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《海洋湖沼通报》2016,(5)
对人工繁育的花鲈(Lateolabrax maculatus)早期发育阶段的形态特征及苗种培育技术进行了观察与研究。结果表明:在水温17±1℃、盐度30、pH8.0、溶解氧7.0mg/L的条件下,花鲈受精卵经过72h完成胚胎发育过程。在胚后发育阶段,根据卵黄囊体积、鳍条发育情况,将花鲈前期发育划分为仔鱼期、稚鱼期、幼鱼期;仔鱼期又可分为前期仔鱼和后期仔鱼。本文对培育过程中死亡率较高的仔鱼期进行了详细观察,发现在水温16~17℃,盐度30的海水中培育,初孵仔鱼至5日龄(day post hatching,dph)仔鱼是前期仔鱼,6~35dph为后期仔鱼。花鲈个体之间发育速度差异较大、仔鱼之间的残食现象是整个培育过程中比较明显的特征,这些特征与冬季水温较低造成的越冬困难一起限制了花鲈苗种的全人工繁育技术的建立。 相似文献
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犬齿牙鲆胚胎及仔、稚、幼鱼形态发育观察 总被引：1，自引：0，他引：1
犬齿牙鲆(Paralichthys dentatus)卵为端黄卵,受精卵浮性,卵径950~1100μm,油球径200~225μm.在水温20.5~22.0℃,盐度33条件下培育,受精后1 h 20 min 进入卵裂期,6 h 10 min 进入囊胚期,11 h 20 min 进入原肠胚期,19 h 10 min 发育到胚孔封闭期,胚体形成,26 h 50 min 尾芽出现,33 h 35 min心跳开始,48 h 10 min 开始孵化出仔鱼.初孵仔鱼平均全长2.59 mm±0.02 mm,在培育水温为17.0~21.0℃,盐度24~34条件下,胚后发育时序为:1日龄~9日龄为仔鱼前期,10日龄平均全长5.52 mm±0.05 mm,卵黄囊和油球完全吸收进入仔鱼后期;40日龄平均全长20.82 mm±0.67 mm,各鳍鳍条发育形成进入稚鱼期;65日龄平均全长41.13 mm±0.88 mm,全身鳞被完整进入幼鱼早期 相似文献
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《海洋科学》2010,(1)
作者对鮸鱼(Miichthys miiuy)的早期发育(从受精卵到45日龄幼鱼)形态特征及生态习性进行了描述。鮸鱼的受精卵在水温21.4℃~22.0℃,盐度25.7条件下,经过29 h30 min仔鱼孵出。从受精卵到仔鱼出膜可分为卵裂期、囊胚期、原肠期、胚体形成期等4个主要时期,然后进入胚后发育阶段。孵出后的3日龄仔鱼已能在水体中平游,极少数个体可开口摄食轮虫。4日龄仔鱼全部开口摄食,并对光反应敏感,出现明显的集群现象。22日龄的后期仔鱼各鳍鳍条发育形成,鳞片开始出现,进入到稚鱼期。39日龄后,鮸鱼全身披满细小的鳞片,全部分布于育苗池的底部,开始进入到幼鱼发育阶段。根据仔、稚、幼鱼形态特征和生活习性对鮸鱼的分类进行了探讨。 相似文献
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为掌握一套可行的七带石斑鱼(Epinephelus septemfasciatus)人工繁育操作规程、积累七带石斑鱼生物学资料和苗种培育技术经验,作者对七带石斑鱼早期发育各个发育阶段的形态特征及苗种培育进行了观察与研究。在水温23.5℃±0.5℃、盐度31、p H7.9~8.2、溶氧量6~8 mg/L的条件下,七带石斑鱼的受精卵历时31 h5 min完成胚胎发育过。胚胎发育可划分5个时期:卵裂期、囊胚期、原肠胚期、神经胚期和器官形成期。根据卵黄囊、第二背鳍棘与腹鳍棘、鳞片和体色的变化,七带石斑鱼胚后发育可划分为仔鱼期、稚鱼期、幼鱼期;仔鱼期又可分为前期仔鱼和后期仔鱼。在水温24~26℃,盐度28的海水中培育,初孵至2日龄(day post hatching,dph)仔鱼是前期仔鱼,3~30dph为后期仔鱼,31~57dph为稚鱼期,58dph进入幼鱼期。第二背鳍棘和腹鳍棘的生长与收缩是七带石斑鱼胚后发育过程中最明显的变化特征。第二背鳍棘的长度在仔鱼28~30 dph达到最大值,占仔鱼全长的81%。这些特点增加了苗种培育的难度和障碍。 相似文献
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斜带石斑鱼仔、稚、幼鱼的形态发育研究 总被引：3，自引：0，他引：3
2005年10～12月,在集美大学水产学院水产试验场,对人工培育的斜带石斑鱼仔、稚、幼鱼各发育阶段的形态特征进行了观察和描述.根据卵黄囊、鳍膜、鳞片以及背鳍长棘和腹鳍长棘的变化,将斜带石斑鱼的胚后发育划分为仔鱼期、稚鱼期和幼鱼期3个时期.初孵仔鱼平均全长1.68mm(1.60～1.78mm).在培育水温为21.0～28.5℃,盐度为24.8～28.3条件下,初孵仔鱼至孵化后5日龄为前期仔鱼,3日龄仔鱼开口;孵化后6日龄至31日龄为后期仔鱼;孵化后32日龄至68日龄为稚鱼期;孵化后69日龄进入幼鱼期.背鳍第二鳍棘和腹鳍鳍棘的长出与收缩是斜带石斑鱼前期发育过程中最明显的变化.此外,本文探讨了斜带石斑鱼与青石斑鱼、点带石斑鱼和赤点石斑鱼仔、稚、幼鱼期发育的异同. 相似文献
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采用干法授精方法获得受精卵,在人工培育条件下观察了光唇鱼胚胎及仔、稚鱼发育过程。结果表明,光唇鱼受精卵呈圆球形,沉性、弱粘性。在水温23—25℃下,胚胎发育历时46h45min,经历了胚盘形成、卵裂、囊胚、原肠胚、神经胚、器官形成和孵化等阶段。在水温24—27℃下,仔、稚鱼发育历时22d,初孵仔鱼具有较大的卵黄囊,胸鳍原基及肛门原基形成;4日龄仔鱼开口摄食,进入混合营养期;7日龄仔鱼卵黄囊消失,营外源性营养,体侧8条横斑形成,各鳍均已出现,进入晚期仔鱼阶段;14日龄仔鱼各鳍鳍条发育基本完成;16日龄仔鱼鳞片开始出现,进入稚鱼期;22日龄稚鱼全身被鳞,进入幼鱼期。 相似文献
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本文报道了菊黄东方纯胚胎及仔稚幼鱼发育情况．其结果表明：在水温20～21℃、盐度20～30、pH值8．0～8．3的条件下，受精卵受精后2h为2细胞期、15h为囊胚期、30h为原肠期、55h为胚体期、152h孵出仔鱼；孵出仔鱼在水温19～28℃、盐度20～30、pH8．0～8．3条件下，孵化后5d开口、18d进入稚鱼期、40d进入幼鱼期．此外，对胚胎及仔稚幼鱼各发育阶段进行较详细描述、测量并给出示意图． 相似文献
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作者对鱼(Miichthys miiuy)的早期发育(从受精卵到45日龄幼鱼)形态特征及生态习性进行了描述。鱼的受精卵在水温21.4℃～22.0℃，盐度25.7条件下，经过29 h30 min仔鱼孵出。从受精卵到仔鱼出膜可分为卵裂期、囊胚期、原肠期、胚体形成期等4个主要时期，然后进入胚后发育阶段。孵出后的3日龄仔鱼已能在水体中平游，极少数个体可开口摄食轮虫。4日龄仔鱼全部开口摄食，并对光反应敏感，出现明显的集群现象。22日龄的后期仔鱼各鳍鳍条发育形成，鳞片开始出现，进入到稚鱼期。39日龄后，鱼全身披满细小的鳞片，全部分布于育苗池的底部，开始进入到幼鱼发育阶段。根据仔、稚、幼鱼形态特征和生活习性对鱼的分类进行了探讨。 相似文献
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Soil-sized particulates have been collected on board ship by a mesh technique from the lower troposphere of the North, Equatorial and South Atlantic Ocean, northern and southern Indian Ocean, South and East China Sea and various coastal localities.Spectrographic analysis reveals that, on average, the particulates have concentrations of Mn, Ni, Co, Ga, Cr, V, Ba, and Sr which are of the same order of magnitude as those in average crustal material. In contrast, the average concentrations of Pb, Sn, and Zn are one order of magnitude higher than those in average crustal material.Within this “world-wide” average there are significant geographical variations in the distributions of Pb, Sn, and Zn which may be related to anthropogenic sources.On the basis of trace-element distributions lower tropospheric soil-sized marine particulates have been divided into four genetic components; local, zonal, inter-zonal, and global. The proportions of these components vary geographically, and each component may have both a natural and an anthropogenic fraction. 相似文献
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Tautog, Tautoga onitis, is an abundant species of fish in estuaries of the northeastern United States. Planktonic tautog larvae are abundant in summer in these estuaries, but there is little information on rates of growth of tautog larvae feeding on natural assemblages of food in the plankton. We examined abundance and growth of larval tautog and environmental factors during weekly sampling at three sites along a nearshore‐to‐offshore transect in Buzzards Bay, Massachusetts, USA during summer 1994. This is the first study of a robust sample size (336 larvae) to estimate growth rates of field‐caught planktonic tautog larvae feeding on natural diets, using the otolith daily‐growth‐increment method. The study was over the entire summer period when tautog larvae were in the plankton. The sampling sites contrasted in several environmental variables including temperature, dissolved oxygen (DO), and chlorophyll a concentration. There was a temporal progression in the abundance of tautog larvae over the summer, in relation to location and temperature. Tautog larvae were first present nearshore, with a pronounced peak in abundance occurring at the nearshore sites during the last 2 weeks in June. Larvae were absent at this time further offshore. From late June through August, larval abundance progressively decreased nearshore, but increased offshore although never approaching the abundance levels observed at the nearshore sites. The distribution and abundance of tautog larvae appeared to be related to a nearshore‐to‐offshore seasonal warming trend and a nearshore decrease in DO. Otoliths from 336 larvae ranging from 2.3 to 7.7 mm standard length had otolith increment counts ranging from 0 to 19 increments. Growth of larval tautog was estimated at 0.23 mm·day?1, and length of larvae prior to first increment formation was estimated at 2.8 mm indicating that first increment formation occurs 3–4 days after hatching at 2.2 mm. Despite spatial and temporal differences in environmental factors, there were no significant differences in growth rates at any of three given sites over time, or between sites. Because larval presence only occurred at a narrow range of temperature (17–23.5 °C) and DO (6.5–9.3 mg·l?1), in situ differences in growth did not appear to be because of differences in larval distribution and abundance patterns relative to these parameters. 相似文献
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P.N. Froelich L.W. Kaul J.T. Byrd M.O. Andreae K.K. Roe 《Estuarine, Coastal and Shelf Science》1985,20(3):239-264
Concentrations of dissolved nutrients (NO3, PO4, Si), germanium species, arsenic species, tin, barium, dimethylsulfide and related parameters were measured along the salinity gradient in Charlotte Harbor. Phosphate enrichment from the phosphate industry on the Peace River promotes a productive diatom bloom near the river mouth where NO3 and Si are completely consumed. Inorganic germanium is completely depleted in this bloom by uptake into biogenic opal. The ratio taken up by diatoms is about 0·7 × 10?6, the same as that provided by the river flux, confirming that siliceous organisms incorporate germanium as an accidental trace replacement for silica. Monomethylgermanium and dimethylgermanium concentrations are undetectable in the Peace River, and increase linearly with increasing salinity to the seawater end of the bay, suggesting that these organogermanium species behave conservatively in estuaries, and are neither produced nor consumed during estuarine biogenic opal formation or dissolution. Inorganic arsenic displays slight removal in the bloom. Monomethylarsenic is produced both in the bloom and in mid-estuary, while dimethylarsenic is conservative in the bloom but produced in mid-estuary. The total production of methylarsenicals within the bay approximately balances the removal of inorganic arsenic, suggesting that most biological arsenic uptake in the estuary is biomethylated and released to the water column. Dimethylsulfide increases with increasing salinity in the estuary and shows evidence of removal, probably both by degassing and by microbial consumption. An input of DMS is observed in the central estuary. The behavior of total dissolvable tin shows no biological activity in the bloom or in mid-estuary, but does display a low-salinity input signal that parallels dissolved organic material, perhaps suggesting an association between tin and DOM. Barium displays dramatic input behavior at mid-salinities, probably due to slow release from clays deposited in the harbor after catastrophic phosphate slime spills into the Peace River. 相似文献
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E. Wolanski P. Colin J. Naithani E. Deleersnijder Y. Golbuu 《Estuarine, Coastal and Shelf Science》2004,60(4):705-716
Three years of temperature data along two transects extending to 90 m depth, at Palau, Micronesia, show twice-a-day thermocline vertical displacements of commonly 50–100 m, and on one occasion 270 m. The internal wave occurred at a number of frequencies. There were a number of spectral peaks at diurnal and semi-diurnal frequencies, as well as intermediate and sub-inertial frequencies, less so at the inertial frequency. At Palau the waves generally did not travel around the island because there was no coherence between internal waves on either side of the island. The internal waves at a site 30 km offshore were out-of-phase with those on the island slopes, suggesting that the waves were generated on the island slope and then radiated away. Palau Island was thus a source of internal wave energy for the surrounding ocean. A numerical model suggests that the tidal and low-frequency currents flowing around the island form internal waves with maximum wave amplitude on the island slope and that these waves radiate away from the island. The model also suggests that the headland at the southern tip of Palau prevents the internal waves to rotate around the island. The large temperature fluctuations (commonly daily fluctuations ≈10 °C, peaking at 20 °C) appear responsible for generating a thermal stress responsible for a biologically depauperate biological community on the island slopes at depths between 60 and 120 m depth. 相似文献
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Klaus Kremling 《Marine Chemistry》1983,13(2):87-108
In June 1981, dissolved Zn, Cd, Cu, Ni, Co, Fe, and Mn were determined from two detailed profiles in anoxic Baltic waters (with extra data for Fe and Mn from August 1979). Dramatic changes across the O2H2S interface occur in the abundances of Cu, Co, Fe, and Mn (by factors of ?100). The concentrations of Zn, Cd, and Ni at the redox front decrease by factors between 3 to 5.Equilibrium calculations are presented for varying concentrations of hydrogen sulfide and compared with the field data. The study strongly supports the assumption that the solubility of Zn, Cd, Cu, and Ni is greatly enhanced and controlled by the formation of bisulfide and(or) polysulfide complexes. Differences between predicted and measured concentrations of these elements are mainly evident at lower ΣH2S concentrations.Cobalt proved to be very mobile in anoxic regions, and the results indicate that the concentrations are limited by CoS precipitation. The iron (Fe2+) and manganese (Mn2+) distribution in sulfide-containing waters is controlled by total flux from sediment-water interfaces rather than by equilibrium concentrations of their solid phases (FeS and MnCO3). The concentrations of these metals are therefore expected to increase with prolonged stagnation periods in the basin. 相似文献