目的:对副溶血弧菌(Vibrio parahaemolyticus,VP)的直接耐热溶血毒素(thermostable direct hemolysin,TDH)进行分离纯化,建立Western斑点印迹法技术检测致病性副溶血弧菌的方法。方法:用直接耐热溶血毒素免疫小鼠得到特异性抗血清,利用...目的:对副溶血弧菌(Vibrio parahaemolyticus,VP)的直接耐热溶血毒素(thermostable direct hemolysin,TDH)进行分离纯化,建立Western斑点印迹法技术检测致病性副溶血弧菌的方法。方法:用直接耐热溶血毒素免疫小鼠得到特异性抗血清,利用棋盘方法确定免疫血清最佳工作浓度,并对致病性与非致病性副溶血弧菌分别进行特异性测定。结果:最佳免疫血清最佳工作浓度为1:3200;检测致病性副溶血弧菌为阳性,非致病性副溶血弧菌属呈阴性。结论:Western斑点印迹法技术可以特异性检测致病性副溶血弧菌,灵敏度高、操作简单,可用肉眼判定结果。展开更多
The western margin of Yangtze block and southwestern Sanjiang region absorbed much attention from geologists. It has been proved that there occurred a series of plate subduction, collision, assembly, rifting and break...The western margin of Yangtze block and southwestern Sanjiang region absorbed much attention from geologists. It has been proved that there occurred a series of plate subduction, collision, assembly, rifting and breakup processes between them since Palaeozoic and the tectonic evolutionary relationship between them is clear. But in Proterozoic this kind of links between them became unclear. Did they undergo the assembly and breakup processes of the Rodinia super continent? This paper will take a primary discussion on this question on the basis of basement component, structure characteristics and magmatic activities.1\ Basement features\;(1) In western margin of Yangtze block its basement is composed of crystalline basement and folded basement, a so\|called double\|layer structure. The crystalline basement is made up of Kangding group, Pudeng Formation and Dibadu Formation, among them Kangding group is a representative and composed mainly of migmatite, compositing gneiss, hornblende schist and granulitite. The isotopic age of crystalline basement is older than 1900Ma, so its geological time is late Archaean to early Proterozoic. The folded basement is composed of Dahongshan group, Hekou group, Kunyang group, Huili group and Yanbian group. Their rock associations are made up mainly of spilite\|keratophyre formation, carbonate formation, clastic rock and clastic rock formation with some basic volcanic rocks. The folded basement is assigned to be early and middle Proterozoic (1000～1700M a).展开更多
文摘目的:对副溶血弧菌(Vibrio parahaemolyticus,VP)的直接耐热溶血毒素(thermostable direct hemolysin,TDH)进行分离纯化,建立Western斑点印迹法技术检测致病性副溶血弧菌的方法。方法:用直接耐热溶血毒素免疫小鼠得到特异性抗血清,利用棋盘方法确定免疫血清最佳工作浓度,并对致病性与非致病性副溶血弧菌分别进行特异性测定。结果:最佳免疫血清最佳工作浓度为1:3200;检测致病性副溶血弧菌为阳性,非致病性副溶血弧菌属呈阴性。结论:Western斑点印迹法技术可以特异性检测致病性副溶血弧菌,灵敏度高、操作简单,可用肉眼判定结果。
文摘The western margin of Yangtze block and southwestern Sanjiang region absorbed much attention from geologists. It has been proved that there occurred a series of plate subduction, collision, assembly, rifting and breakup processes between them since Palaeozoic and the tectonic evolutionary relationship between them is clear. But in Proterozoic this kind of links between them became unclear. Did they undergo the assembly and breakup processes of the Rodinia super continent? This paper will take a primary discussion on this question on the basis of basement component, structure characteristics and magmatic activities.1\ Basement features\;(1) In western margin of Yangtze block its basement is composed of crystalline basement and folded basement, a so\|called double\|layer structure. The crystalline basement is made up of Kangding group, Pudeng Formation and Dibadu Formation, among them Kangding group is a representative and composed mainly of migmatite, compositing gneiss, hornblende schist and granulitite. The isotopic age of crystalline basement is older than 1900Ma, so its geological time is late Archaean to early Proterozoic. The folded basement is composed of Dahongshan group, Hekou group, Kunyang group, Huili group and Yanbian group. Their rock associations are made up mainly of spilite\|keratophyre formation, carbonate formation, clastic rock and clastic rock formation with some basic volcanic rocks. The folded basement is assigned to be early and middle Proterozoic (1000～1700M a).
