A new mineralized tissue in the early vertebrate Astraspis

Lungfish-like antero-labial tooth addition and amphibian-like enameloid-enamel transition in the coronoid of a Devonian stem actinopterygian

New teeth are predominantly initiated lingually or postero-lingually to the old teeth in vertebrates. Osteichthyan dentitions typically consist of linear rows of shedding teeth, but internal to the marginal jawbones osteichthyans primitively have an extra dental arcade, in which teeth are sometimes spread out into a field and not organized in rows. The tooth plates of lungfish are specialized from the jawbones of the inner dental arcade, but the teeth are arranged in radial tooth rows with new teeth added at the anterior and labial end of the rows and without shedding the old teeth, distinct from other osteichthyan dentitions. Actinopterygian teeth can be recognized by a cap of enameloid, while sarcopterygian teeth are only coated by enamel. An enameloid cap is also borne by the unicuspid larval teeth in some amphibians, but it is covered by enamel and eventually disappears in the bicuspid adult teeth. In early osteichthyans, old teeth are often not completely resorbed and shed, and the overlapping relationship of their remnants buried in the bone records the sequence of developmental events. Using synchrotron microtomography, this ontogenetic record of a coronoid tooth field of a Devonian stem actinopterygian is visualized in 3D. As a component of the inner dental arcade, the coronoid displays initial radial non-shedding tooth rows followed by radial shedding tooth rows that are later transformed into linear shedding tooth rows. The teeth are always added antero-labially and replaced labially to keep pace with the labial bone apposition and lingual bone remodeling, which causes the shift of the tooth competent zone. These provide a clue to the evolution of the radial non-shedding dentition with antero-labial tooth addition in lungfish. The tooth patterning process suggests that the superficial disorder of the tooth field is an epiphenomenon of the ever-changing local developing environment of each tooth bud: due to the retention of old tooth bases, a tooth position that has been replaced in place can at some point drift to a site between the adjacent tooth positions, splitting or merging, and then continue being replaced in situ. Primary teeth are capped by enameloid, but replacement teeth bear enamel crests without an enameloid cap. This demonstrates that the transition from enameloid capping to enamel coating through tooth replacement can happen in actinopterygians too, as one of the mechanisms for a dentition to change tooth shape. All these unexpected observations indicate that, during ontogeny, the states of dental characters, such as lingual/labial tooth initiation, linear/radial tooth rows, in situ/cross-position tooth replacement and enameloid/enamel, can be switched and the capacity to produce these characters can be suspended or reactivated; the tremendous dental diversity can thus be attributed to the manipulation in time and space of relatively few dental developmental processes.

Paleo-evo-devo implications of a revised conceptualization of enameloids and enamels

Understanding the origin and evolution of the mineralized skeleton is crucial for unravelling vertebrate history. However, several limitations hamper our progress. The first obstacle is the lack of uniformity and clarity in the literature for the definition of the tissues of concern, especially of enameloid(s) and enamel(s), resulting in ambiguous terminology and inconsistencies among studies. Moreover, the identification criteria currently employed to characterize hypermineralized tissues in extinct taxa, such as the presence or absence of tubules for enameloids, may lead to unsupported conclusions. We suggest that comparative developmental studies may be key to unambiguous terminology, truly diagnostic identification criteria and developmentally informed evolutionary hypotheses. We exemplify this approach by: (i) introducing a new conceptual framework for enameloid(s) and enamel(s), with clear terminologies, definitions and interactions between concepts; (ii) suggesting more rigorous ways to identify tissues, based on the observation of defining or additional properties, as well as on the comparison of developmental scenarios when possible; (iii) constructing a clear phylogenetic framework to discuss their homologies and highlighting possible transitions between these tissues; and by (iv) proposing developmental models that explain both enamel and enameloid formation, and suggest possible transitions between them.

Parallel evolution of ameloblastic scpp genes in bony and cartilaginous vertebrates

In bony vertebrates, skeletal mineralization relies on the secretory calcium-binding phosphoproteins (Scpp) family whose members are acidic extracellular proteins posttranslationally regulated by the Fam20°C kinase. As scpp genes are absent from the elephant shark genome, they are currently thought to be specific to bony fishes (osteichthyans). Here, we report a scpp gene present in elasmobranchs (sharks and rays) that evolved from local tandem duplication of sparc-L 5′ exons and show that both genes experienced recent gene conversion in sharks. The elasmobranch scpp is remarkably similar to the osteichthyan scpp members as they share syntenic and gene structure features, code for a conserved signal peptide, tyrosine-rich and aspartate/glutamate-rich regions, and harbor putative Fam20°C phosphorylation sites. In addition, the catshark scpp is coexpressed with sparc-L and fam20°C in tooth and scale ameloblasts, similarly to some osteichthyan scpp genes. Despite these strong similarities, molecular clock and phylogenetic data demonstrate that the elasmobranch scpp gene originated independently from the osteichthyan scpp gene family. Our study reveals convergent events at the sparc-L locus in the two sister clades of jawed vertebrates, leading to parallel diversification of the skeletal biomineralization toolkit. The molecular evolution of sparc-L and its coexpression with fam20°C in catshark ameloblasts provides a unifying genetic basis that suggests that all convergent scpp duplicates inherited similar features from their sparc-L precursor. This conclusion supports a single origin for the hypermineralized outer odontode layer as produced by an ancestral developmental process performed by Sparc-L, implying the homology of the enamel and enameloid tissues in all vertebrates.