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Glyphostoma andersoni
Taxonomy
Glyphostoma andersoni was named by Oinomikado (1939). Its type specimen is Geo. Surv. Japan (unknown no.), a partial shell, and it is a 3D body fossil. Its type locality is Loc. 05, Río Cucurrupi [Munguidó Fm], which is in a Pliocene marine mudstone in the Munguidó Formation of Colombia.
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 1939 | Glyphostoma andersoni Oinomikado p. 624 figs. pl. 29, figs. 8a, b |
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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.
†Glyphostoma andersoni Oinomikado 1939
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: superf = superfamily, c = class | |||||
| References: Hendy et al. 2009, Kiessling 2004 | |||||
Age range: base of the Middle Miocene to the top of the Pliocene or 15.97000 to 2.58800 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Middle Miocene | Mexico (Michoacan) | Glyphostoma andersoni (66163) | |
| Pliocene | Colombia | Glyphostoma andersoni (type locality: 93725) |