Bregmaceros troelli Dante & Frizzell, 1965
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.7035260 |
persistent identifier |
https://treatment.plazi.org/id/897AA073-FF82-3958-E90C-C1A1FA815AF2 |
treatment provided by |
Felipe |
scientific name |
Bregmaceros troelli Dante & Frizzell, 1965 |
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Bregmaceros troelli Dante & Frizzell, 1965
Fig. 15A–D View Fig
Bregmaceros troelli Dante & Frizzell in Frizzell & Dante, 1965: 699, pl. 87 figs 14–19.
Bregmaceros troelli – Nolf 1985: 59; 2013: 56, pl. 87.
Bregmaceros sp. – Nolf & Stringer 2003: 5, pl. 3 fig. 18.
Remarks
Bregmaceros otoliths are sometimes tricky to identify at the species level ( Přikryl et al. 2016) due to their often insufficient diagnostic features. Several features, including an enlarged part in the antero-ventral area that forms a conspicuous sharp postero-ventral angle and an evident concavity in the dorsal rim, are very consistent in the investigated specimens, and therefore we have assigned them to B. troelli (or a closely related species complex). The species can be very abundant in some of the levels, such as the Landrum Member. In the upper sample of the Yazoo Clay in Louisiana, nearly 92% of the total assemblage was comprised of this species ( Nolf & Stringer 2003).
Stratigraphic and geographic distribution
Lutetian: Weches Formation and “Stone City beds”, Texas; Cane River Formation, Louisiana. Bartonian: Cook Mountain Formation, Texas and Mississippi; “upper” Lisbon Formation, Alabama; Moodys Branch Formation, Louisiana, Mississippi and Alabama. Priabonian: Yazoo Clay, Louisiana and Mississippi.
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Bregmaceros troelli Dante & Frizzell, 1965
Lin, Chien-Hsiang & Nolf, Dirk 2022 |
Bregmaceros sp.
Nolf D. & Stringer G. L. 2003: 5 |
Bregmaceros troelli
Nolf D. 2013: 56 |
Nolf D. 1985: 59 |
Bregmaceros troelli
Frizzell D. L. & Dante J. H. 1965: 699 |