ABSTRACT
Mawsonia, the largest actinistian, was a non-marine form common in continental and estuarine deposits of the Tithonian–Cenomanian of western Gondwana. The genus has been recently reviewed, and only two species are recognized as valid: M. gigas and M. tegamensis. Herein we describe new material that can be referred to this genus, including two basisphenoids, a coronoid, a pterygoid, a metapterygoid, one operculum, and two posparietals. The Uruguayan record represents the southernmost occurrence of Mawsonia and the Mawsoniidae in the world, and strengthens the Late Jurassic–Early Cretaceous age proposed for the unit.
ACKNOWLEDGMENTS
This is a contribution to Project CSIC-UdelaR-C028-348, “El Mesozoico de Uruguay: biotas, estratigrafía, geocronología y ambientes.” Lionel Cavin and an anonymous reviewer greatly contributed to improve an earlier version of the manuscript.
Handling editor: Charlie Underwood.