靶向斑马鱼VEGF的shRNA表达载体的构建及其对斑马鱼胚胎血管发育的影响

血管内皮生长因子(vascular endothelial growth factor, VEGF)是一种多功能的细胞因子，其主要作用是促进血管内皮细胞增殖和增加血管通透性，是肿瘤及正常组织血管生成的中心调控因素，以VEGF为靶点的肿瘤血管靶向性治疗成为近几年肿瘤治疗的新途径。RNAi是近年来新发展的一项反向遗传学技术，是一种研究基因功能的有力工具。斑马鱼作为一种重要的模式生物，被广泛用于胚胎的分子发育机制、疾病模型的构建以及药物筛选等研究中。然而在斑马鱼中运用RNAi技术进行基因功能研究是一个相对较新的领域，研究资料较少，并且目前进行的斑马鱼RNAi实验中，siRNA大都是通过化学方法或体外转录合成的。体外合成的siRNA在进入体内后会被降解而无法达到持久阻抑基因表达的目的。因此本研究旨在探讨VEGF特异性siRNA表达载体对斑马鱼VEGF基因的沉默作用，通过分析表型及相关细胞因子的变化，阐明VEGF对斑马鱼胚胎血管生成的影响及作用机制。 研究通过计算机辅助设计软件，针对斑马鱼VEGF mRNA不同位点设计合成了4段含siRNA特异序列的DNA单链，经退火，克隆入pSilencer 4.1-CMV neo载体CMV启动子下游，构建了重组质粒pS1-VEGF、pS2-VEGF、pS3-VEGF及pS4-VEGF。 通过显微注射的方法将载体导入1-2细胞期斑马鱼体内，于胚胎发育的48 h采用RT-PCR的方法检测VEGF基因的表达量，研究不同干扰序列对VEGF基因表达的干涉作用。结果显示，针对不同位点的表达载体对VEGF基因表达的抑制效率有显著差异。它们对VEGF mRNA的抑制率分别为80.5%，42.8%，12.5%，40.7%。通过筛选我们得到了一条具有高效抑制作用的载体pS1-VEGF，该载体的相应序列靶向斑马鱼两个主要异构体VEGF165和VEGF121的共有外显子序列。 形态学检测结果显示，注射了pS1-VEGF的胚胎出现了心包膜水肿、血流速度减慢、循环红细胞堆积等症状。定量碱性磷酸酶染色显示，注射pS1-VEGF能够抑制斑马鱼胚胎新生血管的形成，当注射剂量为0.4 ng时，血管生成的抑制率为31.8%。NBT/BCIP血管染色显示，注射该载体后72 h，50%的斑马鱼肠下静脉、节间血管以及其它血管的发育受到不同程度的抑制。随着注射剂量的加大，血管发育受抑制的情况也随之加重，当注射剂量为1 ng时，只有心脏、头部及卵黄有血液循环。对干扰效果的特异性进行了研究，结果表明pS1-VEGF对斑马鱼内源基因胸苷酸合成酶（thymidylate synthase, TS）基因的表达没有明显的抑制作用。针对TS基因的shRNA表达载体及与斑马鱼没有同源性的对照载体对VEGF基因表达也没有明显的抑制作用。浓度梯度实验表明在0-1.2 ng的范围内干扰效果具有剂量依赖性。 以胚胎整体原位杂交的方法检测质粒对VEGF基因受体NRP1基因表达的影响，发现VEGF特异性shRNA表达载体能够引起NRP1基因表达的降低，说明斑马鱼中VEGF所介导的血管生成作用至少在部分上是依赖于NRP通路所调节的。 本研究工作为进一步研究斑马鱼基因功能、VEGF调控网络提供了一个快速、有效的手段，为阐明斑马鱼的血管生成机制提供了新的资料，为采用RNAi技术，以VEGF为靶点，以斑马鱼为模型对肿瘤进行基因治疗研究奠定了基础。

地震层析成像与天山地区的壳幔深部结构研究

The Tien Shan is the most prominent intracontinental mountain belt on the earth. The active crustal deformation and earthquake activities provide an excellent place to study the continental geodynamics of intracontinental mountain belt. The studies of deep structures in crust and upper mantle are significantly meaningful for understanding the geological evolution and geodynamics of global intracontinental mountain belts. This dissertation focuses on the deep structures and geodynamics in the crust and upper mantle in the Tien Shan mountain belt. With the arrival time data from permanent and temporal seismic stations located in the western and central Tien Shan, using seismic travel time tomographic method, we inversed the P-wave velocity and Vp/Vs structures in the crust and uppermost mantle, the Pn and Sn velocities and Pn anisotropic structures in the uppermost mantle, and the P-wave velocity structures in the crust and mantle deep to 690km depth beneath the Tien Shan. The tomographic results suggest that the deep structures and geodynamics have significant impacts not only on the deformations and earthquake activities in the crust, but also on the mountain building, collision, and dynamics of the whole Tien Shan mountain belt. With the strongly collision and deformations in the crust, the 3-D P-wave velocity and Vp/Vs ratio structures are highly complex. The Pn and Sn velocities in the uppermost mantle beneath the Tien Shan, specially beneath the central Tien Shan, are significantly lower than the seismic wavespeed beneath geological stable regions. We infer that the hot upper mantle from the small-scale convection could elevate the temperature in the lower crust and uppermost mantle, and partially melt the materials in the lower crust. The observations of low P-wave and S-wave velocities, high Vp/Vs ratios near the Moho and the absences of earthquake activities in the lower crust are consistent with this inference. Based on teleseismic tomography images of the upper mantle beneath the Tien Shan, we infer that the lithosphere beneath the Tarim basin has subducted under the Tien Shan to depths as great as 500 km. The lithosphere beneath the Kazakh shield may have subducted to similar depths in the opposite direction, but the limited resolution of this data set makes this inference less certain. These images support the plate boundary model of converge for the Tien Shan, as the lithospheres to the north and south of the range both appear to behave as plates.