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Organic constituents of the uterine fluid, the acellular milieu in which the eggshell is mineralized, were biochemically characterized at initial, mid and final stages of shell calcification in hens. The electrophoretic protein profiles changed at the different stages of shell mineralization. Two major bands (80-kDa and 43-kDa glycoproteins) with calcium affinity were specific to the initial stage. Four protein bands of 180, 150, 116 and 32 kDa, present at the phase of rapid shell formation, coprecipitated with calcium carbonate in vitro. At this stage were also present a calcium-binding glycoprotein of 36-kDa and a 20-kDa protein. Uterine fluid of the final stage was characterized by a darker intensity of the 66-kDa band, which showed calcium-binding ability and by the presence of three additional proteins (72, 13 and 6 kDa). At least seven bands of the uterine fluid showed similar migration patterns to those of eggshell extracts. Western blotting with ovocleidin and ovalbumin antisera demonstrated the presence of these matrix proteins in uterine fluid collected at initial and mid phase, respectively. Total uterine fluid collected at the end of calcification and dialyzed uterine fluid from the various stages delayed the rate of calcium precipitation in vitro. These observations demonstrate the presence of precursors of eggshell matrix in the uterine fluid and support the hypothesis of their involvement in the process of eggshell mineralization.
Gautron et al. (Wed,) studied this question.