罗源湾口柱状沉积物中的甲藻孢囊

通过时福建罗源湾口海域KMZK5柱状沉积物中甲藻孢囊的分析，共鉴定出15属30种甲藻孢囊，对比发现这30种甲藻孢囊是该湾以前未被记录的种类．其中12种是附近海域也未曾发现的种类，6种为有毒种类：缘亚历山大藻、小型亚历山大藻、塔玛亚历山大藻、具剌膝沟藻、链状裸甲藻、锥状斯氏藻，同时对甲藻孢囊的主要属种和有毒种类的丰度、分布在垂直方向上的变化特征进行了初步研究。     

罗源湾口柱状沉积物中的甲藻孢囊

通过对福建罗源湾口海域KMZK5柱状沉积物中甲藻孢囊的分析,共鉴定出15属30种甲藻孢囊。对比发现这30种甲藻孢囊是该湾以前未被记录的种类。其中12种是附近海域也未曾发现的种类,6种为有毒种类:缘亚历山大藻、小型亚历山大藻、塔玛亚历山大藻、具刺膝沟藻、链状裸甲藻、锥状斯氏藻.同时对甲藻孢囊的主要属种和有毒种类的丰度、分布在垂直方向上的变化特征进行了初步研究.     

厦门湾沉积物中有害有毒甲藻休眠孢囊及塔玛亚历山大藻的潜在危害

本工作通过分析厦门湾表层沉积物中的甲藻休眠孢囊，发现了1种有毒塔玛亚历山大藻(Alexandrium tamarense)休眠孢囊，及两种有害甲藻休眠孢囊：锥状斯氏藻(Scrippsiella trochoidea)、具刺膝沟藻(Gonyaulax spinifera)．对塔玛亚历山大藻进行了培养。并初步研究了该藻的毒性及贝类对其毒素的积累．研究结果表明，厦门海域沉积物中的塔玛亚历山犬藻是有毒的．它的较适宜生长环境条件是：水温20～25℃．盐度为25～30，光照度为3000～50001x．塔玛亚历山大藻在每年的4月26日至6月10日、10月11日至11月20日可能会形成有害藻华，危害厦门海域的海洋生物并可能威胁到人类的健康和生命安全．     

福建东山湾表层沉积物中甲藻孢囊分布研究

本研究于2016年11月在福建东山湾海域采集了表层沉积物, 对沉积物中甲藻孢囊的分布规律进行了研究, 重点揭示了有毒有害甲藻孢囊的分布; 同时测定了沉积物中生源要素含量, 以揭示孢囊分布与生源要素的关系。共鉴定甲藻孢囊22种, 包括自养型14种和异养型8种, 优势种为原多甲藻孢囊。孢囊的种类多样性指数(H')偏低, 为1.70~2.38之间; 均匀度指数(J)为0.64~0.84。孢囊密度介于70.6~136.4个·g^-1, 平均为107.2个·g^-1, 在漳江口和八尺门海域较低。东山湾表层沉积物中较高的异养型甲藻孢囊百分含量(平均75.5%)在一定程度上说明了水体中较高的初级生产力及富营养化水平。值得注意的是, 本研究分析鉴定出7种有毒有害甲藻的孢囊, 包括麻痹性贝类毒素(paralytic shellfish toxin, PSP)原因种奥氏亚历山大藻(Alexandrium ostenfeldii)和链状/塔玛亚历山大藻(Alexandrium catenella/tamarense)孢囊复合体、虾夷扇贝毒素(yessotoxin, YTX)原因种具刺膝沟藻(Gonyaulax spinifera)、环胺藻毒素(azaspiracid, AZP)潜在原因种环胺藻(Azadinium sp)、产生鱼毒素的哈曼褐多沟藻(Polykrikos hartmannii)以及赤潮藻类Barrufeta bravensis和锥状斯氏藻(Scrippsiella acuminate)。整体来说, 这些有毒有害藻类的孢囊密度较低, 但具刺膝沟藻在某些站位的高密度出现需引起关注。     

秋季南黄海表层沉积物中甲藻孢囊分布

2007年秋季(10月)在黄海22个站位采集表层沉积物样品进行甲藻孢囊的种类鉴定与计数,本航次中共鉴定出33种(不包括2个未确定种),优势种是锥状斯克里普藻(Scrippsiella trochoidea)、塔玛亚历山大藻(Alex-andrium tamarense)和膝沟藻属(Gonyaulaxsp.)的种类。与东海和南海甲藻孢囊的同期丰度相比,黄海的相对较低,丰度范围为10~519个/cm3,平均108个/cm3。孢囊丰度总体分布趋势从北向南递增,最高丰度区出现在长江口以北(32°19′59.88″N,122°37′5.16″E),另外,在南黄海调查海域中,中部黄海冷水团区域孢囊丰度较高,膝沟藻成为该区域的优势种,密集中心达101个/cm3。有毒甲藻孢囊在沉积物表层聚集且分布广泛,有爆发赤潮的可能。     

福建兴化湾海域沉积物中的甲藻孢囊记录

通过对福建兴化湾海域表层和柱状沉积物中甲藻孢囊的分析,共鉴定出10 属29种(含不定种)甲藻孢囊.其中发现有毒种类7种:微小亚历山大藻(Alexandrium minutum)、多环旋沟藻(Cochlodinium polykrikoides)、多边舌甲藻(Lingulodinium polyedrum)、具刺膝沟藻(Gonyaulax spinifera)、链状裸甲藻(Gymnodinium catenatum)、网状原角管藻(Protoceratium reticulatum)和锥藻斯氏藻(Scrippsiella trochoidea).表层沉积物中总甲藻孢囊丰度值在13～88粒/g之间,柱状沉积物中总甲藻孢囊的丰度在40～105粒/g以内.通过与周边其他海域甲藻孢囊属种组成及丰度值对比,表明兴化湾甲藻孢囊的丰度值较高,并且7种有毒种类的存在对该海域发生有毒有害赤潮构成潜在威胁,相关政府部门及周围居民应加以重视和防范.     

福建福宁湾表层沉积物中甲藻孢囊分布与多样性研究

孢囊是甲藻生活史中特殊的休眠阶段,被认为是赤潮发生的种源。于2018年4月采集了福建福宁湾海域表层沉积物,对沉积物中甲藻孢囊的分布规律进行了研究,重点揭示有毒有害甲藻孢囊的分布;同时测定了沉积物中生源要素含量,以揭示孢囊分布与生源要素的关系。共鉴定甲藻孢囊25种,其中别什藻(Biecheleria tirezensis)孢囊占据优势。孢囊的种类多样性指数(H'')偏低,为2.06~2.34;均匀度指数(J)为0.71~0.81。孢囊密度介于178.6~386.3 cysts/g (以干重计,下同),平均为286.0cysts/g。孢囊密度高值区位于水深较深、沉积物颗粒较细的长表岛外海域,而低值区则位于长表岛至海尾角的近岸海域。值得注意的是,研究分析鉴定出9种有毒有害甲藻的孢囊,包括麻痹性贝类毒素(paralytic shellfish poisoning,PSP)原因种奥氏亚历山大藻(Alexandrium ostenfeldii)和链状/塔玛亚历山大藻(Alexandrium catenella/tamarense)孢囊复合体、goniodomine A原因种平野亚历山大藻(Alexandrium hiranoi)、虾夷扇贝毒素(yessotoxin,YTX)原因种具刺膝沟藻(Gonyaulax spinifera)和网状原角藻(Protoceratium reticulatum)、产生鱼毒素的哈曼褐多沟藻(Pheopolykrikos hartmannii)以及赤潮藻类Barrufeta bravensis、锥状斯氏藻(Scrippsiella acuminata)和垂裂莱万藻(Levanderina fissa),其中Barrufeta bravensis、Gonyaulax spinifera和Scrippsiella acuminata的孢囊分布广泛且密度较高,需引起关注。     

南麂列岛海域沉积物中甲藻孢囊的多样性和分布

南麂列岛地处亚热带海域,是台湾暖流和江浙沿岸流的交汇处,因而呈现出很好的生物多样性。据调查,南麂列岛附近海域已鉴定的浮游植物甲藻有53种,而到目前为止,对南麂列岛海域甲藻的休眠孢囊种类和分布的调查仍为空白。本文通过对2014年南麂列岛附近海域沉积物中甲藻孢囊的调查研究,在该海域共发现甲藻孢囊10属26种,其中,种类最多的是原多甲藻属(Protoperidinium),有10种;其次是斯氏藻属(Scrippsiella)和亚历山大藻属(Alexandrium),分别有4种,膝沟藻属(Gonyaulax)2种,舌甲藻属(Lingulodinium)、易碎藻属(Fragilidium)、扁甲藻属(Pyrophacus)、翼藻属(Diplopsalis)、裸甲藻属(Gymnodinium)和多沟藻属(Polykrikos)各1种。这些甲藻孢囊中,异养型和自养型甲藻孢囊各13种,自养型甲藻孢囊在数量上所占比例较大(79%)。2014年南麂列岛海域甲藻孢囊丰度较低,每毫升沉积物能检测出2—33个;夏、秋季的孢囊丰富度较高;岙口等相对开放海域的孢囊丰度明显高于岙内各站点。值得注意的是,三种有毒甲藻孢囊,塔玛/相似亚历山大藻(Alexandrium tamarense/affine),具刺膝沟藻(Gonyaulax spinifera)和多边舌甲藻(Lingulodinium polyedra)的孢囊也在样品中检出,并且分别占春季、夏季和秋季孢囊总丰度的37%、23%和27%。本研究为完善南麂列岛甲藻的物种多样性提供了依据。     

胶州湾表层沉积物中甲藻孢囊的分布

为了解胶州湾表层沉积物中甲藻孢囊的分布特征,于2015年7月采集胶州湾12个站位的表层沉积物进行甲藻孢囊分析,共鉴定甲藻孢囊37种(分属5个类群)和2种未定种,包括自养型20种和异养型17种,优势种为膝沟藻。其Shannon-Wiener多样性指数[H′(log2)]介于2.84—3.91,平均值为3.42;均匀度指数介于0.75—0.98,平均值为0.88,总体值较高。胶州湾海域各站位的甲藻孢囊丰度介于96—969cyst/g DW(干重),平均丰度为401cyst/g DW,呈现出临近湾口处丰度较高,而湾内较低的空间分布差异特征。尤其值得注意的是,有两种产虾夷扇贝毒素(Yessotoxin,YTX)甲藻[具刺膝沟藻(Gonyaulax spinifera)和多边舌甲藻(Lingulodinium polyedrum)]的孢囊和3种产麻痹性贝类毒素(PSP)甲藻[塔玛/链状亚历山大藻(Alexandrium catenella/tamarense)、微小/相似亚历山大藻(A.minutum/affine)和链状裸甲藻(Gymnodinium catenatum)]的孢囊在胶州湾海域大多数站位均有分布,尽管其数量不高,但其广泛的分布范围仍需引起我们的重视。     

北黄海表层沉积物中甲藻孢囊的分布特征

2009年和2010年采集北黄海15个站位的表层沉积物样品进行甲藻孢囊分析,共鉴定出甲藻孢囊28种(隶属13个属)和2种未定种,优势种为膝沟藻(Gonyaulax spp.)、塔马/链状亚历山大藻(Alexandriumcatenella/tamarense)和微小/相似亚历山大藻(Alexandrium minutu...     

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.