Ariosoma nonsector Nolf & Stringer, 2003
publication ID |
https://doi.org/ 10.5852/ejt.2022.814.1745 |
publication LSID |
lsid:zoobank.org:pub:74226488-DE8B-4A64-B1D4-A24C15AE79F6 |
DOI |
https://doi.org/10.5281/zenodo.6484255 |
persistent identifier |
https://treatment.plazi.org/id/897AA073-FF8F-3957-E970-C4E0FCD35D8D |
treatment provided by |
Felipe |
scientific name |
Ariosoma nonsector Nolf & Stringer, 2003 |
status |
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Ariosoma nonsector Nolf & Stringer, 2003
Fig. 11A–D View Fig
Ariosoma nonsector Nolf & Stringer, 2003: 7 , pl. 2 figs 1–6.
Otolithus (Platessae) sector – Koken 1888: 292, pl. 17 figs 15–16, non fig. 14 (= lectotype of Paraconger sector ).
Ariosoma nonsector – Nolf 2003: 3, pl. 1 figs 3–4; 2013: 35, pl. 21. — Ebersole et al. 2019: 189, fig. 69g –h. — Stringer et al. 2022: 5, fig. 3c.
Remarks
The otoliths of A. nonsector are deep and more compact than those of similar-looking Paraconger ones; they also have a much broader but shorter and less incised sulcus.
This taxon is the only species of Ariosoma known from the American Eocene.
Stratigraphic and geographic distribution
Lutetian: “Stone City beds”, Texas; Dobys Bluff Tongue of Kosciusko Formation, Mississippi; “lower” Lisbon Formation, Alabama. Bartonian: Wheelock Member, Texas; Cook Mountain Formation, Mississippi; “upper” Lisbon Formation, Alabama; Moodys Branch Formation, Louisiana, Mississippi and Alabama. Priabonian: Yazoo Clay, Louisiana.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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Ariosoma nonsector Nolf & Stringer, 2003
Lin, Chien-Hsiang & Nolf, Dirk 2022 |
Ariosoma nonsector
Nolf D. & Stringer G. L. 2003: 7 |
Otolithus (Platessae) sector
Koken E. 1888: 292 |