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Stenoloron swallovana
Taxonomy
Pleurotomaria swallovana was named by Hall (1856) [Pleurotomaria Swallovana]. It is not a trace fossil. Its type locality is Spergen Hill, near railroad station at Harristown, southeast of Salem, which is in a Meramecian carbonate limestone in the Salem Formation of Indiana.
It was recombined as Bembexia swallowiana by Buddington and Chapin (1929); it was recombined as Stenoloron swallovana by Wagner (2023).
It was recombined as Bembexia swallowiana by Buddington and Chapin (1929); it was recombined as Stenoloron swallovana by Wagner (2023).
Sister species lacking formal opinion data
Synonymy list
Year | Name and author |
---|---|
1856 | Pleurotomaria swallovana Hall p. 24 |
1882 | Pleurotomaria swallovana Whitfield p. 80 figs. pl. 9 f. 1-2 |
1883 | Pleurotomaria swallovana Hall p. 356 figs. pl. 32 f. 1-2 |
1906 | Pleurotomaria swallovana Cumings p. 1349 figs. pl. 26 f. 1-2 |
1929 | Bembexia swallowiana Buddington and Chapin |
2023 | Stenoloron swallovana Wagner p. S3822 |
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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.
†Stenoloron swallovana Hall 1856
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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Source: f = family, o = order | |||||
References: Bambach et al. 2007, Hendy 2009 |
Age range: base of the Meramecian to the top of the Late/Upper Mississippian or 342.90000 to 323.40000 Ma
Collections (4 total)
Time interval | Ma | Country or state | Original ID and collection number |
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Meramecian | USA (Indiana) | Pleurotomaria swallovana (129910 129912 129930) | |
Late/Upper Mississippian | USA (Alaska) | Bembexia swallowiana (112183) |