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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.
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Sutherland first described it in 1954 from a rock containing a fauna of the Middle
Mississippian age in the Northern territory of Canada. Sutherland proposed the genus Zaphriphyllum for those zaphrentids which still possess a trochoid shape and pronounced cardinal fossula and consistently have
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Zaphriphyllum
Sutherland, 1954, Geol. Mag., v. 91, n. 5, p. 363-365. - --- Hill, 1956, Treatise on Invertebrate Paleontology, pt. F (Coelenterata), p. F267.
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Denayer, Julien (September 2015). "Taxonomy, Biostratigraphy and
Palaeobiogeography of the Late Tournaisian rugose corals of north-western Turkey".
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beds in North
America and Turkey. It is the characteristic coral of the
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New Mexico
Institute of Mining and Technology Memoir
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349:Hill, D. (1981). "Rugosa and Tabulata".
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263:. Specimens have been found in
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371:Armstrong, A.K. (1958).
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259:and family
560:Categories
389:12 January
311:References
294:Z. casteri
273:New Mexico
253:horn coral
168:Subclass:
429:129718645
302:Z. daleki
257:Stariidae
232:See text
188:Stauriida
138:Kingdom:
132:Eukaryota
226:Species
194:Family:
152:Cnidaria
148:Phylum:
142:Animalia
128:Domain:
31:Devonian
288:Species
246:extinct
207:Genus:
181:Order:
158:Class:
571:Rugosa
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275:, US.
244:is an
175:Rugosa
511:This
456:coral
454:This
425:S2CID
376:(PDF)
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391:2021
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59:O
54:Ꞓ
38:~
33:-
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