生物矿化
膜
文石
Crystal(编程语言)
图层(电子)
基质(化学分析)
矿化(土壤科学)
化学工程
淡水双壳类
晶体生长
壳体(结构)
生物
生物物理学
结晶学
材料科学
化学
方解石
纳米技术
复合材料
生物化学
生态学
双壳类
软体动物
古生物学
土壤水分
程序设计语言
工程类
计算机科学
摘要
Abstract The squeezing hypothesis and the organic frameworks preformation hypothesis propose two different mechanisms to explain the interaction between organic frameworks and crystals during biomineralization of the prismatic layer of the mollusk shell. In this study, we began to study H yriopsis cumingii shell formation and discover that this species seemed to follow the squeezing hypothesis. During the formation of the aragonite prismatic layer in the freshwater bivalve H . cumingii , we found that crystal growth was involved in controlling initiation of formation of the interprismatic organic membranes. First, newly formed crystals were embedded in the periostracum. Next, the interprismatic organic membranes of the prismatic layer were produced via squeezing between neighboring crystals. The organic matrix secreted by the mantle continuously self‐assembled into the interprismatic organic membranes as the crystals grew. In the mature stage, the interprismatic organic membranes were shaped by crystal growth. These findings provide evidence to support the squeezing hypothesis and add to the existing knowledge about interactions that occur at the organic–inorganic interfaces during mollusk shell biomineralization.
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