Argentina tricrenulata
Argentina tricrenulata
Summary
Argentina tricrenulata was a Palaeogene argentinid, part of the marine lineage represented today by argentines. It is known primarily from sagittal otoliths. Modern revision restores Stinton’s species under Argentina and distinguishes it nomenclaturally from material fixed under the older name Argentina erratica.
Its otolith is thin and broadly pentagonal, with a conspicuous postdorsal angle and a long narrow sulcus. These features provide a more reliable basis for identification than size, colour or a single broken margin.
Quick Identification
Look for: a thin, broadly pentagonal otolith only a few millimetres long, with a massive pointed rostrum, a sharp postdorsal angle and a long narrow supramedian sulcus whose cauda extends far toward the posterior margin.
Diagnostic Features
- Otolith is thin and broadly pentagonal, with five principal angles around the outline.
- Rostrum is massive and pointed; a distinct excisura and antirostrum are absent.
- Postdorsal angle is conspicuous and sharper than the rounded predorsal and posterior angles.
- Sulcus is long, narrow and supramedian; the cauda is about twice the length of the short ostium and reaches far posteriorly.
- Outer face is nearly flat and smooth, while the inner face is comparatively flat with a marked dorsal depression.
Fossil Details
Recorded Fossil Sites
Reculver Sand Member
Synonyms & Previous Names
References
- Schwarzhans, W.; Mörs, T.; Engelbrecht, A.; Reguero, M.; Kriwet, J. (2017). Before the freeze: otoliths from the Eocene of Seymour Island, Antarctica, reveal dominance of gadiform fishes (Teleostei). Journal of Systematic Palaeontology, 15(2), 147–170 View reference
- Stinton, F.C. (1965). Teleost otoliths from the Lower London Tertiaries. Senckenbergiana Lethaea, 46a, 389–425 View reference
- Ward, D.J. (1978). The Lower London Tertiary (Palaeocene) succession of Herne Bay, Kent. Report of the Institute of Geological Sciences. Institute of Geological Sciences View reference