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1.
Mian状黄姑鱼胚胎和仔鱼发育的实验生态 总被引：1，自引：0，他引：1
本实验研究了温度、盐度、ＰＨ对Ｍｉａｎ状黄姑鱼胚胎发育和前期仔鱼存活的影响。结果表明,Ｍｉａｎ状黄姑鱼受精卵孵化的温度范围为１５￣３０℃,最适孵化温度为２５￣３０℃;孵化盐度范围来１５￣４５,最适孵化盐度范围为１５￣２５;ＰＨ值在５．００￣８．９９范围内,受精卵孵化率没有显著的差异。Ｍｉａｎ状黄姑鱼前期仔鱼存活的适合温度为１５￣３０℃,最适温度为２５℃;适合工为１５￣３５;适合ＰＨ值为５．９９￣１ 相似文献
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1996年3~6月采用人工注射LRH-A和HCG诱导状黄姑鱼自然产卵受精,观察6批次胚胎发育的结构特征和1~16日龄仔鱼形态变化及温度、盐度对状黄姑鱼早期发育和存活的影响,为状黄姑鱼大规模人工繁殖和苗种培育提供科学依据。根据其外部形态和胚胎行为的出现将状黄姑鱼胚胎发育划分为17期,3日龄开口;状黄姑鱼受精卵孵化的温度范围为16.3~30℃,最适孵化温度为22~24℃;孵化盐度范围为13.7~53,最适孵化盐度范围为26.9~40.7,其中盐度为7.2时受精卵无法孵化,盐度在40.7以上的受精卵全部为浮性,盐度为26.9以下全部呈沉性;状黄姑鱼仔鱼存活的适合盐度为20.2~33.4,随着仔鱼的生长,对耐盐的适应性也逐渐增强。 相似文献
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观察比较了不同盐度梯度海水下双棘黄姑鱼(Nibeadiacanthus)受精卵的孵化率和畸形率,并测定初孵仔鱼不投饵存活系数(Is,a)。结果表明:(1)双棘黄姑鱼受精卵在盐度15.0～43.0均可孵化,最适盐度为31.0～35.0。盐度高于35.0,孵化率随盐度的升高而降低,仔鱼畸形率则随之升高。盐度低于27.0,孵化率随盐度的降低而降低,仔鱼畸形率则随之升高。(2)盐度为15.0,19.0,23.0,27.0,30.0～33.0的仔鱼不投饵存活系数为4.42～7.13;而盐度为35.0,39.0,43.0的仔鱼不投饵存活系数为1.67～4.48,盐度从35.0~39.0是对双棘黄姑鱼仔鱼Is,a值影响很大的盐度梯度。 相似文献
4.
黄姑鱼胚胎发育及其与温度和盐度的关系 总被引：1，自引：0，他引：1
为研究温度和盐度对黄姑鱼(Nibea albiflora)胚胎发育的影响,作者观察了黄姑鱼受精卵的形态和胚胎发育过程。实验结果表明,温度18~28℃范围内,温度对孵化时间和初孵仔鱼有显著影响,对孵化率影响不大,24~28℃是黄姑鱼胚胎发育的适宜温度范围;盐度低于24时受精卵下沉,26~28内悬浮于水体中,盐度高于34时受精卵浮于水面;黄姑鱼胚胎发育的最适盐度范围26~32,盐度超过或低于其适宜范围时,孵化率明显下降或者幼虫畸形率明显增大。另外,根据其Q10值推算的胚胎发育的适宜水温与实验结果相似。 相似文献
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Mian状黄姑鱼的早期发育研究 总被引：13，自引：2，他引：11
本文对Ｍｉａｎ状黄姑鱼的胚胎和仔、稚鱼各发育阶段的形态特征进行了描述。Ｍｉａｎ状黄姑鱼的爱精卵的为圆球形浮性卵,无色透明。在水温２０￣２３℃,盐度２６￣３０的条件下,经２４ｈ３５ｍｉｎ陆续孵出仔鱼。胚胎发育分为２６期。初孵仔鱼至孵化后４日龄为仔鱼前期;孵化后５￣２２日龄为仔鱼后期;孵化后２３￣３２日龄为雅鱼期;孵化后３３日龄进入幼鱼早期。仔、稚鱼培育水温１８￣２８℃,盐度２０￣３０。仔鱼２日龄稍开 相似文献
6.
温度、盐度及pH对斜带石斑鱼受精卵孵化和仔鱼活力的影响 总被引：28，自引：0，他引：28
比较观察了不同温度(20、22、24、26、28、30和32℃)、不同盐度(5、10、15、20、25、30、35、40和45)及不同pH(5.0、5.5、6.0、6.5、7.0、7.5、8.0、8.5、9.0和9.5)下斜带石斑鱼Epinephelus coioides受精卵的培育周期、孵化周期、孵化率和畸形率。在以上各种条件下对斜带石斑鱼初孵仔鱼进行耐饥饿试验,测定其不投饵存活系数(Survival activity index,SAI)。结果表明,斜带石斑鱼受精卵孵化的适宜温度范围是24—30℃,最适温度范围是24—26℃;受精卵孵化的适宜盐度范围是15—45,最适盐度范围是20—30;受精卵孵化的适宜pH范围是5.5—8.5,最适pH范围是6.5—7.5。仔鱼生存的适宜温度范围是24—32℃,最适温度范围是24—26℃;仔鱼生存的适宜盐度为10—40,最适生存盐度为15—30;仔鱼生存的适宜pH是5.5—9.0,而最适pH是7.0—8.5。斜带石斑鱼受精卵和仔鱼对以上3种环境因子的耐受范围基本相同。 相似文献
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四种重金属对鮸状黄姑鱼胚胎和仔鱼的毒性 总被引：23，自引：0，他引：23
本文研究了汞、铜、锌和铬四种重金属对鮸状黄姑鱼（Ｎｉｂｅａ ｍｉ－ ｉｃｈｔｈｉｏｉｄｅｓ）胚胎发育和仔鱼存活的影响。结果表明;在试验浓度范围内,胚胎发育受 阻,受精卵孵化率显著低于对照组,初孵仔鱼出现不同程度的畸形,这些重金属对鮸 状黄姑鱼仔鱼的毒性强弱依次为Ｈｇ~２＋＞Ｃｕ~２＋＞Ｚｎ２＋＞Ｃｒ~６＋。根据实验数据求得四种 重金属对鮸状黄姑鱼仔鱼的２４、４８、７２和９６ｈ ＬＣ_５０值及安全浓度。 相似文献
10.
温盐度对斜带髭鲷孵化率及仔鱼存活率的影响 总被引：10，自引：2，他引：8
本文对不同温、盐度梯度下斜带髭鲷的孵化情况进行探讨,结果表明：（１）斜带髭鲷的适宜孵化温度为１９－２５℃,最知温度为２３－２５℃。（２）适宜盐度为１６．３－３４．７,最适盐度为２４．２－３２．１,尤以２９．５为好。（３）当温度为２３℃,直２９．５,ＰＨ值为８．１－８．３时,幼体孵化率最高,达９３．３％,（４）温度２２．６－２３．４℃,盐度２４．２－３２．１,４２ｈ孵出的仔鱼至５２ｈ存活率高于８１ 相似文献
11.
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
12.
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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Coastal inundation associated with extreme sea levels is the main factor which leads to the loss of life and property whenever a severe tropical cyclonic storm hits the Indian coasts. The Andhra and Orissa coasts are most vulnerable for coastal inundation due to extreme rise in sea levels associated with tropical cyclones. Loss of life may be minimized if extreme sea levels and associated coastal flooding is predicted well in advance. Keeping this in view, location specific coastal inundation models are developed and applied for the Andhra and Orissa coasts of India. Several numerical experiments are carried out using the data of past severe cyclones that struck these regions. The simulated inland inundation distances are found to be in general agreement with the reported flooding. 相似文献
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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. 相似文献
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《海洋学报(英文版)》2014,(8):F0003-F0003
<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, 相似文献
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Nabil Sultan Pierre Cochonat Jean Fran ois Bourillet Florence Cayocca 《Marine Georesources & Geotechnology》2001,19(2):107-133
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. 相似文献
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Shigehisa Nakamura 《Marine Geodesy》2001,24(1):27-33
This article concerns an interrelation between the sea levels and the western boundary flow near a tectonic boundary in a local zone in the Northwestern Pacific. In this zone, sea level variations at stations located on the coast facing the Pacific are studied to find the interrelation between variations of the Kurosio flow as an index of the distance of the flow axis off a specific coast. The result is discussed after data processing of the monthly means of the sea levels, and a notice is taken of variations caused by active crustal upheavals during a seismic event, a local earthquake. 相似文献
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Hoi-Soo Jung Kap-Sik Jeong Yong-Shik Chu Sung-Hyun Park Ki-Hyune Kim 《Marine Georesources & Geotechnology》2001,19(3):181-195
Grain size and water content in box-core sediments from the Clarion-Clipperton fracture zone (C-C zone) in the northeast equatorial Pacific were analyzed in detail to understand the downcore variations across a hiatus between Quaternary and Tertiary layers. Grain-size distributions in the topmost core sediments show two modes: a coarse mode (peaked at 50 μm) and a fine mode (at 2-25 μm). The coarse mode disappears gradually with depth accompanied by the dissolution of siliceous fossil tests, whereas the fine mode coarsens due to the formation of authigenic minerals. Water content increases abruptly across a color boundary between an upper pale brown layer and a lower dark brown layer that is the hiatus between Quaternary and Tertiary layers. Abundant smectites and microvoid molds, which are created by the prolonged fossil dissolution in the underlying sediment, are attributed for the abrupt downcore variation of water content. Overall variations in grain size and water content in the topmost core sediments in the western C-C zone are possibly constrained by the dissolution of biogenic siliceous fossils. Variations in geotechnical properties related to these changes must be considered in the design of nodule collectors. 相似文献
20.
This study tests the hypothesis that the in situ void ratio of surficial marine sediments may be predicted from shear wave velocity-depth data with a reliability equal to that of other methods currently available. Shear wave velocity is fundamentally controlled by the number of grain-to-grain contacts per unit volume of material and by the effective stress across those contacts. In this study, three previously established empirical formulae are used to predict void ratio from velocity-depth data. Field data were acquired along a transect off the northern Californian coast across which water depth increased from 35 to 70 m and seafloor sediment type varied from sand to silty-sand, respectively. A towed seafloor sled device was used to collect shear wave refraction data, and a marked, systematic decrease in velocity was observed along the line, ranging from 35-70 m/s for the coarse, near-shore material to 25-40 m/s for the finer, offshore deposits. Void ratios predicted from these velocities were compared with data measured directly from box-core samples. Of the formulae used for prediction, two agree remarkably well with the control data. Both predicted and control values increase from 0.6-0.8 for the sandy material to 1.1-1.5 for the silty-sand. Thus, this study does not disprove the hypothesis set and demonstrates the potential of field shear wave velocity-depth data as a means of delineating spatial variation in void ratio for surficial marine sediments in a remote, nondestructive manner. 相似文献