bioRxiv preprint doi: https://doi.org/10.1101/2020.07.27.222737; this version posted July 28, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. 1 Mineralisation of the Callorhinchus vertebral column 2 (Holocephali; Chondrichthyes) 3 4 Running title: Mineralisation of the Callorhinchus vertebral column 5 6 Jacob Pears1, Zerina Johanson2*, Kate Trinajstic1, Mason Dean3, Catherine 7 Boisvert1 8 1School of Molecular and Life Sciences, Curtin University, Perth, Australia. Email: 9
[email protected];
[email protected]; 10
[email protected] 11 2Department of Earth Sciences, Natural History Museum, London, UK. Email: 12
[email protected] 13 14 3Max Planck Institute of Colloids and Interfaces, Department of Biomaterials, Am 15 Muehlenberg 1, 14476 Potsdam, Germany. Email:
[email protected] 16 17 *Correspondence: 18 Zerina Johanson:
[email protected] 19 20 Keywords: Holocephali, Callorhinchus, tesserae, mineralisation, evolution, stem 21 group Holocephali 22 23 Abstract 24 Chondrichthyes (Elasmobranchii and Holocephali) are distinguished by their largely 25 cartilaginous endoskeleton that comprises an uncalcified core overlain by a mineralised layer; 26 in the Elasmobranchii (sharks, skates, rays) this mineralisation takes the form of calcified 27 polygonal tiles known as tesserae. In recent years, these skeletal tissues have been described 28 in ever increasing detail in sharks and rays but those of Holocephali (chimaeroids) have been 29 less well-described, with conflicting accounts as to whether or not tesserae are present. 30 During embryonic ontogeny in holocephalans, cervical vertebrae fuse to form a structure 31 called the synarcual.