中国鱼类名录ⅩⅢ——鲽形目、纯形目、海蛾鱼目、鮟鱇目

鲽形目3亚目8科51属142种。鲀形目2亚目9科57属143种。海蛾鱼目1科2属3种，鮟鱇目3亚目11科23属41种。     

中国鱼类名录Ⅹ Ⅲ--鲽形目、鲀形目、海蛾鱼目、鮟鱇目

鲽形目3亚目8科51属142种.鲀形目2亚目9科57属143种.海蛾鱼目1科2属3种,鮟鱇目3亚目11科23属41种.     

中国鱼类名录Ⅹ——鲈亚目(部分)

鲈亚目 3 总科 53 科 239 属 840 种。     

香鱼(Plecoglossus altivelis)精子的超微结构及其与鲤形目及鲑形目其他鱼类精子结构的比较研究

为了解香鱼(Plecoglossus altivelis)精子的形态结构特点,采用扫描和透射电镜技术观察了香鱼精子的超微结构,并与鲤形目及鲑形目其他鱼类精子结构进行了比较。结果表明,香鱼精子由头部、中段和尾部组成,全长约23.5μm。头部呈弹头形,由细胞核外包质膜构成,长约1.8μm、宽约0.8μm;细胞核从后端中央向前深凹至核的近前端,形成植入窝,使核呈倒U字形,核的前端无顶体;植入窝内有中心粒复合体及小段起始的鞭毛,中心粒复合体由近端中心粒和远端中心粒(基体)组成,两者之间夹角约135o。中段为"半袖套"结构,长约0.5μm,其内部为一较大的"半套筒"形线粒体。鞭毛起始于远端中心粒,由轴丝及外包轴丝的质膜组成,轴丝为典型的"9+2"微管结构;鞭毛两侧有质膜向外突起形成侧鳍。研究显示,香鱼精子与典型的鲤形目(Cypriniformes)鱼类精子卵圆形或圆球形头部及细胞核、不对称的袖套及尾部鞭毛无侧鳍等结构特征不同,也与鲑形目(Salmoniformes)鱼类精子卵圆形或椭圆形头部及马蹄形或浅U形细胞核、两中心粒相互平行或垂直、袖套结构完整等结构特征不同。香鱼精子结构具有种的特异性。     

中国鱼类名录X--鲈亚目(部分)

鲈亚目3总科53科239属840种.     

中国鱼类名录Ⅸ——Yu亚目、马Ba亚目、鲈亚目（部分）

Yu亚目1科1属11种，马Ba亚目1科2属5种。鲈亚目（部分）记述23科。     

中国海平面上升60毫米

中国沿海海平面多年来一直呈波动上升趋势。2003年，中国国家海洋局公布的《2003年中国海平面公报》指出：中国沿海平均海平面比常年平均海平面高60毫米。其中，黄海海平面比常年平均海平面高73毫米，东海、南海次之，分别为66和63毫米，渤海为27毫米。     

中国鱼类名录Ⅺ--隆头鱼亚目、尤鰧鱼亚目、绵鳚亚目、玉筋鱼亚目

隆头鱼亚目5科63属316种，鰧鱼亚目8科19属53种，绵鳚亚日3科7属8种，玉筋鱼亚目1科3属3种。     

中国南海、东海及黄海海域海气二氧化碳通量与生产力的物理生物地球化学模拟研究

Marginal seas play important roles in regulating the global carbon budget, but there are great uncertainties in estimating carbon sources and sinks in the continental margins. A Pacific basin-wide physical-biogeochemical model is used to estimate primary productivity and air-sea CO_2 flux in the South China Sea(SCS), the East China Sea(ECS), and the Yellow Sea(YS). The model is forced with daily air-sea fluxes which are derived from the NCEP2 reanalysis from 1982 to 2005. During the period of time, the modeled monthly-mean air-sea CO_2 fluxes in these three marginal seas altered from an atmospheric carbon sink in winter to a source in summer. On annualmean basis, the SCS acts as a source of carbon to the atmosphere(16 Tg/a, calculated by carbon, released to the atmosphere), and the ECS and the YS are sinks for atmospheric carbon(–6.73 Tg/a and –5.23 Tg/a, respectively,absorbed by the ocean). The model results suggest that the sea surface temperature(SST) controls the spatial and temporal variations of the oceanic pCO_2 in the SCS and ECS, and biological removal of carbon plays a compensating role in modulating the variability of the oceanic pCO_2 and determining its strength in each sea,especially in the ECS and the SCS. However, the biological activity is the dominating factor for controlling the oceanic pCO_2 in the YS. The modeled depth-integrated primary production(IPP) over the euphotic zone shows seasonal variation features with annual-mean values of 293, 297, and 315 mg/(m~2·d) in the SCS, the ECS, and the YS, respectively. The model-integrated annual-mean new production(uptake of nitrate) values, as in carbon units, are 103, 109, and 139 mg/(m~2·d), which yield the f-ratios of 0.35, 0.37, and 0.45 for the SCS, the ECS, and the YS, respectively. Compared to the productivity in the ECS and the YS, the seasonal variation of biological productivity in the SCS is rather weak. The atmospheric pCO_2 increases from 1982 to 2005, which is consistent with the anthropogenic CO_2 input to the atmosphere. The oceanic pCO_2 increases in responses to the atmospheric pCO_2 that drives air-sea CO_2 flux in the model. The modeled increase rate of oceanic pCO_2 is0.91 μatm/a in the YS, 1.04 μatm/a in the ECS, and 1.66 μatm/a in the SCS, respectively.     

南黄海和中国东海中挥发性卤代烃的分布与海气通量

Distributions and sea-to-air fluxes of five kinds of volatile halocarbons(VHCs) were studied in the southern Yellow Sea(SYS) and the East China Sea(ECS) in November 2007. The results showed that the concentrations of 1,1,1-trichloroethane(C2H3Cl3), 1,1-dichloroethene(C2H2Cl2), 1,1,2-trichloroethene(C2HCl3), trichloromethane(CHCl3) and tetrachloromethane(CCl4) in the surface water were 0.31–4.81, 2.75–21.3, 1.21–17.1, 5.02–233 and 0.045–4.47 pmol/L, respectively, with the average values of 1.89, 12.20, 6.93, 60.90 and 0.33 pmol/L. On the whole, the horizontal distributions of C2H3Cl3, C2H2Cl2 and CCl4 were affected mainly by anthropogenic activities, while C2HCl3 and CHCl3 were influenced by biological factors as well as anthropogenic activities. In the study area, the concentrations of VHCs(except C2HCl3) exhibited a decreasing trend from inshore to offshore sites, with the higher values occurring in the coastal waters. The sea-to-air fluxes of C2H3Cl3, C2HCl3, CHCl3 and CCl4 were calculated to be-56.00–(-5.68),-7.31–123.42, 148.00–1 309.31 and-83.32–(-1.53) nmol/(m2·d), respectively, with the average values of-6.77, 17.14, 183.38 and-21.27 nmol/(m2·d). Our data showed that the SYS and ECS in autumn was a sink for C2H3Cl3 and CCl4, while it was a source for C2HCl3 and CHCl3 in the atmosphere.     

中国鱼类名录Ⅸ--魣亚目、马鲅亚目、鲈亚目(部分)

魣亚目1科1属11种,马鲅亚目1科2属5种.鲈亚目(部分)记述23科.     

中国鱼类名录Ⅻ——鳚亚目、Xian亚目、喉盘鱼亚目、鰕虎鱼亚目、微体鱼亚目、刺尾鱼亚目、带鱼亚目、鲭亚目、鲳亚目、金枪鱼亚目、攀鲈亚目、刺鳅亚目

鳚亚目4科33属95种，鰕虎鱼亚目5科98属259种，刺尾鱼亚目5科11属65种，鲈形目19亚目104科535属1799种。     

中国鱼类名录Ⅻ--鳚亚目、(鱼衔)亚目、喉盘鱼亚目、鰕虎鱼亚目、微体鱼亚目、刺尾鱼亚目、带鱼亚目、鲭亚目、鲳亚目、金枪鱼亚目、攀鲈亚目、刺鳅亚目

鳚亚目 4 科 33 属 95 种，鰕虎鱼亚目 5 科 98 属 259 种，刺尾鱼亚目 5 科 11 属 65 种，鲈形目 19亚目 104 科 535 属 1799 种。