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Cheirolepis

From Wikipedia, the free encyclopedia
For a taxonomic synonym of a genus of plants, see Centaurea.

Cheirolepis
Temporal range: Middle Devonian to Late Devonian
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Actinopterygii
Order: †Cheirolepidiformes
Kazantzeva-Selezneva, 1977[2]
Family: †Cheirolepididae
Pander, 1860[1]
Genus: †Cheirolepis
Agassiz, 1835
Type species
†Cheirolepis trailli
Agassiz, 1835
Other species

See text

Cheirolepis (from Greek: χείρ kheír, 'hand' and Greek: λεπίς lepis 'scale')[3] is an extinct genus of marine and freshwater ray-finned fish that lived in the Devonian period of Europe and North America. It is the only genus yet known within the family Cheirolepididae and the order Cheirolepidiformes. It was among the most basal of the Devonian actinopterygians and is considered the first to possess the "standard" dermal cranial bones seen in later actinopterygians.

Cheirolepis was a predatory freshwater and estuarine animal about 55 centimetres (22 in) long. It had a streamlined body with small, triangular ganoid scales similar to those of the Acanthodii. These scales had a basic structure typical of many early osteichthyans, with a superficial of ganoine overlying dentine, and a basal plate of bone.[4] Cheirolepis had well-developed fins which gave it speed and stability, and was probably an active predator. Based on the size of its eyes, it hunted by sight. Cheirolepis's jaws, lined with sharp teeth, could be opened very wide, allowing it to swallow prey two thirds of its own size.[5]

Species

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Cheirolepis trailli fossil at the Museum für Naturkunde, Berlin

The following species are known:[6][7]

C. schultzei is known from Red Hill, Nevada deposited during the Mid-Late Devonian boundary. The specimen from which this species was named, consisting of scales and a lower jaw, was originally referred to C. canadensis.[9] Many species, including C. aleshkai,C. bychovensis, C. gracilis & C. gaugeri are only known from isolated scales.[8]

The species C. sinualis from Belarus is considered a nomen nudum. The species C. cummingae Agassiz, 1845, C. macrocephalus M'Coy 1848, & C. uragus Agassiz, 1835 are considered conspecific with C. trailli [10]

C. canadensis on display at Miguasha National Park.

References

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  1. ^ Cheirolepidae fossiilid.info (in Finnish)
  2. ^ Cheirolepiformes fossiilid.info (in Finnish)
  3. ^ Roberts, George (1839). An etymological and explanatory dictionary of the terms and language of geology. London: Longman, Orme, Brown, Green, & Longmans. p. 29. Retrieved 29 December 2021.
  4. ^ Zylberberg, L.; Meunier, F. J.; Laurin, M. (2016). "A microanatomical and histological study of the postcranial dermal skeleton of the Devonian actinopterygian Cheirolepis canadensis". Acta Palaeontologica Polonica. 61 (2): 363–376. doi:10.4202/app.00161.2015.
  5. ^ Palmer, D., ed. (1999). The Marshall Illustrated Encyclopedia of Dinosaurs and Prehistoric Animals. London: Marshall Editions. p. 34. ISBN 1-84028-152-9.
  6. ^ "PBDB Taxon". paleobiodb.org. Retrieved 2024-06-04.
  7. ^ Newman, Michael J.; Burrow, Carole J.; den Blaauwen, Jan L.; Giles, Sam (2021-04-26). "A new actinopterygian Cheirolepis jonesi nov. sp. from the Givetian of Spitsbergen, Svalbard". Norwegian Journal of Geology. doi:10.17850/njg101-1-3.
  8. ^ a b Plax, Dmitry P. (2022). "A NEW SPECIES OF THE RAY-FINNED FISH (OSTEICHTHYES, ACTINOPTERYGII) FROM THE UPPER EMSIAN AND LOWERMOST EIFELIAN DEPOSITS OF BELARUS". Lithosphere. 1 (56).
  9. ^ a b Arratia, G. and Cloutier, R. (2004). A new cheirolepidid fish from the Middle-Upper Devonian of Red Hill, Nevada, USA. In: Arratia, G., Wilson, M. V. H. and Cloutier, B., eds., Recent Advances in the Origin and Early Radiation of Vertebrates. Verlag Dr. Friedrich Pfeil. München, Germany. pp. 583-598. ISBN 3-89937-052-X
  10. ^ Pearson, D. Michael; Westoll, T. Stanley (1979). "The Devonian actinopterygian Cheirolepis Agassiz". Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 70 (13–14): 337–399. doi:10.1017/S0080456800012850. ISSN 1755-6910.
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