共查询到20条相似文献，搜索用时 46 毫秒
1.
海洋弧菌HN897株是一株高产琼脂糖酶的Vibrio astriarenae菌, 前期功能缺失实验证明其β-琼脂糖酶基因vas1-1339的缺失可显著降低弧菌HN897株的琼脂水解活性。文章在大肠杆菌中异源表达Vas1-1339基因编码蛋白, 分析该基因的表达及蛋白功能活性。首先, 构建含vas1-1339基因开放阅读框全长的表达载体pET28a-1339, 利用原核表达技术在大肠杆菌中成功地异源表达了Vas1-1339琼脂糖酶; 然后, 利用卢戈氏碘液染色分析发现异源表达Vas1-1339琼脂糖酶的大肠杆菌能够高效水解琼脂, 且异丙基硫代半乳糖苷(IPTG)最优诱导浓度为10μmol·L-1; 免疫印迹分析发现胞内基因表达产物羧基端可能存在切割现象, 推测Vas1-1339琼脂糖酶存在复杂的成熟过程。对纯化的琼脂糖酶活性分析发现海洋弧菌HN897株β-琼脂糖酶Vas1-1339能够独立发挥琼脂糖降解功能。 相似文献
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团头鲂(Megalobrama amblycephala)两种热休克蛋白 70(HSP70s)的原核表达、纯化及鉴定 总被引：1，自引：0，他引：1
采用PCR方法扩增团头鲂组成型HSC70和诱导型HSP70基因完整的编码区片段,并分别克隆到原核表达载体pET-22b(+)中,然后转化大肠杆菌BL21(DE3),用1mmol/L IPTG在不同温度及时间下进行诱导表达。采用Ni-NTA His Bind Resins亲和层析和DEAE-Sepharose FF阴离子交换柱层析对目的蛋白进行纯化,并进行SDS-PAGE和Western-blotting分析。结果表明,成功构建了团头鲂两种重组表达质粒pET-22b(+)/Ma-HSC70和pET-22b(+)/Ma-HSP70,表达融合蛋白的相对分子量均约为72kDa,并能与兔抗人HSP70多抗进行特异性结合,这两种HSP70s融合蛋白经纯化后的纯度均达到95%以上。本实验选择融合蛋白Ma-HSC70在25℃和Ma-HSP70在30℃下分别诱导7h作为可溶性表达的最佳条件。 相似文献
3.
草鱼出血病病毒VP7蛋白基因的人工合成与原核表达 总被引：2，自引：0，他引：2
根据GenBank已发表的GCRVVP7蛋白基因序列,设计合成2条特异性引物和19条搭桥引物,通过搭桥PCR人工合成带有3处变异碱基的GCRVVP7蛋白基因整个编码框,经过酶切、连接、PCR鉴定和测序鉴定克隆到原核表达载体pColdTF中,并转化大肠杆菌BL21(DE3),进行IPTG诱导表达和表达产物的SDS-PAGE、Western-blotting分析、纯化以及反应原性的iELISA检测。结果表明,成功人工合成了长831bp的GCRV VP7蛋白基因编码框和构建了VP7蛋白基因的重组质粒pCold TF-VP7,pColdTF-VP7转化菌经IPTG(1mmol/L)诱导3—4h即可获得特异性蛋白VP7重组蛋白的高效表达,VP7重组蛋白相对分子量大小约为73.9ku,与预期大小相符,且与鼠抗GCRV血清有良好反应原性。 相似文献
4.
为探讨大黄鱼(Larimichthys crocea)β-actin基因(Lc Actb)作为内参基因进行相关研究的可行性,从转录和翻译水平研究其组织表达谱,作者以大黄鱼肝脏为材料,扩增Lc Actb的开放阅读框序列,并将其亚克隆至原核表达载体p ET32a(+)。酶切、测序结果表明,p ET32a-Lc Actb构建成功。将p ET32a-Lc Actb转化到大肠杆菌BL21(DE3)中进行优化表达,表达蛋白经纯化后进行Western blotting验证;原核表达结果表明,IPTG可诱导一个分子量约45 ku的特异蛋白,且主要以包涵体的形式存在,优化表达条件为:28℃、0.4mmol/L IPTG、200 r/min诱导表达5 h。用表达蛋白作为抗原,免疫新西兰白兔制备抗Lc Actb的多克隆抗体;用纯化的多抗进行Western blotting的结果表明,获得了特异性的Lc Actb抗体;通过实时荧光定量RT-PCR检测大黄鱼多种组织m RNA的表达,其次,制备了多种组织匀浆蛋白,使用纯化的抗体进行Western blotting分析,结果显示,Lc Actb在大黄鱼成体各组织中转录和翻译水平的表达差异均不显著,可做为研究大黄鱼成体组织中其他基因表达和翻译水平的内参标准。 相似文献
5.
将青岛文昌鱼(Branchiostoma belcheri tsingtauense)肌球蛋白重链基因片段亚克隆到pET-30a质粒,构建出重组表达载体并转化入大肠杆菌Escherichia coli BL21中.经SDS-PAGE和Western杂交检测表明,在IPTG诱导下含有重组载体的菌株可表达分子质量约30 ku的融合蛋白.诱导条件优化实验结果显示,该菌株经0.2 mmol/L IPTG诱导1 h就可大量表达此蛋白.可溶性实验确认该重组蛋白是可溶性蛋白.本研究为文昌鱼肌球蛋白重链特异性抗体的制备奠定了基础. 相似文献
6.
转录因子Sp是一类广泛存在的锌指蛋白超家族成员,可与某些基因的上游调控序列结合,参与基因的转录调控。本研究采用同源克隆和RACE技术,获得单环刺螠的Sp8的全长cDNA,该序列长1 913bp,开放阅读框1 521bp,编码506个氨基酸;将其开放阅读框cDNA克隆到原核表达载体pET28a中,并转化大肠杆菌BL21(DE3)感受态细胞,在37℃条件下,经1mmol/L IPTG诱导表达4h,获得以包涵体形式存在的重组蛋白pET28a-SP,使用8mol/L尿素溶解包涵体,并通过镍离子金属螯合柱纯化获得重组蛋白,SDS-PAGE分析该蛋白的分子量约为50kD。Sp8蛋白体外表达的成功将为研究单环刺螠相关基因的转录调控打下基础。 相似文献
7.
研究了极大螺旋藻(Spirulina maxima)胞内多糖对SMMC7721等肿瘤细胞系的生长及凋亡的影响。在体外培养条件下,用半抑制浓度(80,5 mg/L)的极大螺旋藻胞内多糖(IPSⅠ,IPSⅡ)处理肿瘤细胞,并用MTT,SRB,DNA ladder,AnnexinⅤ等方法测定。结果表明,IPSⅠ(80 mg/L)对SMMC7721,A549,HeLa,U251等肿瘤细胞系抑制率分别为64.97%、46.1%、43.3%、27.02%;IPSⅡ(5 mg/L)能诱导SMMC7721细胞凋亡。 相似文献
8.
牙鲆Myogenin蛋白在大肠杆菌中重组表达的研究 总被引：1，自引：0，他引：1
采用大肠杆菌表达系统及pProEXTMHTc表达载体对牙鲆肌肉发生调节因子myogenin基因进行了体外重组表达研究。通过对诱导时间、IPTG诱导浓度以及诱导温度的优化,确定了最佳诱导条件为:诱导温度31℃,IPTG终浓度0.6mmol/L,诱导时间2 h。在该条件下,重组蛋白表达量最高且是可溶性的。Myogenin融合蛋白的成功表达为进一步深入研究其在牙鲆肌肉发育过程中的分子机制奠定了基础。 相似文献
9.
中国对虾细胞色素P450基因CYP4原核表达条件优化 总被引：1，自引：0，他引：1
根据克隆得到的中国对虾（Fenneropenaeus chinensis）CYP4基因开放阅读框设计引物,构建了中国对虾CYP4基因原核表达载体p28a-CYP4,并对重组菌株Rosetta／28a-CYP4的原核表达条件进行了优化。结果表明：p28a—CYP4转化Rosetta后可实现CYP4基因的原核表达,SDS—PAGE分析显示其在56．0kDa处有显著诱导条带;通过对诱导温度、IPTG浓度、诱导时机（OD600）及诱导时间的优化表明,重组菌株Rosetta／p28a-CYP4的最佳诱导温度为37℃,最佳IPTG浓度为1．2mmol／L,最佳诱导时机及诱导时间分别为0．59和6h。 相似文献
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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.
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
14.
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
15.
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
16.
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
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
19.
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
20.