不同营养状态下3种沉水植物的生理响应

通过静态模拟实验,比较研究了不同营养水平(贫营养、中营养、富营养、重富营养)培养的苦草(Vallisneria spirolis)、伊乐藻(Elodea nattalii)和金鱼藻(Ceracophyllurn dernersurn)的过氧化物酶(POD)、超氧化物歧化酶(SOD)、过氧化氢酶(CAT)活性及丙二醛含量变化.研究发现,3种沉水植物的过氧化物酶、超氧化物歧化酶、过氧化氢酶活性及丙二醛含量均随N,P浓度的增加而上升;3种沉水植物的丙二醛含量均随时间延长而上升,POD活性随时间变化呈先上升后下降的趋势;苦草和伊乐藻的SOD活性及伊乐藻CAT活性随时间延伸呈下降的趋势;金鱼藻的CAT活性随时间延伸呈上升的趋势.     

水体Hg^2＋对中华绒螯蟹（Eriocheir sinensis）血淋巴抗氧化酶活力和丙二醛含量的影响

采用单因子实验设计方法,进行了水体汞（Hg^2＋）在不同暴露时间对中华绒螯蟹血淋巴超氧化物歧化酶（SOD）、谷胱甘肽过氧化物酶（GPX）和过氧化氢酶（CAT）活力以及脂质过氧化产物丙二醛（MDA）含量的影响研究。结果表明,较低浓度Hg^2＋（0．01和0．05mg／L）处理组中华绒螯蟹血淋巴SOD、GPX、CAT活力在...     

氟苯尼考对菲律宾蛤仔抗氧化酶活性的影响

通过室内模拟实验研究了氟苯尼考对菲律宾蛤仔体内超氧化物歧化酶(SOD),过氧化氢酶(CAT),过氧化物酶(POD)和谷胱甘肽还原酶(GR)活性的影响.结果表明,培养7 d后,在氟苯尼考的作用下,菲律宾蛤仔内脏团和肌肉组织的SOD,CAT,POD和GR的活性都发生了变化.低质量比氟苯尼考对SOD,CAT和POD酶活性具有诱导作用,而在高质量比条件下则表现为抑制作用.不同质量比的氟苯尼考对菲律宾蛤仔内脏团和肌肉组织中的GR活性都有明显的抑制作用,且随着氟苯尼考质量比的增加抑制作用加强.     

微塑料对近江牡蛎免疫力的影响

为探究微塑料对牡蛎免疫力的影响,该研究对近江牡蛎(平均壳长:6.6cm)采用壳内推注的方式注入不同浓度的聚苯乙烯微塑料(0.05、0.5、5 mg·L^–1,以无菌生理盐水为稀释液),分别胁迫24 h、48 h和72 h后,检测分析牡蛎鳃组织的免疫指标(碱性磷酸酶(AKP)、超氧化物歧化酶(SOD)、丙二醛(MDA)、过氧化氢酶(CAT)、一氧化氮合成酶(NOS)和乙酰胆碱酯酶(AChE))的变化。结果显示,在胁迫24 h后,微塑料浓度对AKP的活力有显著影响(P<0.05)。SOD、AKP和结构型一氧化氮合成酶的活性呈现明显的先升后降的趋势。在胁迫48 h后,微塑料浓度上升导致A-chE活力显著下降(P<0.05), CAT、SOD和AKP呈现先升后降的趋势。在胁迫72 h后,微塑料浓度的升高, AKP和AChE的活力呈现先降后升的趋势,而SOD、CAT和诱导型一氧化氮合成酶的活力与之呈现相反的趋势,显示先升后降的趋势。随时间和浓度的增长, MDA处于一直上升的趋势。以上结果表明,微塑料可使牡蛎产生免疫应激反应,且胁迫时间越长,牡蛎免疫应激反应越剧烈。     

白藜芦醇对饥饿条件下厚壳贻贝(Mytilus coruscus)抗氧化能力的影响

饥饿胁迫引起的肥满度下降及收割延迟是导致贻贝养殖产量下降的主要原因之一。探究白藜芦醇(Resveratrol,RES)对饥饿条件下贻贝抗氧化能力的影响,揭示贻贝对饥饿胁迫的响应机制,对指导贻贝健康养殖具有重要意义。在饥饿胁迫条件下,分别采用10、20、50、100μmol/LRES处理厚壳贻贝,9d后采集贻贝组织样品并进行氧化应激指标检测。结果表明,饥饿胁迫显著增加厚壳贻贝组织中丙二醛(MDA)含量,同时显著降低过氧化氢酶(CAT)、超氧化物歧化酶(SOD)、谷胱甘肽过氧化物酶(GSH-PX)、碱性磷酸酶(AKP)和酸性磷酸酶(ACP)活性和还原性谷胱甘肽(GSH)含量。RES处理后,厚壳贻贝组织中MDA含量显著降低,但随着RES浓度的增加显著升高;性腺和鳃中CAT、SOD、GSH-PX、AKP、ACP活性和GSH水平、后闭壳肌中CAT、AKP活性和GSH水平以及外套膜中CAT、SOD、GSH-PX、ACP活性和GSH水平均随着RES处理浓度的增加先升高后降低。此外,10或20μmol/LRES处理能显著减轻饥饿胁迫引起的贻贝性腺中滤泡降解、配子退化及鳃丝纤毛脱落及结构受损;且各组贻贝后闭壳肌和外套膜组织形态学无明显变化。研究结果表明饥饿胁迫能显著抑制厚壳贻贝的抗氧化能力,但10或20μmol/LRES处理可减轻饥饿胁迫诱导的脂质过氧化和组织氧化应激损伤,且厚壳贻贝对饥饿胁迫诱导的氧化应激损伤表现出一定的组织差异性。     

维生素C、E对镉致毒后中华绒螯蟹抗氧化系统酶活性的影响

通过在饲料中添加不同浓度的维生素C(VC),维生素E(VE)探讨其对镉致毒后中华绒螯蟹(Eriocheirsinensis)肝脏中超氧化物歧化酶(Superoxidedismutase,SOD)、过氧化氢酶(Catalase,CAT)、谷胱甘肽过氧化物酶(Glutathioneperoxidase,GPx)活性变化的影响。结果表明,与镉中毒对照组相比,添加VC组能延缓抗氧化酶活性降低时间,减小其降低幅度。VC添加量增加(0.5%上升到1%),抗氧化酶降低的延缓减小作用随之增加。而投喂添加了VE的饲料,河蟹肝胰腺中SOD,CAT和GPx的变化与投喂VC组相似,表现为SOD、CAT基础活性下降,GPx活性上升,同时也能减慢抗氧化酶活性降低时间,减小其降低幅度。随VE量增加(0.02%增加到0.06%)以上变化呈增强趋势。从实验结果看VC,VE都可在镉致毒初期起到抗氧化保护作用。     

原油污染对栉孔扇贝抗氧化酶活性的影响

以原油水溶性成分(water soluble fraction of crude oil,WSF)为污染物,采用暴露实验法,研究了栉孔扇贝(Chlamys farreri)鳃和消化腺组织中超氧化物歧化酶(Superoxide Dismutase,SOD)和过氧化氢酶(Catalase,CAT)活性的变化.结果表明,WSF污染下,鳃和消化腺组织SOD和CAT酶活性随暴露时间增加一般表现为降低-升高-降低的趋势,酶活性达到最高的时间随浓度不同而变化.第1天时消化腺SOD在0.08 mg/L浓度下被诱导,而后随时间增加表现为抑制效应;浓度为0.21和0.88 mg/L时消化腺SOD酶活性被抑制,随暴露时间延长而活性增加.暴露时间为4d时,石油烃浓度在0.08和0.88 mg/L时鳃组织SOD酶活性均被抑制,而浓度为0.21 mg/L时被诱导.消化腺和鳃组织SOD可以作为扇贝被污染胁迫的指标.     

栉孔扇贝不同组织SOD、CAT和MPO活力的比较分析

对2龄和3龄栉孔扇贝外套膜、鳃、消化盲囊、肾、闭壳肌、性腺组织超氧化物歧化酶(SOD)、过氧化氢酶(CAT)和髓过氧化物酶(MPO)活力分析表明,检测组织均存在这三种酶,且在不同组织中活力表现存在明显差别,其中肾组织SOD、CAT活力最高,而MPO在消化盲囊中表现最高活力,与其它组织相比均呈显著性差异(P＜0.05).不同贝龄的栉孔扇贝酶活力比较表明,三龄贝各组织SOD、CAT和MPO活力均高于二龄贝.     

半叶马尾藻多糖对γ射线氧化损伤小鼠的保护作用

采用检测小鼠血浆和肝脏超氧化物歧化酶(SOD)、过氧化氢酶(CAT)和丙二醛(MDA)的方法，观察半叶马尾藻多糖[Sargassum hemiphyllum(Turner)C．Ag．polysaccharides，sHP]对2Gy γ射线损伤小鼠氧化自由基的影响。结果发现20mg／kg和40mg／kg的SHP不仅能明显降低辐射损伤小鼠血清和肝脏的MDA含量，而且能够提高辐射损伤小鼠SOD和CAT的活性，并呈剂量依赖性增强。10mg／kg的SHP对辐射损伤小鼠肝脏SOD、小鼠血浆和肝脏CAT也有明显的促进作用。提示半叶马尾藻多糖具有清除γ射线所致自由基和抑制脂质过氧化的作用。     

基于响应曲面法研究亚硝酸盐与养殖密度对吉富罗非鱼幼鱼生长与肝脏抗氧化力的影响

采用中心复合实验设计(CCD)和响应曲面方法(RSM),在实验室条件下探讨了亚硝酸盐(0.02—2.8mg/L)和养殖密度(1—5尾/10L)对吉富罗非鱼幼鱼生长和肝脏抗氧化指标(MDA含量,SOD与CAT活力)的联合影响。整个实验周期持续35d。结果显示,本实验条件下,亚硝酸盐和密度的一次效应和密度的二次效应对特定生长率有极显著影响(P0.01),特定生长率随着亚硝酸盐或密度的上升呈先上升后下降的变化。亚硝酸盐与养殖密度之间存在互作效应(P0.05)。亚硝酸盐浓度和养殖密度分别为1.65mg/L和3.28尾/10L时,肝脏超氧化物歧化酶(SOD)和过氧化氢酶(CAT)的活力同时较高。亚硝酸盐与养殖密度的一次效应对MDA含量和两种酶活力均有显著影响(P0.05),二次效应对两种酶活力的表达有极显著影响(P0.01);亚硝酸盐与密度对SOD和CAT活力有互作效应,高浓度亚硝酸盐与高密度环境会抑制SOD和CAT活力的表达,增加肝脏MDA含量。因子与响应值间二次多项回归方程的决定系数分别达到0.9384、0.9004、0.9520和0.9650(P0.01),可用于响应值预测;亚硝酸盐含量比养殖密度对养殖鱼的生长影响更为明显。建议在罗非鱼集约化养殖中,保持溶氧充足,降低氧化胁迫,提高罗非鱼的生长与抗氧化力。     

海洋中β-二甲基巯基丙酸内盐降解过程的研究进展

二甲基硫(DMS)是海水中一种最重要的、含量最丰富的还原态挥发性生源有机硫化物,前体β-二甲基巯基丙酸内盐(DMSP)的降解过程受各种因素影响。其中主要包括温度、DMSP的浓度、氧气、盐度、酸度、颗粒粒度、藻类生长期、季节变化、氧化压力、抑制剂等。它们均与DMSP降解速率呈一定的函数关系,并对DMSP的降解产物产生影响。藻类是DMSP的主要来源,因此着重讨论了温度、盐度、酸度等对不同浮游植物细胞内DMSP与DMS生物生产和转化过程的影响。结合海洋硫循环的研究现状和海洋化学发展的趋势,探究了用颗粒态DMSP与Chla的比率来量化碳和硫通量的方法及DMSP裂解酶活性的检验技术。大气中CO2压力持续增加导致的海洋酸化对藻类中DMSP降解过程的影响也是进一步研究的重点。     

Tracing dissolved organic matter cycling in the eastern boundary of the temperate North Atlantic using absorption and fluorescence spectroscopy

Apparent oxygen utilization (AOU), dissolved organic carbon (DOC), coloured dissolved organic matter (CDOM) absorption spectra, and CDOM fluorescence characteristic of aromatic amino acids (excitation/emission 280 nm/320 nm; F(280/320)) and marine-humic like substances (320 nm/410 nm; F(320/410)) were measured in full depth during a cruise in the temperate Eastern North Atlantic (ENA). An optimum multi-parameter (OMP) inverse method was run to calculate water mass proportion-weighted average (archetypal) concentrations of these chemical parameters for all water masses and samples. Archetypal concentrations retain the variability due to water mass mixing and basin scale mineralization from the water mass formation sites to the study area. Conversely, the difference between measured and archetypal concentrations, retain the variability due to dissimilarities in mineralization processes within the study area. Our analysis indicates that DOC supported 26±3% of the AOU in the dark temperate ENA and that basin scale processes occurring at and from the formation area of the water masses explained 63% of the total DOC variability. Our data also suggests that DOC remineralized at the basin scale was of lower molecular weight, and with a lower proportion of fluorescent aromatic amino acids than found within the study area. The relationship between the absorption coefficient at 254 nm (a_CDOM(254)) and AOU indicates that a_CDOM(254) was consumed during organic matter remineralization in the dark ocean, with 55% of the variability being explained by basin scale processes. The relationships of F(320/410) with AOU and DOC confirmed that marine humic-like substances are produced by microbial degradation processes, at a rate of 6.1±0.9×10⁻³ mg equivalents of QS mol AOU⁻¹. Our results also indicate that basin-scale remineralization processes account for 85% of the total variability of F(320/410), emphasizing that large scale processes control the formation of humic-like substance in the dark ENA.     

南海名浅考

根据历史文献分析，已知南海海名最早出现于周宣王（827BC--782BC在位）时的《江汉》诗中。秦汉之间214BC—111BC时著的《山海经&#183;海内东经》篇，记述了现时广东省三水和广州以南地区当时为海，称南海。这可从《史记》和《汉书》的记述，以及现代珠江三角洲的考古学、第四纪地质学和河口演变的研究成果所证实。南海古时别名涨海，明清时期外国人称为大明海和大清海。清朝以来，外国人把它翻译成（或称作）英文“South China Sea”，而近代某些中国人再把这个英文名词直译成汉文“南中国海”，忽视“南海”固有的中文名称。民国和中华人民共和国政府先后出版的地图和其他正式出版物，皆只用“南海”名。     

Dissolved organic matter cycling in the confluence of the Atlantic and Indian oceans south of Africa

The boundary between the Atlantic and Indian sectors of the Southern Ocean is a key spot of the thermohaline circulation, where the following water masses mix up: Indian Central water (ICW), South Atlantic Central Water (SACW), Antarctic Intermediate Water (AAIW), Circumpolar Deep Water (CDW), North Atlantic Deep Water (NADW), Weddell Sea Deep Water (WSDW) and Antarctic Winter Water (WW). An optimum multiparameter analysis based on the distributions of potential temperature, salinity, NO (=O₂+9.3×NO₃) and silicate during the GoodHope 2004 (GH04) cruise allowed us to (i) define the realms of these water masses; (ii) obtain the water mass proportion weighted-average (archetypal) apparent oxygen utilization (AOU) and dissolved organic carbon (DOC) concentrations of each water mass; and (iii) estimate the contribution of DOC to the oxygen demand of the study area. WW represented only 5.2% of the water volume sampled during GH04, followed by WSDW with 10.8%, NADW with 12.7%, SACW with 15.3%, AAIW with 23.1% and CDW with 32.8%. The distributions of DOC and AOU were mainly explained by the mixing of archetypal concentrations of these variables, 75±5% and 65±3% respectively, which retained the variability due to the basin-scale mineralization from the formation area to the barycentre of each water mass along the GH04 line. DOC accounted for 26±2% and 12±5% of the oxygen demand of the meso- and bathypelagic ocean, respectively. Conversely, local mineralization processes, retained by the residuals of the archetypal concentrations of DOC and AOU, did not contribute to improve significantly the mixing model of DOC.     

基于MapInfo数据格式在GIS应用环境下等值线综合方法实现

等值线构建是G IS开发、数字地图绘制重要的研究内容之一。重点讨论了基于M apInfo数据格式在G IS应用环境下等值线综合方法的实现,首先根据高程采样点跟踪等高线通过点,再利用五点光滑法、正轴抛物线加权平均光滑法以及M apX提供的光滑方法对等值线通过点进行光滑处理,从而绘制出光滑度好、准确美观的等值线,同时发现M apX所提供的光滑方法可能利用的就是正轴抛物线加权平均光滑法。通过大量的数据验证了绘制的正确性。     

基于Maplnfo数据格式在GIS应用环境下等值线综合方法实现

等值线构建是GIS开发、数字地图绘制重要的研究内容之一。重点讨论了基于Maplnfo数据格式在GIS应用环境下等值线综合方法的实现，首先根据高程采样点跟踪等高线通过点，再利用五点光滑法、正轴抛物线加权平均光滑法以及MapX提供的光滑方法对等值线通过点进行光滑处理，从而绘制出光滑度好、准确美观的等值线，同时发现MapX所提供的光滑方法可能利用的就是正轴抛物线加权平均光滑法。通过大量的数据验证了绘制的正确性。     

莱州湾海域水体中有机氯农药和多氯联苯的浓度水平和分布特征

以固相萃取/气相色谱法测定了莱州湾海域水体中22种有机氯农药和多氯联苯类化合物的浓度水平和分布特征。结果表明,莱州湾海域表层水体中有机氯农药浓度范围为N.D.~32.7ng/L,底层水中的浓度范围为N.D.~11.7ng/L。在该海域水体中共检出有机氯农药3种,β-666是水体中主要的有机氯农药污染物。多氯联苯类在底层水样中检出2种,总浓度范围在4.5~27.7ng/L之间。该海域有机氯农药和多氯联苯的分布特征是近岸高,离岸低,由近岸向湾外延伸方向依次递减。并对莱州湾表层水中总有机氯农药与海水盐度、氯度、溶解氧和pH间的关系作了初步探讨,得出总有机氯农药与盐度、氯度间有一定的相关关系,相关系数均为0.59。方法测定5种有机氯农药化合物的空白加标回收率为97.3%~126.0%,相对标准偏差为2.8%~8.6%;测定5种多氯联苯类化合物的空白加标回收率为88.6%~151.8%,相对标准偏差为6.7%~10.4%。     

Factors determining the vertical profile of dimethylsulfide in the Sargasso Sea during summer

The major source of reduced sulfur in the remote marine atmosphere is the biogenic compound dimethylsulfide (DMS), which is ubiquitous in the world's oceans and released through food web interactions. Relevant fluxes and concentrations of DMS, its phytoplankton-produced precursor, dimethylsulfoniopropionate (DMSP) and related parameters were measured during an intensive Lagrangian field study in two mesoscale eddies in the Sargasso Sea during July–August 2004, a period characterized by high mixed-layer DMS and low chlorophyll—the so-called ‘DMS summer paradox’. We used a 1-D vertically variable DMS production model forced with output from a 1-D vertical mixing model to evaluate the extent to which the simulated vertical structure in DMS and DMSP was consistent with changes expected from field-determined rate measurements of individual processes, such as photolysis, microbial DMS and dissolved DMSP turnover, and air–sea gas exchange. Model numerical experiments and related parametric sensitivity analyses suggested that the vertical structure of the DMS profile in the upper 60 m was determined mainly by the interplay of the two depth-variable processes—vertical mixing and photolysis—and less by biological consumption of DMS. A key finding from the model calibration was the need to increase the DMS(P) algal exudation rate constant, which includes the effects of cell rupture due to grazing and cell lysis, to significantly higher values than previously used in other regions. This was consistent with the small algal cell size and therefore high surface area-to-volume ratio of the dominant DMSP-producing group—the picoeukaryotes.     

网格虚拟地理环境体系结构研究

通过将网格技术与虚拟地理环境结合,以服务为核心,构造虚拟数据库,形成网格虚拟地理环境(G ridV irtual Geograph ic Environm ent,G rid-VGE),实现异构数据的集成与共享、任务的分解、闲散资源的充分利用、扩充虚拟地理环境的服务等。在详细阐述了G rid-VGE的框架结构及其关键技术的探讨后,以三维可视化地形漫游为例展示G rid-VGE中的一个应用实例。     

Study on the analysis and distribution of dimethylsulfoxide in the Jiaozhou Bay

A chemoreduction-purge-and-trap gas chromatographic method has been developed for the determination of trace dimethylsulfoxide (DMSO) in seawater. In the analysis procedure, DMSO was first reduced to dimethylsufide (DMS) by sodium borohydride and then the produced DMS was analyzed using the purge-and-trap technique coupled with gas chromatographic separation and flame photometric detection. Under the optimum conditions, 97% DMSO was reduced in the standard solution samples with a standard deviation of 5% (n=5). The detection limit of DMSO was 2.7 pmol of sulfur, corresponding to a concentration of 0.75 nmol/L for a 40 ml sample. This method was applied to determine the dissolved DMSO (DMSOd) and particulate DMSO (DMSOp) concentrations in the surface seawater of the Jiaozhou Bay, and the results showed that the DMSOd and DMSOp concentrations varied from 16.8 to 921.1 nmol/L (mean:165.2 nmol/L) and from 8.0 to 162.4 nmol/L (mean:57.7 nmol/L), respectively. The high concentrations of DMSOp were generally found in productive regions. Consequently, a significant correlation was found between the concentrations of DMSOp and chlorophyll a, suggesting that phytoplankton biomass might play an important role in controlling the distribution of DMSOp in the bay. Moreover, in the study area, the concentrations of DMSOd were significantly correlated with the levels of DMS, implying that the production of DMSOd is mainly via photochemical and biological oxidation of DMS.