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Wyomingites arnoldi
Taxonomy
Paralecanites arnoldi was named by Hyatt and Smith (1905). It is a 3D body fossil. Its type locality is Wood Canyon, Aspen Range, which is in a Smithian carbonate limestone in the Thaynes Formation of Idaho.
It was recombined as Lecanites (Paralecanites) arnoldi by Smith (1932); it was recombined as Wyomingites arnoldi by Spath (1934), Kummel and Steele (1962).
It was recombined as Lecanites (Paralecanites) arnoldi by Smith (1932); it was recombined as Wyomingites arnoldi by Spath (1934), Kummel and Steele (1962).
Synonymy list
| Year | Name and author |
|---|---|
| 1905 | Paralecanites arnoldi Hyatt and Smith p. 136 figs. Pl 64, figs 1-16; pl 77, figs 9-12 |
| 1932 | Lecanites (Paralecanites) arnoldi Smith p. 41 figs. Plate 28, Figures S-10; Plate 39, Figures 9-12; Plate 59, Figures S-10; Plate 64, Figures 1-16 |
| 1934 | Wyomingites arnoldi Spath |
| 1962 | Wyomingites arnoldi Kummel and Steele p. 694 figs. Pl 99, figs 1,2 |
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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.
†Wyomingites arnoldi Hyatt and Smith 1905
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Diagnosis
No diagnoses are available
Measurements
| part | N | mean | |||||
|---|---|---|---|---|---|---|---|
| shell diameter | 1 | 29.7 |
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| Source: o = order, c = class | |||||
| References: Kiessling 2003, Kiessling 2004 | |||||
Age range: Smithian or 249.90000 to 248.10000 Ma
Collections (6 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Early/Lower Triassic | USA (Idaho) | Lecanites arnoldi (33285) | |
| Early/Lower Triassic | USA (Nevada) | Lecanites arnoldi (33313) | |
| Smithian | USA (Nevada) | Wyomingites arnoldi (61515 62098 97121) | |
| Smithian | USA (Idaho) | Paralecanites arnoldi (type locality: 33288) |