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Koninckites truncatus
Taxonomy
Koninckites truncatus was named by Spath (1934). It is a 3D body fossil. Its type locality is Chidroo, Lower Ceratite Limestone, Salt Range, which is in a Dienerian marine sandstone in the Lower Ceratite Limestone Formation of Pakistan.
It was recombined as Radioceras truncatum by Ware and Bucher (2018) and Ware and Bucher (2018).
It was recombined as Radioceras truncatum by Ware and Bucher (2018) and Ware and Bucher (2018).
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 1934 | Koninckites truncatus Spath |
| 2018 | Radioceras truncatum Ware and Bucher |
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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.
†Koninckites truncatus Spath 1934
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Diagnosis
No diagnoses are available
Measurements
| part | N | mean | |||||
|---|---|---|---|---|---|---|---|
| shell height | 1 | 32.0 | |||||
| shell diameter | 1 | 61.0 | |||||
| shell inflation | 1 | 8.00 |
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| Source: o = order, c = class | |||||
| References: Kiessling 2004, Kiessling 2003 | |||||
Age range: Smithian or 251.30000 to 247.20000 Ma
Collections (3 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Smithian | China (Guangxi) | Koninckites truncatus (44016) | |
| Dienerian | Pakistan | Koninckites davidsonianus (type locality: 143834) Koninckites truncatus (215004) |