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1.
采用RT-PCR和快速扩增cDNA末端(rapid amplification of cDNA ends, RACE)技术首次克隆了曼氏无针乌贼?-肌动蛋白基因的 cDNA 全序列, 该序列全长为 2000bp, 由长 197bp 的 5’非翻译区(untranslated region, UTR), 669bp 的 3’非翻译区, 和 1134bp 的开放阅读框(open reading frame, ORF)组成。阅读框共编码 377 个氨基酸, 推算的分子量约为 42.0kDa, 理论等电点为 5.16。曼氏无针乌贼-actin 氨基酸序列中 Ile12、Ser172、Ser174、Gln223、His227、Ile231、Gly232、Ser320、Glu328、
Thr360等10个氨基酸残基具有特异性, 以及2个特殊的氨基酸残基位点和2个软体动物特有的氨基酸残基。曼氏无针乌贼?-actin 氨基酸序列与软体动物、节肢动物、脊椎动物的相似性高达 97%。NJ法系统进化分析显示曼氏无针乌贼首先与软体动物聚在一起, 然后与节肢动物聚在一起, 再与鱼类、两栖类、哺乳类聚在一起。 相似文献
2.
硬脂酰辅酶A去饱和酶(SCD)是脂肪代谢的关键酶。本研究采用RT-PCR和RACE技术克隆了曼氏无针乌贼(Sepiella maindroni)SCDcDNA的全序列,序列全长1513bp,由261bp的5′非翻译区、编码306个氨基酸的921bp开放阅读框和331bp的3′非翻译区组成。在线翻译所得多肽理论分子量为34.92kDa,等电点为8.95,是疏水性蛋白,含有丰富的螺旋结构(45.10%),存在4个跨膜区。其氨基酸序列与真蛸(Octopus vulgaris)和长牡蛎(Crassostrea gigas)相似性达到91%,与其它非软体动物也表现为50%以上的相似性,说明SCD结构相对保守;系统进化树结果表明曼氏无针乌贼和真蛸及牡蛎进化关系最近,与鱼类稍远,与人及大鼠等哺乳动物亲缘关系最远。SCD基因是改善曼氏无针乌贼肉质的重要候选基因,其成功克隆及相关分析对于深入探讨软体动物脂肪酸代谢相关基因在生物体内作用机制及调控机理具有重要意义。 相似文献
3.
精子表面蛋白17(Sp17)是参与受精过程的关键分子。本研究采用RT-PCR以及RACE技术克隆得到了曼氏无针乌贼(Sepiella japonica)Sp17简称Sj-Sp17 c DNA的全长序列,序列全长1463bp,5′和3′非编码区分别为92bp和222bp,预测的开放阅读框(ORF)全长1149bp。编码的蛋白理论分子量为42.0548k Da,等电点4.66,是一种亲水性蛋白,不存在跨膜区以及信号肽序列,含有丰富的螺旋结构(54%)。同源氨基酸序列比对发现,与其他软体动物的相似性最高仅为44%,表明Sp17在进化中并不保守。基于Sp17氨基酸序列构建的系统进化分析表明,曼氏无针乌贼和加州双斑蛸(Octopus bimaculoides)进化关系最近。组织特异性分析发现Sp17在曼氏无针乌贼的生殖系统中均有较高的表达量,其中在精巢和储精囊中有显著表达。Sp17基因的成功克隆以及组织表达特异性分析对于深入研究其细胞定位以及生物学功能具有重要意义。 相似文献
4.
曼氏无针乌贼(Sepiella maindroni)sigma-型谷胱甘肽硫转移酶基因的克隆及重组表达 总被引：1，自引：0，他引：1
采用EST结合RACE技术进行了曼氏无针乌贼(Sepiella maindroni)sigma-型GST(SmGST)基因的克隆。结果表明,该基因的cDNA全长为838bp,其中5′非编码区为73bp,3′非编码区为150bp,开放阅读框为615bp,编码的蛋白含有204个氨基酸。该基因的氨基酸序列中包含1个典型的GST-N结构域和一个GST-C结构域,与栉孔扇贝和长牡蛎的sigma-型GST的相似度分别为40.3%和39.3%。将该基因的编码区重组到pET-21(a+)载体后在大肠杆菌中得到诱导表达。重组SmGST的GST活力为(12.22±0.92)U/mg蛋白。 相似文献
5.
以FMRFamide为典型代表的FMRFamide相关肽,是目前已知的最大的神经肽家族。FMRFamide广泛参与多种生理过程,包括摄食、心跳、渗透平衡、变态、防御和免疫等。采用同源克隆法与RACE技术获得了虎斑乌贼FMRFamide的G蛋白偶联受体基因cDNA全长序列(命名为SpFaGPCR,OL765295),SpFaGPCR cDNA全长1514bp,包括222bp的5''-非编码区(5''-UTR)、35 bp的3''-UTR以及1257bp的开放阅读框(ORF),共编码418个氨基酸。预测相对分子量(MW)为49.8kDa,等电点(pI)为9.76,具有7个跨膜结构域、糖基化位点7个、磷酸化位点36个。同源序列比对分析表明,SpFaGPCR与曼氏无针乌贼的FaGPCR氨基酸序列相似度最高达98%。系统发育分析显示SpFaGPCR与双壳纲的FaGPCR聚为姐妹支。荧光定量结果显示SpFaGPCR在视叶、视腺、脑、缠卵腺中表达量相对较高(P<0.05)。进一步利用原位杂交技术检测到虎斑乌贼视叶的髓质区、视网膜的感光细胞和缠卵腺的瓣叶外层具有明显的阳性杂交信号。实验结果为进一步探讨FMRFamide通过FaGPCR的介导参与虎斑乌贼生理代谢功能奠定了前期基础。 相似文献
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采用RT-PCR和RACE技术克隆了大黄鱼胰岛素样生长因子-Ⅰ(IGF-Ⅰ)cDNA的全序列,序列全长2027bp,由57bp的5’非翻译区、1409bp的3’非翻译区和561bp的开放阅读框组成。序列分析表明,大黄鱼IGF-Ⅰ编码区包括信号肽、成熟肽(B、C、A、D)和E等6个区域的186个氨基酸,形成成熟肽时,信号肽和E区被切除,成熟肽分子量7.5kDa,等电点(pI)为7.76,成熟肽的B区和A区有6个保守的半胱氨酸残基,形成3对二硫键,起到了稳定IGF-Ⅰ三维结构的作用。与其它物种的IGF-Ⅰ比对后发现A、B区域比较保守,C、D区域保守性较差;E区域的分析结果表明,大黄鱼IGF-ⅠcDNA序列为Ea-4亚型。核苷酸同源性分析发现,大黄鱼IGF-ⅠcDNA与美国红鱼同源性最高,为99.47%;与斜带石斑鱼、金头鲷和褐牙鲆的同源性依次降低,分别为97.68%、97.50%和95.90%。 相似文献
7.
脊尾白虾(Exopalaemon carinicauda)ferritin 基因克隆及表达分析 总被引：1，自引：1，他引：0
采用RT-PCR及RACE技术获得了总长度为755bp的脊尾白虾ferritin基因cDNA序列。该基因序列5’和3’的非编码区分别为112bp和146bp,开放阅读框497bp,推测编码169个氨基酸,预测蛋白分子量19.1kDa,等电点5.46,该基因命名为Ecfer基因。利用Neighbor-joining法构建系统进化树分析结果表明,Ecfer基因氨基酸序列与无脊椎动物中的甲壳动物聚为一支(同源性为64%—67%)。此外,Ecfer基因氨基酸序列与脊椎动物铁蛋白H链同源性为53%—57%。采用荧光定量RT-PCR研究Ecfer基因在组织中以及经WSSV刺激后血淋巴、肝胰腺中的表达变化情况。研究结果表明,Ecfer在肝胰腺、卵巢、肌肉、鳃和血淋巴中均有分布。注射WSSV后3h和6h,肝胰腺和血淋巴Ecfer基因表达较对照组均显著上调(P<0.05),并具有显著的时间差异性。说明Ecfer基因可能参与了脊尾白虾抵抗WSSV入侵的免疫反应。 相似文献
8.
热休克蛋白70(HSP70)是生物体内一种重要的机体与细胞保护性蛋白。本文利用RT-PCR以及RACE技术首次克隆获得太平洋真宽水蚤(Eurytemora pacifica)HSP70简称Ep.HSP70 c DNA的全长序列,序列全长为2252bp(KY807149),开放阅读框(ORF)长1947bp,编码649个氨基酸,5′端99bp,3’端206bp;预测蛋白分子量为70.81k Da,等电点为5.16,为一种亲水性蛋白,不存在信号肽及跨膜区,含有丰富的α螺旋结构(37.60%),β折叠(18.80%)。同源氨基酸序列比对发现,与其他甲壳动物的同源基因保守性较高,尤其是HSP70家族典型的结构位点序列在甲壳类动物中具有高度保守性。系统进化分析表明,太平洋真宽水蚤和安氏伪镖水蚤(Pseudodiaptomus annandalei)进化关系最近;桡足类种内同源性要高于虾蟹类,与虾类同源性高于蟹类。荧光定量数据分析表明,不同浓度铜、镉、锌胁迫下太平洋真宽水蚤HSP70基因表达水平具有显著的时间效应与浓度效应的特征,三种金属对Ep.HSP70抑制效应呈现CuCdZn的趋势。Ep.HSP70基因的成功克隆及金属胁迫下的表达分析为深入研究HSP70蛋白生物学功能具有重要意义。 相似文献
9.
采用RACE技术克隆了单细胞绿藻蛋白核小球藻820Rubisco活化酶基因(rca)序列,并用荧光定量PCR方法研究了rca和Rubisco小亚基基因(rbcS)的表达规律。结果获得了1703bp的rcacDNA序列,包括66bp的5’非翻译区、1242bp的开放阅读框和395bp的3’非翻译区。序列比较和分析表明该蛋白核小球藻rca序列与其它绿藻的同源性高达78%—85%;偏好使用以G/C/T结尾的密码子;推测的RCA蛋白等电点和分子量分别为8.44和45.71kDa。荧光定量PCR结果表明随光照时间增加rca与rbcS转录表达逐渐降低;不同盐度处理下rbcS的mRNA量变化不大,而rca在37.5盐度下表达量为25盐度的2.69倍;1.0—3.0mmol/L水杨酸处理rca与rbcS表达均降低。 相似文献
10.
以坛紫菜丝状体为材料,采用RACE方法获得坛紫菜碳酸酐酶(CA)基因的全长cDNA。该cDNA全长1 081 bp,具有一个825 bp的开放阅读框,可编码274个氨基酸。序列同源性分析显示该cDNA序列推导的氨基酸序列与其他物种的碳酸酐酶具有较高的一致性,其中与条斑紫菜的一致性达到96%。氨基酸序列分析表明该蛋白为β-CA,含有两个CA活性位点,无跨膜结构,可能存在一个信号肽将其定位到叶绿体中,与藻类和细菌聚类。原核诱导表达得到一个72 kDa左右的融合蛋白,酶活测定结果显示此蛋白具有碳酸酐酶活性。该实验对进一步深入研究坛紫菜CA的功能及坛紫菜碳代谢、光合作用等生理过程具有重要的参考价值。 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.
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
13.
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
14.
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
15.
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
16.
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
17.
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
18.
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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