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Eusthenopteron
fordii is a species of sarcopterygian (lobe-finned) fishes dating from the Late Devonian period (385 mya), with a close
relationship to tetrapods. It is in the class
Sarcoptergerii, the subclass Tetrapodomorpha, the superorder Osteolepidida, and the family Tristichopteridae. Eusthenopteron was first
described by J. F. Whiteaves in 1881 as part of a large collection of
fishes from Miguasha, Quebec. At
least 2,000 Eusthenopteron fossils have been found at Miguasha,
including those studied between the1940s and 1990s by
paleoichthyologist Erik Jarvik, focusing on their close linkage to early tetrapods. While Eusthepteron was a strictly aquatic
animal, it is classed as a Tetrapodomorph, considered the most direct
precursors to tetrapods. The largest
individuals grew up to 1.8 m (6.5 ft) in length. Eusthenopteron shares many unique features with the
earliest known tetrapods. It has a similar pattern of skull roofing
bones with Ichthyostega and Acanthostega. Importantly, its fin
endoskeleton also bears a distinct humerus, ulna, and
radius. Eusthenopteron had labyrinthodont teeth, characterized by infolded enamel, which characterizes all of the
earliest known tetrapods. Like other fish-like sarcopterygians, Eusthenopteron possessed a two-part cranium, which
hinged at mid-length along an intracranial joint. It also had internal
nostrils (or a choana); which are found only in land animals and
sarcopterygians. The reptilian
stapes or middle ear ossicle seems to have evolved from the hyomandibular bone of
sacropterygians like Eusthenopteron, which has prominent hyomandibular
facets. Differing morphology of the stapes vs. the hyomandibular relates
to the orbital (stapedial) artery.
References:Clack 1994Janvier 1996Jarvik 1980Smithson, T.R. and K.S. Thompson 1982 The hyomandibular of Eusthenopteron foordi Whiteaves (Pisces: Crossopterygii) and the early evolution of the tetrapod stapes Werstoll 1943 . |
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