| Crossopholis Temporal range: | |
|---|---|
| | |
| Crossopholis magnicaudatus | |
| Scientific classification | |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Actinopterygii |
| Order: | Acipenseriformes |
| Family: | Polyodontidae |
| Genus: | † Crossopholis Cope, 1883 [1] |
| Type species | |
| Crossopholis magnicaudatus | |
Crossopholis is an extinct fish known from the early Eocene (Ypresian) of North America, approximately 52 million years ago. It is a close relative of the contemporary American paddlefish, belonging to the paddlefish family Polyodontidae.
First described by Edward Drinker Cope in 1883, the first specimen consisted of an incomplete section of the fish's body and tail. In 1886, a partial skull was recovered by Cope. A nearly complete fossil wasn't recorded until 1980. This was due, in part, to the comparative rarity of the fossil as well as the similarities to other species found within the site.
With a maximum recorded length of 1.48 metres (4 ft 10 in), it is smaller than its recent relatives. Unlike the living American paddlefish, it does not have filter feeding gill rakers. The skull and paddle morphology is intermediate between that of Chinese and American paddlefish, with the rostrum having a high density of stellate (star-like) bones, more similar to modern American than to Chinese paddlefish. Unlike American paddlefish, but similar to Chinese paddlefish and other fossil paddlefish, the upper jaw is not attached to the braincase, which in life would have allowed the jaws to move separately (protrude) from the rest of the skull to help sieze prey, similar to sturgeons. [3]
A member of the family Polyodontidae, Crossopholis is most closely related to the American paddlefish. [4] Crossopholis means "fringed scales"; a reference to the thousands of tiny (less than 0.5mm) scales which covered the body of the animal. [5]
Relationships of recent and fossil paddlefish genera, after Grande et al. (2002). [6]
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The fossils of this fish are found in the Fossil Lake area of the Green River Formation. It is more commonly found in shallower deposits of the Thompson Ranch sandwich bed in the Northeast corner of the site than in the deeper midlake sediment deposits. As the species comprises less than .02% of fossils found in the formation, it is probable that Crossopholis spent much of its life in the connecting rivers that existed to the North. This is further evidenced by that lack of juvenile specimens found in the lake area. [5]
Crossopholis was a predator, with fossil evidence of it consuming small schooling fish such as Knightia eocaena . This is in contrast to the American paddlefish, which primarily consumes zooplankton. Research has indicated that the rostrum was an electro-sensory organ, similar to the function in extant relatives. This allowed it to find prey in poor lighting or murky water. [5]