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Evolution of median fin patterning and modularity in living and fossil osteichthyans

View ORCID ProfileFrance Charest, Jorge Mondéjar Fernández, Thomas Grünbaum, Richard Cloutier
doi: https://doi.org/10.1101/2022.07.18.500482
France Charest
1Département de biologie, chimie et géographie, Université du Québec à Rimouski, Rimouski, Québec, Canada
2Parc national de Miguasha, Nouvelle, Québec, Canada
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  • For correspondence: charest.france@sepaq.com
Jorge Mondéjar Fernández
3UMR 7207 (MNHN–Sorbonne Université–CNRS), Centre de Recherche en Paléontologie – Paris, Département Origines & Évolution, Muséum national d’Histoire naturelle, Paris, France.
4Senckenberg Forschungsinstitut und Naturmuseum Frankfurt, Frankfurt am Main, Germany
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Thomas Grünbaum
1Département de biologie, chimie et géographie, Université du Québec à Rimouski, Rimouski, Québec, Canada
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Richard Cloutier
1Département de biologie, chimie et géographie, Université du Québec à Rimouski, Rimouski, Québec, Canada
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Abstract

Morphological and developmental similarities, and interactions among developing structures are interpreted as evidences of modularity. Such similarities exist between the dorsal and anal fins of living actinopterygians: (1) both fins differentiate in the same direction [dorsal and anal fin patterning module (DAFPM)], and (2) radials and lepidotrichia differentiate in the same direction [endoskeleton and exoskeleton module (EEM)]. To infer the evolution of these common developmental patternings among osteichthyans, we address (1) the complete description and quantification of the DAFPM and EEM in a living actinopterygian (the rainbow trout Oncorhynchus mykiss) and (2) the presence of these modules in fossil osteichthyans (coelacanths, lungfishes, porolepiforms and ‘osteolepiforms’). In Oncorhynchus, sequences of skeletal elements are determined based on (1) apparition (radials and lepidotrichia), (2) chondrification (radials), (3) ossification (radials and lepidotrichia), and (4) segmentation plus bifurcation (lepidotrichia). Correlations are then explored between sequences. In fossil osteichthyans, sequences are determined based on (1) ossification (radials and lepidotrichia), (2) segmentation, and (3) bifurcation of lepidotrichia. Segmentation and bifurcation patterns were found crucial for comparisons between living and extinct taxa. Our data suggest that the EEM is plesiomorphic at least for actinopterygians, and the DAFPM is plesiomorphic for osteichthyans, with homoplastic dissociation. Finally, recurrent patterns suggest the presence of a Lepidotrichia Patterning Module (LPM).

Competing Interest Statement

The authors have declared no competing interest.

Copyright 
The copyright holder for this preprint is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under a CC-BY 4.0 International license.
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Posted July 20, 2022.
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Evolution of median fin patterning and modularity in living and fossil osteichthyans
France Charest, Jorge Mondéjar Fernández, Thomas Grünbaum, Richard Cloutier
bioRxiv 2022.07.18.500482; doi: https://doi.org/10.1101/2022.07.18.500482
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Evolution of median fin patterning and modularity in living and fossil osteichthyans
France Charest, Jorge Mondéjar Fernández, Thomas Grünbaum, Richard Cloutier
bioRxiv 2022.07.18.500482; doi: https://doi.org/10.1101/2022.07.18.500482

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