Abstract

Teeth were an important innovation in vertebrate evolution but basic aspects of early dental evolution remain poorly understood. Teeth differ from other odontode organs, like scales, in their organized, sequential pattern of replacement. However, tooth replacement patterns also vary between the major groups of jawed vertebrates. Although tooth replacement in stem-osteichthyans and extant species has been intensively studied it has been difficult to resolve scenarios for the evolution of osteichthyan tooth replacement because of a dearth of evidence from living and fossil sarcopterygian fishes. Here we provide new anatomical data informing patterns of tooth replacement in the Devonian sarcopterygian fishes Onychodus, Eusthenopteron and Tiktaalik and the living coelacanth Latimeria based on microfocus- and synchrotron radiation-based X-ray microtomography. Early sarcopterygians generated replacement teeth on the jaw surface in a pattern similar to stem-osteichthyans, with damaged teeth resorbed and replacement teeth developed on the surface of the bone. However, resorption grades and development of replacement teeth vary spatially and temporally within the jaw. Particularly in Onychodus, where teeth were also shed through anterior rotation and resorption of bone at the base of the parasymphyseal tooth whorl, with new teeth added posteriorly. As tooth whorls are also present in more stem-osteichthyans, and statodont tooth whorls are present among acanthodians (putative stem-chondrichthyans), rotational replacement of the anterior dentition may be a stem-osteichthyan character. Our results suggest a more complex evolutionary history of tooth replacement.

Highlights

  • Teeth are a shared feature of all the jawed vertebrate groups and were an important innovation in the radiation of jawed vertebrates [1,2]

  • This contrasts with most fossil and extant osteichthyans where only the tooth crown is shed while the tooth base is resorbed to differing extents [7,8,9,13]

  • Specimens were obtained from the Natural History Museum, London, United Kingdom (NHM UK), Naturhistoriska Riksmuseet, Stockholm, Sweden (NRM), Nunavet Fossil Vertebrate collection (NUFV), Canadian Museum of Nature, Ottawa, Ontario, Canada (NMC); tomographic data were obtained from the Muséum National d’Histoire Naturelle, Paris, France (MNHN)

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Summary

Introduction

Teeth are a shared feature of all the jawed vertebrate (gnathostome) groups and were an important innovation in the radiation of jawed vertebrates [1,2]. Entire teeth, including the tooth base, are shed by linguolabial rotation of the tooth out of the jaw and replacement teeth are formed within a permanent dental lamina (a tooth generating epithelial organ) situated along the lingual jaw margin [6,7,8]. This contrasts with most fossil and extant osteichthyans where only the tooth crown is shed while the tooth base is resorbed to differing extents [7,8,9,13]. As early as the Late Devonian (360 Ma), had acquired a unique, non-replacing dentition [17]

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