Abstract

AbstractThe morphology of the vertebrate lower jaw has been used to infer feeding ecology, with transformations in mandibular shape and structure likely to have facilitated the emergence of different feeding behaviours in vertebrate evolution. Here we present elliptical Fourier shape and principal component analyses, characterizing and comparing the disparity of jaw shape in early gnathostomes and their modern primitively aquatic counterparts. 83% of shape variation is summarized on the first three principal component axes and all component clades of early gnathostomes exhibit overlapping morphological variation. Non‐tetrapodomorph Palaeozoic sarcopterygians are more disparate than their extant counterparts whereas extant chondrichthyans are more disparate than their Palaeozoic counterparts. More generally, extant jawed fishes are more disparate than their Palaeozoic relatives largely because of the extensive shape variation exhibited by mandibles of extant actinopterygians. Only some areas of shape space vacated by Palaeozoic gnathostomes have been convergently refilled by living taxa. Characterization of theoretical jaw morphologies demonstrates that fewer than half of all possible shapes are realized by the jawed fishes that comprise our empirical dataset; many of these morphologies are realized by unrepresented terrestrial tetrapods, implying environmental constraint. Our results are incompatible with the early burst model of clade evolution and contradict the hypothesis that maximum disparity is reached early in the evolutionary history of jawed fishes.

Highlights

  • The morphology of the vertebrate lower jaw has been used to infer feeding ecology, with transformations in mandibular shape and structure likely to have facilitated the emergence of different feeding behaviours in vertebrate evolution

  • We test whether the full extent of jaw morphological variation was established early in gnathostome evolutionary history, consistent with an early burst model of morphological evolution (Simpson 1944; Givnish 2015), or whether extant jaw morphological diversity exceeds that of Palaeozoic fossil taxa

  • Actinopterygians contribute more than half of the morphological disparity (60%), followed by chondrichthyans (18%), placoderms (12%), non-tetrapodomorph sarcopterygian fish (5%), and acanthodians (5%)

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Summary

Introduction

The morphology of the vertebrate lower jaw has been used to infer feeding ecology, with transformations in mandibular shape and structure likely to have facilitated the emergence of different feeding behaviours in vertebrate evolution. Our results are incompatible with the early burst model of clade evolution and contradict the hypothesis that maximum disparity is reached early in the evolutionary history of jawed fishes. Anderson et al (2011) demonstrated that disparity of functional characters associated with gnathostome feeding plateaued soon after the origin of the jaw, but they did not consider the evolution of gnathostomes beyond their initial radiation or the implications of mandibular innovation. We test whether the full extent of jaw morphological variation was established early in gnathostome evolutionary history, consistent with an early burst model of morphological evolution (Simpson 1944; Givnish 2015), or whether extant jaw morphological diversity exceeds that of Palaeozoic fossil taxa. Through characterization of theoretical jaw shapes throughout morphospace, we explore the reasons for variance in morphospace occupation and potential functional constraints

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