Gadophycis ovalis
Gadophycis ovalis
Summary
Gadophycis ovalis was an early Eocene ophidiiform known from sagittal otoliths. Its relationship with cusk-eel lineages is supported by otolith morphology, although the precise placement of the extinct otolith-based genus Gadophycis is less secure than that of living genera.
The fossil record is therefore almost entirely otolith-based. Its morphology is consistent with a marine, probably demersal ophidiiform ecology, but body form, swimming behaviour and diet cannot be reconstructed directly from the otolith alone.
Quick Identification
Look for: an elongate oval sagittal otolith with a noticeably deep, smoothly curved ventral rim and smooth rather than serrated margins. Use the sulcus and inner-face relief as supporting characters; eroded otoliths that no longer preserve these features should be left at a broader ophidiiform identification.
Diagnostic Features
- Overall outline is elongate oval rather than short or strongly angular.
- Ventral rim is distinctly deep and smoothly curved.
- Dorsal and ventral margins are smooth rather than conspicuously serrated.
- A distinct ventral furrow of the type developed in Gadophycis serratus is absent.
- Species-level identification requires the deep smooth ventral outline together with the preserved sulcus pattern; outline alone is insufficient.
Fossil Details
Similar Species
Recorded Fossil Sites
Lessness Shell Bed
References
- Schwarzhans, W.; Bratishko, A. (2011). The otoliths from the middle Paleocene of Luzanivka (Cherkasy district, Ukraine). Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen, 261(1), 83–110 View reference
- White, E.I. (1931). The vertebrate faunas of the English Eocene. I. From the Thanet Sands to the Basement Bed of the London Clay. 121 pp.. British Museum (Natural History), London View reference