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本文采用低温２～９℃和高温３５～３９℃温度休克法，在受精后１０～２５ｍｉｎ进行１０～２５ｍｉｎ处理，诱导牡蛎三倍体。结果表明：各处理组都有不同程度的三倍体产生，其中受精后２０ｍｉｎ开始在４～５℃下处理１５ｍｉｎ诱导三倍体效果最好，诱导率为６８×１０－２，幼贝三倍体率为６０．５×１０－２，生长速度处理组壳高明显超过对照组，而壳长生长和幼虫死亡率无明显差异。 相似文献
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温度休克诱导长牡蛎三倍体的研究 总被引：2，自引：0，他引：2
本文采用低温２～９℃和高温３５～３９℃温度休克法、在受精后１０～２５ｍｉｎ，进行１０～２５ｍｉｎ处理，诱导牡蛎三倍体。结果表明：各处理组都有不同程度的三倍体产生，其中受精后２０ｍｉｎ开始在４～５℃下处理１５ｍｉｎ诱导三倍体效果最好，诱导率为６８×１０＾－２，幼贝三倍体率为６０．５×１０＾－２，生长速度处理组壳高明显超过对照组，而壳长生长和幼虫死亡率无明显差异。 相似文献
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１９９６～１９９７年,在进行６－二甲基氨基嘌呤（６－ＤＭＡＰ）诱导太平洋牡蛎产生三倍体的实验过程中,发现一定数量的四倍体。解剖法获取精卵,人工授精。染色体倍性鉴别采用染色体计数法。（１）三因素四水平Ｌ１６（４５）正交设计。试验平行重复２次。最高四倍体诱导率为４０．０±０．０％。太平洋牡蛎四倍体各诱导因素的最优水平组合：当精卵混合２０ｍｉｎ时,将受精卵浸泡在含６－ＤＭＡＰ４５０μｍｏｌＬ－１的海水中１０ｍｉｎ;决定四倍体产生的三因素的主次顺序：６－ＤＭＡＰ浓度→诱导时机→诱导持续时间。（２）三因素三水平Ｌ９（３４）正交设计。试验平行重复３次。最高四倍体诱导率为９．６±４．９％。诱导太平洋牡蛎四倍体各因素的最优水平组合：当５０％受精卵出现第一极体时,将受精卵浸泡在含６－ＤＭＡＰ４５０μｍｏｌＬ－１的海水中１５ｍｉｎ;决定四倍体产生的三因素的主次顺序：诱导时机→６－ＤＭＡＰ浓度→诱导持续时间。 相似文献
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华贵栉孔扇贝三倍体的研究 总被引：2，自引：1，他引：2
本文报道了用细胞松驰素B、高温和低温休克等方法诱导华贵栉孔扇贝（Chlamys nobilis）三倍体的实验结果。在26.0～28.0℃条件下，选用不同浓度的细胞松驰素B0.1、0.3、0.5、0.7和1.0mg/dm^3，在受精后15min，处理受精卵15min，三倍体诱导率分别为12.5%、37.5%、68.0%、66.6%和81.0%，其中0.5～1.0mg/dm^3浓度的细胞松驰素B对改变倍性最有效。高温休克选用31.0、33.0、35.0和37.0℃处理受精卵，最高三倍体诱导率达46.7%（33.0℃,处理15min）。低温休克选用6.0、8.0、10.0和12.0℃处理受精卵，最高三倍体诱导率为40.7%（10.0℃，处理20min）。实验结果表明，随着处理强度的增大和处理时间的延长，三倍体诱导率增高、但孵化率下降，畸型率上升。用高温休克处理的实验组幼虫生长速度较对照组快。作者认为，在商业性生产中，温度休克是诱导扇贝三倍体的一种简便、有效的方法。文中还就细胞松驰素B与温度休克诱导三倍体的机制进行了讨论。 相似文献
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大菱鲆(Scophthalmus maximus)是我国重要的海水养殖鱼种,三倍体诱导对其种质改良、产业提升和生态安全具有重要的价值。目前有关大菱鲆三倍体的人工诱导虽已有报道,但对其诱导条件缺乏细致的研究。本文采用冷休克法抑制第二极体排放,通过对诱导处理起始时刻、温度和持续时间3个主要因素的单因子实验,筛选其最佳诱导条件。结果显示,在受精和孵化水温为15.0±0.5℃条件下,受精后6 min,用–2～–1℃处理25 min可获得较好的诱导效果,流式细胞仪检测其诱导率可达100%。随后在最适条件下进行了规模化诱导,获得鱼苗200万尾以上,其诱导率高于98%。跟踪观察发现,三倍体诱导组胚胎的形态及孵化时间与二倍体对照组基本一致。本研究结果可为大菱鲆三倍体的产业化应用提供基础。 相似文献
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用6-二甲基氨基嘌呤(6-DMAP)进行了黄河口近江牡蛎(Crassostreaariakensis)的三倍体诱导,以卵裂率、孵化率、诱导三倍体率和三倍体诱导组幼虫的生长率、存活率、三倍体率为指标,研究了诱导浓度、起始诱导时间、诱导持续时间三个因素对黄河口近江牡蛎三倍体的诱导效果。结果表明,三因素对近江牡蛎三倍体诱导效果的影响程度为起始诱导时间诱导持续时间诱导浓度。温度25℃,诱导浓度为300—450μmol/L,起始诱导时间为受精后14min,诱导持续时间为15min时,诱导三倍体率可达51.39%—71.67%,卵裂率、孵化率、幼虫壳高日平均生长率和幼虫平均存活率分别能达到65.16%—81.57%、61.25%—86.78%、8.76—9.88μm/d、69.16%—73.29%,眼点幼虫时期三倍体率达53.33%—62.16%。本研究为黄河口近江牡蛎的三倍体诱导提供了理论依据。 相似文献
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真鲷三倍体诱导初步研究 总被引：9，自引：0，他引：9
在南鲷Ｐａｇｒｏｓｏｍｕｓ ｍａｊｏｒ三倍体诱导研究中，对染色体倍数的分析表明，受精卵受精５ｍｉｎ后，在１．５℃冰水中处理５ｍｉｎ可获得１７％的三倍体诱导率和２８％的嵌合体比率，染色体数分别是：２Ｎ＝４８，３Ｎ＝７２，嵌合体５０－６８。仔鱼红血细胞测量和组织切片分析显示，三倍体和二倍体的红血细胞核直径，视网膜神经节细胞核直径物中脑细胞核直径大小存在差异，其比率分别是１．４２，１．３５和１．４１，这 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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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
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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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Lars-Göran Danielsson 《Marine Chemistry》1980,8(3):199-215
Results of trace-metal analyses of water samples obtained during a cruise with the Soviet R.V. “Akademik Kurchatov” in the Indian Ocean are presented. The determinations were performed on board with atomic absorption spectrophotometry after a two-stage dithiocarbamate—Freon extraction procedure. Trace-metal concentrations found are in the same range as those found recently for similar open-ocean areas by other workers. The values for lead and zinc are probably high due to contamination. Vertical profiles indicate biogenic processes as controlling factors for the increase of cadmium, copper and nickel concentrations with depth. Iron shows an irregular depth distribution as a result of large random variations in concentration. 相似文献