方解石
球霰石
球粒岩
赫氏颗石藻
生物矿化
碳酸钙
文石
颗石藻
成核
材料科学
碳酸盐
化学工程
矿物学
生物
生物物理学
地质学
化学
天体生物学
有机化学
生态学
冶金
复合材料
营养物
工程类
浮游植物
作者
Jessica M. Walker,Bartosz Marzec,Renee B. Y. Lee,Kristyna Vodrazkova,Sarah J. Day,Chiu C. Tang,Rosalind E. M. Rickaby,Fabio Nudelman
标识
DOI:10.1002/adfm.201807168
摘要
Abstract Coccolith‐associated polysaccharides (CAPs) are thought to be a key part of the biomineralization process in coccolithophores; however, their role is not fully understood. Two different systems that promote different polymorphs of calcium carbonate are used to show the effect of CAPs on nucleation and polymorph selection in vitro. Using a combination of time‐resolved cryo‐transmission electron microscopy and scanning electron microscopy, the mechanisms of calcite nucleation and growth in the presence of the intracrystalline fraction are examined containing CAPs extracted from coccoliths from Gephyrocapsa oceanica and Emiliania huxleyi , two closely related coccolithophore species. The CAPs extracted from G. oceanica are shown to promote calcite nucleation in vitro, even under conditions favoring the kinetic products of calcium carbonate, vaterite, and aragonite. This is not the case with CAPs extracted from E. huxleyi , suggesting that the functional role of CAPs in vivo may be different between the two species. Additionally, high‐resolution synchrotron powder X‐ray diffraction has revealed that the polysaccharide is located between grain boundaries of both calcite produced in the presence of the CAPs in vitro and biogenic calcite, rather than within the crystal lattice.
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