Abstract

Environment parameters, diet and genetic factors interact to shape tooth morphostructure. In the human lineage, archaic and modern hominins show differences in dental traits, including enamel thickness, but variability also exists among living populations. Several polymorphisms, in particular in the non-collagenous extracellular matrix proteins of the tooth hard tissues, like enamelin, are involved in dental structure variation and defects and may be associated with dental disorders or susceptibility to caries. To gain insights into the relationships between tooth protein polymorphisms and dental structural morphology and defects, we searched for non-synonymous polymorphisms in tooth proteins from Neanderthal and Denisova hominins. The objective was to identify archaic-specific missense variants that may explain the dental morphostructural variability between extinct and modern humans, and to explore their putative impact on present-day dental phenotypes. Thirteen non-collagenous extracellular matrix proteins specific to hard dental tissues have been selected, searched in the publicly available sequence databases of Neanderthal and Denisova individuals and compared with modern human genome data. A total of 16 non-synonymous polymorphisms were identified in 6 proteins (ameloblastin, amelotin, cementum protein 1, dentin matrix acidic phosphoprotein 1, enamelin and matrix Gla protein). Most of them are encoded by dentin and enamel genes located on chromosome 4, previously reported to show signs of archaic introgression within Africa. Among the variants shared with modern humans, two are ancestral (common with apes) and one is the derived enamelin major variant, T648I (rs7671281), associated with a thinner enamel and specific to the Homo lineage. All the others are specific to Neanderthals and Denisova, and are found at a very low frequency in modern Africans or East and South Asians, suggesting that they may be related to particular dental traits or disease susceptibility in these populations. This modern regional distribution of archaic dental polymorphisms may reflect persistence of archaic variants in some populations and may contribute in part to the geographic dental variations described in modern humans.

Highlights

  • Dental morphology shows variability between extant and extinct human groups, and among modern humans according to a regional distribution [1,2,3]

  • This is the case of the Asian-specific non-synonymous polymorphism (V370A, rs3827760) in the ectodysplasin A receptor gene (EDAR) which is associated with the expression of shoveling and double-shoveling in upper first incisors, a particular trait of extant Asian populations [43]. This variant, in addition to T648I in the enamelin protein, emphasizes the role a single amino acid change may play in tooth morphostructure. In light of these data, the present study aimed to investigate whether tooth protein variants in archaic hominins could provide valuable molecular information to help understand past and present human dental morphostructural variability

  • The alignment with the sequences of chimpanzee and gorilla indicates that only two amino acid changes, K55E in Cementum protein 1 (CEMP1) and T127A in Matrix Gla protein (MGP) are common with apes (Table 2)

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Summary

Introduction

Dental morphology shows variability between extant and extinct human groups, and among modern humans according to a regional distribution [1,2,3]. Teeth are composed of three hard tissues (enamel, dentine and cementum) surrounding the pulp and expressing specific non-collagenous proteins including extracellular matrix proteins and proteases involved in the control of mineralization process and crystal deposition during tooth development [11, 12]. The composition of the cementum organic extracellular matrix shows similarities with that of the alveolar bone. It is rich in growth factors and glycoproteins that participate in periodontal tissue repair and regeneration after damage. The bone matrix Gla protein is not specific to cementum but is expressed in the cementum mineralization front where it exerts an inhibitory control on calcification essential for proper mineralization

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