水稻富含甘氨酸蛋白在细胞中的定位及其基因调控元件的转基因分析

水稻Angrp-1基因编码富含甘氨酸蛋白质。氨基酸序列分析表明该蛋白在氨基端可能存在一个信号肽序列，其后为富含甘氨酸序列。亲水性指数显示AnGRP-1蛋白包含两个区域。第一个区域由氨基端的1到27氨基酸残基组成。为强疏水性区。该肽段的氨基端为带正电荷号肽特征。与水稻Osgrp-1和菜豆grp1.8基因编码的信号肽进行同源性比较，发现这三种信号肽具有alafLvLLNIg同源序列。AnGRP-1蛋白的第二区域由第28到183氨基酸残基组成。该区域富含甘氨酸，具轻度亲水性，并且含有15个Gly-Tyr-Gly基序，这些基序中的酷西安酸残基之间相互作用，有可能形成分子间或分子内的连接。 利用水稻原生质体瞬间表达系统，比较Angrp-1基因启动子283bp和－1020bp片段，以及Ubiquitin启动子、Actin启动子和35S启动子的活性。结果表明，在水稻原生质体瞬间表达中，Angrp-1基因的两个启动子片段活性较低，接近本底。三个对照的组成型启动子中，以Ubiquitin启动子的活性最强，Actin启动子次之， 35S启动子最弱。根据以上结果推测水稻Angrp-1基因的表达可能具有组织或发育特异异表达和特性。 为研究Angrp-1基因的稳定表达与调控特性，将Angrp-1基因的启动子缺失片段1020bp、941bp、568bp和182bp分别与GUS基因融合，得到pGRP6-121、pGRP7-121、pGRP8-121和pGRP9-121等4个克隆，进行烟草转化，获得转基因植株。GUS活性测定表明在－1020到－568之间，随缺失增多，启动子活性下降。当缺失至－182时，182bp的启动子片段活性高于568bp片段。因此，Angrp-1基因5'端－1020到－568之间存在正调控序列，在－568至－182之间存在负调控序列。对pGRP6-121的烟草转基因植株进行GUS组织染色和活性测发现，GUS基因在维管组织优先表达。在根、茎、叶三种器官中，叶和茎的表达量最高。营养生长期的表达量高于生殖生长期。用2283bp和1020bp的启动子片段分别与GUS基因融合，转化水稻，转化体的GUS组织学染色表明Gus基因具有维管束优先表达特性。因此，Angrp-1基因的表达具有较明显的组织、器官和发育特异性。 水稻AnGRP-1蛋白的免疫组织定位分析表明，Angrp-1基因产物主要定位于水稻的维管组织。利用免疫金方法对AnGRP-1蛋白进行超微结构定位，发现金颗粒主要分布于水稻细胞的细胞壁中。因此，可基本确定AnGRP-1蛋白为细胞壁蛋白。在细胞内的内质网和高尔基体上面或附近也有金颗粒的分布，表明至少有部分AnGRP-1蛋白经过内质网－高尔基体－质膜途径，最终达到细胞壁。 为研究Angrp-1基因编码的信号肽功能，将其信号肽与GUS的氨基端融合，分别置于35S启动子和Angrp-1基因1020bp启动子片段控制之下，得到克隆p35s-SP-GUS-121和pGRP6-SP-GUS-121，分别以pBI121和pGRP6-121作对照，进行烟草基因转化。转化体的GUS活性分析表明，在35S启动子控制下，加与不加信号肽对GUS活性影响不大。但是，在Angrp-1基因的1020bp启动子片段作用下，信号肽与GUS融合后的转化体中其本不表现GUS活性。利用免疫金方法进行的超微结构定位表明，在p35S-SP-GUS-121和pGRP6-SP-GUS-121转化的烟草植株中，均可在细胞壁中检测室GUS产物的存在，因此AnGRP-1的信号肽能引导GUS从细胞质分泌细胞壁中。 以Angrp-1基因5'端的－568到＋1作探针，发现Angrp-1基因以在水稻窄叶青和京系17两个亲本中存在多态性，并进一步将Angrp-1基因定位于水稻第10号染色体上。

Frontal and cingulate gray matter volume reduction in heroin dependence: Optimized voxel-based morphometry

Aims: Repeated exposure to heroin, a typical opiate, causes neuronal adaptation and may result in anatomical changes in specific brain regions, particularly the frontal and limbic cortices. The volume changes of gray matter (GM) of these brain regions, ho

利用噬菌体展示技术制备识别酵母RNR3原核表达片段的单链抗体

选取酵母细胞RNR3蛋白序列中高保守片段:145-298位氨基酸序列,命名为RNR3h进行原核表达.并利用噬菌体展示技术从非免疫小鼠噬菌体展示抗体库中淘选到能与该原核表达产物特异性结合的单链抗体.得到的3种单链抗体均识别原核表达片段的空间抗原位点.为寻找酵母RNR1和RNR3的诱导表达水平与DNA损伤信号的相互关系,将真核生物RNRs发展为检测环境化学致癌物DNA损伤效应的生物标志物进行了尝试.

福尔马林灭活柱状黄杆菌对草鱼免疫相关基因表达的影响

在本研究中,将福尔马林灭活的柱状黄杆菌菌苗(FKG4)经腹腔注射免疫草鱼,以注射灭菌PBS作对照,分别在免疫后1、7、15和28d,提取受免鱼和对照鱼肝脏、脾脏和头肾3种组织中的总RNA并反转录成cDNA,利用Real-time PCR方法对不同组织中C-反应蛋白(CRP)、主要组织相容性复合体I(MHCⅠ)、肿瘤坏死因子(TNFα)、白介素1(IL-1β)、白介素8(IL-8)、Ⅰ型干扰素(IFNⅠ)等6种免疫相关基因的表达进行定量分析。结果发现CRP在受免鱼肝脏中的表达于免疫后1、7d显著高于对照鱼,

圆形碘孢虫单链抗体库的筛选与阳性克隆特征分析

噬菌体抗体库已成为单克隆抗体生成的重要技术之一。本文通过用圆形碘孢虫相关抗原对已构建的鼠源免疫噬菌体展示单链组合抗体文库进行生物淘选,并对几株相对亲和力较高的阳性单克隆序列特征、相对亲和力及热稳定性等进行了分析。ELISA、间接免疫荧光及免疫印迹等进行特征鉴定。结果表明,噬菌体抗体库技术对于分离抗圆形碘孢虫不同表位抗原是可行的,将为粘体动物的抗原物质及分布、寄生虫-宿主相互关系等研究提供丰富的抗体来源。

细菌DC_(10)的溶藻作用及环境因子对该作用的影响

从云南滇池分离获得溶藻细菌DC10,该菌属于假单胞菌属(Pseudomonassp.),它能强烈地溶解绿色微囊藻(Microcystisviridis,FACHB102)等6种蓝藻及月芽藻(Selenastrumcapricornutum,FACHB271)等2种绿藻.试验发现,该菌通过分泌某种物质来溶解藻类,较低的温度以及黑暗条件有利于细菌溶藻,不同浓度的氯化钙、硝酸钠对该菌的溶藻作用有一定影响;不同pH条件下,溶藻作用的强弱依次为:pH4>pH9>pH7>pH5.5.发展利用该菌进行水华控制的技术具有

鱼类微孢子虫的研究进展

中国科学院知识创新重大项目 (编号KZCX1 SW 12 ); 中国博士后科学基金项目 (编号 :2 0 4180 171)资助

Carbon source/sink function of a subtropical, eutrophic lake determined from an overall mass balance and a gas exchange and carbon burial balance

Although studies on carbon burial in lake sediments have shown that lakes are disproportionately important carbon sinks, many studies on gaseous carbon exchange across the water-air interface have demonstrated that lakes are supersaturated with CO2 and CH4 causing a net release of CO2 and CH4 to the atmosphere. In order to more accurately estimate the net carbon source/sink function of lake ecosystems, a more comprehensive carbon budget is needed, especially for gaseous carbon exchange across the water-air interface. Using two methods, overall mass balance and gas exchange and carbon burial balance, we assessed the carbon source/sink function of Lake Donghu, a subtropical, eutrophic take, from April 2003 to March 2004. With the overall mass balance calculations, total carbon input was 14 905 t, total carbon output was 4950 1, and net carbon budget was +9955 t, suggesting that Lake Donghu was a great carbon sink. For the gas exchange and carbon burial balance, gaseous carbon (CO2 and CH4) emission across the water-air interface totaled 752 t while carbon burial in the lake sediment was 9477 t. The ratio of carbon emission into the atmosphere to carbon burial into the sediment was only 0.08. This low ratio indicates that Lake Donghu is a great carbon sink. Results showed good agreement between the two methods with both showing Lake Donghu to be a great carbon sink. This results from the high primary production of Lake Donghu, substantive allochthonous carbon inputs and intensive anthropogenic activity. Gaseous carbon emission accounted for about 15% of the total carbon output, indicating that the total output would be underestimated without including gaseous carbon exchange. (C) 2007 Elsevier Ltd. All rights reserved.

Sediment sources and the flood record from Wanghu lake, in the middle reaches of the Yangtze River

A sediment core was collected from the centre of Wanghu Lake, in the Middle Reaches of the Yangtze River. The recent part of the core was dated using a combination of Pb-210 and spheroidal carbonaceous particle (SCP) techniques. Extrapolating this chronology dated the laminated section of the core, between 723 and 881 mm, to the first half of the 18th century and this section was selected for detailed study. The thicknesses of the laminae were measured using reflecting and polarizing microscopes whilst geochemistry was determined by an electron probe. The thickness of the dark layers was found to be positively correlated with titanium concentrations, and negatively correlated with aluminium and potassium concentrations. The thickness of the light layers was found to be negatively correlated with the concentrations of titanium. It is concluded that the dark layers were deposited from the Fushui River, a tributary of the Yangtze River, under periods of normal flow whilst the light Layers were mainly deposited from the Yangtze River itself during flood periods. Documentary evidence for floods occurring in the take catchment corresponded with thick laminations of high titanium concentration. Further, two of the three thickest, light laminations with low titanium concentrations were found to be synchronous with recorded flood dates of the main Yangtze River in its Middle Reaches, but one was synchronous with a local drought. These data suggest that the Lake sediment provides an archive of the relative water levels of the Yangtze and Wanghu including floods of both the main Yangtze River and the local hydrological regime. (c) 2006 Elsevier B.V. All rights reserved.