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Elkoceras volborthi
Taxonomy
Elkoceras volborthi was named by Lintz and Lohr (1958). Its type specimen is Mackay School of Mines Museum 918, a shell, and it is a 3D body fossil. Its type locality is Carbon Ridge locality about nine miles south of Eureka., which is in a Chesterian carbonate limestone in the Diamond Peak Formation of Nevada. It is the type species of Elkoceras.
It was recombined as Euomphalus volborthi by Lintz (1962).
It was recombined as Euomphalus volborthi by Lintz (1962).
Synonymy list
Year | Name and author |
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1958 | Elkoceras volborthi Lintz and Lohr pp. 979 - 980 figs. pl. 128 f. 1 |
1962 | Euomphalus volborthi Lintz p. 612 |
1981 | Elkoceras volborthi Morris and Cleevely p. 208 |
2023 | Elkoceras volborthi Wagner p. 671 |
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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.
†Elkoceras volborthi Lintz and Lohr 1958
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Diagnosis
Reference | Diagnosis | |
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J. Lintz and L.S. Lohr 1958 | Taphyroconic neanic stage of two or three whorls followed by gyroconic adult whorl of living chamber. Whorl profile subtrigonal, height greater than maximum width which occurs at venter. Prominent alternating nodes at ventral-lateral shoulder beginning on the last taphyroconic whorl. Growth lines perpendicular to direction of growth visible on living chamber. Sutures and siphuncle not seen. |
Measurements
No measurements are available
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Source: f = family, c = class | |||||
Reference: Kiessling 2004 |
Age range: Chesterian or 335.40000 to 323.40000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
---|---|---|---|
Chesterian | USA (Nevada) | Elkoceras volborthi (type locality: 156534) |