Marion Chevrinais, C. Morel, C. B. Renaud, R. Cloutier
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Ontogeny of Euphanerops longaevus from the Upper Devonian Miguasha Fossil-Fish-Lagerstätte and comparison with the skeletogenesis of the Sea Lamprey Petromyzon marinus
Ontogeny is of paramount importance to understand evolutionary relationships of organisms. However, in the fossil record, early developmental stages are rarely preserved because of their unmineralized skeleton. Here, we describe the ontogeny of the Devonian jawless fish Euphanerops longaevus based on observations from more than 3,500 specimens. The ontogeny of Euphanerops is compared with the development of the median fins of the extant jawless fish, the Sea Lamprey (Petromyzon marinus). From a sub-sample of 216 specimens of Euphanerops, we define three ontogenetic stages: larvae (2-38 mm total length; mostly composed of “Scaumenella mesacanthi”); juveniles (28-98 mm total length); and adults (≥ 90 mm total length) based on the degree of skeletal development, chemical and microscopic compositions. Larvae display three cranial plates, a simple branchial apparatus, notochordal elements and caudal fin supports. In juveniles, we document the development of paired anteroventral, anal and median dorsal fins. Given how little information is generally available on ostracoderm ontogeny, the growth series of Euphanerops provides an unparalleled opportunity to understand the development of early vertebrate characters.
期刊介绍:
The Canadian Journal of Earth Sciences reports current research in climate and environmental geoscience; geoarchaeology and forensic geoscience; geochronology and geochemistry; geophysics; GIS and geomatics; hydrology; mineralogy and petrology; mining and engineering geology; ore deposits and economic geology; paleontology, petroleum geology and basin analysis; physical geography and Quaternary geoscience; planetary geoscience; sedimentology and stratigraphy; soil sciences; and structural geology and tectonics. It also publishes special issues that focus on information and studies about a particular segment of earth sciences.