Polyptychoceras

Polyptychoceras
Temporal range: 100.5–66.0 Ma

Late Cretaceous

Subptychoceras yubarense
Scientific classification
Kingdom: Animalia
Phylum: Mollusca
Class: Cephalopoda
Subclass: Ammonoidea
Order: Ammonitida
Suborder: Ancyloceratina
Superfamily: Turrilitaceae
Family: Diplomoceratidae
Genus: Polyptychoceras
Yabe, 1927 [1]
Subgenus: Subptychoceras
Yabe
Species
  • †P. mihoense
  • †P. pseudogaultinum
  • †P. haradanuin
  • †P. obatai
  • †P. obliquecostatum
  • †P. subunduratum
  • †P. vancouverensis
  • †P. obstrictum

Polyptychoceras is an extinct genus of ammonites from the Late Cretaceous of Asia, Europe, and North[2] and South America. It was first named by Hisakatsu Yabe in 1927.[3]

Species and Subspecies

This genus contains the following eight species and one subgenus, Subtychoceras, which contains one subspecies. [3]

Description

Fossil shell of Polyptychoceras on display at the Museo Civico di Storia Naturale di Milano

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.[4] This would have caused the shell to topple over if on land.[4] The soft body of the animal would have to have been large, in order to keep the falling shaft off of the ground.[4] The body would not have been resistant to the pressing shell.[4]

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.[5]

Life

A Japanese study in 1979 suggested that Polyptychoceras lived and travelled in schools, similarly to modern cuttlefish.[3] 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.[3] Polyptychoceras was probably buoyant, and swam in a slow, somewhat up-and-down locomotion.[3] It also likely preferred living in sheltered parts of deep sea levels, although how deep is uncertain.[3] Subptychoceras yubarense was likely very long like an eel,[3] and preferred a benthic mode of life.[3]

References

  1. ↑ Yabe, H., 1927: Cretaceous stratigraphy of the Japanese Islands. Science Reports of the Tohoku Imperial University, Second Series (Geology), vol. 11, p. 27–100.
  2. 1 2 3 "Cretaceous Ammonite: Polyptychoceras". northislandexplorer.com. Retrieved 2008-07-09.
  3. 1 2 3 4 5 6 7 8 9 10 Tatsuro Matsumoto and Mitsutoshi Nihongi (1979) An Interesting Mode of Occurrence of Polyptychoceras Japan Academy
  4. 1 2 3 4 "Heteromorphs". www.ebel-k.de. Retrieved 2008-07-10.
  5. ↑ 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

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