Cryptoplax pritchardi Hall, 1905
publication ID |
https://doi.org/10.24199/j.mmv.2024.83.02 |
DOI |
https://doi.org/10.5281/zenodo.14703325 |
persistent identifier |
https://treatment.plazi.org/id/03F487BA-8F85-C7A8-FCB5-52EC2D43F8F6 |
treatment provided by |
Felipe |
scientific name |
Cryptoplax pritchardi Hall, 1905 |
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Cryptoplax pritchardi Hall, 1905 View in CoL
Cryptoplax pritchardi Hall, 1905: 391 View in CoL , pl. 30, figs 1–6.— Ashby, 1925: 183, pl. 18, figs 11, 12, pl. 19, figs 13–16; Ashby and Cotton, 1939: 217, pl. 19, fig. 19; Cotton and Godfrey, 1940: Fig. 581; Cotton, 1964: Fig. 131.
Cryptoplax gatliffi Hall, 1905: 392 View in CoL , pl. 30 figs 7–9.— Ashby, 1925: 184, pl. 18, figs 10a, b.
Distribution. Otway Basin: Grange Burn Formation (type). Age : early Pliocene.
Remarks. Ashby and Cotton (1939) concluded that C. gatliffi was a synonym of C. pritchardi because all the sculpture had been worn off and that the lobe-shaped plate said to be present in the former and absent in the latter was in fact present in all valves. The type specimen of C. gatliffi was said to be Clifton Bank on Muddy Creek, thus from the Miocene Muddy Creek Formation, whereas the type specimen of C. pritchardi was from McDonalds Bank on Muddy Creek, thus from the Pliocene Grange Burn Formation further upstream, so the specimen could have been washed downstream. No other specimens seem to have been found in the Muddy Creek Formation, so Ashby and Cotton’s opinion on the synonymy is accepted pending further specimens from the Muddy Creek Formation being found in situ.
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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Cryptoplax pritchardi Hall, 1905
Darragh, Thomas A. 2024 |
Cryptoplax pritchardi
Ashby, E. & Cotton, B. C. 1939: 217 |
Ashby, E. 1925: 183 |
Hall, T. S. 1905: 391 |
Cryptoplax gatliffi
Ashby, E. 1925: 184 |
Hall, T. S. 1905: 392 |