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Exceptional In Situ Preservation of Chondrocranial Elements in a Coniacian Mosasaurid from Colombia
Exceptional In Situ Preservation of Chondrocranial Elements in a Coniacian Mosasaurid from Colombia
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Exceptional In Situ Preservation of Chondrocranial Elements in a Coniacian Mosasaurid from Colombia
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Exceptional In Situ Preservation of Chondrocranial Elements in a Coniacian Mosasaurid from Colombia
Exceptional In Situ Preservation of Chondrocranial Elements in a Coniacian Mosasaurid from Colombia

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Exceptional In Situ Preservation of Chondrocranial Elements in a Coniacian Mosasaurid from Colombia
Exceptional In Situ Preservation of Chondrocranial Elements in a Coniacian Mosasaurid from Colombia
Journal Article

Exceptional In Situ Preservation of Chondrocranial Elements in a Coniacian Mosasaurid from Colombia

2024
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Overview
The first record of well-preserved chondrocranial elements in mosasaurids is here described. These elements are preserved in situ in a Coniacian skull found in north-central Colombia, inside a calcareous concretion. Based on a 3D model generated from computed tomography scans, we identified elements of the nasal and orbitotemporal regions. Our descriptions show that in this specimen, the chondrocranium was reduced, more so than in most lacertilians (including their closest recent relatives, the varanids), but not as severely as in snakes or amphisbaenians (which have an extremely reduced chondrocranium and limbs). The new evidence suggests that the reduction in the chondrocranium in mosasaurids could be related to modification of their limbs when adapting to aquatic environments, but also that in mosasaurids, the olfactory tract was reduced, and the optic muscle insertions occurred mainly in the interorbital septum. The exceptional preservation of the chondrocranial elements in the specimen is facilitated by a gray mineralization covering them. XRD analysis and thin section observations indicated that this mineralization is composed of microcrystalline quartz and calcite. We infer that this material was produced by a partial silicification process promoted by lower pH microenvironments associated with bacterial breakdown of non-biomineralized tissues during early diagenesis.