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幼虫海胆骨针 SM50 结构域在有机基质自组装和碳酸钙矿化中的作用。

Roles of larval sea urchin spicule SM50 domains in organic matrix self-assembly and calcium carbonate mineralization.

机构信息

Physical Chemistry, Department of Chemistry, University of Konstanz, Universitätsstraße 10, PO Box 714, D-78457 Konstanz, Germany.

出版信息

J Struct Biol. 2013 Aug;183(2):205-15. doi: 10.1016/j.jsb.2013.06.004. Epub 2013 Jun 21.

Abstract

The larval spicule matrix protein SM50 is the most abundant occluded matrix protein present in the mineralized larval sea urchin spicule. Recent evidence implicates SM50 in the stabilization of amorphous calcium carbonate (ACC). Here, we investigate the molecular interactions of SM50 and CaCO3 by investigating the function of three major domains of SM50 as small ubiquitin-like modifier (SUMO) fusion proteins - a C-type lectin domain (CTL), a glycine rich region (GRR) and a proline rich region (PRR). Under various mineralization conditions, we find that SUMO-CTL is monomeric and influences CaCO3 mineralization, SUMO-GRR aggregates into large protein superstructures and SUMO-PRR modifies the early CaCO3 mineralization stages as well as growth. The combination of these mineralization and self-assembly properties of the major domains synergistically enable the full-length SM50 to fulfill functions of constructing the organic spicule matrix as well as performing necessary mineralization activities such as Ca(2+) ion recruitment and organization to allow for proper growth and development of the mineralized larval sea urchin spicule.

摘要

幼虫刺针基质蛋白 SM50 是矿化幼虫海胆刺针中含量最丰富的封闭基质蛋白。最近的证据表明 SM50 参与了无定形碳酸钙 (ACC) 的稳定。在这里,我们通过研究 SM50 的三个主要结构域作为小泛素样修饰物 (SUMO) 融合蛋白的功能来研究 SM50 和 CaCO3 的分子相互作用 - C 型凝集素结构域 (CTL)、富含甘氨酸的区域 (GRR) 和富含脯氨酸的区域 (PRR)。在各种矿化条件下,我们发现 SUMO-CTL 是单体的,并影响 CaCO3 的矿化,SUMO-GRR 聚集成大的蛋白质超结构,而 SUMO-PRR 则修饰早期 CaCO3 的矿化阶段以及生长。这些矿化和主要结构域的自组装特性的结合使全长 SM50 能够发挥构建有机刺针基质的功能,并进行必要的矿化活动,如 Ca(2+)离子的募集和组织,以允许矿化幼虫海胆刺针的适当生长和发育。

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