Ctenacanthiformes
| Ctenacanthiformes | |
|---|---|
| File:Dracopristis hoffmanorum.png | |
| Life restoration of Dracopristis | |
| File:Ctenacanthus formosus (fossil shark spine) (Pennsylvanian; Kansas or Nebraska, USA) 1.jpg | |
| Fin spine of Ctenacanthus formosus | |
| Scientific classification Edit this classification | |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Chondrichthyes |
| Subclass: | Elasmobranchii |
| Order: | †Ctenacanthiformes Glikman, 1964 |
| Subtaxa | |
|
See text | |
| Synonyms | |
| |
Ctenacanthiformes is an extinct order of cartilaginous fish. They possessed ornamented fin spines at the front of their dorsal fins and cladodont-type dentition,[1] that is typically of a grasping morphology, though some taxa developed cutting and gouging tooth morphologies.[2] Some ctenacanths are thought to have reached sizes comparable to the great white shark, with body lengths of up to 7 metres (23 ft) and weights of 1,500–2,500 kilograms (3,300–5,500 lb),[3] while others reached lengths of only 30 centimetres (12 in).[4] The earliest ctenacanths appeared during the Frasnian stage of the Late Devonian (~383-372 million years ago), with the group reaching their greatest diversity during the Early Carboniferous (Mississippian), and continued to exist into at least the Middle Permian (Guadalupian).[4] Some authors have suggested members of the family Ctenacanthidae may have survived into the Cretaceous based on teeth found in deep water deposits of Valanginian age in France[5] and Austria,[6] however, other authors contend that the similarity of these teeth to Paleozoic ctenacanths is only superficial, and they likely belong to neoselachians instead.[7]
Taxonomy
[edit | edit source]Ctenacanthiformes are suggested to be more closely related to living elasmobranchs (modern sharks and rays) than to Holocephali (which includes living chimaeras), though less closely than euselachians like hybodonts.[8] The monophyly of the Ctenacanthiformes has been questioned, with some studies recovering the group as a whole as paraphyletic or polyphyletic with respect to other groups of total group elasmobranchs like Xenacanthiformes.[9]
Following Hodnett et al. 2024[4]
Ctenacanthidae Dean 1909
- Ctenacanthus Agassiz, 1837 (Late Devonian)
- Cladodoides Maisey, 2001 (Late Devonian-Early Carboniferous)
- Cladodus Agassiz, 1843 (Early Carboniferous)
- Goodrichthys Moy-Thomas, 1951 (Early Carboniferous)
- Troglocladodus Hodnett et al. 2024 (Early Carboniferous)
Heslerodidae Maisey 2010
- Avonacanthus Maisey 2010 (Early Carboniferous)
- Bythiacanthus St. John and Worthen 1875 (Early Carboniferous)
- Dracopristis Hodnett et al. 2021 (Late Carboniferous)
- Glencartius Ginter and Skompski 2019 (Early Carboniferous)
- Glikmanius Ginter et al. 2005 (Early Carboniferous-Middle Permian)
- Heslerodus Ginter 2002 (Late Carboniferous-Middle Permian)
- Heslerodoides Ivanov 2022 (Late Carboniferous)
- Kaibabvenator Hodnett et al. 2012 (Early-Middle Permian)
- Nanoskalme Hodnett et al. 2012 (Early-Middle Permian)
"Saivodus group"
- Tamiobatis Eastman, 1897 (Late Devonian-Early Carboniferous)
- Saivodus Duffin & Ginter, 2006 (Early Carboniferous-Middle Permian, one of the largest ctenacanths, estimated to reach 6–8 metres (20–26 ft) in length[4])
- Neosaivodus Hodnett et al. 2012 (Middle Permian)
References
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