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PU14,一种新型基质蛋白,参与珍珠贝,珠母贝,贝壳形成。

PU14, a Novel Matrix Protein, Participates in Pearl Oyster, Pinctada Fucata, Shell Formation.

机构信息

Ministry of Education Key Laboratory of Protein Sciences, School of Life Sciences, Tsinghua University, Beijing, 100084, China.

Zhe Jiang Provincial Key Laboratory of Applied Enzymology, Yangtze Delta Region Institute of Tsinghua University, 705 Yatai Road, Jiaxing, 314006, China.

出版信息

Mar Biotechnol (NY). 2021 Apr;23(2):189-200. doi: 10.1007/s10126-020-10014-3. Epub 2021 Mar 10.

Abstract

Biomineralization is a widespread biological process, involved in the formation of shells, teeth, and bones. Shell matrix proteins have been widely studied for their importance during shell formation. In 2015, our group identified 72 unique shell matrix proteins in Pinctada fucata, among which PU14 is a matrix protein detected in the soluble fraction that solely exists in the prismatic layer. However, the function of PU14 is still unclear. In this study, the full-length cDNA sequence of PU14 was obtained and functional analyses of PU14 protein during shell formation were performed. The deduced protein has a molecular mass of 77.8 kDa and an isoelectric point of 11.34. The primary protein structure contains Gln-rich and random repeat units, which are typical characteristics of matrix protein and indicate its potential function during shell formation. In vivo and in vitro experiments indicated PU14 has prismatic layer functions during shell formation. The tissue expression patterns showed that PU14 was mainly expressed in the mantle tissue, which is consistent with prismatic layer formation. Notching experiments suggested that PU14 responded to repair and regenerate the injured shell. After inhibiting gene expression by injecting PU14-specific double-stranded RNA, the inner surface of the prismatic layer changed significantly and became rougher. Further, in vitro experiments showed that recombinant protein rPU14 impacted calcite crystal morphology. Taken together, characterization and functional analyses of a novel matrix protein, PU14, provide new insights about basic matrix proteins and their functions during shell formation.

摘要

生物矿化是一种广泛存在的生物过程,参与了壳、牙和骨的形成。壳基质蛋白因其在壳形成过程中的重要性而被广泛研究。2015 年,我们的研究小组在菲律宾蛤仔(Pinctada fucata)中鉴定出 72 种独特的壳基质蛋白,其中 PU14 是一种仅存在于棱柱层的可溶部分的基质蛋白。然而,PU14 的功能仍不清楚。本研究获得了 PU14 的全长 cDNA 序列,并对其在壳形成过程中的功能进行了分析。推导的蛋白质分子量为 77.8 kDa,等电点为 11.34。主要蛋白质结构含有富含谷氨酰胺和随机重复单元,这是基质蛋白的典型特征,表明其在壳形成过程中的潜在功能。体内和体外实验表明,PU14 在壳形成过程中具有棱柱层功能。组织表达模式表明,PU14 主要在套膜组织中表达,这与棱柱层的形成一致。缺口实验表明,PU14 对修复和再生受损的壳有响应。通过注射 PU14 特异性双链 RNA 抑制基因表达后,棱柱层的内表面发生明显变化,变得更加粗糙。此外,体外实验表明重组蛋白 rPU14 影响方解石晶体形态。综上所述,新型基质蛋白 PU14 的特征和功能分析为基本基质蛋白及其在壳形成过程中的功能提供了新的见解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7aeb/8032588/7f486b2007b9/10126_2020_10014_Fig1_HTML.jpg

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