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Zaphriphyllum

From Wikipedia, the free encyclopedia

Zaphriphyllum
Temporal range: Devonian-Mississippian
~365–343 Ma
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Cnidaria
Subphylum: Anthozoa
Class: Rugosa
Order: Stauriida
Family: Ekvasophyllidae
Genus: Zaphriphyllum
Sutherland 1954[1]
Species

See text

Zaphriphyllum is an extinct genus of horn coral belonging to the suborder Stariidae and family Ekvasophyllidae.[2] Specimens have been found in Mississippian beds in North America[3] and Turkey.[4] It is the characteristic coral of the Kelly Limestone of New Mexico, US.[3]

Original description

[edit]

Sutherland first described it in 1954 from a rock containing a fauna of the Middle Mississippian age in the Northern territory of Canada.[3] Sutherland proposed the genus Zaphriphyllum for those zaphrentids which still possess a trochoid shape and pronounced cardinal fossula and consistently have dissepiments. These forms usually also show a tendency toward a radial arrangement of the septa in the immediate area of the cardinal fossula. Zaphriphyllum closely resembles Amplexizaphrentis Vaughan; except that, as Sutherland (personal communication) has pointed out, the latter is characterized by the absence, or very sparse and discontinuous development, of dissepiments.[citation needed]

Species

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  • Z. casteri Armstrong 1958[3]
  • Z. daleki Denayer 2015[4]

References

[edit]
  1. Zaphriphyllum Sutherland, 1954, Geol. Mag., v. 91, n. 5, p. 363-365. - --- Hill, 1956, Treatise on Invertebrate Paleontology, pt. F (Coelenterata), p. F267.
  2. Hill, D. (1981). "Rugosa and Tabulata". Treatise on Invertebrate Paleontology. F. Vol. 1.
  3. 1 2 3 4 Armstrong, A.K. (1958). "The Mississippian of west-central New Mexico" (PDF). New Mexico Institute of Mining and Technology Memoir. 5. Retrieved 12 January 2021.
  4. 1 2 Denayer, Julien (September 2015). "Taxonomy, Biostratigraphy and Palaeobiogeography of the Late Tournaisian rugose corals of north-western Turkey". Paläontologische Zeitschrift. 89 (3): 313–333. doi:10.1007/s12542-014-0245-1. S2CID 129718645.