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1.
采用淀粉凝胶电泳技术研究了青岛近海毛蚶自然群体的等位基因酶遗传变异。在十二种等位基因酶中共检测到了二十七个基因座位，多态位点比例为５１．８５％，位点有效等位基因数分布从１．０３０…２．５７７（平均值１．３８１±０．３４５），位点杂合度观察值分布为０．０２９…０．６１２（平均杂合度０．１３３±０．０３６），在六个基因座位上存在相当明显的杂合子缺失现象。文中讨论了杂合子缺失的原因。 相似文献
2.
青岛近海魁蚶群体等位基因酶遗传变异研究 总被引：7，自引：1，他引：7
采用淀粉凝胶电泳技术研究了青岛近海魁蚶自然群体的等位基因酶遗传变异。在十种等位基因酶中共检测到了二十二个基因座位，多态位点比例为45．5％，位点有效等位基因数分布从1．000～2．469（平均值1．415），位点杂合度观察值分布为0．000～0．595（平均杂合度0．105±0．023），在六个基因座位上存在相当明显的杂合子缺失现象。文中讨论了杂合子缺失的原因。 相似文献
3.
凡纳滨对虾（Litopenaeus vannamei）不同世代养殖群体的遗传多样性分析 总被引：5，自引：1，他引：4
采用微卫星位点对凡纳滨对虾的海南群体（进口亲虾繁育的第1世代：G1）、山东和饶平群体（G2）、湛江2和湛江3群体（G3）、湛江1和上海群体（G4）共4个世代7个养殖群体的遗传多样性进行了分析。从21对微卫星引物中筛选出12对有效扩增引物,对7个群体共280个个体进行扩增,得到10个多态位点,共获得等位基因数63个。各位点的等位基因数在2-15个之间,各群体的平均等位基因数在4．70—5．80之间。平均观测（期望）杂合度在0.36—0．43（0．53—0．65）之间。杂合子偏离指数（D）为负值,表明存在杂合子缺失现象。对7个群体、10个多态位点进行Hardy—Weinberng平衡检测,共有54个偏离平衡。对7个群体间的遗传分化水平进行检测,得到近交系数FIS在9个多态位点均为正值,两两群体间的固定指数FST值在0．149-O．375之间。FST显著性检验表明,各群体之间的遗传分化极显著（P〈0．01）。分子方差分析结果显示,大部分遗传变异（72．17％）来自于群体内,来自于群体间的遗传变异（27．83％）较小。凡纳滨对虾不同世代间遗传变异大,随着繁育世代的增加,遗传多样性降低。 相似文献
4.
五个短蛸群体等位基因酶的遗传变异 总被引：11，自引：1，他引：11
采用水平淀粉凝胶电泳技术研究了山东沿海莱州（LZ），烟台（YT）、青岛（QD），日照（RZ）和大连（DL）五地短蛸自然群体的等位基因酶遗传变异。分析了AAT，ALP，EST，GRS，G6PD，SDH，CAT，SOD，IDH，GPI，PGM，G3PD，MPI，ME，MDH，CK，AK等同工酶在短蛸外套肌和肝脏组织中的表达情况，并对同工酶进行了生化遗传分析，LZ，YT，QD，RZ，DL五个群体的多态位点比例分别为15％，5％，10%,10%,10%(P0．99），群体平均杂合度观测值分别为0．024，0．001，0．009，0．007，0．006，平均位点有效等位基因数分别为1．200，1．022，1．061，1．103，1．077。结果表明，LZ群体的遗传多样性较高，同时，各群体中普遍存在杂合子缺失现象，对五个群体的遗传距离进行聚类分析，构建了系统树图。 相似文献
5.
西施舌（Coelomactra antiquata）群体遗传多样性与分化的研究 总被引：2，自引：1，他引：1
采用不连续垂直板聚丙烯酰胺凝胶电泳技术,对广西北海、福建漳港和江苏启东3个西施舌自然群体的7个等位酶12个位点进行检测分析。结果表明,西施舌群体的遗传多样性较高,平均每位点等位基因数目（A）范围为1．5833—2．0000、平均每位点有效等位基因数目（Ae）范围为1．2850—1．5373、多态位点百分数（P）为33．33％、观察杂合度（Hc）为0．2389-0．3083、期望杂合度（He）为0．1496—0．2041之间。西施舌群体间有一定的遗传分化,遗传分化系数（FST）为0．0719,福建漳港群体与广西北海群体之间的FST为0．0413,但福建漳港群体和广西北海群体与江苏启东群体之间的FST为0．0505。 相似文献
6.
栉孔扇贝(Chlamys farreri)自然群体遗传多样性的RAPD分析 总被引：7，自引：0，他引：7
利用RAPD技术对栉孔扇贝(Chlamysfarreri)的四个自然群体(大连、烟台、青岛、韩国)的遗传多样性进行了分析。12个随机引物在四个群体中共检测到123个位点,其中多态位点109个,多态位点比例为88.62%;四个群体中均未检测到各群体特有的扩增带。韩国、烟台、大连、青岛四个群体的遗传多样性指数(Shannon指数)分别为0.2557、0.2557、0.2344和0.2249,以韩国和烟台群体遗传多样性较高,其次为大连群体,青岛群体最低,但它们之间无明显差异。不同群体的遗传多样性指数的平均数Hpop为0.2427,整个栉孔扇贝自然群体的遗传多样性指数Hsp为0.2503。遗传多样性剖分显示,绝大多数(97%)的遗传多样性是由群体内不同个体间的差异造成的,只有很小部分(3%)的遗传多样性与群体间的遗传分化有关。而采用基于单倍型(等位基因)之间的进化距离的AMOVA分析得到的这两个数据则分别为99%和1%,Φ值为0.010,且P=0.05,表明群体间遗传分化明显程度位于临界值。 相似文献
7.
长毛明对虾野生群体的杂合性研究 总被引：1，自引：0，他引：1
应用聚丙烯酰胺凝胶电泳技术,研究了长毛明对虾（Fenneropenaeus penicillatus）9个野生群体杂合子缺乏及过量情况;测定了8个酶系统,共检测到15个酶位点和32个等位基因．有7个多态位点,它们是Me-1、Me-2、Mdh-2、Aat-1、Sod-2、Est-1、Amy-1位点,在这些位点有2～5个等位基因．结果表明,在长毛明对虾9个群体的全部多态位点中,共有6个位点符合哈温平衡（P〉0．05）,30个位点偏离哈温平衡（p〈0．05）;除宁德群体外,其他8个群体中共有13个多态位点表现为杂合子缺失,结合每个群体中各个多态位点的期望杂合度与观察杂合度,认为导致杂合子缺乏的主要原因可能是种群内交、自然选择、Wahland效应、哑等位基因等．另外,在本研究中共有23个位点表现为杂合子过剩（F〈0）,且在长毛明对虾9个群体中均有出现,从而认为长毛明对虾的种质资源较好． 相似文献
8.
分离了鼠尾藻14个微卫星标记并用这些标记分析了鼠尾藻青岛群体遗传多样性和遗传结构。开发的14个标记在青岛群体中共检测到45个等位基因,各标记位点等位基因数在2和6之间,平均3.2个,平均有效等位基因2.1个,群体香农信息指数、观测杂合度、基因多样性指数、多态信息含量分别为0.799、0.449、0.466和0.406。青岛鼠尾藻种群体遗传多态性中等偏高。青岛4个鼠尾藻采集点的56个鼠尾藻个体在聚类图上无明显聚群和谱系。开发的标记将促进鼠尾藻遗传资源评价、保护和开发利用。 相似文献
9.
采用高通量测序法从单环刺螠基因组中开发微卫星标记,并通过一个秦皇岛单环刺螠野生群体对其进行多态性评价,利用获得的多态性引物对秦皇岛、烟台、潍坊、青岛、大连5个不同海区的野生单环刺螠群体进行了遗传多样性及遗传结构分析。结果表明:本实验设计的50个微卫星标记能稳定扩增的有38个,其中22个微卫星位点在5个群体中均表现为高多态性,等位基因数(Na)介于24—44之间,多态信息含量(PIC)介于0.921—0.967之间。5个群体总的平均有效等位基因数(N_e)范围为6.629—8.850,平均观测杂合度(Ho)和平均期望杂合度(He)范围分别为0.790—0.912、0.851—0.896,大连群体的杂合度最大(H_e=0.8962),潍坊群体的最小(H_e=0.8510),其中有12个微卫星位点在不同群体中出现显著偏离Hardy-Weinberg平衡的现象。平均遗传分化指数(FST)表明,群体分化水平处于中等分化水平(FST值为0.0880—0.1136);聚类分析显示烟台群体先与青岛群体聚为一支,再与秦皇岛群体聚类,然后跟潍坊群体聚为一支,大连群体单独聚为一支;遗传距离模式(IBD)显示单环刺螠群体的地理距离与遗传距离间不存在显著的线性关系。本研究开发的22对微卫星标记可以用于单环刺螠遗传结构分析研究,为下一步单环刺螠种质资源保护和人工繁育提供参考依据。 相似文献
10.
海湾扇贝养殖群体遗传多样性的研究 总被引：13，自引：4，他引：13
用等位基因酶的聚丙烯酰胺凝胶电泳技术,研究了大连沿岸不同生态环境条件下的大李家湾低排筏、大李家湾高排筏、凌水桥、棋盘磨4个海湾扇贝养殖群体的遗传多样性.在4个群体的7种等位基因酶和闭壳肌蛋白中均检测到了22个基因位点,各群体的多态位点比例分别为22.73%,22.73%,22.73%,18.18%(P≤0.95)和27.27%,27.27%,31.82%,36.36%(P≤0.99);杂合度观测值分别为0.064,0.071,0.075,0.069;Hardy-Weinberg平衡偏离指数分别为-0.068,-0.020,-0.032,-0.050;近交系数分别为0.568,0.565,0.487,0.550;位点等位基因有效数分别为1.102,1.109,1.143,1.122;遗传变异综合评价指数分别为0.0060,0.0071,0.0088,0.0073.海湾扇贝养殖群体遗传多样性总体水平较低,但在这4个群体中,凌水桥群体的遗传多样性水平最高,大李家湾高排筏和棋盘磨群体的遗传多样性水平较高,大李家湾低排筏群体遗传多样性水平最低. 相似文献
11.
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
12.
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
13.
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
14.
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
15.
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
16.
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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《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
20.
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