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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Pagodia seelyi
Taxonomy
Pagodia seelyi was named by Walcott (1912). It is not a trace fossil. Its type locality is Loc. 136a. Large brook at point of Mineville Railroad at the turning of the first Y near Port Henry, which is in a Trempealeauan marine sandstone in the Keeseville Formation of New York.
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 1912 | Pagodia seelyi Walcott p. 269 figs. pl. 44 f. 12-14a |
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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.
†Pagodia seelyi Walcott 1912
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: f = family, o = order, c = class | |||||
| References: Whittington et al. 1997, Hendy et al. 2009, Aberhan et al. 2004 | |||||
Age range: Trempealeauan or 490.20000 to 486.85000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Trempealeauan | USA (New York) | Pagodia seelyi (type locality: 74550) |