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1.
本文研究了L-多巴、多巴胺、肾上腺素、去甲肾上腺素等儿茶酚胺类物质对魁蚶幼虫的变态诱导作用。结果显示:10-4mol/L的L-多巴有较为显著的诱导能力，而各浓度组多巴胺都不能诱导幼虫变态,且高浓度L-多巴和多巴胺对幼虫有毒害效应。10-4-10-6mol/L的肾上腺素和去甲肾上腺素都能表现出诱导作用并且对幼虫无害,为应用于魁蚶的苗种生产提供了可能。 相似文献
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使用γ-氨基丁酸(γ-aminobutyric acid, GABA)、氯化钾和5-羟色胺,进行羊鲍(Haliotis ovina)幼虫存活、附着和变态过程中的诱导实验。结果表明,γ-氨基丁酸对羊鲍幼虫存活、附着及变态都有促进作用。γ-氨基丁酸浓度为10–4mol/L时处理72h的附着率(26.27%)和变态率(22.26%)高于其他组别, 10–6mol/L处理72h存活率(30.84%)高于其他组别。氯化钾能在高浓度(10–2—10–3mol/L)下诱导附着,而对变态和存活没有影响。氯化钾浓度为10–3mol/L处理时间为24h和72h的附着率高于其他组别,分别为11.3%和16.4%。5-羟色胺可诱导附着和变态,对幼虫的存活无影响或有抑制作用。5-羟色胺浓度为10–5mol/L处理72h的附着率(20.73%)和变态率(20.18%)高于其他组别。因此,γ-氨基丁酸可作为羊鲍育种培育过程的有效诱导剂,可以应用推广于羊鲍幼虫的培育过程乃至大规模生产养殖中。 相似文献
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几种神经活性物质对海湾扇贝幼虫变态诱导作用的研究 总被引：14，自引：3，他引：11
本文研究了儿茶酚胺类和金属离子对海湾扇贝幼虫变态的诱导作用,结果显示;外加10-4-10-6mol/dm3的肾上腺素,10-5mol/dm3的去甲肾上腺素和L-多巴具有十分显着的诱导能力;外加10-15mmol/dm3K+和Ca2+处理幼虫一段时间后,对其变态有明显促进作用。实验研究了最适浓度下肾上腺素、L-多巴和KCl不同处理时间对幼虫变态的影响,表明幼虫对肾上腺素和L-多巴表现出很高的敏感性,而对KCl则表现出对时间和剂量较强的依赖性。 相似文献
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几种化学物质对两种牡蛎幼虫附着和变态的诱导 总被引：4，自引：1，他引：4
本文研究5种神经递质和1种神经肽对两种牡蛎幼虫附着和变态的诱导效应。结果表明：L－多巴对牡蛎幼虫附着行为的诱导快速而有效，浓度10μmol/dm^3，2h内有附着行为的幼虫约占50％，并使之正常变态，肾上腺素、去甲肾上腺素和L－多巴均能有效地诱导两种牡蛎幼虫变态，它们的最适诱导浓度分别为50、50和5μmol/dm^3，诱导变态率分别达97．1％、90．6％和70．5％（长牡蛎），74．9％、74．3％和37．2％（僧帽牡蛎）；多巴胺的诱导变态效果不显著，而γ－氨基丁酸和5－羟色胺不能有效诱导变态。两种牡蛎幼虫对上述有效诱导药物的反应，长牡蛎优于僧帽牡蛎。肾上腺素诱导长牡蛎，最适处理时机在眼点幼虫后期，持续处理时间为2h之内。 相似文献
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两种东风螺幼虫附着和变态的化学诱导研究 总被引：15，自引：1，他引：15
在持续24h作用下,12×10-3mol/dm3 K+可有效地诱导台湾东风螺(Babylonia formosae)和方斑东风螺(B.aerolata)的浮游幼虫90%以上完全变态.持续作用24h,15×10-3mol/dm3 K+对方斑东风螺幼虫有毒害作用,但作用12h可取得较好的诱导效果.增加K+诱导变态的稚贝能正常活动和摄食.增加K+诱导的幼虫变态率随幼虫平均壳高的增大而提高.L-多巴、肾上腺素和去甲肾上腺素在5.5×10-6～5.5×l0-5mol/dm3时对方斑东风螺幼虫的变态无诱导活性,而多巴胺在10-4mol/dm3时可诱导较12×10-3mol/dm3 K+约少一半的变态率.钾通道阻滞剂TEA对K+诱导两种东风螺幼虫变态无阻抑作用.根据添加KCl诱导幼虫变态试验结果,初步认为幼虫获得变态能力时的壳高,在台湾东风螺是860.2～1009.8μm,在方斑东风螺是849.6～956.0μm.两种东风螺的浮游幼虫均有变态延迟现象. 相似文献
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《海洋湖沼通报》2016,(5)
以不同浓度的氯化钾(KCl)和γ-氨基丁酸(GABA)处理皱纹盘鲍后期面盘幼虫,处理不同时间后,观察并分析KCl和GABA对皱纹盘鲍幼虫附着变态的诱导作用。结果表明,低浓度组,KCl(10mmol/L、12h)和GABA(10~(-6) mmol/L、6和12h)均可显著提高其附着和变态率,GABA组诱导效果优于KCl组,GABA(10~(-6) mmol/L、6h)处理组优于12h处理组。高浓度组,KCl(100、200和300mmol/L)和GABA(10~(-4)、10~(-3)和10~(-2) mmol/L)随着浓度的提升和诱导时间的延长,幼虫附着变态率降低,死亡率升高。综合考虑附着率、变态率、死亡率及实验成本等因素,低浓度的KCl(10mmol/L、12h)和GABA(10-6 mmol/L、6h)都可以广泛应用于生产中,来提高幼虫的附着变态率,增加发育的同步性,降低死亡率。 相似文献
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以不同浓度的氯化钾(KCl)和γ-氨基丁酸(GABA)处理皱纹盘鲍后期面盘幼虫,处理不同时间后,观察并分析KCl和GABA对皱纹盘鲍幼虫附着变态的诱导作用。结果表明,低浓度组,KCl(10mmol/L、12h)和GABA(10-6 mmol/L、6和12h)均可显著提高其附着和变态率,GABA组诱导效果优于KCl组,GABA(10~(-6) mmol/L、6h)处理组优于12h处理组。高浓度组,KCl(100、200和300mmol/L)和GABA(10~(-4)、10~(-3)和10~(-2) mmol/L)随着浓度的提升和诱导时间的延长,幼虫附着变态率降低,死亡率升高。综合考虑附着率、变态率、死亡率及实验成本等因素,低浓度的KCl(10 mmol/L、12h)和GABA(10~(-6) mmol/L、6h)都可以广泛应用于生产中,来提高幼虫的附着变态率,增加发育的同步性,降低死亡率。 相似文献
8.
L-DOPA对西施舌眼点幼虫附着变态诱导的研究 总被引：2，自引：0，他引：2
采用试验水体中添加化学诱导物的方法研究L-DOPA(L-多巴)对西施舌(Coelomctraantiquata)眼点幼虫附着变态的诱导作用。结果表明,L-DOPA能诱导西施舌眼点幼虫变态,但对其附着的诱导效果不明显。用直径小于1 mm的细沙为附着基质,1×10-6mol/L的L-DOPA处理西施舌眼点幼虫12 h,变态率为73.3%,对照组为62.6%。浓度为1×10-7mol/L的L-DOPA处理西施舌幼虫12 h,生长速率为25.6%,对照组为14.7%,表明适当浓度的L-DOPA能促进西施舌幼虫的生长。在无沙附着的条件下,西施舌幼虫可正常附着变态,但生长速率较低且变态后死亡率高。 相似文献
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报道了KCl对方斑东风螺(Babylonia aerolato Link)浮游幼虫变态的诱导作用.结果表明,在水体200 mL,幼虫20只,KCl连续作用12 h的条件下,当KCl浓度不超过8×10-3 mol/L且幼虫日龄小于12 d时,诱导变态率为0～15%,诱导效果不稳定;当KCl浓度达到11×10-3 mol/L且幼虫日龄达到15 d时,浮游幼虫变态率超过95%.在水体850 L,幼虫2.0×105～2.5×105只,KCl连续作用9 h的条件下,KCl浓度为17×10-3mol/L,日龄15 d的幼虫变态率达90%.浮游幼虫日龄越大,KCl添加浓度越高,作用时间越长,KCl诱导变态作用越明显.KCl对方斑东风螺幼虫有毒性作用,日龄越小,浓度越大,作用时间越长,毒性越大.日龄12 d的浮游幼虫,KCl添加浓度11×10-3mol/L作用20 h诱导变态的稚螺,未发现其生长和存活受到KCl的不良影响.综合本实验的结果,KCl诱导变态较为安全有效的条件是:浮游幼虫日龄不小于15 d,添加浓度11×10-3～14×10-3 mol/L,作用时间不超过12 h. 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
18.
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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