Pamphilites abdita
publication ID |
https://doi.org/ 10.5281/zenodo.583183 |
publication LSID |
lsid:zoobank.org:pub:2D00AFF5-4FE2-4EC1-A328-C8670CFB8D6D |
DOI |
https://doi.org/10.5281/zenodo.6046905 |
persistent identifier |
https://treatment.plazi.org/id/03AA87D3-284E-FFD9-F7F0-FEF7FA3EB445 |
treatment provided by |
Plazi |
scientific name |
Pamphilites abdita |
status |
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abdita . Pamphilites abdita Scudder, 1875
France, Bouches-du-Rhône, Aix-en-Provence; Chattian–Aquitanian, Late Oligocene–early Miocene.
Depositories: MVMF (holotype lost); MNHN (neotype: IPM B-24308).
Published figures: Scudder (1875: Pl. III, Figs. 14, 17, 18); Leestmans (1983: Figs 11, 12 View FIGURES 11 – 13 ); Nel & Nel (1986: Fig. 1 View FIGURE 1 a-b, Pl. I Fig. 1 View FIGURE 1 ).
One forewing only. All veins originate from the cell, showing attribution of the fossil to the Hesperiidae ; the character recurs in a few subordinate taxa in other superfamilies, but associated with different wing shape. Origin of M2 closer to M3 than to M1, within the Hesperiidae a unique but non-universal character of the Hesperiinae ( Ackery et al. 1999). Wing shape and spotting agree with this subfamily.
Scudder thought it probable that the fossil wing belonged to a female, apparently only because he found a resemblance with Pansydia mesogramma Latreille (now in Atalopedes ), a species of the Greater Antilles in which the male has a stigma. The fossil wing lacks any trace of a stigma, but so do the males of many Hesperiinae . Scudder also found a resemblance with Carystus lucasii (Fabricius) , now Turesis lucas (Fabricius) , a South American species. Therefore, he decided a South American relationship for this European fossil. Scudder remarked that R4 terminated on the termen close to the apex. I have not seen this condition in any Hesperiidae , R4 always terminating on the costa just or well before the apex.
The type of the fossil species seems to be lost, and Nel & Nel (1986) designated a neotype that seems to be conspecific with it. They correctly remarked that the venation and markings agree with numerous extant Hesperiinae species in the Old World and New World , so that a South American affinity of the fossil species is not obvious. If used for calibration, the fossil should be used as an estimated minimum age for the root of Hesperiinae .
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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