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Antiquaobatis

Antiquaobatis is an extinct genus of ray from the Early Jurassic of Europe, containing the single species A. grimmenensis. It is the oldest known described member of the Rajiformes, and is based on a single tooth from Pliensbachian of Northern Germany. It was recovered from the Grimmen Clay Pit, on Spinatum strata that belongs in the region to the Komorowo Formation. The holotype is a single antero-lateral tooth, very small and slightly asymmetrical, measuring 0.25 mm in maximum height and 0.26 mm in maximum width, that has an overall morphology, that suggests a consistent referral to Batoidea, encompassing all skates and rays. The tooth has an overall rather gracile crown morphology, different from any other know jurassic batomorphs, indicating closest affinities to the monotypic genus Engaibatis schultzei from the Kimmeridgian-Tithonian of Tanzania.

Paleoenvironment
The Late Pliensbachian level of the Grimmen clay pit was thought to be part of the Allenstein (Komorowo Formation), but due to being composed by sandstones there was a strong disagreement linking the fluvial Olsztyn with Germany, as it comes from the Mazury area - the easternmost part of the Polish basin - and there is no link with the local Amaltheenton Beds, unlike the Komorowo Formation. But it also could have been moved from the Polish Basin, as on the deposition of this tooth it was flooded by the sea, as proven by the find of ammonites on central Poland. A Nectobenthic lifestyle has been suggested for Jurassic batomorphs, specially complete taxa such as Belemnobatis and Spathobatis, that are superficially similar to extant members of which are generally characterized by sharing a bauplan similar to extant Rhinobatidae, adapted to eat hard-shelled prey. Antiquaobatis grimmenensis appears to have used different, less specialized and probably more opportunistic feeding strategies, as suggested by the gracile and high tooth morphology. ==References==
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