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1.
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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合浦珠母贝三倍体和二倍体的生长比较 总被引：13，自引：0，他引：13
合浦珠母贝Pinctada martensii(D.)三倍体和二倍体的生长测定表明,三倍体成贝平均壳高、壳长、壳宽和体重均超过二倍体同胞,差异极显著(P<0.01)。特别是抑制第一极体形成的三倍体,经两年养殖,壳高、体重和肉重分别比二倍体增加13.01％,44.03％和58.37％。在繁殖期,三倍体的增长率显著超过二倍体。非繁殖期的大多数月份,三倍体的增长率和二倍体相差不大。因此,可以认为三倍体生长速度快主要是由于三倍体的生殖腺发育受阻,体内积累的能量转移到体细胞生长所致。 相似文献
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三倍体合浦珠母贝不育性研究 总被引：10，自引：0，他引：10
对三倍体合浦珠母贝Ｐｉｎｃｔａｄａ ｍａｒｔｅｎｓｉｉ（Ｄ．）春、秋两繁殖盛期的生殖腺进行了组织学观察，并对其配子形成及受精、发育进行了研究。结果表明：合浦珠母贝三倍体的生殖腺发育差，生殖细胞数量少，极少个体能见到成熟卵母细胞和精子；三倍体的配子能完成受精作用，能发育至直线铰合期。配子多为非整倍体，其染色体数目多为１４－２８，胚胎染色体数目主要为２８－４２，故胚胎不能正常发育。因此，三倍体合浦珠母 相似文献
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三倍体和二倍体合浦珠母贝育珠比较初步研究 总被引：2，自引：0，他引：2
利用人工诱导培育的三倍体合浦珠母贝Pinctada martensii(D.)进行插核育珠试验,并同处理组内的二倍体同胞进行比较。结果表明:三倍体合浦珠母贝的留核率和正圆珠比率分别为81.0％和58.8％,而二倍体则为71.3％和37.8％;在非正圆珠中两者的污珠率差别不大,但三倍体的尾巴珠和素珠的比率明显低于二倍体;三倍体的正圆珠珍珠层平均厚度和平均重量分别为381μm和163mg,二倍体分别为265μm和105mg,两者差异极显著(P<0.01)。初步表明,利用三倍体合浦珠母贝培育珍珠,能缩短育珠期,提高珍珠的产量和质量。 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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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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人工诱发合浦珠母贝雌核二倍体发生及“Hertwig效应”的初步研究 总被引：2，自引：0，他引：2
用中心波长为254nm、光照强度为4μW/cm~2的紫外线,照射合浦珠母贝[Pinctada ma-tensil(D_o)]和长耳珠母贝[Pinctada chemnitzi(P_o)]的精子,然后与合浦珠母贝的正常卵授精,在0-150s的照射范围内,从早期胚胎存活率上可以观察到“Hertwig效应”的存在,由此得到的单倍体和非整倍体胚胎在孵化前死亡。精子经120s紫外线照射后,染色体完全失活,但受精作用仍能正常发生。长耳珠母贝精子经 120s照射,异种授精(♀合×♂长)后21min,用浓度为0.4mg/l的细胞松弛素B处理15min,抑制受精卵的第二极体排放,可以诱发合浦珠母贝产生74.0％雌核二倍体胚胎,其孵化率为2.1％。 相似文献
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非整倍体太平洋牡蛎的存活、生长与性腺发育 总被引：1，自引：1，他引：0
在二倍体与四倍体杂交产生的三倍体牡蛎群中检测到了非整倍体 ,其中 3n± 1非整倍体相对于三倍体的存活率为 6 0 .98%。非整倍体牡蛎作为一个群体 ,其生长与其三倍体同胞在体重上无明显差异 ,且与三倍体一样明显大于其二倍体对照组。非整倍体牡蛎的性腺发育情况与三倍体个体相当 ,也能产生成熟的生殖细胞 相似文献
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Arne Schnack-Friedrichsen Angela M. Davis Jim D. Bennell Dei G. Huws 《Marine Georesources & Geotechnology》2001,19(4):221-243
The interdependence between the seismo-acoustic properties of a marine sediment and its geotechnical/physical parameters has been known for many years, and it has been postulated that this should allow the extraction of geotechnical information from seismic data. Though in the literature many correlations have been published for the surficial layer, there is a lack of information for greater sediment depths. In this article, a desktop study on a synthetic seafloor model illustrates how the application of published near-surface prediction equations to subsurface sediments (up to several tens of meters burial depth) can lead to spurious predictions. To test this further, acoustic and geotechnical properties were measured on a number of sediment core samples, some of which were subjected to loading in acoustically-equipped consolidation cells (oedometers) to simulate greater burial depth conditions. For low effective pressures (representing small burial depths extending to around 10 meters subsurface), the general applicability of established relationships was confirmed: the prediction of porosity, bulk density, and mean grain size from acoustic velocity and impedance appears generally possible for the investigated sedimentary environments. As effective pressure increases through, the observed relationships deviate more and more from the established ones for the near-surface area. For the samples tested in this study, in some instances increasing pressure even resulted in decreasing velocities. There are several possible explanations for this abnormal behavior, including the presence of gas, overconsolidation, or bimodal grain size distribution. The results indicate that an appropriate depth correction must be introduced into the published prediction equations in order to obtain reliable estimates of physical sediment properties for greater subsurface depths. 相似文献
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Shigehisa Nakamura 《Marine Geodesy》2000,23(1):55-61
Specific properties of the interannual sea level variations and annual tides in the Northwestern Pacific were studied. Several tide stations were monitored. The monthly mean sea level for the year of 1995 was analyzed at each tide station. A seismic event in 1995, some tectonic activity around the subject area, and the Kuroshio (the oceanic western boundary current) may possibly contaminate results which would have occurred from the astronomical annual tide alone. 相似文献
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The effect of different fixation and storage protocols on the flow cytometric (FCM) simultaneous analysis of bacterioplankton and phytoplankton in coastal seawater samples (Mediterranean coastal lagoons) was investigated. FCM measurements (cell number, fluorescence and scatter characteristics) were obtained through DAPI staining. Three fixatives [glutaraldehyde (GA), formaldehyde (FA) and paraformaldehyde (PFA)] and two storage (3 months duration) methods (5 °C and −196 °C) were tested. Two dominant populations were detected in studied samples: bacteria and eukaryotic picophytoplankton. Adding fixatives (2% final concentration) appears necessary to obtain FCM exhaustive counts of all the bacteria and phytoplanktonic cells. This was related to the permeation effect of fixatives which allowed a better DAPI staining of the cells. Maximum fluorescence, i.e. optimal staining of the cells was obtained with FA or PFA, and significant lower fluorescences with GA. Fixed samples stored at 5 °C induced rapid cell loss. Only storage in liquid nitrogen of samples fixed with FA or PFA, allows mid-term (≥4 months) preservation of bacteria or picophytoplankton cell numbers, and limited evolution of DAPI-induced fluorescence and scatter characteristics. 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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《海洋学报(英文版)》2014,(9):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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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
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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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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
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Particulate samples were collected from the Changjiang river system during a flood period, in May 1997, and POC, stable isotope and lipids associated with particles were examined. Results showed the decrease (0.84% ～ 1.88%) of organic carbon content from the upper reaches to the estuary.δ13C values of particulate organic carbon was in the range of -24.9×10-3 to -26.6×10-3, which were close to the isotopic signature of continental C3 vegetation. Total particulate n-alkanes concentrations varied from 1.4 to 10.1μg/dm3,or from 23.7 to 107μg/g of total suspended matter. Fatty acids were present in all the samples, from 1.4 to 5.4μg/dm3, with saturated and unsaturated straight-chain and branched compounds in the carbon number range from C12 to C30. Both δ13C and the ratio of carbon content to nitrogen content indicate the predominance of terrestrial inputs (soil organic matter) among the particles. The biomarker approach has been used to identify the relative portion of terrigenous and autochthonous fraction in the particulate samples. The distribution of fatty acids suggests a striking phytoplanktonic and microbial signal in most particle samples. The terrestrial alkanes are used to estimate the contribution of terrestrial inputs along the mainstream. 相似文献