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多倍体贝类的繁殖生物学研究进展 总被引：2，自引：0，他引：2
本文综述了国内外多倍体贝类繁殖生物学的研究现状。主要是从多倍体贝类的性腺发育、生殖细胞、减数分裂、繁殖力以及其性成熟年龄和性比等方面进行了论述。三倍体贝类的性腺虽然有一定程度的发育，但总体表现出高度的不育，而四倍体贝类的性腺发育正常；三倍体、四倍体贝类的生殖细胞明显大于同龄的二倍体的生殖细胞；多出的几套染色体使多倍体贝类减数分裂时染色体的分离形式复杂化；多倍体贝类的性成熟年龄与二倍体基本一致，三倍体贝类雌雄比例与二倍体有所不同，雌雄同体的比例增大。 相似文献
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将中华绒螯蟹三倍体大眼幼体群体 (三倍体率 64.38% )在池塘中养殖 ,对其早期生长及营养进行测定。结果表明 ,从三倍体群体自身的生长状况看 ,放养后 68— 78天是整个测量期间三倍体群体生长最快的阶段 ,其中壳长增长显著 (P <0 .0 5 ) ,壳宽和体重的增加极显著 (P <0 .0 1 )。与二倍体群体相比 ,放养后 68— 1 0 6天 ,三倍体群体在壳长、壳宽、体重上都表现出明显的生长优势 (P <0 .0 1 )。三倍体幼蟹蟹体氨基酸总量高于正常二倍体幼蟹 ,必需氨基酸中苏氨酸、苯丙氨酸、缬氨酸、亮氨酸、精氨酸、异亮氨酸、组氨酸和赖氨酸的含量高于二倍体 ,而蛋氨酸的含量则低于二倍体幼蟹。蟹体中不饱和脂肪酸所占比例三倍体幼蟹低于正常二倍体 ,EPA、DHA及多不饱和脂肪酸所占的比例也低于二倍体。结果表明 ,三倍体幼蟹的生长比正常二倍体具有优势 ,并且在营养组成上也和二倍体有所差异。 相似文献
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三倍体牡蛎在繁殖季节的生长研究 总被引：2，自引：0，他引：2
研究了在繁殖季节内三倍体太平洋牡蛎的生长情况。结果表明 ,三倍体牡蛎比二倍体对照组具有明显的生长优势。在整个繁殖期间 ,三倍体的体重明显高于二倍体。三倍体的生长速度较均匀 ,而二倍体变化较大。在集中排放前体重增长较快 ,集中排放后体重增长明显减慢。三倍体的平均体重在排放前比二倍体高 17%左右 ,在排放后则高达 30 %以上。集中排放前 ,二倍体的软体重增长很快并超过了三倍体 ,其出肉率比三倍体高 2 6 .4 8%。排放后二倍体的软体重明显降低 (降低 4 8% ) ,出肉率降低 4 0 .0 % ,而三倍体变化不明显 ,出肉率仅降低 5 .79%。繁殖高峰后三倍体的软体重比二倍体高 4 1.2 2 %。三倍体牡蛎较低但稳定的出肉率表明三倍体太平洋牡蛎具有高度的不育性 ,但三倍体的不育性并不是引起三倍体生长优势的主要原因 相似文献
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合浦珠母贝二倍体、三倍体和非整倍体群体的基因杂合度与生长比较 总被引：6，自引：0，他引：6
采用淀粉凝胶电泳方法对合浦珠母贝Pinctadamartensi(D.)雌性三倍体与雄性二倍体交配,细胞松弛素B抑制其受精卵第一极体释放产生的二倍体、三倍体及非整倍体3个群体进行了同工酶研究。二倍体、三倍体及非整倍体群体在6个多态位点的平均基因杂合度分别为0.255±0.087,0.286±0.097,0.275±0.089,三倍体的杂合度高出二倍体约12%,表明多倍体诱导能增加诱导群体的杂合度。但在单个位点上,三倍体的杂合度不一定高于二倍体;在各自群体内,平均杂合位点数与生长间无明显的相关性,单个位点上的杂合子也未完全表现出其生长大于纯合子,且差异不明显(p>0.05)。因此,合浦珠母贝三倍体的快速生长难以完全用杂合度增高假说解释,只能说明诱导处理能使三倍体的杂合度增高,而能量再分配和"巨型性"可能对其快速生长起着不可忽视的作用。非整倍体群体的杂合度高于二倍体群体,但其生长却小于二倍体,其原因可能是染色体的增减对机体的生长有一定的影响。 相似文献
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为了评估香港牡蛎二倍体及三倍体幼虫生物学特征,于2013~2015年,在湛江和北海两地比较了二倍体及三倍体幼虫生长、存活及变态差异,计算了三倍体优势率,评估了倍性与环境效应互作对其表型性状的影响。结果表明:三倍体D形幼虫显著大于二倍体幼虫,之后,伴随着个体增长,生长优势逐渐增大,15日龄时的三倍体优势率为8.9%~9.1%。三倍体幼虫存活力与二倍体相当,未出现大量致死现象。三倍体变态规格显著大于二倍体,其优势率为5.1%~5.3%;三倍体变态时间显著低于二倍体,但其变态率与二倍体相当,不存在显著差异(p>0.05)。经过双因子分析模型的方差分析检测,发现倍性和环境效应都会对香港牡蛎幼虫生长产生显著影响(p<0.001),环境是影响幼虫存活率及变态的主要因子(p<0.05)。 相似文献
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太平洋牡蛎多倍体研究 总被引：6，自引：0，他引：6
本文综述了太平洋牡蛎多倍体产生的途径、诱导方法、诱导结果、诱导机制、倍性鉴别方法、繁殖、生长、生理指标、抗逆性和口味等。提出：６－ＤＭＡＰ诱导牡蛎三倍体的技术前景广阔;四倍体与二倍体杂交的方法是产生三倍体的最好途径;四倍体是生物方法产生三倍体的中间材料,可以存活,应加大力度地研究和开发;三倍体的性腺能够发育,并可产生具有繁殖力的配子;在良好的环境里,四倍体的生长和抗逆性较二倍体优势;在繁殖季节,三 相似文献
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探讨多倍体牡蛎的遗传基础,通过染色体计数法对2龄杂交三倍体太平洋牡蛎(Crassostrea gigas)群体的染色体数目组成进行了分析,发现在80个具良好中期分裂相的牡蛎中,有56个三倍体(70.0%);12个非整倍体(15.0%),4个2n/3n嵌合体(5.0%);8个二倍体(10.0%)。12个非整倍体中包括9个29条染色体的亚三倍体(3n-1)和3个31条染色体的超三倍体(3n 1)。非整倍体与三倍体的生长差异不明显(P>0.05)。可能由于数量较少的原因,嵌合体和二倍体的生长没有表现明显生长滞后(P>0.05)。 相似文献
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栉孔扇贝三倍体与二倍体的生长比较 总被引：8，自引：0，他引：8
近几年在我国栉孔扇贝养殖业中出现了单产降低、品质下降、大面积死亡问题 ,其主要原因是缺少生长快、品质优、抗逆能力强的养殖新品种。对于养殖贝类来说 ,性成熟往往导致生长抑制、抗逆性下降和肉质下降。目前广泛开展的多倍体贝类研究的主要目的是产生不育的三倍体 ,充分利用三倍体的不育性和生长优势 ,为海水养殖业健康、稳定、持续地发展提供技术支持。通过对栉孔扇贝三倍体和二倍体的生长比较 ,证实栉孔扇贝三倍体具养殖实用价值。１材料与方法１．１材料栉孔扇贝Ｃｈｌａｍｙｓ(Ａｚｕｍａｐｅｃｔｅｎ) ｆａｒｒｅｒｉ取自青岛太平… 相似文献
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盘鲍三倍体及二倍体生长的比较 总被引：5，自引：0，他引：5
在室内工厂化养殖条件下 ,于 1 997年 1 0月对正常盘鲍二倍体个体及用细胞松驰素 B诱导法获得的盘鲍三倍体群的生长情况进行了比较。结果表明 :(1 )在育苗期的 1 4月龄内 ,盘鲍的三倍体群与二倍体个体间在生长上无明显差异 ;(2 ) 1 4月龄后盘鲍的三倍体群与二倍体个体间在生长上出现分化。两周龄的盘鲍三倍体群在壳长和体重上分别比二倍体个体大 1 4.76 %和5 0 .1 9%;两周龄半的盘鲍三倍体群在壳长和体重上分别比二倍体个体大 2 0 .0 0 %和 41 .89%;(3 )如按 6 cm壳长作为商品盘鲍的标准 ,则盘鲍三倍体群只需养殖 2 6个月 (包括育苗期 )即可达到商品盘鲍的标准 ,而二倍体个体则需养殖 3 0个月 (包括育苗期 )。由此可见 ,三倍体商品盘鲍比二倍体商品盘鲍在养殖时间上可缩短 4个月 ;(4)盘鲍三倍体群与二倍体个体群的氨基酸组分相同 ,但盘鲍三倍体群的氨基酸总量比二倍体个体的氨基酸总量高。 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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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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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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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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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
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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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Phylogenetic diversity and phenotypic characterization of cultivable bacterioplankton isolated from polar oceans 总被引：1，自引：0，他引：1
A set of 27 marine planktonic bacteria isolated from the polar regions was characterized by 16S rDNA sequencing and physiological and biochemical testing. More than half of these bacteria were positive for caseinase, gelatinase and 13-glucosidase, and could utilize glucose, maltose or malic acid as carbon source for cell growth. Twelve isolates expressed nitrate reduction activities. Except for one antarctic isolate BSwlO175 belonging to Actinobacteria phylum, these isolates were classified as γ-Proteobacteria, suggesting that γ-Proteobacteria dominated in cultivable marine bacterioplankton at both poles. Genus Pseudoalteromonas was the predominant group in the Chukchi Sea and the Bering Sea, and genus ShewaneUa dominated in cultivable bacterioplankton in the Prydz Bay. With sequence similarities above 97%, genus Psychrobacter was found at both poles. These 27 isolates were psychrotolerant, and significant 16S rDNA sequence similarities were found not only between arctic and antarctic marine bacteria （ 〉 99% ）, but also between polar marine bacteria and bacteria from other aquatic environments （ ≥ 98.8% ）, including temperate ocean, deep sea, pond and lake, suggesting that in the polar oceans less temperature-sensitive bacteria may be cosmopolitan and have a bipolar, even global, distribution at the species level. 相似文献