Paraconger sector ( Koken, 1888 )
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.6492706 |
persistent identifier |
https://treatment.plazi.org/id/897AA073-FF8D-3955-E949-C3C9FEA15338 |
treatment provided by |
Felipe |
scientific name |
Paraconger sector ( Koken, 1888 ) |
status |
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Paraconger sector ( Koken, 1888)
Fig. 12A–C View Fig
Otolithus (Platessae) sector Koken, 1888: 292 , fig. 14, non figs 15–16.
Paraconger americanus Müller, 1999: 70 , fig. 20/11–17.
Paraconger sector – Nolf 1985: 43; 2003: 4, pl. 1 fig. 2; 2013: 36, pl. 24. — Nolf & Stringer 2003: 5, pl. 2 figs 9–10. — Ebersole et al. 2019: 190 View Cited Treatment , fig. 69i–j. — Stringer et al. 2022: 5, fig. 3d.
Remarks
The differences between the otoliths of P. sector and P. brazosensis are mentioned above. Interestingly, there appears to be a spatial separation in the occurrence of the two species ( Table 1 View Table 1 ): P. brazosensis is known mainly from the western part of the Gulf Coast (Lutetian and Bartonian of Texas and the upper Lutetian Dobys Bluff Tongue of Mississippi), whereas P. sector is found in the Piney Point Formation of Virginia and throughout the Gulf Coast from Louisiana, Mississippi and Alabama (see Nolf 2003: 4).
Stratigraphic and geographic distribution
Lutetian: “lower” Lisbon Formation, Alabama; Piney Point Formation, Virginia. Bartonian: Cook Mountain Formation, Mississippi; Moodys Branch Formation, Louisiana and Mississippi; “upper” Lisbon Formation, Gosport Sand and Moodys Branch Formation, Alabama. Priabonian: Yazoo Clay, Louisiana.
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Genus |
Paraconger sector ( Koken, 1888 )
Lin, Chien-Hsiang & Nolf, Dirk 2022 |
Paraconger americanus Müller, 1999: 70
Muller A. 1999: 70 |
Paraconger sector
Stringer G. L. & Parmley D. & Quinn A. 2022: 5 |
Ebersole J. A. & Cicimurri D. J. & Stringer G. L. 2019: 190 |
Nolf D. & Stringer G. L. 2003: 5 |
Nolf D. 1985: 43 |
Otolithus (Platessae) sector
Koken E. 1888: 292 |