24 Morphology and Evolutionary Trends
Friday, 13 April 2018
8:00 AM - 12:00 PM
Room 301 B
POSTCRANIAL MORPHOLOGY AND THE LOCOMOTOR ADAPTATIONS OF EXTANT AND EXTINCT CROCODYLOMORPHS AND LEPIDOSAURS
Paper number: 24-11
Program: Theme Sessions
Time: 11:20 AM – 11:40 AM
Authors
-
Joshua SamuelsEast Tennessee State University, Johnson City, TN
Abstract
We have collected a series of linear measurements of the axial and appendicular skeletons of 55 extant crocodilian and lepidosaur taxa to determine if those engaging in similar locomotor behavior display similar morphology despite phylogenetic differences. A stepwise discriminant function analysis using 28 osteological indices reveals reptile locomotor mode can be accurately predicted (over 80% correct) based on morphology. Semi-aquatic taxa appear to be distinguished by a shorter proximal forelimb relative to scapula length, a longer ischium relative to pubis length, and a shorter distal hindlimb than terrestrial and arboreal taxa. These features potentially reflect adaptations to reduce drag while swimming and increase surface area for the attachment of muscles used in lateral undulations of the tail during aquatic locomotion. Semi-aquatic lizards from four families show parallel divergences from their terrestrial relatives, suggesting similar evolutionary responses in both lepidosaurs and crocodylomorphs. Arboreal taxa display a more elongate humerus and relatively smaller humeral proximal end, possibly to allow for a wider range of motion at the shoulder joint. This morphometric data can potentially be used to predict the locomotor behavior of a wide range of extinct reptile taxa, including both archosaurs and lepidosaurs. Within this study, five extinct crocodylomorph taxa were examined including Hyposaurus rogersii, Necrosuchus ionensis, Alligator sp. of the Gray Fossil Site, Crocodylus affinis, and Allognathosuchus mooki, all of which were inferred to be semi-aquatic by the discriminant function analysis.
Geological Society of America Abstracts with Programs. Vol. 50, No. 3
doi: 10.1130/abs/2018SE-312835
© Copyright 2018 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.