Yonezawa Mai, Sakuda Shohei, Yoshimura Etsuro, Suzuki Michio
Department of Applied Biological Chemistry, Graduate School of Agricultural and Life Sciences, The University of Tokyo, 1-1-1 Yayoi, Bunkyo-ku, Tokyo 113-8657, Japan.
Department of Applied Biological Chemistry, Graduate School of Agricultural and Life Sciences, The University of Tokyo, 1-1-1 Yayoi, Bunkyo-ku, Tokyo 113-8657, Japan.
J Struct Biol. 2016 Nov;196(2):107-118. doi: 10.1016/j.jsb.2016.02.021. Epub 2016 Mar 3.
Molluscan shells, consisting of calcium carbonate, are typical examples of biominerals. The small amount of organic matrices containing chitin and proteins in molluscan shells regulates calcification to produce elaborate microstructures. The shells of gastropods have a spiral shape around a central axis. The shell thickness on the internal side of the spiral becomes thinner than that on the outer side of the spiral during the growth to expand the interior space. These observations suggest that a dissolution process works as a remodeling mechanism to change shell shape in molluscan shells. To reveal the dissolution mechanism involved in the remodeling of gastropod spiral shells, we focused on chitinases in the fresh water snail Lymnaea stagnalis. Chitinase activity was observed in the acetic acid-soluble fraction of the shell and in the buffer extract from the mantle. Allosamidin, a specific inhibitor of family 18 chitinases, inhibited the chitinase activity of both fractions completely. Homology cloning and transcriptome analyses of the mantle revealed five genes (chi-I, chi-II, chi-III, chi-IV, and chi-V) encoding family 18 chitinases. All chitinases were expressed in the mantle and in other tissues suggesting that chitinases in the mantle have multiple-functions. Treatment with commercially available chitinase obtained from Trichoderma viride altered the shell microstructure of L. stagnalis. Larvae of L. stagnalis cultured in allosamidin solution had a thinner organic layer on the shell surface. These results suggest that the chitinase activities in the shell and mantle are probably associated with the shell formation process.
由碳酸钙构成的软体动物贝壳是生物矿物的典型例子。软体动物贝壳中含有几丁质和蛋白质的少量有机基质调节钙化过程,以产生精细的微观结构。腹足纲动物的贝壳围绕中心轴呈螺旋状。在生长过程中,螺旋内侧的贝壳厚度比外侧变薄,以扩大内部空间。这些观察结果表明,溶解过程作为一种重塑机制,在软体动物贝壳中改变贝壳形状。为了揭示参与腹足纲螺旋贝壳重塑的溶解机制,我们聚焦于淡水螺椎实螺中的几丁质酶。在贝壳的醋酸可溶部分和外套膜的缓冲提取物中观察到了几丁质酶活性。18 家族几丁质酶的特异性抑制剂别洛沙米定完全抑制了这两个部分的几丁质酶活性。对外套膜的同源克隆和转录组分析揭示了五个编码 18 家族几丁质酶的基因(chi-I、chi-II、chi-III、chi-IV 和 chi-V)。所有几丁质酶都在外套膜和其他组织中表达,这表明外套膜中的几丁质酶具有多种功能。用从绿色木霉获得的市售几丁质酶处理改变了椎实螺的贝壳微观结构。在别洛沙米定溶液中培养的椎实螺幼虫在贝壳表面有一层较薄的有机层。这些结果表明,贝壳和外套膜中的几丁质酶活性可能与贝壳形成过程有关。