Pygopterus is an extinct genus of prehistoric bony fish that lived during the Wuchiapingian to Olenekian ages (late Permian to Early Triassic epochs) in what is now England, Germany (Baden-Württemberg, Saxony-Anhalt), Greenland and Svalbard (Spitsbergen).[2][3] It is one of the few genera of ray-finned fish known to cross the Permian-Triassic boundary.[3]

Pygopterus
Temporal range: WuchiapingianOlenekian
P. humboldti fossil
(Museum of Paleontology, Tübingen)
Scientific classification
Kingdom:
Phylum:
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Genus:
Pygopterus

Agassiz, 1833
Type species
Palaeothrissium humboldti
Other species[1]
  • P. degeeri Stensiö, 1921
  • P. crecelli Wilser, 1923
  • P. gleerupi Aldinger, 1937
  • P. nielseni Aldinger, 1937
Pygopterus humboldti
Pygopterus humboldti fossil

Fossils have been found in the Marl Slate Formation, Kupferschiefer (Werra Formation), Ravnefjeld Formation, Vikinghøgda Formation and Buntsandstein.[1][2] A report about the discovery of this fish in Westphalian deposits of Belgium was likely caused by the presence of Nematoptychius which was referred to as Pygopterus in late 19th century.[4]

Synonyms edit

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References edit

  1. ^ a b c Schultze, Hans-Peter; Mickle, Kathryn E.; Poplin, Cecile; Hilton, Eric J.; Grande, Lance (2021). Handbook of Paleoichthyology, 8A. Actinopterygii I. Palaeoniscimorpha, Stem Neopterygii, Chondrostei. Dr. Friedrich Pfeil, München. p. 299. ISBN 978-3-89937-272-4.
  2. ^ a b Aldinger, Hermann (1937). "Permische Ganoidfische aus Ostgrönland". Meddelelser om Grønland (in German). 102 (3): 1–392.
  3. ^ a b Romano, Carlo; Koot, Martha B.; Kogan, Ilja; Brayard, Arnaud; Minikh, Alla V.; Brinkmann, Winand; Bucher, Hugo; Kriwet, Jürgen (2016). "Permian-Triassic Osteichthyes (bony fishes): diversity dynamics and body size evolution". Biological Reviews. 91 (1): 106–147. doi:10.1111/brv.12161. PMID 25431138. S2CID 5332637.
  4. ^ C. Derycke, R. Cloutier, A.-M. Candilier (1995). "Palaeozoic vertebrates of northern France and Belgium: Part II - Chondrichthyes, Acanthodii, Actinopterygii (Uppermost Silurian to Carboniferous)". Geobios. 28 (1889–1890): 347. doi:10.1016/S0016-6995(95)80136-7.{{cite journal}}: CS1 maint: multiple names: authors list (link)