TY - JOUR
T1 - Influence of ovalbumin on CaCO3 precipitation during in vitro biomineralization
AU - Wang, Xiaoqiang
AU - Wu, Congmeng
AU - Tao, Kai
AU - Zhao, Kang
AU - Wang, Jiqian
AU - Xu, Hai
AU - Xia, Daohong
AU - Shan, Honghong
AU - Lu, Jian R.
PY - 2010/4/29
Y1 - 2010/4/29
N2 - As a major constituent of egg white matrix, ovalbumin has long been perceived to be implicated in the formation of avian eggshells, in particular, the mammillary layer. However, very little is known about the detailed mechanism by which this protein mediates shell calcification. By the combined studies of AFM, SEM, and TEM, we have investigated the influence of ovalbumin on CaCO 3 precipitation under in vitro mineralization conditions. We observed that the influence was multifold. This protein modified the morphology of calcite crystals through a distinct anisotropic process with respect to the four crystal step edges. AFM characterization revealed that the modification was initiated at the obtuse-obtuse step corner and propagated predominantly along the obtuse steps. Furthermore, the protein favored the existence of unstable phases such as amorphous calcium carbonate and crystalline vaterite. In contrast, lysozyme, another protein also present in the system, played a very different role in modifying calcite morphology. The mechanistic understanding gained from this study is clearly also of practical significance in developing advanced inorganic CaCO3 materials with the aid of morphological manipulation of crystalline structures via different protein mediation.
AB - As a major constituent of egg white matrix, ovalbumin has long been perceived to be implicated in the formation of avian eggshells, in particular, the mammillary layer. However, very little is known about the detailed mechanism by which this protein mediates shell calcification. By the combined studies of AFM, SEM, and TEM, we have investigated the influence of ovalbumin on CaCO 3 precipitation under in vitro mineralization conditions. We observed that the influence was multifold. This protein modified the morphology of calcite crystals through a distinct anisotropic process with respect to the four crystal step edges. AFM characterization revealed that the modification was initiated at the obtuse-obtuse step corner and propagated predominantly along the obtuse steps. Furthermore, the protein favored the existence of unstable phases such as amorphous calcium carbonate and crystalline vaterite. In contrast, lysozyme, another protein also present in the system, played a very different role in modifying calcite morphology. The mechanistic understanding gained from this study is clearly also of practical significance in developing advanced inorganic CaCO3 materials with the aid of morphological manipulation of crystalline structures via different protein mediation.
UR - http://www.scopus.com/inward/record.url?scp=77951578061&partnerID=8YFLogxK
U2 - 10.1021/jp1008237
DO - 10.1021/jp1008237
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C2 - 20369864
AN - SCOPUS:77951578061
SN - 1520-6106
VL - 114
SP - 5301
EP - 5308
JO - Journal of Physical Chemistry B
JF - Journal of Physical Chemistry B
IS - 16
ER -