Micro-computed tomography imaging reveals the development of a unique tooth mineralization pattern in mackerel sharks (Chondrichthyes; Lamniformes) in deep time

• Published in: Scientific Reports
• Main Authors: Patrick L. Jambura, René Kindlimann, Faviel López-Romero, Giuseppe Marramà, Cathrin Pfaff, Sebastian Stumpf, Julia Türtscher, Charlie J. Underwood, David J. Ward, Jürgen Kriwet
• Other Authors: Patrick L. Jambura, René Kindlimann, Faviel López-Romero, Giuseppe Marramà, Cathrin Pfaff, Sebastian Stumpf, Julia Türtscher, Charlie J. Underwood, David J. Ward, Jürgen Kriwet
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2019
• Subjects: Cetorhinus maximus
• Online Access: http://hdl.handle.net/2318/1758442; https://doi.org/10.1038/s41598-019-46081-3

The cartilaginous fishes (Chondrichthyes) have a rich fossil record which consists mostly of isolated teeth and, therefore, phylogenetic relationships of extinct taxa are mainly resolved based on dental characters. One character, the tooth histology, has been examined since the 19th century, but its implications on the phylogeny of Chondrichthyes is still in debate. We used high resolution micro-CT images and tooth sections of 11 recent and seven extinct lamniform sharks to examine the tooth mineralization processes in this group. Our data showed similarities between lamniform sharks and other taxa (a dentinal core of osteodentine instead of a hollow pulp cavity), but also one feature that has not been known from any other elasmobranch fish: the absence of orthodentine. Our results suggest that this character resembles a synapomorphic condition for lamniform sharks, with the basking shark, Cetorhinus maximus, representing the only exception and reverted to the plesiomorphic tooth histotype. Additionally, †Palaeocarcharias stromeri, whose affiliation still is debated, shares the same tooth histology only known from lamniform sharks. This suggests that †Palaeocarcharias stromeri is member of the order Lamniformes, contradicting recent interpretations and thus, dating the origin of this group back at least into the Middle Jurassic.