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对29种(株)海洋微藻进行不充气培养,用Bligh-Dyer法提取总脂,皂化后氯仿和正己烷(体积比为1:4)提取甾醇,BSTFA衍生后用岛津QP2010气相色谱-质谱分析仪进行GC/MS分析.从29种海洋微藻中共检测到47种甾类化合物,鉴定出36种甾醇和一种甾酮.其中,4位无甲基Δ5甾醇在所有的微藻中均有分布,一些高等生物中常见的甾醇如胆甾醇、菜子甾醇、菜油甾醇、豆甾醇、谷甾醇和褐藻中常见的岩藻甾醇等,在微藻中均有广泛的分布.相对而言,4位无甲基5位饱和甾(烷)醇、4-甲基甾(烷)醇和双羟基甾醇的分布则相对较少,其中许多甾醇如甲藻甾醇、巴夫甾醇、C27:2(Δ5,22/24Me)和C28:3(Δ5,7,22/24Me)等,只在一种藻或同一纲的微藻中被检测到,可以作为对应微藻或对应纲微藻的特征甾醇.认为海洋微藻甾醇的研究可以为海洋微藻化学分类学及饵料营养学研究提供重要参考依据. 相似文献
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一种饵料微藻的脂肪酸甾醇分析及化学分类的探讨 总被引：5，自引：1，他引：5
对一种重要的未知生物饵料微藻在充气和瓶中静态两种生态条件下进行培养,设计了一种分步衍生化脂肪酸与甾醇的GC/MS连续分析法,对微藻脂肪酸甾醇进行了定性和定量分析,结果表明,这种微藻主要含有丰富的二十碳五烯酸(EPA),C14:0,C16:0,C16:1以及一定量的二十二碳六烯酸(DHA),C22:5(n-6)和C18不饱和脂肪酸;共鉴定出11种甾醇组分,主要是24-甲基(乙基)胆甾醇,碳数分布从27到30,特别含有甲基巴夫甾醇和乙基巴夫甾醇;可以把这种微藻归到Prymnesiophyceae纲Pavlovales目Pavlovaceae科.通过实例分析证明,脂类分析结果可以作为海洋微藻化学分类学的一个重要依据. 相似文献
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巴夫藻脂肪酸和奋醇的同步测定研究 总被引：4，自引：0，他引：4
建立了一种脂肪酸甾醇分步衍生气相色谱／质谱(GC／MS)同步分析新方法，使用一份干质量约20mg的巴夫藻(Pavlova virdis)样品，采用SPB-5色谱柱，在岛津QP2010气相色谱／质谱联用分析仪上，实现可靠的定量定性分析。方法回收率为93％～107％；方法的重现性较好，各组分3次测定结果的标准相对偏差都小于10％；方法的检测限为3．5ng。选取巴夫藻(Pavlova sp．)进行分析，可初步确定出26种脂肪酸和10种甾类化合物以及它们的含量。 相似文献
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将瘤背石磺(Onchidium struma)、里氏拟石磺(Paraoncidium reevesii)、平疣桑椹石磺(Platevindex mortoni)和紫色疣石磺(Peronia verruculata)样品,经活体解剖取四种石磺肌肉组织,运用高效液相色谱法对其可食部分进行了胆甾醇含量测定。结果表明:瘤背石磺胆甾醇平均浓度最高,达5 870.00 mg/kg;平疣桑椹石磺、紫色疣石磺、里氏拟石磺的胆甾醇平均质量分别为3 480.00、388.00、316.00 mg/kg,统计分析显示四种石磺可食部分的胆甾醇含量差异显著。 相似文献
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应用色谱－质谱（GC－MS）方法分别鉴定了从广西海涠洲岛水域和海南省陵水县水域采集的莳萝曲网海绵Sigmadocia cymiformis的甾醇类化合物,涠洲岛水域的莳萝曲网海绵所含的旮醇类化合物主要是：胆甾－4，6－二烯3β－醇（1），27－降麦角甾5，22－二烯－3β－醇，（2），胆甾醇（3），（24S）－麦角甾5，22－二烯3β－醇（40，麦角甾5－烯C－3β－醇（5），麦角甾－2，22－二烯－3β－醇（6），豆甾醇（7），β－谷甾醇（8），麦角甾－4，24（28）－二烯－3－酮（9），柳珊瑚甾醇（10）；而陵水县水域的莳萝曲网海绵所含甾醇类化合物主要是：（3），（4），（5），（6），（8），胆甾－2，55－二烯－3β－醇（11），胆旨－3，5－二烯－7－酮（12），这是莳萝曲网海绵中甾醇类化合物组成的首次报道。 相似文献
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瓷海星科是一类深海底栖海星，广泛分布于全球大洋深海中。其模式种蓝泥瓷海星（Porcellanaster ceruleus Wyville Thomson 1878）具有全球分布性与多态性。本文报道了该物种在中国海的首次记录。2015年6月6日，在向阳红10号执行的南海底栖生物调查航次中，于C19站位（10.15°N，110.03°E；水深1400m）由三角形拖网采集到海星一只，经鉴定为蓝泥瓷海星。本文提供了该样品的形态描述与细节照片，讨论了其与该种模式样品的共同形态特征及个体差异，并总结了蓝泥瓷海星的全球分布记录。该种在中国海的首次发现，进一步拓展了其地理分布范围。 相似文献
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长得像一个五角星，其体外附着一层坚硬的石灰甲，并带有美丽色彩的海洋棘皮动物海星，是以贝壳类小动物为食物的。进餐时，海星先将贝类包住，然后从口中翻出胃来，再从胃里分泌出一种液体，使贝类麻醉而张开贝壳，最后，就可吃掉贝类的肉。因此，养殖贝类的渔民们往往想方设法消灭海星。起初，他们以为只要把海星撕碎就可以消灭它，没想到海星繁殖得更多了。这到底是怎么回事呢？原来，海星的再生功能很强。因为它的行动又笨又慢，所以常常会被鱼、鸟撕碎，它的这种本领就是它的防御和繁殖的手段。它的再生能力是如此之强，以致只要还有一个腕，过了几天就能再生出４个小腕和１个小口，再过一个月时间，旧腕脱落，又再生一个小腕，于是，一个五腕的海星得以重现。人们在海滨经常可以看到“断腿断臂”的海星，就是受过伤正在再生的海星。其实，这种再生能力在低等动物中很常见。壁虎被敌人追赶紧迫时，能够断尾而逃。以保全性命。过上一段时间，断尾的壁虎又能重新长出一条新尾巴。一到冬天，章鱼就潜入海底，为了生存，它开始吃自己的脚爪。直到把八只脚爪都吃完为止，然后就闭眼不动了，等到第二年春天，它又长出八条新的脚爪。海参遇到敌害时，可以把自己趁机逃之夭夭，大约５０天后，它可以再生出一... 相似文献
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柄海鞘Styela clava中的甾醇化合物的分离和鉴定 总被引：2，自引：0，他引：2
应用GC-MS技术从青岛海域产柄海鞘Styela
clava中分离鉴定出5种甾醇化合物,分别是(22Z)-26,27-二降-麦角甾-5,22-二烯-3β-醇(1),胆甾-5,22-二稀-3β-醇(2),胆甾醇(3),胆甾烷醇(4),(22E)-麦角甾-5,22-二烯-3β-醇(5)。 相似文献
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Chandralata Raghukumar G. Sheelu P. A. Loka Bharathi Shanta Nair C. Mohandass 《Marine Georesources & Geotechnology》2001,19(1):1-16
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. 相似文献
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Derek V. Ellis 《Marine Georesources & Geotechnology》2001,19(1):51-63
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. 相似文献
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G. Parthiban 《Marine Georesources & Geotechnology》2000,18(3):223-235
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. 相似文献
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Arne Schnack-Friedrichsen Angela M. Davis Jim D. Bennell Dei G. Huws 《Marine Georesources & Geotechnology》2001,19(4):221-243
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. 相似文献
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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. 相似文献
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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。 相似文献
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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. 相似文献
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Shigehisa Nakamura 《Marine Geodesy》2000,23(1):55-61
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. 相似文献
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