蟾蜍皮肤活性蛋白与多肽的研究

近年来，我们致力于蟾蛛（Bufo andrewski）皮肤活性组份的研究，构建了缥蛛皮肤cDNA文库，检测了蟾蛛皮肤分泌液中多种生物活性，进一步纯化得到了四个新的生物活性蛋白：溶菌酶、抗爱滋病毒蛋白以及两个丝氨酸蛋粼酶抑制剂，并，简述如下；I、第三章报导了我们从蟾蛛皮肤分泌液中分离得到的一个谊薇酚犷杰女呱BA一娜"zym"）·BA一lvs"Zym"经5DS一PAGE检测为一条带，其分子量约为巧k珍。·它是一个高效的溶菌酶，每毫克蛋白的溶菌活性为2．7xl护俪ts，还能抑制革兰氏阳性菌（金黄色葡萄球菌Slaj，匆褚ococcusaureus）和革兰氏阴性菌（大肠杆菌Esch邵ichiacoli）生长，其最小抑菌浓度（MIC）分别为1．36拼M和84并M。使用PCR筛选法，我们从蟾蛛皮肤c溯A文库中克隆得到编码BA一lyso即me的cDNA序列。BA一lysozymeN末端测序和肤质量图谱确认了蛋白和基因的网一性。它的蛋白全序列与鸡溶菌酶的相似性为5氏5％。系统发育分析显示，与其最相似的是来源于海龟的溶菌酶。11、第四章介绍了我们从蟋蛛皮肤分泌液中分离得到的一个新的抗lllV蛋白，命名为BAS一AH。BAS一AH是一个分子量为63kD。的单链蛋白，每摩尔蛋白质含有0．89摩尔血红素辅基。BAS一AH对人T淋巴细胞系CS166细胞的毒性（CCS。）为9．5尽M。BAs一AH具有较强的抗HIV活性，它对HIV感染和复制具有剂量依赖抑制效应，其选择指数（CCso／Ecs。）分别为14．4和11．4·BAS一麟J也能抑制HIV的逆转录酶，其1C5（）为L32冬以。BAs一AH的N末端氨基酸为NA以KADvIGKIsILLGQDI』slvAAM，与己知的抗Hlv蛋白没有同源性·表明它可能是一个新的抗川v蛋自。BAs一AH没有检测到抗菌活性、蛋自酶水解活性、胰蛋自酶抑制剂活性、L一氨基酸氧化酶活性和过氧化氢酶活性。班、第五伞报导了我们通过离子交换、分子筛和反向层析，从蟾赊皮肤中分离得到的一个新的胰蛋白酶抑制剂，命名为BATI。BATI是一个单链糖蛋自·其分子量为22kD。。它是吵～个热稳定的竞争性的抑制剂，能有效抑制胰蛋自酶·其抑制常数凡为14nM。B灯I对凝血酶、弹性蛋白酶以及糜蛋白酶都没有抑制作用。BATI的N末端序列为El犯ITD，不同于其它物种来源的蛋白酶抑制剂。W、第六章介绍了蟾蛛皮肤分泌液中纯化得到的另外一个蛋白酶抑制剂（命名为baserpin）。与上述BATI不同的是，basel咖n不可逆地抑制多种蛋白酶。它是一个分子量约为60kDa的单链糖蛋白，除了能抑制胰蛋白酶，还能有效抑制糜蛋白酶和弹性蛋白酶。它抑制上述三种酶的二级反应常数（编）分别为4．6x1护M一，s一l、8．9》1护M一15一I以及6．8xl护M一ls一l。BaserPin是第一个来源于两栖类皮肤的不可逆抑制剂，其N末端氨基酸序列为HTQYPDILIAKPxDK，与其它物种来源的蛋白酶抑制剂不同。本论文综述了蟾蛛皮肤中的活性组份，报导了我们近年来研究蟾蛛皮肤活性蛋白与多肤的进展，分四章详细介绍了蟾蛛皮肤中纯化得到的四个活性蛋白。BA一lysozyme是两栖类动物中第一个得到蛋白质全序列的溶菌酶，能有效抑制革兰氏阳性菌和革兰氏阴性菌生长；BA象AH是一个含血红素辅基的抗HIV蛋白，其独特的理化性质和功能证明它是一个新的抗病毒蛋白。根据所鉴定的性质判断，BATI和bos仰in分别属于竞争性抑制剂和不可逆抑制剂。其中，base印in是第一个从两栖类皮肤中分离得到的不可逆抑制剂。

东喜马拉雅构造结新生代碰撞变形与岩石圈演化

The Eastern Himalayan Syntaxis (EHS) is one of the strongest deformation area along the Himalayan belt resulted from the collision between Indian plate and the Eurasian Plate since the 50～60Ma, and has sensitivity tracked and preserved the whole collisional processes. It should depend on the detail geological investigations to establish the deformational accommodate mode, and the uplift history, to elucidate the deep structure and the crust-mantle interaction of the Tibet Plateau of the EHS. The deep-seated (Main Mantle Thrusts) structures were exhumed in the EHS. The MMT juxtapose the Gangdese metamorphic basement and some relic of Gangdese mantle on the high Himalayan crystalline series. The Namjagbawa group which is 1200～1500Ma dated by U/Pb age of zircon and the Namla group which is 550Ma dated by U/Pb age of zircon is belong to High Himalayan crystalline series and Gangdese basement respectively. There is some ophiolitic relic along the MMT, such as metamorphic ocean mantle peridotite and metamorphic tholeiite of the upper part of ocean-crust. The metamorphic ocean mantle peridotites (spinel-orthopyroxene peridotite) show U type REE patterns. The ~(87)Sr/~(86)Sr ratios were, 0.709314～0.720788, and the ~(143)Nd/~(144)Nd ratios were 0.512073～0.512395, plotting in the forth quadrant on the ~(87)Sr/~(86)Sr-~(143)Nd/~(144)Nd isotope diagram. Some metamorphic basalt (garnet amphibolite) enclosures have been found in the HP garnet-kynite granulite. The garnet amphibolites can be divided two groups, the first group is deplete of LREE, and the second group is flat or rich LREE, and their ~(87)Sr/~(86)Sr, ~(143)Nd/~(144)Nd ratios were 0.70563～0.705381 and 0.512468～0.51263 respectively. Trace element and isotopic characteristics of the garnet amphibolites display that they formed in the E-MORB environment. Some phlogolite amphibole harzburgites, which exhibit extensive replacement by Phl, Amp, Tc and Dol etc, were exhumed along the MMT. The Phl-Amp harzburgites are rich in LREE and LILE, such as Rb, K etc, and depletes Eu (Eu~* = 0.36 ～ 0.68) and HFSE, such as Nb, Ta, Zr, Hf, P, Ti etc. The trace element indicate that the Phl-Amp harzburgites have island arc signature. Their ~(87)Sr/~(86)Sr are varied from 0.708912 to 0.879839, ~(143)Nd/~(144)Nd from 0.511993 to 0.512164, ε Nd from- 9.2 to - 12.6. Rb/Sr isochrone age of the phlogolite amphibole harzburgite shows the metasomatism took place at 41Ma, and the Amp ~(40)Ar/~(39)Ar cooling age indcate the Phl-Amp harzburgite raising at 16Ma. There is an intense crust shortening resulted from the thrust faults and folds in the Cayu block which is shortened more 120km than that of the Lasha block in 35～90Ma. With the NE corner of the India plate squash into the Gangdese arc, the sinistral Pai shear fault and the dextral Aniqiao shear fault on the both sides of the Great bent of Yalun Zangbu river come into active in 21～26Ma. On the other hand, the right-lateral Gongrigabu strike-slip faults come into activity at the same period, a lower age bound for the Gongrigabu strike-slip fault is estimated to be 23～24Ma from zircon of ion-probe U/Pb thermochronology. The Gongrigabu strike-slip faults connect with the Lhari strike-slip fault in the northwestern direction and with the Saganing strike-slip at the southeastern direction. Another important structure in the EHS is the Gangdese detachment fault system (GDS) which occurs between the sedimental cover and the metamorphic basement. The lower age of the GDS is to be 16Ma from the preliminary 40Ar/39Ar thermochronology of white mica. The GDS is thought to be related to the reverse of the subducted Indian crust and the fast uplift of the EHS. Structural and thermochronology investigation of the EHS suggest that the eastern Tibet and the western Yunnan rotated clockwise around the EHS in the period of 35～60Ma. Later, the large-scale strike-slip faults (RRD, Gaoligong and Saganing fault) prolongate into the EHS, and connect with the Guyu fault and Gongrigabu fault, which suggest that the Indianchia block escape along these faults. Two kind of magmatic rocks in the EHS have been investigated, one is the mantle-derived amphibole gabbro, dioposide diorite and amphibole diorite, another is crust origin biotit-garnet adamellite, biotit-garnet granodiorite and garnet-amphibole-biotite granite. The amphibole gabbro dioposite diorite and amphibole diorite are rich in LREE, and LILE, such as Ba, Rb, Th, K, Sr etc, depleted in HFSE, such as Nb, Ta, Zr, Hf, Ti etc. The ratio of ~(87)Sr/~(86)Sr are from 0.7044 to 0.7048, ~(143)Nd/~(144)Nd are from 0.5126 to 0.5127. The age of the mantle origin magamatic rocks, which result from the partial melt of the raising and decompression anthenosphere, is 8Ma by ~(40)Ar/~(39)Ar dating of amphibole from the diorite. The later crust origin biotite-garnet adamellite, biotite-garnet granodiorite and garnet-amphibole-biotite granite are characterized by aboudance in LREE, and strong depletion of Eu. The ratios of ~(87)Sr-~(86)Sr are from 0.795035 to 0.812028, ~(143)Nd/~(144)Nd from 0.51187 to 0.511901. The ~(40)Ar/~(39)Ar plateau age of the amphibole from the garnet-amphibole-biotite granite is 17.5±0.3Ma, and the isochrone age is 16.8±0.6Ma. Their geochemical characteristics show that the crust-derived magmatic rocks formed from partial melting of the lower curst in the post-collisional environment. A group of high-pressure kaynite-garnet granulites and enclave of high-pressure garnet-clinopyroxene grnulites and calc-silicate grnulites are outcroped along the MMT. The peak metamorphic condition of the high-pressure granulites yields T=800～960 ℃, P=1.4～1.8Gpa, corresponding the condition of 60km depth. The retrograde assemblages of the high-pressure grnulites occur at the condition of T=772.3～803.3 ℃, P=0.63～0.64Gpa. The age of the peak metamorphic assemblages are 45 ～ 69Ma indicated by the zircon U/Pb ion-plobe thermochronology, and the retrograde assemblage ages are 13～26Ma by U/Pb, ~(40)Ar/~(39)Ar thermochronology. The ITD paths of the high-pressure granulites show that they were generated during the tectonic thickening and more rapid tectonic exhumation caused by the subducting of the Indian plate and subsequent break-off of the subducted slab. A great deal of apatite, zircon and sphene fission-track ages, isotopic thermochronology of the rocks in the EHS show that its rapid raising processes of the EHS can be divided into three main periods. There are 35～60Ma, 13～25Ma, 0～3Ma. 3Ma is a turn in the course of raising in the EHS which is characterized by abruptly acceleration of uplifting. The uplift ratios are lower than 1mm .a~(-1) before 3Ma, and higher than 1mm .a~(-1) with a maximum ratio of 30mm .a~(-1) since 3Ma. The bottom (knick point) of the partial anneal belt is 3.8km above sea level in the EHS, and correspond to age of 3Ma determined by fission-track age of apatite. The average uplift ratio is about 1.4 mm .a~(-1) below the knick point. The EHS has raised 4.3km from the surface of 2.36km above sea level since 3Ma estimated by the fossil partial anneal belt of the EHS. We propose a two-stage subduction model (B+A model) basing on Structural, thermochronological, magmatical, metamorphic and geophysical investigations of the EHS. The first stage is the subduction of the Indian continental margin following after the subduction of the Tethys Ocean crust and subsequent collision with the Gangdese arc, and the second stage is the Indian crust injecting into the lower crust and upper mantle of the Tibet plateau. Slab break-off seems to be occurred between these two stages.