Dasyatis undetermined
publication ID |
https://doi.org/ 10.5070/P9361043964 |
publication LSID |
lsid:zoobank.org:pub:3F95876E-933FF-48AF-9CF0-A840A333220B |
persistent identifier |
https://treatment.plazi.org/id/03E787A6-FE3A-FF95-A9D4-F8BDFBF2FB36 |
treatment provided by |
Felipe |
scientific name |
Dasyatis undetermined |
status |
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DASYATIS SP. CF. D. TRICUSPIDATUS CASIER 1946
( FIG. 6I–P View Figure 6 )
Referred specimens —SC2013.38.41, tooth; SC2013.38.42, male tooth; SC2013.38.43, male tooth; SC2013.38.44, six teeth.
Remarks —Nine large Dasyatis teeth are characteristic in their lack of enameloid ornamentation, a feature that readily distinguishes them from most other species that have been reported from Eocene strata (Ward 1979b, Noubhani and Cappetta 1997). The intersection of the transverse crest with a sagittal lingual crest results in a tripartite division of the crown (i.e., Fig. 6M View Figure 6 ). This species was originally reported from lower Eocene strata of Belgium ( Casier 1946), and the taxon has subsequently been documented in middle Eocene strata of Europe ( Kemp et al. 1990, Van den Eeckhaut and de Schutter 2009).
Dasyatis exhibits gynandric heterodonty (male teeth differ from those of females), but the identification of male and female teeth of a fossil species may not be as clear cut as previously thought. Kajiura and Tricas (1996) found that male and female teeth of Dasyatis sabina (= Hypanus sabinus ) (Lesueur, 1824) may be nearly indistinguishable from each other, with both sexes having low-crowned teeth. However, as mating season approaches, male teeth exhibit a transition ( Fig. 6K View Figure 6 ) to taller, highly cuspidate crowns that are effective at grasping pectoral fins of females during copulation ( Kajiura et al. 2000). Assuming this phenomenon was developed in Eocene fossil species, isolated low-crowned teeth ( Fig. 6M–P View Figure 6 ) in the Dry Branch sample could belong to males or females, whereas high-crowned cuspidate teeth belonged to males ( Fig. 6I–J View Figure 6 ).
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