UV-B辐射增强对泥鳅红细胞遗传毒理学指标的影响研究     

李美芹  肖慧  唐学玺 《中国海洋大学学报(自然科学版)》2007,37(3):453-456,448

利用红细胞微核和核异常的遗传毒理学方法,研究UV-B辐射增强对泥鳅红细胞核的细胞遗传毒性效应,评价2种毒理学指标在UV-B辐射监测应用中的可行性。结果显示,随着UV-B辐射剂量的加大,泥鳅红细胞的微核细胞率持续上升,表现出明显的剂量-效应关系,微核细胞率与辐射剂量显著正相关。而泥鳅红细胞核异常率随着UV-B辐射剂量的加大无规律性的变化,没有表现出剂量-效应关系,核异常率与辐射剂量无相关性。脱离UV-B辐射处理6 d后泥鳅红细胞的微核细胞率不能够恢复正常的对照水平,而核异常细胞率随着时间的延长,逐渐得以恢复。结果指示泥鳅红细胞微核率是用于UV-B辐射监测的灵敏和可行的细胞遗传毒理学指标,而核异常率不能用于UV-B辐射的监测。  相似文献   

Tectonic core of a sedimentary drift: a potential ridge propagation feature beneath the Blake Outer Ridge     

Dayton Dove  Steven C. Jaume  Erin Beutel 《Marine Geophysical Researches》2007,28(1):1-11

The Blake Outer Ridge is a 480–kilometer long linear sedimentary drift ridge striking perpendicular to the North American coastline. By modeling free-air gravity anomalies we tested for the presence of a crustal feature that may control the location and orientation of the Blake Outer Ridge. Most of our crustal density models that match observed gravity anomalies require an increase in oceanic crustal thickness of 1–3 km on the southwest side of the Blake Outer Ridge relative to the northeast side. Most of these models also require 1–4 km of crustal thinning in zone 20–30 km southwest of the crest of the Blake Outer Ridge. Although these features are consistent with the structure of oceanic fracture zones, the Blake Outer Ridge is not parallel to adjacent known fracture zones. Magnetic anomalies suggest that the ocean crust beneath this feature formed during a period of mid-ocean ridge reorganization, and that the Blake Outer Ridge may be built upon the bathymetric expression of an oblique extensional feature associated with ridge propagation. It is likely that the orientation of this trough acted as a catalyst for sediment deposition with the start of the Western Boundary Undercurrent in the mid-Oligocene.  相似文献   

南极中山站大气气溶胶的化学组成及其来源的判别   总被引：1，自引：1，他引：1  

黄自强  暨卫东  杨绪林  黄荣坦  汤荣坤  于涛  张功勋 《台湾海峡》2003,22(3):334-346

从1998年3月7日至1999年11月23日历时21个月，在南极中山站连续采集89个海洋气溶胶样品，本文提供全部样品的13种化学元素Cu、Pb、Zn、Cd、Fe、Al、Mn、Cr、V、K、Na、Ca、Mg含量的实测值．研究表明中山站气溶胶化学成份的含量具有季节性变化的特征．通过相关分析、因子分析、富集因子等方法判别不同时间段中山站气溶胶化学成份的来源。  相似文献   

Thermohaline Anomalies in the Spring and Early Summer of 2000 in the Gulf of Trieste   总被引：1，自引：0，他引：1  

Massimo Celio  Cinzia Comici  rea Bussani 《Marine Ecology》2002,23(S1):101-110

Abstract. In the framework of the Interreg II Project (July 1998 - June 2001), hydro-logical, chemical and biological data were collected in the Gulf of Trieste.
During spring and summer 2000, some particular thermohaline anomalies were observed in the Gulf of Trieste. Especially in May and June the water body showed: a very strong thermohaline stratification, an increase of advective salt water coming from the south and the presence of sharp pycnoclines. In July the temperature was higher than usual in the whole water column. Moreover, in late May and in June, massive mucilaginous aggregates were observed along the water column and at the surface.
In order to highlight these particular thermohaline features the hydrological data of 16 stations were analysed (Fig. 1). Two stations, in particular, were considered: one offshore (St. AA1, average depth 20 m) and one close to the coast (St. C1, average depth 17 m). For these two stations a best-fit analysis, computed over 11 and 7 years, respectively, was performed on temperature, salinity and density excess data.
Moreover, the hydrological features were compared with the rainfall, air temperature, wind speed data (Istituto Sperimentale Talassografico di Trieste - ISTT) and the Isonzo River's flow rate (Direzione Regionale dell'Ambiente - Regione F. V. G.) collected from January 1998 to December 2000.  相似文献   

南海西南部晚更新世以来元素地球化学特征的古环境意义   总被引：3，自引：0，他引：3  

乔培军  邵磊  杨守业 《海洋地质与第四纪地质》2006,26(4):59-65

对南海西南部近湄公河三角洲中陆坡上的MD01-2392站样品进行的地球化学分析表明,该站的沉积物主要为湄公河带来的陆源碎屑,并且其物源四十万年来没有发生明显变化。分别用元素TiO2、CaO估算出沉积物中陆源碎屑的含量及CaCO3的含量,结果显示CaCO3在间冰期时高,而在冰期时低,表现出“大西洋旋回”的特征。陆源碎屑含量与CaCO3含量相反,显示出南海CaCO3旋回属于稀释旋回。元素的Ti标准化值表明,该站沉积物源区在冰期时化学风化弱,而在间冰期时相对较强,说明间冰期时物源区存在相对温暖湿润的气候环境。  相似文献   

Risk assessment of TBT in the Japanese short-neck clam (Ruditapes philippinarum) of Tokyo Bay using a chemical fate model     

Fumio Horiguchi  Kisaburo Nakata  Naganori Ito  Ken Okawa 《Estuarine, Coastal and Shelf Science》2006,70(4):589

A risk assessment of Tributyltin (TBT) in Tokyo Bay was conducted using the Margin of Exposure (MOE) method at the species level using the Japanese short-neck clam, Ruditapes philippinarum. The assessment endpoint was defined to protect R. philippinarum in Tokyo Bay from TBT (growth effects). A No Observed Effect Concentration (NOEC) for this species with respect to growth reduction induced by TBT was estimated from experimental results published in the scientific literature. Sources of TBT in this study were assumed to be commercial vessels in harbors and navigation routes. Concentrations of TBT in Tokyo Bay were estimated using a three-dimensional hydrodynamic model, an ecosystem model and a chemical fate model. MOEs for this species were estimated for the years 1990, 2000, and 2007. Estimated MOEs for R. philippinarum for 1990, 2000, and 2007 were approximately 1–3, 10, and 100, respectively, indicating a declining temporal trend in the probability of adverse growth effects.A simplified software package called RAMTB was developed by incorporating the chemical fate model and the databases of seasonal flow fields and distributions of organic substances (phytoplankton and detritus) in Tokyo Bay, simulated by the hydrodynamic and ecological model, respectively.  相似文献   

胶州湾海水微表层粘度及其在海-气通量计算中的作用     

张安慧  张正斌  刘莲生  林彩 《中国海洋大学学报(自然科学版)》2002,32(3):456-462

物质海 -气通量计算新建议中将物质海 -气通量计算公式 F=K(CL- b Cg)中的 CL 用CL ( SML ) 代替。本文着重于对公式中质量迁移系数 K的讨论。在测定了海水微表层、次表层水粘度并同时测定了其它一些化学参量基础上 ,得出如下结论 :海水粘度与盐度、碱度有一定相关性 ;微表层与次表层海水的粘度变化小于 3%。因此 ,海水微表层效应影响 K值 ,与海水微表层效应影响物质浓度相比 ,可以不考虑。  相似文献   

A Preliminary Study of Oceanic Bomb Radiocarbon Inventory in the North Pacific during the Last Two Decades     

Yutaka W. Watanabe  Tsuneo Ono  Koh Harada  Masao Fukasawa 《Journal of Oceanography》1999,55(6):705-716

Radiocarbon and total carbonate data were obtained near the 1973 GEOSECS stations in the North Pacific along 30°N and along 175°E between 1993 and 1994. In these stations, we estimated radiocarbon originating from atomic bomb tests using tritium, trichlorofluoromethane and silicate contents. The average penetration depth of bomb radiocarbon during the two decades has deepened from 900 m to 1300 m. Bomb radiocarbon inventories above the average value for the whole North Pacific were found widely in the western subtropical region around 30°N both in the 1970s and 1990s, and its area in the 1990s was broader than that in the 1970s. In most of the North Pacific, while the bomb radiocarbon has decreased above 25.4, the bomb radiocarbon flux below 25.4 was over 1 × 10¹² atom m^-2yr^-1 in the subtropical region around 30°N. In the tropical area south of 20°N, the bomb radiocarbon inventory below 25.4 increased from zero to over 10 × 10¹² atom m^-2 during the last three decades. These distributions suggest that the bomb radiocarbon removed from the surface is currently accumulated with bomb ¹⁴C flux of over 1 × 10¹² atom m^-2yr^-1 below 25.4 in the subtropical region, mainly by advection from the higher latitude, and that part of the accumulated bomb ¹⁴C gradually spread southward with about 30 years.  相似文献   

山东省大中型水库水化学性状研究──几种主要水化因子的变化及其在评价水库鱼产力中的作用     

刘新  李德尚  李静 《中国海洋大学学报(自然科学版)》1994,(4)

本文通过对山东省３８座代表性大、中型水库总氮（ＴＮ）、总磷（ＴＰ）、化学耗氧量、硬度及电导率（λ）五种主要水化因子连续两年（１９８９～１９９０）的调查与研究，探讨了水化因子与水库鱼产力的关系。用反映鲢、鳙生长状况的综合生长指数（ＧＩ）作为水库鱼产力的指标。它与水化因子相关分析表明，总磷是山东省３８座水库鱼产力的主要影响因子。提出ＧＩ与总磷、总氮及电导率等水化因子的逐步回归方程关系非常显著。证明利用水化因子作为水库鱼产力的评价指标是可行的。并指出：同一水库的相同水化因子存在年间差异，其主要原因在于降雨量和水库进水量的不同，鉴于此．同一水库鱼产力也存在年间差异。  相似文献   

Tetraploid induced by physical and chemical methods in Jinjiang oyster(Crassostrea rivularis)   总被引：1，自引：0，他引：1  

Rong Shoubai  Shi Shumei  Mo Qirong  Liu Shaeqiong  Liang Ze  Zhao Xiuzhu  Tong Wangdong  Li Shouwu  Li Yimin 《海洋学报(英文版)》1994,13(2):275-283

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