Polyptychoceras

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Polyptychoceras
Temporal range: 100.5–66.0 Ma
Late Cretaceous
File:Polyptychoceras (Subptychoceras) yubarense.jpg
Subptychoceras yubarense
Scientific classification
Kingdom:
Animalia
Phylum:
Mollusca
Class:
Cephalopoda
Subclass:
Ammonoidea
Order:
Ammonitida
Suborder:
Ancyloceratina
Superfamily:
Turrilitaceae
Family:
Diplomoceratidae
Genus:
Polyptychoceras

Yabe, 1927
Subgenus:
Subptychoceras

Yabe
Species
  • †P. mihoense
  • †P. pseudogaultinum
  • †P. haradanuin
  • †P. obatai
  • †P. obliquecostatum
  • †P. subunduratum
  • †P. vancouverensis
  • †P. obstrictum

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Polyptychoceras is an extinct genus of ammonite from the Late Cretaceous of Asia, Europe, and North[1] and South America. It was first named by Hisakatsu Yabe in 1927.[2]

Species and Subspecies

This genus contains the following eight species and one subgenus, Subtychoceras, which contains one subspecies. [2]

  • Polyptychoceras mihoense
  • Polyptychoceras pseudogaultinum could reach a length of 100 - 120 mm,[2]
  • Polyptychoceras haradanum (Yokoyama)
  • Polyptychoceras obatai
  • Polyptychoceras obliquecostatum
  • Polyptychoceras subunduratum
  • Polyptychoceras obstrictum (Jimbo)
  • Polyptychoceras vancouverensis located around the Trent River and Puntledge River.[1] Due to its shape, collectors of P. vancouverensis fossils often call it the "paperclip ammonite" or "candy cane".[1]
  • Polyptychoceras (Subptychoceras) yubarense could reach a maximum length of 200 mm.[2]

Description

Polyptychoceras is a heteromorph ammonite, meaning that its shell does not curl up into the tight spiral shape which shells of ammonites from the subclass Ammonoidea typically do.

Polyptychoceras shells have an abrupt weight increase after formation of the initial shaft, which represents the shell's automatic balance condition.[3] This would have caused the shell to topple over if on land.[3] The soft body of the animal would have to have been large, in order to keep the falling shaft off of the ground.[3] The body would not have been resistant to the pressing shell.[3]

Although the shafts in the fossils of the shells are usually parallel to each other, small aberrations during each growth stage often caused abrupt constrictions in the shape of the shell.[4]

File:Diplomoceratidae - Polyptychoceras species.JPG
Fossil shell of Polyptychoceras on display at the Museo Civico di Storia Naturale di Milano

Life

A Japanese study in 1979 suggested that Polyptychoceras lived and travelled in schools, similarly to modern cuttlefish.[2] Individual fossil specimens of a particular species of Polyptychoceras are frequently found in sediments laid down in the same bed of water, around the Santonian and Upper Coniacian faunal stages of the Late Cretaceous Epoch.[2] Polyptychoceras was probably buoyant, and swam in a slow, somewhat up-and-down locomotion.[2] It also likely preferred living in sheltered parts of deep sea levels, although how deep is uncertain.[2] Subptychoceras yubarense was likely very long like an eel,[2] and preferred a benthic mode of life.[2]

References

  1. ↑ 1.0 1.1 1.2 Lua error in package.lua at line 80: module 'strict' not found.
  2. ↑ 2.0 2.1 2.2 2.3 2.4 2.5 2.6 2.7 2.8 2.9 Tatsuro Matsumoto and Mitsutoshi Nihongi (1979) An Interesting Mode of Occurrence of Polyptychoceras Japan Academy
  3. ↑ 3.0 3.1 3.2 3.3 Lua error in package.lua at line 80: module 'strict' not found.[dead link]
  4. ↑ Ammonoid Paleobiology (Topics in Geobiology) by Neil H. Landman, Kazushige Tanabe, and Richard Arnold Davis; page 224. Published 1996 Springer. ISBN 0-306-45222-7 Retrieved on 2008-05-02

Suggested further reading

  • West Coast Fossils: A Guide to the Ancient Life of Vancouver Island by Rolf Ludvigsen and Graham Beard
  • Special papers / Nihon Koseibutsu Gakkai; page 29. Published 1984; Original from the University of California
  • Geological Abstracts; page 1324. By Geo Abstracts Bibliography; Published 1986, Elsevier/Geo Abstracts
  • Memoirs; page 157. By Fukuoka, Japan Kyushu University. Faculty of Science, Hokkaido University Faculty of Engineering; Published 1959
  • Memoirs of the Faculty of Science, Kyushu University; pages 117 - 119. By Kyūshū Daigaku Rigakubu; Published 1940
  • Ammonite Faunas of the Upper Cretaceous Rocks of Vancouver Island, British Columbia; pages 100 - 101. By J L Usher, Geological Survey of Canada; Published 1952 E. Cloutier, Queen's Printer

External links

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