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1.
藻胆蛋白裂合酶是催化藻胆色素与脱辅基藻胆蛋白亚基共价连接的裂合酶,在藻胆蛋白的生物合成途径中发挥着重要作用。本实验以藻蓝蛋白裂合酶Cpc E/F为研究对象,采用基因工程组合表达技术,构建了pCDFDuet-apcA-cpcE/F-hox1-pebS、pCDFDuet-pecA-cpcE/F-hox1-pebS等重组质粒,并导入大肠杆菌中,在IPTG的诱导下,成功表达得到两种非天然藻胆蛋白ApcA-PEB和PecA-PEB,这表明Cpc E/F不仅可以催化藻蓝胆素和脱辅基藻蓝蛋白的结合,还可以催化藻红胆素(PEB)与别藻蓝蛋白α-亚基(ApcA)和藻红蓝蛋白α-亚基(PecA)的结合,因此是一种多功能的裂合酶。根据重组产物的光谱特征峰分析发现,ApcA-PEB和PecA-PEB作为两种非天然存在的重组藻胆蛋白,具有与对应天然藻胆蛋白有着相近的特征吸收光谱和荧光发射峰,但同时具有明显的波长偏移并伴有色素异化现象,其光谱学性质主要由其所携带的色素基团决定。另外,荧光寿命衰减分析发现,不同脱辅基蛋白对于重组藻胆蛋白的光谱稳定性具有重要的影响。  相似文献   

2.
坛紫菜藻红蛋白α,β亚基基因的克隆和序列分析   总被引:1,自引:0,他引:1       下载免费PDF全文
藻胆蛋白(Phycobiliprotein,PBP)是原核藻类和真核藻类进行光合作用的捕光色素蛋白,占藻体干重的2%左右,主要分为3类:藻红蛋白(phycoer-ythrin,PE)、藻蓝蛋白(phycocyanin,PC)和别藻蓝蛋白(allophycocyanin,APC)[1].藻胆蛋白一般由α亚基和β亚基组成,部分藻胆蛋白中还存在γ亚基.一般由α和β亚基形成稳定的单体(αβ),再由单体聚合为多聚体(αβ)n.从蓝藻和红藻中分离的藻胆蛋白为三聚体(αβ)3或六聚体(αβ)6[2].  相似文献   

3.
坛紫菜(Porphyra haitanensis T.J.Chang et B.F.Zheng)中的R-藻蓝蛋白在Bio-Rex 70柱上用脲溶液(pH3.0)解离和层析,得到了α和β两个亚基,用SDS-PAGE测定α和β亚基的分子量分别为18 400和20 500。变藻蓝蛋白的α和β两亚基均分子量经测定,分别为18 800和19 700。R-藻蓝蛋白和变藻蓝蛋白的分子量分别确定为117 000和112 000,两藻胆蛋白中α和β两个亚基的摩尔比都为1:1,确定两藻胆蛋白的亚基组成都为(αβ)_3。各亚基的发色团含量为:R-藻蓝蛋白中,α亚基含1个藻蓝胆素,β亚基含1个藻蓝胆素和1个藻红胆素。变藻蓝蛋白中,α和β亚基各含1个藻蓝胆素。  相似文献   

4.
为探究蓝藻藻胆体核心色素蛋白-别藻蓝蛋白单个亚基的光学活性和功能,本研究克隆了钝顶节旋藻(Arthrospira platensis FACHB314)中的脱辅基别藻蓝蛋白基因apcAB及其亚基基因apcA和apcB。节旋藻基因组中apcAB全长共1 056 bp,由apcA和apcB串联组成,中间间隔84 bp。其中,apcA和apcB基因的全长均为486 bp,且均编码161个氨基酸,预测分子量分别约为17.39和17.33 kDa,它们分别编码的α和β亚基均属于Globin_like超级家族,系统进化树分析显示其氨基酸序列在蓝藻和节旋藻中较为保守。将克隆出的亚基基因apcA、apcB分别同前期A.platensis FACHB314中获得的藻蓝胆素合成相关基因ho和pcyA以及色基裂合酶基因(cpcE、cpcF、cpcU、cpcS、cpcT)共同转化至大肠杆菌中,获得重组别藻蓝蛋白亚基菌株E.coli HPEFUSTA、E.coli HPEFUSTB。SDS-PAGE和Western Blot均显示重组菌株中已成功表达别藻蓝蛋白单亚基。荧光检测结果显示,在600 nm波长激发下,...  相似文献   

5.
坛紫菜R-藻蓝蛋白和变藻蓝蛋白的亚基组成和发色团含量   总被引:1,自引:0,他引:1  
坛紫菜中的R-藻蓝蛋白在Bio-Rex70柱上用脲溶液(pH3.0)解离和层析,得到了α和β两个亚基。用SDS-PAGE测定α和β亚基的分子量分别为18400和20500,变藻蓝蛋白的α和β两亚基的分子量经测定,分别为18800和19700。R-藻蓝蛋白和变藻蓝蛋白的分子量分别确定为117000和122000,两藻胆蛋白中α和β两个亚基的摩尔比都为1:1,确定两藻胆蛋白的亚基组成都为(αβ)3。各  相似文献   

6.
光学活性藻蓝蛋白β亚基的体内重组   总被引:1,自引:0,他引:1  
在Synechococcus sp.PCC 7002中,首先发现了特异性催化脱辅基藻蓝蛋白β亚基(153位)与藻蓝胆素(phycocyanobiling, PCB)连接的裂合酶基因cpcT.本实验在Synechocystis sp.PCC 6803中找到与cpcT具有高度同源性的基因slr1649.构建2组相容的重组质粒pCDF-cpcB(C82I)或(C153I)-ho1-pcyA和pRSF-slr1649,cpcB(C82I)和cpcB(C153I)分别编码82和153位被突变的脱辅基藻蓝蛋白β亚基,slr1649编码可能的特异性裂合酶,在大肠杆菌体内生成PCB必需的2个基因(ho1编码血红素氧化酶,pcyA编码藻蓝胆素合成酶),将这些基因共同转化到大肠杆菌诱导表达,利用亲和层析柱对可溶性蛋白进行纯化,产物进行SDS-PAGE、色素蛋白锌电泳和光谱检测.结果表明基因slr1649能够特异性催化CpcB(153位)与PCB的连接,产生了具有光学活性的CpcB(C82I)-PCB,为进一步研究螺旋藻藻蓝蛋白的生物活性奠定了基础.  相似文献   

7.
采用亚克隆方法,将别藻蓝蛋白(allophycocyanin,APC)基因插入到毕赤酵母整合型表达载体pPIC6αA中,再用SacⅠ线性化,纯化后,用氯化锂法转化毕赤酵母菌株X-33,筛选表达APC的重组子。PCR和序列分析表明,APC基因已整合到酵母染色体中。重组子经甲醇诱导,用Western blotting在培养基上清液检测到APC,表明别藻蓝蛋白(APC)在毕赤酵母中可以表达。APC由两种亚基组成,分子量分别为19kDa和21kDa。重组子经摇瓶培养48h表达量达4.4mg/L。  相似文献   

8.
藻胆蛋白脱辅基蛋白对其抗氧化活性的影响   总被引:10,自引:1,他引:10       下载免费PDF全文
探讨了光照和脱辅基蛋白结构对藻胆蛋白抗免化活性的影响,结果表明,光照下,藻胆蛋白能够产生自由基,黑暗下,则能够清除自由基,因此,藻胆蛋白具有产生和清除自由基的双重功能。在光照下,用SDS(十二烷基硫酸钠)、脲及碱性条件下,对藻胆蛋白进行变性,藻胆蛋白产生自由基的能力消失,清除自由基的能力明显增强,因此,藻胆蛋白清除自由基主要由藻胆色素完成,天然状态下藻胆蛋白中脱辅基蛋白三维结构更有利于色素基团对光能的吸收与传递,这与其在体内的生理功能相一致。  相似文献   

9.
本文从条斑紫菜(Porphyra yezoensis)中提取了藻胆蛋白,找到了一种新的简便有效的提纯R-藻红蛋白的方法。用Bio-GelP300柱进一步纯化后,得到了高纯度的R-藻红蛋白。用Bio-Rex 70柱分离R-藻红蛋白,得到了它的α和β亚基溶液。对亚基溶液进行的一些光谱分析表明亚基溶液具有R-藻红蛋白的一些性质。本文对α和β亚基的发色团含量进行了测定:α亚基含2个藻红胆素,β亚基含3个藻红胆素和1个藻尿胆素。  相似文献   

10.
坛紫菜别藻蓝蛋白α,β亚基基因的克隆和序列分析   总被引:3,自引:0,他引:3  
以野生坛紫菜色素体DNA为模板, 通过PCR扩增获得编码坛紫菜别藻蓝蛋白α亚基和β亚基的序列及两者之间的间隔序列,该序列全长为1 055 bp,其中编码α和β亚基的序列均为486 bp,间隔序列为83 bp.该序列与GenBank收录的其他4种红藻相关序列的同源性在75.6%~87.4%,与2种蓝藻的同源性分别为66.9%,68.5%,其中编码区同源性更高.  相似文献   

11.
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.
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.
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.
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.
17.
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   

18.
19.
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   

20.
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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