Abstract
Among amniote and non-amniote tetrapod trackways from late Carboniferous to early Permian deposits, certain trackway measures vary notably. Some of this variability can be attributed to evolutionary changes in trackmaker anatomy and locomotion style close to the origin of amniotes. Here we demonstrate that steps in early amniote locomotion evolution can be addressed by applying methods of ancestral state reconstruction on trackway data – a novel approach in tetrapod ichnology. Based on (a) measurements of 186 trackways referred to the Carboniferous and early Permian ichnogenera Batrachichnus, Limnopus, Hylopus, Amphisauropus, Matthewichnus, Ichniotherium, Dimetropus, Tambachichnium, Erpetopus, Varanopus, Hyloidichnus, Notalacerta and Dromopus, (b) correlation of these ichnotaxa with specific groups of amphibian, reptiliomorph, synapsid, and reptilian trackmakers based on imprint morphology and (c) known skeletal-morphology-based phylogenies of the supposed trackmakers, we infer ancestral states for functionally controlled trackway measures in a maximum likelihood approach. The most notable finding of our analysis is a concordant change in trackway parameters within a series of ancestral amniote trackmakers, which reflects an evolutionary change in locomotion: In the ancestors of amniotes and diadectomorphs, an increase in body size was accompanied by a decrease in (normalized) gauge width and glenoacetabular length and by a change in imprint orientation toward a more trackway-parallel and forward-pointing condition. In the subsequent evolution of diadectomorph, synapsid and reptilian trackmakers after the diversification of the clades Cotylosauria (Amniota + Diadectomorpha) and Amniota, stride length increased whereas gauges decreased further or remained relatively narrow within most lineages. In accordance with this conspicuous pattern of evolutionary change in trackway measures, we interpret the body size increase as an underlying factor that triggered the reorganization of the locomotion apparatus. The secondary increase in stride length, which occurred convergently within distinct groups, is interpreted as an increase in locomotion capability when the benefits of reorganization came into effect. The track-trackmaker pair of Ichniotherium sphaerodactylum and Orobates pabsti from the early Permian Bromacker locality of the Thuringian Forest, proposed in earlier studies as a suitable ancestral amniote track-trackmaker model, fits relatively well with our modeled last common ancestor of amniotes – with the caveat that the Bromacker material is younger and some of the similarities appear to be due to convergence.
Highlights
Movement traces represent an additional source of information about the locomotion of a fossil trackmaker, amending the functional interpretation of body fossil morphology
Apart from diadectomorphs, several Paleozoic tetrapod groups have been classified as amniote relatives: Embolomeres, gephyrostegids, seymouriamorphs, and lepospondyls have been regarded as successively more closely related to Cotylosauria according to several morphology-based phylogenetic studies (Vallin and Laurin, 2004; Ruta and Coates, 2007; Clack et al, 2012; Witzmann and Schoch, 2017)
These groups are referred to as “reptiliomorphs” in this study – in agreement with the temnospondyl hypothesis of lissamphibian ancestry. Embolomeres and their allies were more distantly related to amniotes than temnospondyls, Embolomeri would not be part of the clade Reptiliomorpha and if lepospondyls instead of temnospondyls were ancestral to lissamphibians, the amniote stem-group would be much smaller and various groups, including embolomeres, gephyrostegids, seymouriamorphs and lepospondyls would not be part of the Reptiliomorpha
Summary
Movement traces represent an additional source of information about the locomotion of a fossil trackmaker, amending the functional interpretation of body fossil morphology. Apart from diadectomorphs, several Paleozoic tetrapod groups have been classified as amniote relatives: Embolomeres, gephyrostegids, seymouriamorphs, and lepospondyls have been regarded as successively more closely related to Cotylosauria according to several morphology-based phylogenetic studies (Vallin and Laurin, 2004; Ruta and Coates, 2007; Clack et al, 2012; Witzmann and Schoch, 2017). For practical reasons, these groups are referred to as “reptiliomorphs” in this study – in agreement with the temnospondyl hypothesis of lissamphibian ancestry. Embolomeres and their allies were more distantly related to amniotes than temnospondyls, Embolomeri would not be part of the clade Reptiliomorpha and if lepospondyls instead of temnospondyls were ancestral to lissamphibians, the amniote stem-group would be much smaller and various groups, including embolomeres, gephyrostegids, seymouriamorphs and lepospondyls would not be part of the Reptiliomorpha (see discussion in Marjanovicand Laurin, 2019; it should be noted that lissamphibian ancestry and other aspects of tetrapod evolution after the Cisuralian are not of much relevance for our approach – apart from questions of terminology)
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