Tucetona decurrens ( Chapman and Singleton, 1925 )
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publication ID |
https://doi.org/10.24199/j.mmv.2024.83.02 |
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DOI |
https://doi.org/10.5281/zenodo.14701810 |
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persistent identifier |
https://treatment.plazi.org/id/03F487BA-8F6A-C747-FF0F-57922A15FDED |
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treatment provided by |
Felipe |
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scientific name |
Tucetona decurrens ( Chapman and Singleton, 1925 ) |
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Tucetona decurrens ( Chapman and Singleton, 1925) View in CoL
Glycymeris decurrens Chapman and Singleton, 1925: 42 View in CoL , pl. 3, figs 24, 25, pl. 4, fig. 16.
Glycymeris (Tucetona) decurrens Chapman and Singleton, 1925 View in CoL : Ludbrook, 1965: 91, pl. 3, figs 9, 10.
Distribution. Otway Basin: Grange Burn Formation (type). Gippsland Basin: Jemmys Point Formation. Age : early Pliocene.
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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Tucetona decurrens ( Chapman and Singleton, 1925 )
| Darragh, Thomas A. 2024 |
Glycymeris (Tucetona) decurrens
| Ludbrook, N. H. 1965: 91 |
Glycymeris decurrens
| Chapman, F. & Singleton, F. A. 1925: 42 |