Tucetona convexa (Tate, 1886)
publication ID |
https://doi.org/10.24199/j.mmv.2024.83.02 |
DOI |
https://doi.org/10.5281/zenodo.14701808 |
persistent identifier |
https://treatment.plazi.org/id/03F487BA-8F6B-C747-FCB5-50752860FE13 |
treatment provided by |
Felipe |
scientific name |
Tucetona convexa (Tate, 1886) |
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Tucetona convexa (Tate, 1886) View in CoL
Pectunculus convexus Tate, 1886b: 138 , pl. 11, figs 7a, b.— Harris, 1897: 342.
Glycimeris maccoyi (Johnston) .— Chapman and Gabriel, 1914: 303, pl. 24, fig. 5: Chapman, 1916: pl. 67, fig. 5, non Johnston, 1880.
Glycymeris convexa (Tate, 1886) .— Chapman and Singleton, 1925: 37, pl. 2, figs 16a, b, 17–20, pl. 4, figs 12, 13.
Tucetona crama Cotton, 1947: 660 View in CoL , pl. 20, figs 1, 2.
Glycymeris (Tucetona) convexa (Tate, 1886) .— Ludbrook, 1955: 26; Ludbrook, 1965: 90, pl. 3, figs 15–20; Ludbrook, 1973: pl. 27, fig. 84; Ludbrook, 1983: 39, fig. 2e; Ludbrook, 1984: 238, Figs 58d, e.
Distribution. St Vincent Basin: Dry Creek Sands, Point Ellen Formation, Hallett Cove Sandstone. Murray Basin: Bookpurnong Formation, Norwest Bend Formation. Otway Basin: Grange Burn Formation (type). Port Phillip Basin: Sandringham Sandstone. Bass Basin: Cameron Inlet Formation. Age : middle Miocene–late 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 convexa (Tate, 1886)
Darragh, Thomas A. 2024 |
Glycymeris (Tucetona) convexa (Tate, 1886)
Ludbrook, N. H. 1984: 238 |
Ludbrook, N. H. 1983: 39 |
Ludbrook, N. H. 1965: 90 |
Ludbrook, N. H. 1955: 26 |
Tucetona crama
Cotton, B. C. 1947: 660 |
Glycymeris convexa (Tate, 1886)
Chapman, F. & Singleton, F. A. 1925: 37 |
Glycimeris maccoyi (Johnston)
Chapman, F. & Gabriel, C. J. 1914: 303 |
Pectunculus convexus
Harris, G. F. 1897: 342 |
Tate, R. 1886: 138 |