Habraken Wouter J E M, Masic Admir, Bertinetti Luca, Al-Sawalmih Ali, Glazer Lilah, Bentov Shmuel, Fratzl Peter, Sagi Amir, Aichmayer Barbara, Berman Amir
Max Planck Institute of Colloids and Interfaces, Department of Biomaterials, 14424 Potsdam, Germany.
Max Planck Institute of Colloids and Interfaces, Department of Biomaterials, 14424 Potsdam, Germany.
J Struct Biol. 2015 Jan;189(1):28-36. doi: 10.1016/j.jsb.2014.11.003. Epub 2014 Nov 26.
Previous studies on pre-molt gastroliths have shown a typical onion-like morphology of layers of amorphous mineral (mostly calcium carbonate) and chitin, resulting from the continuous deposition and densification of amorphous mineral spheres on a chitin-matrix during time. To investigate the consequences of this layered growth on the local structure and composition of the gastrolith, we performed spatially-resolved Raman, X-ray and SEM-EDS analysis on complete pre-molt gastrolith cross-sections. Results show that especially the abundance of inorganic phosphate, phosphoenolpyruvate (PEP)/citrate and proteins is not uniform throughout the organ but changes from layer to layer. Based on these results we can conclude that ACC stabilization in the gastrolith takes place by more than one compound and not by only one of these additives.
先前对蜕皮前胃石的研究表明,无定形矿物(主要是碳酸钙)和几丁质层呈现出典型的洋葱状形态,这是由于无定形矿物球在几丁质基质上随时间不断沉积和致密化所致。为了研究这种分层生长对胃石局部结构和成分的影响,我们对完整的蜕皮前胃石横截面进行了空间分辨拉曼光谱、X射线和扫描电子显微镜-能谱分析。结果表明,特别是无机磷酸盐、磷酸烯醇丙酮酸(PEP)/柠檬酸盐和蛋白质的含量在整个器官中并不均匀,而是随层变化。基于这些结果,我们可以得出结论,胃石中无定形碳酸钙(ACC)的稳定是由多种化合物而非仅一种添加剂实现的。