Abstract
The transition from invertebrate calcium carbonate-based calcite and aragonite exo- and endoskeletons to the calcium phosphate-based vertebrate backbones and jaws composed of microscopic hydroxyapatite crystals is one of the great revolutions in the evolution of terrestrial organisms. To identify potential factors that might have played a role in such a transition, three key domains of the vertebrate tooth enamel protein amelogenin were probed for calcium mineral/protein interactions and their ability to promote calcium phosphate and calcium carbonate crystal growth. Under calcium phosphate crystal growth conditions, only the carboxy-terminus augmented polyproline repeat peptide, but not the N-terminal peptide nor the polyproline repeat peptide alone, promoted the formation of thin and parallel crystallites resembling those of bone and initial enamel. In contrast, under calcium carbonate crystal growth conditions, all three amelogenin-derived polypeptides caused calcium carbonate to form fused crystalline conglomerates. When examined for long-term crystal growth, polyproline repeat peptides of increasing length promoted the growth of shorter calcium carbonate crystals with broader basis, contrary to the positive correlation between polyproline repeat element length and apatite mineralization published earlier. To determine whether the positive correlation between polyproline repeat element length and apatite crystal growth versus the inverse correlation between polyproline repeat length and calcium carbonate crystal growth were related to the binding affinity of the polyproline domain to either apatite or carbonate, a parallel series of calcium carbonate and calcium phosphate/apatite protein binding studies was conducted. These studies demonstrated a remarkable binding affinity between the augmented amelogenin polyproline repeat region and calcium phosphates, and almost no binding to calcium carbonates. In contrast, the amelogenin N-terminus bound to both carbonate and apatite, but preferentially to calcium carbonate. Together, these studies highlight the specific binding affinity of the augmented amelogenin polyproline repeat region to calcium phosphates versus calcium carbonate, and its unique role in the growth of thin apatite crystals as they occur in vertebrate biominerals. Our data suggest that the rise of apatite-based biominerals in vertebrates might have been facilitated by a rapid evolution of specialized polyproline repeat proteins flanked by a charged domain, resulting in apatite crystals with reduced width, increased length, and tailored biomechanical properties.
Highlights
Produced minerals are among the functionally most important and long-lasting components of living organisms: they provide strength and defense through the formation of endo– and exoskeletons and contribute the main structural components of the powerful dentate masticatory apparatus
The N-terminal amelogenin fragment N33 caused calcium carbonate crystals to arrange in ring-shaped assemblies of hexagonal crystals, while the PXX repeat region peptide and the Cterminus augmented PXX fragment resulted in fused CaCO3 crystal conglomerates (Figures 2A–C)
We have tested the effect of amelogenin and some of its domains on both calcium carbonate and calcium phosphate mineral growth and binding to determine whether the interaction of amelogenin fragments with calcium phosphates when compared to calcium carbonates provided any unique insights into the evolutionary benefits of protein mediated calcium phosphate growth for vertebrate skeletal tissue function
Summary
Produced minerals are among the functionally most important and long-lasting components of living organisms: they provide strength and defense through the formation of endo– and exoskeletons and contribute the main structural components of the powerful dentate masticatory apparatus. Biominerals are important for auditory perception (Tohno et al, 1997) and a sense of equilibrium (Pote and Ross, 1991). Pathological examples of biomineralization include calcified arteries, ectopic bone, and renal stones, to name just a few (Russell et al, 1986). Among the major mineral constituents of biominerals are carbonates, opal, ferric oxides, and magnetites, and phosphates (Lowenstam and Weiner, 1989). Biominerals are manufactured in many different fashions, through the help of organic matrix scaffolds or www.frontiersin.org. Protein scaffold-grown biominerals have emerged as some of the most prominent tissues in modern vertebrates, including bone, dentin, and enamel
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