Abstract

Ostracoderms (fossil armoured jawless fishes) shed light on early vertebrate evolution by revealing the step-wise acquisition of jawed vertebrate characters, and were important constituents of Middle Palaeozoic vertebrate faunas. A wide variety of head shield shapes are observed within and between the ostracoderm groups, but the timing of these diversifications and the consistency between different measures of their morphospace are unclear. Here, we present the first disparity (explored morphospace) versus diversity (number of taxa) analysis of Pteraspidiformes heterostracans using continuous and discrete characters. Patterns of taxic diversity and morphological disparity are in accordance: they both show a rise to a peak in the Lochkovian followed by a gradual decline in the Middle-Late Devonian. Patterns are largely consistent for disparity measures using sum of ranges or total variance, and when using continuous or discrete characters. Pteraspidiformes heterostracans can be classified as a “bottom-heavy clade”, i.e., a group where a high initial disparity decreasing over time is detected. In fact, the group explored morphospace early in its evolutionary history, with much of the subsequent variation in dermal armour occurring as variation in the proportions of already evolved anatomical features. This Early Devonian radiation is also in agreement with the paleobiogeographic distribution of the group, with a maximum of dispersal and explored morphospace during the Lochkovian and Pragian time bins.

Highlights

  • Ostracoderms are a paraphyletic assemblage comprising the jawed vertebrate stem group, which dominated the early vertebrate assemblages, first appearing with high levels of diversity in the Silurian (Sansom, Randle & Donoghue, 2015)

  • The first occurrence of Pteraspidiformes heterostracans is in the Pridoli (Upper Silurian) with fairly low levels of diversity (Fig. 2A), and the clade is represented by just 4 genera

  • Sum of ranges disparity begins to decline from the Emsian onwards mirroring that of diversity; disparity as total variance shows the same value for the Emsian and Eifelian after which it decreases abruptly until it reaches the minimum in the Givetian-Frasnian

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Summary

Introduction

Ostracoderms (extinct, bony jawless vertebrates) are a paraphyletic assemblage comprising the jawed vertebrate stem group, which dominated the early vertebrate assemblages, first appearing with high levels of diversity in the Silurian (Sansom, Randle & Donoghue, 2015). The Anchipteraspididae have a few anatomical differences to the remaining Pteraspidiformes including; a pineal plate enclosed within their dorsal plate, rather than positioned between the rostral and dorsal plates as seen in all other Pteraspidiformes, a fused orbito-cornual plate (with are completely separate in other Pteraspidiformes taxa) and the centre of growth in the dorsal plate anterior to the midline, whereas, in other forms it is centrally or posteriorly positioned (Randle & Sansom, 2017a; Elliott, 1983). The Psammosteidae are stratigraphically the youngest heterostracans and are characterised by having a dorsally orientated mouth and small ‘platelets’ separating their major plates (Blieck, 1984; Janvier, 1996) (Fig. 1E)

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