厦门海域小型浮游动物和桡足类的摄食对浮游植物生长的影响

2005年11月16日和27日,运用稀释法和桡足类添加法,对厦门宝珠屿海域小型浮游动物及桡足类的摄食对浮游植物生长的影响进行了研究.结果表明,各粒级浮游植物的生长率均大于小型浮游动物的摄食率,小型浮游动物对总的Chla和nano-Chla具有一致的显著的摄食作用(0.51～0.78d-1),当存在螺旋环沟藻等大型的异养甲藻时,亦能摄食micro-级浮游植物.所添加的桡足类主要摄食micro-级的浮游植物,也显著摄食小型浮游动物,16日,所添加的桡足类促进nano-级浮游植物的每天生长效应达0.03ind/dm3.说明了厦门海域小型浮游动物及桡足类的摄食共同控制着浮游植物的生长,由于桡足类的杂食性,可产生一定的营养级联效应.     

高浓度硅藻对桡足类繁殖的影响

近年来,许多现场和实验室研究表明:一直被看作是桡足类主要食物来源的硅藻对桡足类繁殖、生长和发育具有抑制作用.本文通过桡足类体内因素和体外因素两方面介绍了高浓度硅藻对桡足类种群动态的影响.体内因素主要体现在硅藻的营养缺陷和次级代谢物毒性伤害上,体外因素主要为硅藻胞外分泌物、环境因素以及实验方法不同等.文章在介绍其研究现状的基础上,对今后的工作加以展望.     

重金属及沉积物对实验海洋生态系中浮游动物的影响

应用濒海陆基水池中8个围隔生冬系实验袋研究污染物对浮游动物的影响,结果表明:低浓度Cd,Cu,Pb,Zn,Hg的混合物对草食性桡足类的生长发育有一定的抑制作用,当浓度增到高值,抑制作用更为强烈.低浓度沉积物对草食性桡足类的生长发育同样具有一定的抑制作用,当浓度增到高值,抑制作用也更为明显,两类污染物均在不同程度上改变了生态系的结构,肉食性桡足类对污染物的反应并不明显,但幼形类住囊虫(Oikipleura sp.)对低,高浓度混合重金属则较为敏感,而对低、高浓度的沉积物却没有表现出明显的反应迹象.     

南极夏季宇航员海浮游动物群落结构及其与环境因子的关系

基于中国第36次南极科学考察期间(2019年12月至2020年1月)于南极宇航员海使用北太平洋网(0.5m~2,330μm)采集的浮游动物样品,对浮游动物的丰度、群落结构、优势种种群结构及其与环境因子之间的关系进行了研究。结果表明:2019/2020年南极夏季宇航员海浮游动物总丰度在8.93—102.00 ind./m3之间,最高丰度记录在宇航员海中部靠北区域,浮游动物主要由桡足类、磷虾、毛颚类、浮游被囊类等类群组成。调查海域桡足类丰度对浮游动物总丰度的贡献可达90%以上,其中、大中型桡足类Calanoides acutus, Metridia gerlachei, Calanus propinquus和Rhincalanus gigas分布广泛,而小型桡足类Oithona similis、Oithona frigida、Ctenocalanus citer、Oncaea conifera等在丰度上占比较高。通过聚类分析可将宇航员海浮游动物在区域上划分为5个群落,普里兹湾涡流、威德尔涡流、南极绕极流南界等物理海洋学过程是宇航员海浮游动物群落分布模式的主要控制因素。另外,生物环境匹配(Bio-env)分析显示,饵料(叶绿素a)也对该海区浮游动物的种群和群落结构具有重要影响。     

长江口几种优势桡足类对微型浮游动物的摄食研究

利用现场海水培养实验,结合浮游动物网样数据,研究长江口邻近海域几种优势桡足类(中华哲水蚤、背针胸刺水蚤、太平洋纺锤水蚤和精致真刺水蚤)对微型浮游动物的摄食影响。结果表明,精致真刺水蚤虽然属于肉食性种类,但几乎不摄食微型浮游动物;其余三种杂食性桡足类中华哲水蚤、背针胸刺水蚤和太平洋纺锤水蚤对微型浮游动物(纤毛虫+异养甲藻)的摄食率分别为0.66、0.09和0.59μg C/(ind·d),分别占其日总摄食量的29%、24%和37%。其中,异养甲藻在初始生物量和对桡足类饵料贡献上分别占整个微型浮游动物的30%和28%,是微型浮游动物中一个重要的组成类群。中华哲水蚤对微型浮游动物的摄食率与初始食物浓度有显著的正相关关系,并且对体长20μm纤毛虫的清滤率要明显高于对体长20μm的纤毛虫(P0.01)的清滤率,表明其偏好摄食较大个体的食物。通过Chesson选择性指数显示,尽管微型浮游动物在生物量上远小于浮游植物,但桡足类能优先选择摄食微型浮游动物;进一步结合网采浮游动物数据,获得各站三种优势桡足类丰度平均占桡足类总丰度的77%,但它们对微型浮游动物现存生物量的摄食压力仅为0.8%,表明桡足类对微型浮游动物群落的下行控制作用并不明显,仍有大部分微型浮游动物生物量未通过摄食途径进入到桡足类群落中。     

利用脂肪酸标记法对南极罗斯海桡足类优势物种的食性研究

脂肪酸标记法是浮游动物食性研究的一种重要方法.将提取的脂质区分为中性脂和极性脂,可以进一步查明不同脂质在浮游动物食性研究中的作用.本研究通过分析不同脂质的脂肪酸构成,对2013年1月中国第29次南极考察期间在罗斯海采集的5种优势种桡足类的食性进行了研究.结果显示:5种桡足类的极性脂脂肪酸具有相似的组成,无法给出桡足类食性差异信息,食性信息主要体现于中性脂脂肪酸组成的差异.通过分析中性脂脂肪酸的组成信息,将5种桡足类的食性分为三类:Cala-noides acutus和Calanus propinquus主要摄食浮游植物,Metridia gerlachei及小型桡足类Oncaea curvata为杂食性种,Paraeuchaeta antarctica为肉食性种.本文的结果说明,在应用脂肪酸作为浮游动物食性标记的研究中,应尽量区分不同脂质种类的脂肪酸信息,从而得到更为精确的浮游动物食性信息.     

典型河口浮游动物种类数及生物量变化趋势的研究

依据国家海洋局2004-2006年每年5月和8月的黄河口、长江口和珠江口生态监控区浮游动物的监测结果,对上述河口浮游动物和桡足类种类数及浮游动物生物量分布进行了分析,并将结果与历史资料进行同测区、同季节的对比。结果表明,与全国海洋普查时期相比,2006年黄河口浮游动物种类数下降了50．6％,桡足类种类数下降了53.3％;桡足类在浮游动物中所占比重由1985年的42.4％下降到2006年的32．6％。长江口浮游动物种类数有所上升,但是桡足类种类数由1985年的62种降低到2006年的37种;桡足类在浮游动物中的比重从1958年的54．2％降低到2006年的42．5％。珠江口桡足类在浮游动物中所占的比例由1959年的59．3％下降到54．4％,未发生明显变化。黄河口春季、夏季浮游动物生物量上升趋势不明显,夏季增幅较小;长江口自2000年以后春季浮游动物平均生物量为528．36mg／m^3,是1958年的2．4倍,2005年与2006年夏季浮游动物生物量分别是1958年的2．2和2．7倍,增加趋势十分明显;珠江口春季浮游动物生物量上升趋势最为显著,2004-2006年3年春季浮游动物平均生物量是1959年同期的5．7—8．7倍,1981年、2006年夏季生物量分别比1959年增加了3．1倍和11倍。就这3个河口生物量变化趋势看,珠江口生物量的上升趋势最为明显,长江口次之,黄河口变化幅度较小。     

滦河口近岸海域浮游动物群落与环境因子的关系（英文）

本研究对滦河口近岸海域19个站点浮游动物群落结构的时空分布及其与环境因子的关系进行了分析。结果表明,共发现浮游动物种类25个。其中,桡足类是最丰富的类群(春季和夏季分别占浮游动物总丰度的93.6%和74.9%)。春、夏季桡足类的种类组成相同,其中,小拟哲水蚤(Paracalanus parvus)和双毛纺锤水蚤(Acartia bifilosa)为两季优势种,都超过桡足类总丰度的15%。春季浮游动物的总丰度比夏季高,它们的平均值分别11 657 ind/m~3和1 549 ind/m~3。One-Way ANOVA分析表明,春、夏季浮游动物丰度差异显著(p0.001)。冗余分析(RDA)表明,盐度和营养盐分别是影响春季和夏季浮游动物分布的主要环境因子。     

渤海湾浮游桡足类群落特征

采用浅水Ⅰ型浮游生物网,分别于2017年春、夏、秋和冬季在渤海湾海域采集浮游动物,分析了桡足类群落的组成种类、生物多样性和丰度分布特征及环境因子与桡足类群落特征之间的关系.结果如下:调查海域共出现桡足类20种,其中秋季种类最多达到13种,春季和冬季分别为12种和9种,夏季最少为8种.渤海湾海域桡足类丰度的平均值在春季最...     

南京玄武湖浮游动物的种类组成及其数量周年变动的研究

本文报道了玄武湖Ⅰ、Ⅱ站1987～1988一周年浮游动物种类组成,以及个体数和生物量的调查结果。浮游动物数量的周年变动曲线,一般有夏季、秋季两个高蜂,浮游动物总数的消长完全受原生动物个体数的支配。年平均生物量统计结果:Ⅰ站,原生动物占浮游动物总量的43.9%,轮虫占43.0%,枝角类占3.9%,桡足类占9.2%;Ⅱ站,原生动物占总量的47.3%,轮虫占39.1%,枝角类占3.8%,桡足类占9.8%。     

Microbial Biomass and Organic Nutrients in the Deep-Sea Sediments of the Central Indian Ocean Basin

In order to assess the impact of deep-sea mining on the in situ benthic life, we measured the microbial standing stock and concentration of organic nutrients in the deep-sea sediments of the Central Indian Ocean Basin in the Indian pioneer area. Sediments were collected using box core and grab samples during September 1996. The total bacterial numbers ranged from 10 10 -10 11 cells per g -1 dry weight sediment. There was a marginal decrease in the number of bacteria from surface to 30 cm depth, though the subsurface section registered a higher number than did the surface. The highest numbers were encountered at depths of 4-8 cm. The retrievable number of bacteria were two orders less in comparison with the direct total counts of bacteria. An almost homogeneous distribution of bacteria, total organic carbon, living biomass, and lipids throughout the depth of cores indicates active microbial and benthic processes in the deep sea sediments. On the other hand, a uniform distribution of total counts of bacteria, carbohydrates, and total organic carbon in all the cores indicates their stable nature and suggests that they can serve as useful parameters for long-term monitoring of the area after the benthic disturbance. Further studies on temporal variability in this region would not only verify the observed norms of distribution of these variables but would also help to understand restabilization processes after the simulated benthic disturbance.     

海上大直径钢管桩打桩过程中桩周土强度弱化研究

海上大直径钢管桩打桩过程中,桩周土体受到强烈扰动而发生强度弱化,掌握桩周土体强度弱化规律对于准确预测打桩过程、保证工程安全具有重要意义。为研究土体强度弱化规律,开展了环剪试验模拟打桩对桩周土体的扰动,测试土体强度随剪切速率的变化规律,建立了描述土体强度弱化规律的拟合公式,引入到打桩分析软件中。研究结果表明：土体的强度折减程度不仅与土体本身的性质有关还受到土体的埋深和剪切速率的影响,埋深越深土体强度折减程度越低,剪切速率越高土体强度折减越高,在打桩分析中可采用这里推荐的线性折减方法来模拟不同深度处土体强度的折减规律。     

Geoacoustic Inversion via Genetic Algorithm and Its Application to Manganese Sediment Identification

An acoustic inversion method using a wide-band signal and two near field receivers is proposed and applied to multiple layered seabed models including a manganese sediment. The inversion problem can be formulated into a probabilistic model comprised of signals, a forward model, and additive noise. The forward model simulates wide-band signals, such as chirp signals, and is chosen to be the source-waveletconvolution plane wave modeling method. The wavelet matching technique, using weighted least-squares fitting, estimates the sediment sound-speed and thickness on which determination of the possible numerical ranges for a priori uniform distribution is based. The genetic algorithm is applied to a global optimization problem to find a maximum a posteriori solution for determined a priori search space. Here the object function is defined by an L 2 norm of the difference between measured and modeled signals. Not only the marginal pdf but also its statistics are calculated by numerical evaluation of integrals using the samples selected during importance sampling process of the genetic algorithm.     

Phylogenetic diversity and phenotypic characterization of cultivable bacterioplankton isolated from polar oceans

A set of 27 marine planktonic bacteria isolated from the polar regions was characterized by 16S rDNA sequencing and physiological and biochemical testing. More than half of these bacteria were positive for caseinase, gelatinase and 13-glucosidase, and could utilize glucose, maltose or malic acid as carbon source for cell growth. Twelve isolates expressed nitrate reduction activities. Except for one antarctic isolate BSwlO175 belonging to Actinobacteria phylum, these isolates were classified as γ-Proteobacteria, suggesting that γ-Proteobacteria dominated in cultivable marine bacterioplankton at both poles. Genus Pseudoalteromonas was the predominant group in the Chukchi Sea and the Bering Sea, and genus ShewaneUa dominated in cultivable bacterioplankton in the Prydz Bay. With sequence similarities above 97%, genus Psychrobacter was found at both poles. These 27 isolates were psychrotolerant, and significant 16S rDNA sequence similarities were found not only between arctic and antarctic marine bacteria （ 〉 99% ）, but also between polar marine bacteria and bacteria from other aquatic environments （ ≥ 98.8% ）, including temperate ocean, deep sea, pond and lake, suggesting that in the polar oceans less temperature-sensitive bacteria may be cosmopolitan and have a bipolar, even global, distribution at the species level.     

Deep-Sea Sediment Compression Curves: Some Controlling Factors, Spurious Overconsolidation, Predictions, and Geophysical Reproduction

Oedometer tests have been carried out on 70 undisturbed surficial clays (at approximately 250 mm below the mudline), mostly collected by free-fall corers from sites widely scattered throughout the deep-sea North Atlantic. Acoustic measurements were also made, initially on contiguous samples and ultimately on the same sample using a geophysically instrumented oedometer which also collected electrical resistivity data. Apart from those quiescent areas below the carbonate compensation depth, such as north of the West Indies where very fine clays exist, most of the samples are silty clays whose geotechnical-geophysical properties are dependent on the type of clay minerals present (and their ability to take in moisture), the sand-size fraction, and the quantity of carbonate present. Thus the pure clays have high compressibilities which decrease on the addition of coarse particles, while the converse is true for the acoustic parameters, these increasing with the sand fraction. Using the notion of the intrinsic compression line for all samples, and comparison to it of the measured compression curves, it is clear that, contrary to some previously held ideas, most deep-sea clays are normally consolidated; the addition of carbonate has the effect of creating an open, stronger sediment skeleton. Interestingly, where information is available, the variation with depth of a sample's acoustic velocity follows the void ratio pressure relationship of the compression curve. This allows the construction of an in-situ sediment compression curve using the in-situ geophysical observations.     

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,     

Evaluation of the Risk of Marine Slope Instability: A Pseudo-3D Approach for Application to Large Areas

This article presents a methodology developed to evaluate the instability of submarine slopes that extend over a large area. Special attention was paid to (1) the complex geometry (bathymetry) and the expanse of the slope, (2) the heterogeneity of the sediment, and (3) the distribution of the pore pressure. The safety factor was considered as a spatially varying quantity. The General Formulation (GLE, Fredlund and Krahn 1977), which fully satisfies equilibrium conditions, was used for evaluating the stability of the marine slope. The submarine slope failure, which occurred on 16 October 1979 during the construction of the new Nice airport, was studied in order to test the developed model. Geotechnical parameters were taken from experimental tests carried out by IFREMER on 19 cores extracted at different depths (from 27 m to 1300 m) (Cochonat, Bourillet, and Savoye, 1993; Mulder et al., 1994). Many scenarios were proposed in order to explain the cause of the Nice slope failure (Habib, 1994). In this article, two of those scenarios were tested. Simulation results are presented and discussed.