Pratulum quinarium ( Marwick, 1944 )
publication ID |
https://doi.org/ 10.11646/zootaxa.4154.1.1 |
publication LSID |
lsid:zoobank.org:pub:1FAB3228-9274-42D8-A2AF-AE19999E17E8 |
DOI |
https://doi.org/10.5281/zenodo.5676858 |
persistent identifier |
https://treatment.plazi.org/id/086C87BA-0019-1766-FF45-F925FB55FD15 |
treatment provided by |
Plazi |
scientific name |
Pratulum quinarium ( Marwick, 1944 ) |
status |
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Pratulum quinarium ( Marwick, 1944) View in CoL
( Fig. 6 View FIGURE 6 )
Nemocardium (Pratulum) quinarium Marwick, 1944: 266 ; pl. 36, figs. 10, 16.
Material. Sixteen specimens, 12 numbered: two from Moonlight North (Y16/f0694), L4653 ( Fig. 6 View FIGURE 6 A), L4654 ( Fig. 6 View FIGURE 6 D); 14 from Tauwhareparae (Y16/f0539), L4655 ( Fig. 6 View FIGURE 6 C), L4656–4663, L4664 ( Fig. 6 View FIGURE 6 B), UOA.
Remarks. Details of the muscle scars of Pratulum quinarium ( Marwick, 1944) remained unobserved or unreported before this study, and are described here from a single small specimen ( Fig. 6 View FIGURE 6 A). The anterior adductor scar is elongate dorsoventrally, rather thin anteroposteriorly; posterior adductor scar arcuate, about twice as wide (anteroposteriorly) as anterior adductor scar, ca. 50% longer dorsoventrally, situated slightly lower than anterior adductor scar; pallial line entire, parallel to (antero- and postero-) ventral margin and rather distant from it (ca. 60– 70% towards margin from shell centre).
The occurrence of P. quinarium at two Lillburnian-age New Zealand fossil seep sites extends the stratigraphic range of this species back from its previous earliest report in the Tongaporutuan. In fact, none of the species currently assigned to Pratulum have ever been recorded from the Lillburnian, but the genus is known throughout the Cenozoic from Danian to Recent ( Beu & Maxwell 1990). P. quinarium is morphologically close to Pratulum pulchellum ( Gray, 1843) , distinguished from it by the finer and more numerous ribs, and by the narrow interstices, well developed transverse bars and absence of tubercles on the posterior area ( Marwick 1944). At 11–13 mm in length, P. quinarium is among the smallest of New Zealand cardiids. The specimens were predominantly found in a single aggregation at Tauwhareparae, reflecting a gregarious habit that is typical for the genus.
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