4 种经济海藻脂肪酸组成分析

采用改进的Bligh-Dyer法提取脂溶性成分,气相色谱-质谱联用法(GC-MS)进行分离和鉴定,C19:0内标确定总脂及各组分含量,研究了鼠尾藻(Sargassum thunbergii)、浒苔(Enteromorpha prolifera)、龙须菜(Gracilaria lemaneiformis)和红毛菜(Bangia sp.)4种经济海藻的脂肪酸组成及含量。结果表明,4种海藻都检测出C14-C22脂肪酸,总脂含量在12～19 mg/g之间,不饱和脂肪酸为主要组成成分,含量均超过60%。不饱和脂肪酸中以多不饱和脂肪酸(PUFAs)为主,富含n-3和n-6系列PUFAs,n-6与n-3系列PUFAs之比均低于2。比较4种海藻脂肪酸组成特点表明,鼠尾藻以C16、C18和C20为主要组成成分,具褐藻类脂肪酸组成特征;浒苔以C16和C18为主要组成成分,具绿藻类脂肪酸组成特征;龙须菜和红毛菜以C16和C20类脂肪酸为主,具典型红藻类脂肪酸组成特征,同时二者又有不同之处,分别显示真红藻与原始红藻脂肪酸组成的特点。     

十四株海洋微藻脂肪酸组成的研究

对 4个门的 14株 (红藻门 8株 ,甲藻门 1株 ,隐藻门 2株 ,绿藻门 3株 )海洋微藻进行了脂肪酸含量测定 ,微藻在确定的条件下生长 ,指数生长末期收获。结果表明 ,各门的微藻都有其独特的脂肪酸特征 :红藻中含有大量的 2 0 :4 n- 6和 2 0 :5n- 3,其中紫球藻 R2 5含量最高 ,占总脂肪酸的4 9.8% (AA占总脂肪酸的 2 0 .5% ,EPA占总脂肪酸的 2 9.3% )。隐藻的主要脂肪酸是 16 :0、18:1n- 9、18:3n- 3、18:4 n- 3、2 0 :5n- 3、2 2 :5n- 3。与其它甲藻有别的虫黄藻 ,18:4 n- 3含量很少并且不含EPA,其主要合成的是 16 :0、18:1n- 9和 2 2 :6 n- 3。 C16和 C18的不饱和脂肪酸是本实验研究的 3株绿藻的主要脂肪酸     

30种海洋绿藻的脂肪酸分类与评价

以平方欧氏距离为相似性测度，类间距用离差平方和法，对11属30株海洋绿藻所含脂肪酸进行聚类分析，结果分为5类。类I含EPA和DHA最高；类Ⅳ含总(n-3)PUFAs最高。混合培养小球藻C95，C97与杜氏藻C33，C42，可能得到EPA，DHA和其它（n-3)PUFAs含量最丰的绿藻种群。系统聚类分析为海洋绿藻分类与量化评价提供了一种好方法。     

7种(13株)杜氏藻的总脂含量和脂肪酸组成

在实验室条件下培养7种(13株)杜氏藻(Dunaliella),在生长的平衡期收获.分别采用索氏提取法和气相色谱法进行了总脂含量和脂肪酸组成的测定.它们的总脂含量在6.64%~16.18%(m/m,干重,下同)之间,其中7株的总脂含量超过10%.杜氏藻的16碳和18碳脂肪酸含量丰富,有着较高的C16∶0、C18∶1(n-12)、C18∶2(n-6)和C18∶3(n-3)脂肪酸,其中8株的不饱和脂肪酸含量超过总脂肪酸的50%.杜氏藻的EPA和DHA的含量较低,但是有5株超过总脂肪酸的10%.     

30株海洋绿藻的总脂含量和脂肪酸组成

对 11属 (小球藻属、绿囊藻属、微绿球藻属、海绿球藻属、卵胞藻属、原球藻属、咸胞藻属、杜氏藻属、裂丝藻属、塔胞藻属和衣藻属 )的 30株海洋绿藻进行特定条件下的一次性培养 ,在指数生长末期收获 ,进行了总脂含量和脂肪酸组成的分析。 2 1株海洋绿藻的总脂含量超过干重的10 % ,达 11.6 1%～ 34.4 9% ,其它 9株在 4 .2 5%～ 9.4 8%之间 ,绿藻的 16碳和 18碳脂肪酸最为丰富 ,有着含量较高的 16∶ 0、16∶ (n- 3)、18∶ 2 (n- 6 )和 18∶ 3(n- 3)脂肪酸。两株小球藻 (C95,C97)的2 0∶ 5(n- 3)脂肪酸含量较高 ,分别为 2 0 .8%和 2 6 .1%。另一株小球藻 (C10 2 )和两株裂丝藻 (C19和C2 0 ) EPA含量居中 ,分别为 8.0 % ,6 .0 %和 8.1%。其它藻株一般只含有少量的 2 0∶ 5(n- 3)和 2 2∶ 6 (n- 3)或不含 2 2∶ 6 (n- 3)     

螺旋藻硫酸喹诺糖二酰基甘油酯脂肪酸分子组成分析

本文采用硅胶柱层析法 ,从螺旋藻总脂中分离提取出硫酸喹诺糖二酰甘油酯 (SQDG) ,通过高压液相色谱 (HPL C)分离纯化得到 7个主要组分。采用气相色谱法 ,分析 SQDG中脂肪酸的含量和分子组成。结果表明 ,SQDG中主要脂肪酸为 16 :0 ,18:3n- 6 ,18:2 n- 6 ,而花生四稀酸 (2 0 :4 )及EPA(2 0 :5 )的含量要低于其他几种红藻和褐藻 ,未发现 16 :2。 SQDG中 sn- 1位 79%为不饱和脂肪酸 ,95 %以上的 sn- 2位脂肪酸为 16 :0。根据测得的 7种组分的含量和 sn- 1和 sn- 2位脂肪酸的分析计算可得 ,SQDG主要分子组成为 5 2 %～ 5 7% (18:2 ,16 :0 ) ,11% (16 :0 ,16 :0 ) ,7.1% (16 :1,16 :0 ) ,7.7% (18:1,16 :0 )     

海洋微藻Chlorella sp．1061的脂类特征与分类探讨

采用生化分析方法研究了海洋微藻Chlorella sp．1061色素、极性脂及其脂肪酸组成特点。结果表明，Chlorella sp．1061色素、极性脂及其脂肪酸组成均与小球藻属的其它藻类存在着很大差异。绿藻纲中的主要化合物，如叶绿素b、十六碳四烯酸[16：4(n-3)]和亚麻酸[18：3(n-3)]均未在Chlorella sp．1061中检测到。从Chlorella sp．1061中分离到占总极性甘油脂8mol％的甜菜碱-1，2-二酰基甘油一O-4’-(N，N，N-三甲基)高丝氨酸(DGTS)，并从半乳糖脂和DGTS等极性甘油脂中检测到大量的二十碳五烯酸[20：5(n-3)](EPA)。但是一般认为，小球藻属藻类中不含这两种化合物。根据Chlorella sp．1061的这些特点，作者认为它不应该被归到小球藻属中。由于Chlorella sp．1061在色素、极性甘油脂及其脂肪酸组成特征方面与大眼藻纲(Eustigmatophyceae)中的拟微绿球藻(Nannochloropsis)非常相似，因此，Chlorella sp．1061可能是Nannochloropsis中的一个种。     

四种绿藻和四种褐藻脂肪酸组成的比较研究

对绿藻门和褐藻门8种大型海藻的脂肪酸组成进行了研究,发现两类海藻都有其特征脂肪酸或有几种特征脂肪酸组合做为其化学分类的标记。4种绿藻的主要脂肪酸是16:0、16:1ω7、18:4ω3、18:1ω7、18:2ω6、18:3ω3、18:1ω9,其中18:1ω7和18:3ω3的含量相对较高;4种褐藻中16:0、18:1ω9、18:2ω6、18:3ω3、18:4ω3、20:5ω3、20:4ω6的含量占绝对优势,十八碳和二十碳多不饱和脂肪酸是褐藻门脂肪酸的典型特征。另外,褐藻中含有较高含量的EPA,海带和裙带菜尤为明显。对2门类5属8株海藻所含脂肪酸进行聚类分析的结果显示海藻各门及种间的亲缘关系,表明利用静态条件下海藻脂肪酸的聚类分析结果,可在一定程度上判别海藻在分类上亲缘关系的远近,海藻脂肪酸组成的差异可以作为海藻分类的一个辅助技术手段。     

海水仔稚鱼必需脂肪酸--n-6系列高度不饱和脂肪酸研究概况

近些年来,国内外的研究证实,n3高度不饱和脂肪酸(n-3HUFA)是海水仔稚鱼的必需脂肪酸,它们是海水仔惟鱼正常生长和成活所必需的,尤其是廿碳五烯酸(EPA,20：5 n-3)和廿二碳六烯酸(DHA,22：6n-3)业已进行了大量的研究。这些脂肪酸的重要作用与它们在细胞膜磷脂结构中的特殊位置有关。此外,海水鱼不能把亚麻酸(18：3n-3)自身生物合成为EPA和DHA,所需要的EPA和DHA只能从饲料中摄取。     

大西洋庸鲽(Hippoglossus hipoglossus L.)精液脂肪酸分析及激素GnRHa诱导对其组成的影响

采用气相色谱检测的方法,进行大西洋庸鲽精液脂肪酸组成分析及激素GnRHa诱导对其组成影响的研究。结果表明,大西洋庸鲽精液中含量最高的脂肪酸种类为22:6n-3(DHA,二十二碳六烯酸),占总脂肪酸比例25.67%±0.94%;其次为16:0(PA,棕榈酸)、20:5n-3(EPA,二十碳五烯酸);重要必需不饱和脂肪酸20:4n-6(AA,花生四烯酸)含量较低,为1.76%±0.01%。精液中高不饱和脂肪酸(PUFA)含量较高,为44.25%±0.30%;饱和脂肪酸(SAT)含量为27.72%±0.22%。重要脂肪酸比例DHA/EPA为2.33±0.26;EPA/AA为6.30±0.51;n-3/n-6为9.22±0.60。激素诱导未对精液中脂肪酸组成产生显著影响。重要必需脂肪酸DHA、EPA、AA,以及n-3、n-6等重要种类的脂肪酸总量在激素诱导组与非诱导对照组样品间无显著差异;在激素诱导后的三个取样时间的样品间也无显著差异(P0.05)。     

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.     

A Review of Some Environmental Issues Affecting Marine Mining

This article reviews information recently available from existing marine and coastal mining for responses to environmental issues affecting marine mining at different depths. It is particularly but not exclusively concerned with those issues affecting seabed biodiversity impact and recovery. Much information has been gathered in the past 10 years from shallow mining operations for construction aggregate, diamonds, and gold, from coastal mines discharging tailings to shallow and deep water, and from experimental deep mining tests. The responses to issues identified are summarized in a series of eight tables intended to facilitate site-specific consideration. Since impacts can spread widely in the surface mixing layer SML, and can affect the biologically productive euphotic zone, the main issues considered arise from the depth of mining relative to the SML of the sea. Where mining is below the SML, the issue is whether it is environmentally better to bring the extraction products to the surface vessel for processing (and waste discharge), or to process the extraction products as much as possible on the seabed. Responses to the issues need to be sitespecific, and dependent on adequate preoperational environmental impact and recovery prediction. For deep tailings disposal from a surface vessel, there are four important environmental unknowns: (1) the possible growth of "marine snow" (bacterial flocs) utilizing the enormous quantities of fine tailings particles (hundreds or thousands of metric tons per day) as nuclei for growth, (2) the possibility that local keystone plankton and nekton species may migrate diurnally down to and beyond the depth of deep discharge and hence be subjected to tailings impact at depth, (3) the burrow-up capability of deep benthos and their ability to survive high rates of tailings deposition, and (4) the pattern and rate of dispersion of a tailings density current through the deep water column from discharge point to seabed. Actions to obtain relevant information in general and site-specifically are suggested.     

Increased Particle Fluxes at the INDEX Site Attributable to Simulated Benthic Disturbance

Particle fluxes were measured 7 m above the sea bottom during the predisturbance, disturbance, and postdisturbance periods by using time series sediment traps attached to seven deep-sea moorings deployed in the INDEX experiment site in the Central Indian Basin. The predisturbance particle fluxes varied between 22.3 to 55.1 mg m -2 day -1 . Increased and variable particle fluxes were recorded by the sediment traps during the disturbance period. The increase observed was 0.5 to 4 times more than the background predisturbance fluxes. The increases in particle fluxes (~4 times) recorded by the sediment trap located in the southwestern direction (DMS-1) were the greatest, which could be the result of preferential movement of resuspended particles generated during the deep-sea benthic disturbance along the general current direction prevailing in this area during the experimental period. Also, the traps located closer to the disturbance area recorded greater fluxes than did the traps far away, across the Deep Sea Sediment Resuspension System path. This variability in recorded particle fluxes by the traps around the disturbance area clearly indicates that physical characteristics such as grain size and density of the resuspended particles produced during the disturbance had an important effect on particle movement. The postdisturbance measurements during ~5 days showed a reduction in particle fluxes of ~50%, indicating rapid particle settlement.     

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.     

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.     

Determination of In Situ Sediment Shear Strength from Advanced Piston Corer Pullout Forces

The advanced piston corer (APC) has been used by the Ocean Drilling Program since 1985 for recovering soft sediments from the ocean floor. The pullout force measured on extracting the core barrel from the sediment is shown to correlate with the average shear strength of the sediment core measured in the ship's laboratory. A simple rule of thumb is derived relating the shear strength of the sediment to the pullout force. Multiple APC holes at individual sites allow the consistency of the pullout measurements to be assessed. The effects of different operational procedures during APC coring are also explored. Although generally applicable, the correlation between pullout force and laboratory measurements of shear strength breaks down for some APC holes, possibly because of the disturbance of some sediment types during the APC coring process. A better understanding of the physical process of APC coring, and its effect on the properties of the sediment both inside and immediately outside the core barrel, would indicate what confidence can be put on the measurement of pullout force as a way of evaluating the in situ shear strength of deep sea sediments.     

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.     

《Acta Oceanologica Sinica》Vol. 33(2014) contents

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