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港养黄鳍鲷性腺发育和性转变研究 总被引：4，自引：2，他引：4
本文利用光镜和电镜显微技术研究了福建东山县西埔湾黄鳍鲷性腺发育过程和性转变规律。结果表明,港养黄鳍鲷雌性性腺不能向产卵状态过渡,因而不能自然产卵,其卵细胞发育可分为5个时相,卵巢发育也可相应地分为5期。雄性性腺在港养条件下能够发育成熟,其精巢发育可分为6期。Ⅰ龄组雄性个体和雌雄同体并存;Ⅱ龄组大多数个体为雌雄同体,少数个体已转变为雌性鱼;Ⅲ龄组和Ⅳ龄组的个体均为雌性鱼。本文还对卵黄的形成、卵母细胞的退化吸收以及排卵的机制等问题进行了讨论。 相似文献
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本文以市售黄鳍鲷(体重96—225g,体长150—250mm)的肾细胞为材料,注射入PHA,用空气干燥法制片,姬姆萨染色,对其染色体组型进行了分析。 相似文献
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海水养鱼的优良品种——黄鳍鲷 总被引：1，自引：0，他引：1
黄鳍鲷(Sparus latus Houttuyn)又名阔黑鲷,隶属于(鱼户)亚目Pencoidei,鲷科Sparidae,鲷属Sparus。俗称黄脚(鱼立)、黄翅嘉腊、赤翅。台湾省等地称之为乌(鱼宗)(乌格仔)(Acanthopagrus latus Houttuyn)的鱼,认为与黄鳍鲷是同一种。 相似文献
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半胱胺盐酸盐和LHRH-A对黄鳍鲷生长激素分泌的影响 总被引：10，自引：1，他引：9
研究了生长抑素抑制剂半胱胺盐酸盐(CSH)和促黄体素释放激素类似物(LHRH-A)对黄鳍鲷生长激素(GH)分泌的影响.黄鳍鲷垂体GH含量在单独注射不同剂量CSH(25,50,100μg/gb.w)后2h均显著提高,注射后24h恢复正常.黄鳍鲷血清中GH水平在注射CSH(100μg/gb.w)后2h和CSH(25,50μg/gb.w)后6h均明显提高.单独注射LHRH-A(0.1μg/gb.w)后2h黄鳍鲷垂体GH含量和血清中GH水平均明显提高.注射CSH和LHRH-A后6h垂体GH含量明显高于单独注射CSH或LHRH-A,而血清GH水平在注射后12h明显高于单独注射CSH或LHRH-A.结果表明CSH和LHRH-A都能明显刺激黄鳍鲷垂体合成和释放GH,并且与CSH作用存在剂量依存关系,CSH和LHRH-A联合注射比单独注射作用更明显,作用的时间更持久. 相似文献
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本文研究环境光强与黄鳍鲷(Sparus latus)和普通鲻鱼(Mugil cephalus)两种幼鱼视网膜运动反应的关系,结果表明:当光强分别低于10~(-3)1x和10~(-2)1x时,对黄鳍鲷和普通鲻鱼幼鱼视网膜运动反应无明显影响;当光强分别高于10~(-3)1x和10~(-2)1x时,光强越高,两种幼鱼视网膜从暗适应状态过渡到明适应状态的时程越短。黄鳍鲷幼鱼从暗视向明视过渡的照度界限为10~(-3)—10~(-1)1x;普通鲻鱼幼鱼的相应过渡照度界限为10~(-2)—10~01x。 相似文献
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用RFLP(限制性片段长度多态性,Restriction fragment length polymorphism)技术研究了红鳍笛鲷Lutjanus erythropterus Bloch、紫红笛鲷Lutjanus argentimaculatus Forskal、勒氏笛鲷Lutja-nus russelli Bleeker和约氏笛鲷Lutjanus johni Bloch的遗传多样性关系,检测到4种笛鲷的分子标记。通过差速离心、核酸酶消化、苯酚抽提,从4种笛鲷肝脏组织中分离纯化线粒体DNA(mtDNA),用19种5到6碱基对的限制性内切酶进行单酶、双酶和部分酶切,琼脂糖凝胶电泳,进行了RFLP分析,构建了4种笛鲷mtDNA的物理图谱。红鳍笛鲷、紫红笛鲷、勒氏笛鲷和约氏笛鲷的mtDNA大小分别为17.36±0.09kb、17.58±0.08kb、17.50±0.18kb和17.56±0.12kb。红鳍笛鲷和紫红笛鲷种群间平均mtDNA多态度π为0.106 2,红鳍笛鲷和勒氏笛鲷群体间平均mtDNA多态度π为0.130 5,红鳍笛鲷和约氏笛鲷群体间平均mtDNA多态度π为0.151 5,紫红笛鲷和勒氏笛鲷群体间平均mtD-NA多态度π为0.130 3,紫红笛鲷和约氏笛鲷群体间平均mtDNA多态度π为0.119 5,勒氏笛鲷和约氏笛鲷群体间平均mtDNA多态度π为0.139 4。红鳍笛鲷和紫红笛鲷种群间净遗传距离Pnet为0.102 0,红鳍笛鲷和勒氏笛鲷群体间净遗传距离Pnet为0.128 5,红鳍笛鲷和约氏笛鲷群体间净遗传距离Pnet为0.149 1,紫红笛鲷和勒氏笛鲷群体间净遗传距离Pnet为0.127 0,紫红笛鲷和约氏笛鲷群体间净遗传距离Pnet为0.115 7,勒氏笛鲷和约氏笛鲷群体间净遗传距离Pnet为0.137 8。 相似文献
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黄鳍鲷不同组织同工酶的研究 总被引：15，自引：2，他引：13
运用聚丙烯酰胺垂直梯度凝胶电泳法对黄鳍鲷的7种组织(心肌、肝脏、肾脏、肌肉、性腺、脾脏、脑)进行了4种同工酶(EST,LDH,MDH,ME)的初步研究,并对几种酶的同工酶位点及酶谱表型进行了分析。结果表明：黄鳍鲷的4种同工酶系统具有明显的组织特异性。同时还分析了聚丙烯酰胺垂直梯度凝胶电泳法对同工酶电泳的分离效果,认为该种方法对同工酶系统的分辨率高,分离效果好,可得到更精确的结果。 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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以苯酚和4—溴苯甲酸为原料,合成一种尚未见文献记载的新化合物——4—溴苯甲酸—2,3,4,5,6—五溴苯酯,用无水三氯化铝催化苯酚的全溴化。此产物可望在阻燃剂方面得到应用。 相似文献