤泡细胞一般为单层,具较强的合成活性,其合成产物系卵周隙内含物的一部分.东方扁虾卵巢和滤泡的结构特征表明外源性(卵母细胞外及卵巢外)的卵黄合成在卵黄发生上起重要的作用.     

饵料对锯缘青蟹大眼幼体生长发育的影响

以不同比例的轮虫和卤虫无节幼体搭配成各种饵料组合，分别喂养不同发育期的锯缘青蟹幼体，重点研究大眼幼体的存活、生长发育、变态和干重及化学元素(C、H、N)含量的情况.结果表明饵料搭配得当，适时适量的投喂，其幼体的生长发育和变态都正常，并可获得较高的存活率，若饵料搭配不当不仅会导致幼体出现高死亡率，而且还能诱发发育期变化的现象；不同饵料搭配对大眼幼体干重及化学元素(C、H、N)含量的影响很显著，相差60％～70％，约一个发育期，而这差异可以通过该期幼体投喂足量卤虫无节幼体来加以弥补，大眼幼体的C、H、N占干重的百分比仅次于溞V，这表明青蟹幼体在这两次变态前需在体内积累高比例的有机营养物质来保证变态的顺利进行.     

锯缘青蟹幼体饵料蛋白质的营养价值评价

本文分析测定了锯缘青蟹幼体从刚孵化至大眼幼体各发育阶段及其饵料轮虫和卤虫无节幼体的氨基酸组成，并使用必需氨基酸指数(EAAI)来评价饵料蛋白质的质量.结果表明，青蟹各期幼体的氨基酸组成基本趋于一致，且与饵料转换不存在明显的相关性.对于各期幼体，饵料轮虫和卤虫无节幼体的必需氨基酸指数均大于90，可以认为，轮虫和卤虫无节幼体能够满足锯缘青蟹幼体对饵料中必需氨基酸的营养需求.     

海洋浮游甲壳类分子系统学研究进展

回顾海洋浮游甲壳类系统学研究的基础上，综述了生化水平和DNA(mtDNA和核DNA)水平的分子系统学研究现状。分子标记中DNA序列分析最为常用，其次是RFLP和RAPD分析，mtDNA主要应用于分类学、群体遗传学、种间分子进化和系统发育重建研究，而核DNA则应用于科以上较高阶元的系统发育和种内、近缘种间的遗传结构和遗传分化研究。最后对存在的问题和应用前景进行了展望。     

锯缘青蟹视神经节免疫细胞化学研究

采用兔抗哺乳类血清,应用链霉菌抗生物素蛋白-过氧化物酶免疫细胞化学技术,观察了锯缘青蟹视神经节中5羟色胺、胰高血糖素、神经肽Y和生长抑素免疫阳性细胞和神经纤维的形态和分布,结果发现,视神经节的4个神经髓均有5羟色胺免疫阳性细胞,除X器检出1个较大型阳性细胞外,其余均为小型细胞.视外髓、视内髓和视端髓都具有胰高血糖素免疫阳性细胞,视端髓的神经髓质阳性染色深,X器中阳性细胞成群分布,窦腺免疫阳性反应强.神经肽Y免疫阳性细胞在视神经层和视外髓为小型阳性细胞,在视内髓和视端髓检出较大型阳性细胞,另有小型阳性细胞散布于X器中.生长抑素免疫阳性细胞分布于4个神经髓,数量少.4种免疫阳性物的特异性分布模式,可为其不同的神经生理作用提供形态学证据.     

The progress in the study of Arctic pack ice ecology

The sea ice community plays an important role in the Arctic marine ecosystem. Because of the predicted environmental changes in the Arctic environment and specifically related to sea ice, the Arctic pack ice biota has received more attention in recent years using modem ice-breaking research vessels. Studies show that the Arctic pack ice contains a diverse biota and besides ice algae, the bacterial and protozoan biomasses can be high. Surprisingly high primary production values were observed in the pack ice of the central Arctic Ocean. Occasionally biomass maximum were discovered in the interior of the ice floes, a habitat that had been ignored in most Arctic studies. Many scientific questions, which deserve special attention, remained unsolved due to logistic limitations and the sea ice characteristics. Little is know about the pack ice community in the central Arctic Ocean. Almost no data exists from the pack ice zone for the winter season. Concerning the abundance of bacteria and protozoa, more studies are needed to understand the microbial network within the ice and its role in material and energy flows. The response of the sea ice biota to global change will impact the entire Arctic marine ecosystem and a long-term monitoring program is needed. The techniques, that are applied to study the sea ice biota and the sea ice ecology, should be improved.     

Abundance, biomass and composition of spring ice algal and phytoplankton communities of the Laptev Sea （Arctic）

Abundance,biomass and composition of the ice algal and phytoplank-ton communities were investigated in the southeastern Laptev Sea in spring 1999.Diatoms dominated the algal communities and pennate diatoms dominated the dia-tom population.12 dominant algal species occurred within sea ice and underlyingwater column,including Fragilariopsis oceanica,F.cylindrus,Nitzschiafrigida,N.promare,Achnanthes taeniata,Nitzschia neofrigida,Naviculapelagica,N.vanhoef fenii,N.septentrionalis,Melosira arctica,Clindrothecaclosterium and Pyrarnimonas sp.The algal abundance of bottom 10 cm sea icevaried between 14.6 and 1562.2×10~4 ceils l~(-1)with an average of 639.0×10~4cells l~(-1),and the algal biomass ranged from 7.89 to 2093.5μg C l~(-1)with an av-erage of 886.9μg C l~(-1),which were generally one order of magnitude higherthan those of sub-bottom ice and two orders of magnitude higher than those ofunderlying surface water.The integrated algal abundance and biomass of lower-most 20 cm ice column were averagely 7.7 and 12.2 times as those of upper 20 mwater column,respectively,suggesting that the ice algae might play an importantrole in maintaining the coastal marine ecosystem before the thawing of sea ice.Icealgae influenced the phytoplankton community of the underlying water column.However,the“seeding”of ice algae for phytoplankton bloom was negligible be-cause of the iow phytoplankton biomass within the underlying water column.     

快速升温后极地甲藻Polarella glacialis的生理响应

Polarella glacialis最早发现于南极固定冰和北冰洋水层,最近在温带海域也发现其相关基因。专抗甲藻的Rubisco、PCNA抗体在该藻细胞内各检测到~53 kDa和~55 kDa的特异性条带。对该藻的梯度温度培养实验显示,4℃生长的P. glacialis细胞密度为1.1×105 cells/ml时仍能继续增殖,一天中藻细胞内Rubisco的表达量基本保持恒定,PCNA的表达量峰值与%S峰值相对应,当温度迅速上升至15、20℃时,藻株处于胁迫状态,细胞密度迅速减少,正常的细胞周期被干扰,大多数细胞分裂活动不活跃或停止分裂,Rubisco、PCNA的表达量大幅减少甚至消失,昼夜表达特征改变,其中20℃对藻株的胁迫作用更加显著。15℃培养下的P. glacialis细胞密度并不立即减少,细胞周期与两种指示蛋白表达特征显示仍有部分细胞完成分裂。本研究为该藻的相关基因在温带水域的出现提供了可能的解释,并推测在相对长期渐进的极地增温过程中,P. glacialis可能继续存在。