Jolly Cécile, Berland Sophie, Milet Christian, Borzeix Sandrine, Lopez Evelyne, Doumenc Dominique
Département Milieux et Peuplements Aquatiques, Unité associée au CNRS, Muséum National d'Histoire Naturelle, Biologie des Organismes Marins et Ecosystémes, 55 rue Buffon, Paris Cedex 05, 75231, France.
Mar Biotechnol (NY). 2004 Nov-Dec;6(6):541-51. doi: 10.1007/s10126-004-3129-7.
Organic matrix from molluscan shells has the potential to regulate calcium carbonate deposition and crystallization. Control of crystal growth thus seems to depend on control of matrix protein secretion or activation processes in the mantle cells, about which little is known. Biomineralization is a highly orchestrated biological process. The aim of this work was to provide information about the source of shell matrix macromolecule production, within the external epithelium of the mantle. An in vivo approach was chosen to describe the histologic changes in the outer epithelium and in blood sinus distribution, associated with mantle cells implicated in shell matrix production. Our results characterized a topographic and time-dependent zonation of matrix proteins involved in shell biomineralization in the mantle of Haliotis.
软体动物贝壳的有机基质具有调节碳酸钙沉积和结晶的潜力。因此,晶体生长的控制似乎取决于外套膜细胞中基质蛋白分泌或激活过程的控制,而对此我们知之甚少。生物矿化是一个高度协调的生物过程。这项工作的目的是提供有关外套膜外部上皮内贝壳基质大分子产生来源的信息。我们选择了一种体内方法来描述与参与贝壳基质产生的外套膜细胞相关的外部上皮和血窦分布的组织学变化。我们的结果表征了参与皱纹盘鲍外套膜贝壳生物矿化的基质蛋白的地形和时间依赖性分区。