混合氮源对扁藻与金藻共培养和单种培养生长的影响

采用均匀设计,研究了硝酸钠(NO3-N)、尿素(NH2-N)和硫酸铵(NH4-N)3种氮源对亚心形扁藻(Platymonas subcordiformis)与球等鞭金藻(Isochrysis galbana)共培养和单种培养生长的影响。结果表明,不同氮源对扁藻与金藻在不同培养方式下的生长均存在显著差异(P<0.05)。共培养时,硝酸钠质量浓度对扁藻和金藻的总细胞密度(Yt)和最终细胞密度的体积比(Yr)没有影响,尿素质量浓度对Yt有正调节作用,而硫酸铵质量浓度对Yt有负调节作用、对Yr有正调节作用。当培养液中NH2-N质量浓度为21.01 mg/L,扁藻和金藻接种体积比(Xv)为14.15时,Yt最大(1 508.9×104个/mL);当NH4-N质量浓度、Xv分别为21.00 mg/L和14.15时,Yr最大,为87.46。单种培养金藻时,硝酸钠略优于尿素,2种氮源对其生长均有正调节作用,而硫酸铵起负调节作用。当培养液中加21.01 mg/L的NO3-N和NH2-N时,金藻的细胞密度达到最大值(862.6×104个/mL);不同氮源对扁藻生长的调节作用与金藻相反,当扁藻接种密度为4.6×104个/mL,培养液中NH4-N质量浓度为21.00mg/L时,扁藻细胞密度达到102.2×104个/mL,其值最大。     

蒽与苯并[a]芘对海洋微藻致毒影响的比较研究

新月菱形藻 ,球等鞭金藻 870 1和亚心形扁藻 ,分别用不同浓度的蒽和苯并 [a]芘胁迫72 h,测定三种藻的生长速率 ,叶绿素 a含量。实验表明 ,三种微藻对蒽的敏感性由高到低依次为新月菱形藻、球等鞭金藻 870 1和亚心形扁藻 ,它们 72 h的半抑制浓度 EC50 分别是 0 .0 6 0 mg/L、0 .0 6 5mg/L和 0 .0 94 mg/L。而对苯并 [a]芘的敏感性由高到低依次为亚心形扁藻、新月菱形藻和球等鞭金藻 870 1,它们的 72 h· EC50 分别是 0 .0 76 mg/L、0 .0 88mg/L 和 >0 .10 mg/L(在本实验范围内未测到 )。叶绿素 a含量与各自的相对增长率呈一定的正相关。不同的海洋微藻对蒽和苯并 [a]芘的敏感性不同。     

油菜素内酯对两种单细胞藻生长和某些生理活性的影响

研究于１９９１年３月－１９９２年７月在大连进行，实验藻取自大连凌水养殖二场饵料室。分别用浓度为５，１０，５０μｇ／Ｌ和１，５，１０μｇ／Ｌ的油菜素内酯处理亚心形扁藻及球等鞭金藻，研究其对单细胞藻生长的结果表明，两种藻的各处理组的瞎缓期均缩短，细胞生长加快。促进生长最佳浓度。亚心形扁藻的１０μｇ／Ｌ，球等鞭金藻的５μｇ／Ｌ；油菜素内酯可提高实验藻的叶绿素含量并促进其光合作用；在处理组的亚心形扁藻和球     

磷浓度对球等鞭金藻3011和8701叶绿素荧光特性及生长的影响

本文研究了球等鞭金藻3011和8701一次性培养过程中,培养基中不同磷浓度(0μM、2.27μM、18.15μM、36.3μM、72.6μM、290.4μM)对其PS最大光能转化效率(Fv/Fm)、叶绿素含量以及细胞密度的影响。培养温度为(23±1)℃,盐度为31,光照强度为5000 lx。单因子方差分析结果表明,随着培养时间的延长,磷浓度对两株微藻的光合作用及生长均有显著影响(P<0.05)。球等鞭金藻3011和8701的Fv/Fm比值、叶绿素含量以及细胞密度均随着起始磷浓度的增加而增加,在290.4μmol/L处达到最大值;球等鞭金藻3011和8701进行光合作用和生长的最适磷浓度均为290.4μmol/L。     

2-(N-芳基氨甲基)苯并异噻唑啉酮类化合物对海洋浮游生物的生长抑制活性研究

本文研究了13个2-(N-芳基氨甲基)苯并异噻唑啉-3-酮类化合物对球等鞭金藻Isochrysis galbana、亚心形扁藻Platymonas subcordiformis及舟形藻Navicula的生长抑制性能,并测试了其对藤壶二期无节幼虫的生物活性。结果表明:2-(N-芳基氨甲基)苯并异噻唑啉-3-酮类化合物对球等鞭金藻、亚心形扁藻和舟形藻都有良好的生长抑制活性,其中对球等鞭金藻和亚心形扁藻的抑制作用较强;对藤壶幼虫的生物活性测试表明,化合物最低质量浓度为2.0 mg/L时,除化合物g和l,都具有良好的生长抑制活性。化合物的结构与浮游生物的生长抑制活性关系表现为间位取代优于对位取代。     

两种光强条件下亚心形扁藻各生长阶段的产氢能力

海洋亚心形扁藻(Platymonas subcordiformis)在光照生长后,经过暗培养诱导其可逆产氢酶,然后转移到光照下可产生氢气。在300 mL产氢反应器中对海洋亚心形扁藻产氢情况的考察表明,不同的光强条件可导致扁藻产生不同的生长曲线,而在不同的培养阶段,扁藻的产氢能力也有很大的差别。其他培养条件相同,高光照强度(E=13000 lx)条件下,扁藻生长较快,而且可以获得更大的产氢能力,300 mL密度为3×106个/mL、叶绿素质量浓度为5.8 mg/L的藻液最大产氢浓度可达17.5%,比低光照强度(E=5000 lx)时提高了32%,叶绿素含量降低了61%。根据产氢前后以及暗诱导后扁藻生理状态的考察结果,可以推测出是不同生长阶段扁藻的生理状态差异导致了其产氢能力的变化。     

重金属胁迫对两种海洋饵料微藻的急性毒性效应研究

在模拟生态环境条件下研究了铜(Cu2+)、镉(Cd2+)和锌(Zn2+)3种重金属离子对2种海洋饵料微藻(青岛大扁藻(Platymonas helgolandica)和等鞭金藻8701(Isochrysis galbana 8701))的急性毒性效应,分析其对种群增长的影响,并利用透射电镜对微藻亚显微结构的变化进行分析。在实验浓度范围内,2种微藻的种群增长对3种重金属离子的急性胁迫表现出类似的变化趋势,随着胁迫浓度的增加,微藻的相对增长率均呈现出不断下降的趋势;通过比较2种微藻的48hEC50和96h-EC50发现:3种重金属离子的毒性程度为Cu2+Cd2+Zn2+,等鞭金藻8701对重金属胁迫的敏感性高于青岛大扁藻。2种微藻的亚显微结构观察显示,二者的膜结构及细胞核对Cu2+胁迫并不太敏感;与对照组相比等鞭金藻8701的色素体及贮能物质受影响较严重,而青岛大扁藻的叶绿体及淀粉粒受影响较大。     

几种单胞藻对双刺纺锤水蚤雌体繁殖的影响

研究6种饵料微藻：微绿球藻（Nannochloropsis oculata）、小球藻（Chlorella．sp）、球等鞭金藻（Isochrysis galbana）、三角褐指藻（Phaeodactylum tricornutum）、亚心形扁藻（Platymonas subordi-formis）、中肋骨条藻（Skeletonema costatum）对双刺纺锤水蚤（Acartia bifilosa）雌体繁殖的影响，以探索适合培养双刺纺锤水蚤的藻类。应用解剖镜下计数方法对雌体存活率、产卵率、孵化率、排粪率几个指标进行检测。结果表明微绿球藻、小球藻和球等鞭金藻明显不适于用作雌体饵料；中肋骨条藻组产卵率最高，亚心形扁藻和三角褐指藻组的产卵率没有显著差异；亚心形扁藻组的排粪率明显低于中肋骨条藻和三角褐指藻组；摄食三角褐指藻的雌体所产的卵其平均孵化率要显著低于亚心形扁藻和中肋骨条藻；亚心形扁藻组雌体的产卵率尽管较中肋骨条藻组低，但却保持最高的雌体存活率，而且排粪率也要比中肋骨条藻低得多。综合比较得出结论：6种饵料微藻中，亚心形扁藻和中肋骨条藻是两种最适宜培养双刺纺锤水蚤雌体的优良饵料，二者混合使用效果会更好。     

香港巨牡蛎对3种微藻的选择性摄食研究

从微藻粒径大小、饵料密度以及营养价值角度，选取牟氏角毛藻（Chaetoceros muelleri）、亚心形扁藻（Platymonas subcordiformis）、球等鞭金藻（Isochrysis galbana）分别作为硅藻、绿藻和金藻的代表，开展了不同规格的香港巨牡蛎对3种微藻在同等密度、同等生物量混合条件下的摄食选择性研究。结果显示，香港巨牡蛎在两种不同混合藻条件下对3种不同微藻摄食选择性有显著性差异（P<0.01）。3种藻相同密度混合条件下，大、中、小3种规格香港巨牡蛎更倾向摄食粒径较大的亚心形扁藻，且贝类规格越大选择倾向性越低，摄食选择效率分别为0.32、0.35、0.48，对球等鞭金藻无明显选择性。3种藻等生物量混合条件下，香港巨牡蛎对亚心形扁藻和球等鞭金藻的摄食有选择性，且规格大小对选择效率影响显著（P<0.01），个体越小选择性越强，小规格香港巨牡蛎倾向滤食亚心形扁藻（P<0.01），大、中规格更倾向摄食粒径较小的球等鞭金藻。两种混合条件下，香港巨牡蛎都对牟氏角毛藻都有负的选择效率，而且牟氏角毛藻密度越高负值绝对值越大。微藻的细胞大小、形状、营养价值以及香港巨牡蛎的个体大小都对摄食选择性有着明显的影响，香港巨牡蛎的摄食选择性在现场海区中还明显受到生境及食物条件的限制。     

亚心形扁藻培养基的筛选与优化

在500mL三角瓶中对亚心形扁藻培养基的筛选与优化结果表明,原“海洋三号”培养基中需添加0.8 g/L的NaHCO_3,且 K_2HPO_4的浓度需由原来的 0.01g/L调整为 0.06 g/L。10 L全自动封闭式光生物反应器分批培养结果表明,优化后的“海洋三号”培养基不仅可加快亚心形扁藻的生长速率而且可延长生长时间,培养 4 d时最高藻细胞密度可达 426×10~4细胞/mL,比原“海洋三号”培养基的最高培养密度提高42％。优化后的“海洋三号”培养基为亚心形扁藻的最适培养基。     

Assessing the Validity of Seismo-Acoustic Predictor Equations for Obtaining Seabed and Sub-Surface Sediment Physical Properties

The interdependence between the seismo-acoustic properties of a marine sediment and its geotechnical/physical parameters has been known for many years, and it has been postulated that this should allow the extraction of geotechnical information from seismic data. Though in the literature many correlations have been published for the surficial layer, there is a lack of information for greater sediment depths. In this article, a desktop study on a synthetic seafloor model illustrates how the application of published near-surface prediction equations to subsurface sediments (up to several tens of meters burial depth) can lead to spurious predictions. To test this further, acoustic and geotechnical properties were measured on a number of sediment core samples, some of which were subjected to loading in acoustically-equipped consolidation cells (oedometers) to simulate greater burial depth conditions. For low effective pressures (representing small burial depths extending to around 10 meters subsurface), the general applicability of established relationships was confirmed: the prediction of porosity, bulk density, and mean grain size from acoustic velocity and impedance appears generally possible for the investigated sedimentary environments. As effective pressure increases through, the observed relationships deviate more and more from the established ones for the near-surface area. For the samples tested in this study, in some instances increasing pressure even resulted in decreasing velocities. There are several possible explanations for this abnormal behavior, including the presence of gas, overconsolidation, or bimodal grain size distribution. The results indicate that an appropriate depth correction must be introduced into the published prediction equations in order to obtain reliable estimates of physical sediment properties for greater subsurface depths.     

Interannual Sea Level Variations and Annual Tides in the Northwestern Pacific

Specific properties of the interannual sea level variations and annual tides in the Northwestern Pacific were studied. Several tide stations were monitored. The monthly mean sea level for the year of 1995 was analyzed at each tide station. A seismic event in 1995, some tectonic activity around the subject area, and the Kuroshio (the oceanic western boundary current) may possibly contaminate results which would have occurred from the astronomical annual tide alone.     

Flow Cytometric Analysis of Coastal Lagoon Bacterioplankton and Picophytoplankton: Fixation and Storage Effects

The effect of different fixation and storage protocols on the flow cytometric (FCM) simultaneous analysis of bacterioplankton and phytoplankton in coastal seawater samples (Mediterranean coastal lagoons) was investigated. FCM measurements (cell number, fluorescence and scatter characteristics) were obtained through DAPI staining. Three fixatives [glutaraldehyde (GA), formaldehyde (FA) and paraformaldehyde (PFA)] and two storage (3 months duration) methods (5 °C and −196 °C) were tested. Two dominant populations were detected in studied samples: bacteria and eukaryotic picophytoplankton. Adding fixatives (2% final concentration) appears necessary to obtain FCM exhaustive counts of all the bacteria and phytoplanktonic cells. This was related to the permeation effect of fixatives which allowed a better DAPI staining of the cells. Maximum fluorescence, i.e. optimal staining of the cells was obtained with FA or PFA, and significant lower fluorescences with GA. Fixed samples stored at 5 °C induced rapid cell loss. Only storage in liquid nitrogen of samples fixed with FA or PFA, allows mid-term (≥4 months) preservation of bacteria or picophytoplankton cell numbers, and limited evolution of DAPI-induced fluorescence and scatter characteristics.     

INFORMATION FOR AUTHORS

<正>Acta Oceanologica Sinica(AOS)is a comprehensive academic journal edited by the Editorial Committee of Acta Oceanologica Sinica and is designed to provide a forum for important research papers of the marine scientific community which reflect the information on a worldwide basis.The journal publishes scholarly papers on marine science and technology,including physics,chemistry,biology,     

Net Sand Transport Direction in a Tidal Inlet, using Foraminiferal Tests as Natural Tracers

The relationship between the flux of exotic benthic foraminiferal tests (i.e. tests which are supplied from open-sea sources alone) in a tidal inlet and that of bulk sediment was analysed, which can be expressed as two first-order linear equations. According to this relationship, in order to determine net sediment transport directions in the entrance, the test concentration in surficial sediments of the tidal basin can be compared against a ‘ critical level ’. The critical level is determined for the conditions that no net transport of bulk sediment is present within the entrance. If the observed concentration (averaged over the tidal basin) is higher than the simulated critical level, then the net sediment transport is directed to landward. This method is applied to the analysis of net sand transport at Christchurch Harbour, a tidal inlet system located in southern England. In this investigation, concentrations of exotic foraminiferal tests in the surficial sediments of the tidal basin and ebb tidal delta area were obtained from the analysis of sea-bed sediment samples. A series of probable critical levels were calculated based upon the data sets with regard to: (1) sediment discharge from the rivers; (2) magnitude of sediment discharge within the entrance during the ebb; (3) the test concentration outside the harbour; (4) the thickness of the moving layer; and (5) two parameters associated with dispersive processes. The results show that the concentration in the tidal basin sediment is higher than a number of simulated critical concentrations for representative cases. Consequently, the high level of the concentration of exotic benthic foraminiferal tests within the harbour should be explained as a result of landward net transport of sands within the entrance.     

Sea Levels and Coastal Inundation Due to Tropical Cyclones in Indian Coastal Regions of Andhra and Orissa

Coastal inundation associated with extreme sea levels is the main factor which leads to the loss of life and property whenever a severe tropical cyclonic storm hits the Indian coasts. The Andhra and Orissa coasts are most vulnerable for coastal inundation due to extreme rise in sea levels associated with tropical cyclones. Loss of life may be minimized if extreme sea levels and associated coastal flooding is predicted well in advance. Keeping this in view, location specific coastal inundation models are developed and applied for the Andhra and Orissa coasts of India. Several numerical experiments are carried out using the data of past severe cyclones that struck these regions. The simulated inland inundation distances are found to be in general agreement with the reported flooding.     

Role of Siliceous Fossil Dissolution in Downcore Variations of Grain Size and Water Content: Western Margin of Clarion-Clipperton Fracture Zone, NE Equatorial Pacific

Grain size and water content in box-core sediments from the Clarion-Clipperton fracture zone (C-C zone) in the northeast equatorial Pacific were analyzed in detail to understand the downcore variations across a hiatus between Quaternary and Tertiary layers. Grain-size distributions in the topmost core sediments show two modes: a coarse mode (peaked at 50 μm) and a fine mode (at 2-25 μm). The coarse mode disappears gradually with depth accompanied by the dissolution of siliceous fossil tests, whereas the fine mode coarsens due to the formation of authigenic minerals. Water content increases abruptly across a color boundary between an upper pale brown layer and a lower dark brown layer that is the hiatus between Quaternary and Tertiary layers. Abundant smectites and microvoid molds, which are created by the prolonged fossil dissolution in the underlying sediment, are attributed for the abrupt downcore variation of water content. Overall variations in grain size and water content in the topmost core sediments in the western C-C zone are possibly constrained by the dissolution of biogenic siliceous fossils. Variations in geotechnical properties related to these changes must be considered in the design of nodule collectors.     

Sea Levels and Western Boundary Flow Near a Tectonic Zone in the Northern Pacific

This article concerns an interrelation between the sea levels and the western boundary flow near a tectonic boundary in a local zone in the Northwestern Pacific. In this zone, sea level variations at stations located on the coast facing the Pacific are studied to find the interrelation between variations of the Kurosio flow as an index of the distance of the flow axis off a specific coast. The result is discussed after data processing of the monthly means of the sea levels, and a notice is taken of variations caused by active crustal upheavals during a seismic event, a local earthquake.