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This fossilized structure was found close to several coelacanth bones, from the Late Jurassic – Early Cretaceous of Uruguay (South America). The accompanying fauna include theropod dinosaurs, crocodyliforms, turtles, ginglymodian and dipnoan fishes.
It is bean-shaped, compact, measuring about 1,5 cm long, and it has what appear to be growth layers. These layers are continued through the interior of the piece, as can be seen from high resolution CT scan (see figure). Some kind of periodicity between thin dense layers, and thick less dense layers can be perceived, with all of them becoming narrower towards the flat face of the piece.
It is tempting to assume it is an otolith. But after consulting several colleagues around the world who work with fossil and Recent otoliths, they tend to disagree with this. Those who work with teleostean otolihts rejected this possibility, mainly based on general morphology (which is rather simple) and kind of growth. Those who are more familiarized with fossil otoliths from other groups than Teleostei were more cautious (even more considering the fact that otoliths are almost unknown in fossil coelacanths and other sarcopterygians). Nevertheless, all of them agreed with the idea this is a biogenic structure, with some kind of seasonal growth.
Mineral composition was approached through EDS but the results are not conclusive (for now). Main elements are Ca, P, O and C, but I’m unable to discriminate between calcium carbonate/phosphate. Si and O seem to be more abundant in the fractures and interstices (maybe it’s diagenetic silicon oxide).
SEM images are not conclusive either. Each layer seems to be constituted mainly of a matrix of micrometric granular bodies, or filiform bodies, agglomerated (see figures).
After several months studying this piece without reaching a taxonomic identification, I’m turning to fellow paleontologists and neontologists, to ask for your help.
Thanks in advance!