厚壳贻贝一种新型贝壳胶原蛋白的重组表达与功能分析

贝壳是一种具有优异力学性能的生物硬组织,贝壳基质蛋白质对贝壳的形成具有重要意义。厚壳贻贝(Mytilus coruscus)贝壳中发现一种类似胶原蛋白质的新型贝壳基质蛋白质,命名为collagen-like protein 2（CLP-2）。然而,该蛋白质的结构与功能以及对贝壳形成的影响机制尚不清楚。为此,本研究对CLP 2开展了序列分析;进一步采取密码子优化结合原核重组表达策略,开展了CLP-2的重组表达;在此基础上分析了重组CLP-2对酸钙结晶的诱导、结晶速率抑制以及碳酸钙结合能力。对CLP-2的序列分析结果表明,该蛋白质序列中含有信号肽及两个Von Willebrand factor A（VWA）结构域。CLP-2在数据库中尚无高同源性蛋白质存在,表明这是一种较为新颖的贝壳基质蛋白。所获得的重组CLP-2对碳酸钙体外结晶表现出明显的诱导作用,扫描电镜以及傅里叶红外光谱结果表明,重组CLP-2可诱导碳酸钙晶体的形貌由立方体形转化为球形,并在高浓度下进一步转化为哑铃形;同时,重组CLP-2可促使碳酸钙晶体的晶型由方解石型向文石型转化;重组CLP-2在体外具有碳酸钙晶体结合作用;此外,重组CLP-2能显著抑制碳酸钙晶体的结晶速度（P<0.01）,并具有浓度依赖性。上述结果表明,厚壳贻贝贝壳CLP-2蛋白质在贝壳,特别是文石型肌棱柱层的生物矿化过程中具有重要作用。上述研究为深入了解贻贝贝壳的形成机制,以及胶原类蛋白质对生物矿化过程的影响奠定了基础。     

翡翠贻贝外套膜转录组及贝壳珍珠质层和肌棱柱层蛋白质组分析

贝类贝壳在生物材料学及仿生学研究中占据着重要地位。贝壳基质蛋白质是贝壳中的主要有机质成分,对贝壳的形成以及贝壳的力学性能至关重要。翡翠贻贝(Perna viridis)贝壳主要由肌棱柱层和珍珠质层两种微观结构组成,其结构层次较简单,是研究贝壳基质蛋白质及其与贝壳形成关系的极好材料。为深入研究翡翠贻贝贝壳基质蛋白质的分子组成以及分布特点,首先采用扫描电子显微镜,观察翡翠贻贝贝壳内表面珍珠质层和肌棱柱层的微观结构;采用刮取法获得贝壳内表面珍珠质层和肌棱柱层的粉末;对不同层次的贝壳粉末,利用酸溶法去除碳酸钙成分,所获得的有机质组分通过离心将其分为酸可溶性组分和酸不溶性组分。采用Illumina深度测序技术对翡翠贻贝外套膜组织进行大规模测序和序列组装,在此基础上,采用LC-MS/MS质谱技术结合外套膜转录组数据库搜索,对翡翠贻贝肌棱柱层和珍珠质层贝壳基质蛋白质开展组学分析。扫描电镜观察结果表明,翡翠贻贝贝壳有两种不同形貌结构的层次,其中珍珠质层为片状堆叠结构,而肌棱柱层为柱状结构。翡翠贻贝外套膜转录组测序共计获得 69 859 条Unigene。蛋白质组学鉴定结果表明,翡翠贻贝贝壳中总计鉴定到蛋白质54种,其中38种为肌棱柱层所特有蛋白质,3种珍珠质层特有蛋白质,另有13种在珍珠质层和肌棱柱层均被鉴定到。肌棱柱层特有蛋白质的分子多样性明显强于珍珠质层。上述研究为进一步探讨贝壳不同微观层次的形成机制,以及贝壳基质蛋白质对贝壳不同结构层次的调控作用机制奠定了基础。     

不溶性基质中天冬氨酸丰富的蛋白在珊瑚的钙质骨片形成中的重要作用

一般认为, 酸性蛋白在控制矿物的形成和发展中发挥重要作用。因此, 在不溶性有机基质中鉴定酸性蛋白对于理解珊瑚中个体蛋白的功能是非常重要的一步。在短指多型软珊瑚(Sinularia polydactyla)的可溶性和不溶性基质层中分析蛋白组分表明, 在不溶性基质和可溶性基质层中天冬氨酸的含量分别是61%和29%。利用体外分析法发现, 基质蛋白诱导碳酸钙形成非晶态析出相先于其形成钙质的结晶态。利用X-射线衍射来鉴定骨片上结晶态的碳酸钙, 结果表明钙质的多晶态呈现强反射。傅利叶变换红外光谱分析表明珊瑚基质中富含天冬氨酸的蛋白和多醣的结构。在不溶性基质组分中用钙离子结合分析显示一个分子量为109 kD的蛋白质可以与形成骨片的钙离子结合, 这一过程对骨片形成非常重要。在对生物钙化过程中起重要作用的碳酸酐酶的分析中显示了此酶的新颖的活性。以上结果显示珊瑚中不溶性基质内的富含天冬氨酸的蛋白在生物矿化调控过程中起重要作用。     

离子液体1-丁基-3-甲基咪唑氯代盐对溶菌酶结晶的影响

以亲水性离子液体1-丁基-3-甲基咪唑氯盐(BmimCl)为添加剂,研究离子液体对溶菌酶结晶的影响.分别考察了离子液体对溶菌酶晶体数量与尺寸、晶体形貌及蛋白质纯度的影响,并探讨了离子液体对结晶过程影响的作用机制.离子液体通过增大溶菌酶的溶解度和其自身低蒸气压两种途径,降低了溶菌酶在结晶过程中的过饱和度,更有利于晶体的成核和生长,得到更好的结果.如避免多晶态现象的发生,增大晶体的尺寸,降低溶菌酶样品纯度的要求.X-射线衍射分析表明,离子液体未改变晶体的晶型结构,但可提高晶体的衍射分辨率.     

离子液体1-丁基-3-甲基咪唑氯盐对溶菌酶结晶的影响

以亲水性离子液体1-丁基-3-甲基咪唑氯盐(BmimCl)为添加剂,研究离子液体对溶菌酶结晶的影响.分别考察了离子液体对溶菌酶晶体数量与尺寸、晶体形貌及蛋白质纯度的影响,并探讨了离子液体对结晶过程影响的作用机制.离子液体通过增大溶菌酶的溶解度和其自身低蒸气压两种途径,降低了溶菌酶在结晶过程中的过饱和度,更有利于晶体的成核和生长,得到更好的结果.如避免多晶态现象的发生,增大晶体的尺寸,降低溶菌酶样品纯度的要求.X-射线衍射分析表明,离子液体未改变晶体的晶型结构,但可提高晶体的衍射分辨率.     

不同培养条件对胶质芽孢杆菌诱导碳酸钙晶体形成的影响

【目的】研究不同培养条件对胶质芽孢杆菌(Bacillus mucilaginosus)菌体形态、数量和分泌的碳酸酐酶(CA酶)活性的影响,以及不同方式培养的菌体与碳酸钙晶体的生长及其形貌、数量之间的联系。【方法】分别采用无氮和有氮培养基培养胶质芽孢杆菌,进行菌体形态、数量及CA酶活性的比较,收集不同培养方式的菌体加入碳酸钙结晶体系中以研究细菌与碳酸钙晶体形成的联系。【结果】在无氮培养条件下,胶质芽孢杆菌数量少、荚膜肥厚,细菌培养液CA酶活力较低;有氮培养条件下,菌体数量多、荚膜单薄,细菌培养液CA酶活力较高。在碳酸钙结晶体系中加入无氮培养的菌体,生成的碳酸钙晶体表面光滑,体积较大但数量较小,加入有氮条件下培养的菌体形成的碳酸钙晶体表面粗糙,数量大但体积较小。【结论】不同培养条件能够引起胶质芽孢杆菌菌体数量、荚膜多糖及CA酶活的明显差异,进而对碳酸钙晶体的生成和形貌产生影响。     

锌指蛋白的设计及其应用

人工设计的锌指蛋白一般包括两个结构域：DNA结合结构域和效应结构域。DNA结合结构域主要采用对DNA序列特异性识别结合的C2H2型锌指结构域,而功能结构域常常采用某些转录激活结构域、转录抑制结构域或某些酶的活性结构域。这样进行设计的锌指蛋白就可以在特定的核酸序列上行使相应的功能,这对于目的基因的表达调控及蛋白质与核酸的相互作用研究提供了新的思路。     

Oct-4/Sox-2 协同调控下游基因表达的分子机制

Oct-4属POU家族蛋白,是一类在动物早期胚胎发育过程中起重要作用的转录因子,参与维持细胞的全能性及未分化状态。Oct-4蛋白的主要结构特征为具有POU家族特有的保守结构域（POUS）和POU同源异型结构域（POUHD）,这两个结构域可与DNA上特定区域形成双向结合,进而对基因转录进行调控。Sox-2是另一种转录因子,其HMG结构域可结合在DNA的特定序列上,并可通过与Oct-4的POUs结构域之间的蛋白质．蛋白质相互作用形成POU／HMG／DNA三元复合体以调控下游靶基因的表达。文章就POU家族成员Oct-4和HMG-box家族成员Sox-2在动物早期胚胎发育中调控部分下游基因表达的分子机制进行了概述。     

BAR结构域蛋白质的功能

近期对果蝇双载蛋白(amphiphysin)BAR结构域晶体结构的报道,使得BAR结构域研究成为热点。虽然在序列水平上保守性较低,但双载蛋白的BAR结构域与Arfaptin 2的GTP酶结合结构域在结构上极为相似。通过对两种蛋白质的BAR结构域同源序列进行检索分析,发现了大量含BAR结构域相关蛋白质。研究发现,BAR结构域蛋白质多数都参与细胞内物质转运及胞吞作用;BAR结构域不仅可以通过其二聚化基元感知和诱导膜的弯曲,而且某些蛋白质的BAR结构域还具有与小GTP酶结合的功能。     

杂质对蛋白质晶体影响研究进展

综述了杂质对蛋白质晶体生长影响研究领域的进展情况. 对可能的杂质来源以及杂质对结晶过程的影响进行了介绍.重点介绍了和结晶蛋白质分子结构相似的杂质分子的影响, 包括晶体成核、生长形态、表面形貌、生长动力学、质量等,以及杂质在晶体中的重新分配.     

Characterization of a novel shell matrix protein with vWA domain from Mytilus coruscus

ABSTRACT

Mollusk shell is a product of biomineralization with excellent mechanical properties, and the shell matrix proteins (SMPs) have important functions in shell formation. A vWA domain-containing protein (VDCP) was identified from the shell of Mytilus coruscus as a novel shell matrix protein. The VDCP gene is expressed at a high level in specific locations in the mantle and adductor muscle. Recombinant VDCP (rVDCP) showed abilities to alter the morphology of both calcite and aragonite, induce the polymorph change of calcite, bind calcite, and decrease the crystallization rate of calcite. In addition, immunohistochemistry analyses revealed the specific location of VDCP in the mantle, the adductor muscle, and the myostracum layer of the shell. Furthermore, a pull-down analysis revealed eight protein interaction partners of VDCP in shell matrices and provided a possible protein–protein interaction network of VDCP in the shell.     

Ubiquitylation functions in the calcium carbonate biomineralization in the extracellular matrix

Mollusks shell formation is mediated by matrix proteins and many of these proteins have been identified and characterized. However, the mechanisms of protein control remain unknown. Here, we report the ubiquitylation of matrix proteins in the prismatic layer of the pearl oyster, Pinctada fucata. The presence of ubiquitylated proteins in the prismatic layer of the shell was detected with a combination of western blot and immunogold assays. The coupled ubiquitins were separated and identified by Edman degradation and liquid chromatography/mass spectrometry (LC/MS). Antibody injection in vivo resulted in large amounts of calcium carbonate randomly accumulating on the surface of the nacreous layer. These ubiquitylated proteins could bind to specific faces of calcite and aragonite, which are the two main mineral components of the shell. In the in vitro calcium carbonate crystallization assay, they could reduce the rate of calcium carbonate precipitation and induce the calcite formation. Furthermore, when the attached ubiquitins were removed, the functions of the EDTA-soluble matrix of the prismatic layer were changed. Their potency to inhibit precipitation of calcium carbonate was decreased and their influence on the morphology of calcium carbonate crystals was changed. Taken together, ubiquitylation is involved in shell formation. Although the ubiquitylation is supposed to be involved in every aspect of biophysical processes, our work connected the biomineralization-related proteins and the ubiquitylation mechanism in the extracellular matrix for the first time. This would promote our understanding of the shell biomineralization and the ubiquitylation processes.     

The interstitial crystal-nucleating sheet in molluscan Haliotis rufescens shell: A bio-polymeric composite

The interstitial green sheets in abalone shell nacre are shown to be bifacially differentiated trilaminate polymeric complexes, with glycoprotein layers sandwiching a central core containing chitin. They share some common feature with the organic matrix layers between the aragonite tablets in the nacre and the periostracum, and show similarities to the myostracum. Thus, although the green sheet is reported to be unique to the abalone shell, it represents an interesting model for the study of molluscan shell biomineralization processes. Indeed, during shell formation, prismatic and spherulitic aragonite precedes and follows the deposition of the interstitial green polymeric composite sheets, and there is evidence to suggest that these sheets demark the interruption of nacre synthesis and serve to nucleate the resumption of calcium carbonate crystal growth. The green polymeric interstitial sheet purified from the abalone shell was investigated by spectroscopic and imaging techniques: FTIR, confocal microscopy, scanning and transmission electron microscopy, and by pyrolysis combined with GC–MS. Structural and compositional differences are observed between the surfaces of the two sides of the interstitial polymeric composite sheets. Moreover, comparative crystallization experiments on the green sheet sides also reveal asymmetry with respect to the nucleation of calcium carbonate. These findings suggest that these bifacially differentiated interstitial composites may play an active role in the mineral assembly processes, with one of the surfaces acting as a crystal nucleator.     

A novel extrapallial fluid protein controls the morphology of nacre lamellae in the pearl oyster, Pinctada fucata

Mollusk shell nacre is known for its superior mechanical properties and precisely controlled biomineralization process. However, the question of how mollusks control the morphology of nacre lamellae remains unresolved. Here, a novel 38-kDa extrapallial fluid (EPF) protein, named amorphous calcium carbonate-binding protein (ACCBP), may partially answer this question. Although sequence analysis indicated ACCBP is a member of the acetylcholine-binding protein family, it is actively involved in the shell mineralization process. In vitro, ACCBP can inhibit the growth of calcite and induce the formation of amorphous calcium carbonate. When ACCBP functions were restrained in vivo, the nacre lamellae grew in a screw-dislocation pattern, and low crystallinity CaCO(3) precipitated from the EPF. Crystal binding experiments further revealed that ACCBP could recognize different CaCO(3) crystal phases and crystal faces. With this capacity, ACCBP could modify the morphology of nacre lamellae by inhibiting the growth of undesired aragonite crystal faces and meanwhile maintain the stability of CaCO(3)-supersaturated body fluid by ceasing the nucleation and growth of calcite. Furthermore, the crystal growth inhibition capacity of ACCBP was proved to be directly related to its acetylcholine-binding site. Our results suggest that a "safeguard mechanism" of undesired crystal growth is necessary for shell microstructure formation.     

A Bivalve Biomineralization Toolbox

Mollusc shells are a result of the deposition of crystalline and amorphous calcite catalyzed by enzymes and shell matrix proteins (SMP). Developing a detailed understanding of bivalve mollusc biomineralization pathways is complicated not only by the multiplicity of shell forms and microstructures in this class, but also by the evolution of associated proteins by domain co-option and domain shuffling. In spite of this, a minimal biomineralization toolbox comprising proteins and protein domains critical for shell production across species has been identified. Using a matched pair design to reduce experimental noise from inter-individual variation, combined with damage-repair experiments and a database of biomineralization SMPs derived from published works, proteins were identified that are likely to be involved in shell calcification. Eighteen new, shared proteins likely to be involved in the processes related to the calcification of shells were identified by the analysis of genes expressed during repair in Crassostrea gigas, Mytilus edulis, and Pecten maximus. Genes involved in ion transport were also identified as potentially involved in calcification either via the maintenance of cell acid–base balance or transport of critical ions to the extrapallial space, the site of shell assembly. These data expand the number of candidate biomineralization proteins in bivalve molluscs for future functional studies and define a minimal functional protein domain set required to produce solid microstructures from soluble calcium carbonate. This is important for understanding molluscan shell evolution, the likely impacts of environmental change on biomineralization processes, materials science, and biomimicry research.