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Neoloculicyathus grandis
Taxonomy
Ardrossacyathus grandis was named by Gravestock (1984). It is not a trace fossil. Its type locality is Mount Scott Range, Tor Herm (section N), Epiphyton-archaeocyath bioherms, which is in an Atdabanian reef, buildup or bioherm limestone in the Ajax Limestone Formation of Australia.
It was recombined as Neoloculicyathus grandis by Kruse and Moreno-Eiris (2014).
It was recombined as Neoloculicyathus grandis by Kruse and Moreno-Eiris (2014).
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 1984 | Ardrossacyathus grandis Gravestock |
| 2014 | Neoloculicyathus grandis Kruse and Moreno-Eiris pp. 42 - 44 fig. 26 |
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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.
†Neoloculicyathus grandis Gravestock 1984
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Diagnosis
| Reference | Diagnosis | |
|---|---|---|
| P. D. Kruse and E. Moreno-Eiris 2014 | Outer wall with 3–5 (rarely six) pores per outer wall intersept in cups of diameter 6.8–12.8 mm; orientation of pseudoseptal pore rows variable, generally parallel to cup walls, less commonly divergent from outer wall. |
Measurements
No measurements are available
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| Source: p = phylum | |||||
| References: Bambach et al. 2007, Kiessling 2004 | |||||
Age range: Atdabanian or 521.00000 to 516.00000 Ma
Collections (4 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Atdabanian | Australia (South Australia) | Ardrossacyathus grandis (81171 type locality: 81173 81177 81180) |