The Allen Formation is a geological formation in Argentina whose strata date back to the Late Cretaceous (middle Campanian to late Maastrichtian).[1][2] Dinosaur remains are among the fossils that have been recovered from the formation.[3] Indeterminate chelid remains and other vertebrates have also been discovered in this formation.[4]
The interpreted sedimentary paleoenvironments range from purely continental such as ephemeral lacustrine, aeolian and fluvial systems to coastal marine paleoenvironments with development of estuaries and tidal flats, followed by a lagoon sedimentary stage from marsh to sea with carbonate precipitation in an area protected from waves, ending with a retraction leading to the accumulation of evaporites.[5]
Armas and Sánchez performed a detailed facies analysis of the formation in 2015, where the authors concluded the formation represents a hybrid coastal system
of tidal flats, dominated by Atlantic ingressions, with a large storm influence in some areas linked to aeolian systems.[6]
A study of pollen found in outcrops of the middle member of the Allen Formation supported a late Maastrichtian age for these layers.[2]
A fragmentary skeleton including parts of the skull, lower jaw, a few neck and torso vertebrae, some ribs, a humerus, and assorted bones from both legs
A holotype consists of a mid-dorsal vertebra, both scapulocoracoids, left tibia and femur, left pubis articulated with the pubic peduncle of the ilium, the anterior blade of the left ilium, and two partially preserved eggs.