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Paleofavosites mccullochae

Anthozoa - Favositida - Favositidae

Taxonomy
Paleofavosites mccullochae was named by Flower (1961). It is not a trace fossil. Its type locality is Tank Canyon, Hillsboro, which is in a Richmondian shallow subtidal limestone in the Cutter Formation of New Mexico.

Synonymy list
YearName and author
1961Paleofavosites mccullochae Flower
1985Paleofavosites mccullochae Pandolfi p. 25 figs. Pl. 8, fig. 2; Pl. 9, figs. 1, 3; Pl. 10, fig. 1

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RankNameAuthor
kingdomAnimalia()
phylumCnidariaHatschek 1888
classAnthozoaEhrenberg 1834
subclassTabulataMilne-Edwards and Haime 1850
orderFavositidaWedekind 1937
RankNameAuthor
suborderFavositinaWedekind 1937
superfamilyFavositoidea(Dana 1846)
familyFavositidaeDana 1846
genusPaleofavositesTwenhofel 1914
speciesmccullochae

If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.

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Diagnosis
ReferenceDiagnosis
J. M. Pandolfi 1985Mean diameter of corallites is 2.4 mm. Budding individuals appear initially as small rounded tubes. Walls are thin, commonly 0.1 mm, straight in transverse section, and may be straight, slightly curved or corrugated in longitudinal section. Mural pores, 0.1-0.2 mm in diameter, are commonly spaced 0.5-1.0 mm apart in the corallite corners and are rare in the walls. Tabulae are complete and commonly depressed at their margins. Septa! spines are absent.