Allen Formation


The Allen Formation is a geological formation in Argentina whose strata date back to the Late Cretaceous (middle Campanian to early Maastrichtian. Dinosaur remains are among the fossils that have been recovered from the formation. Indeterminate chelid remains and other vertebrates have also been discovered in this formation.

Description

Uliana and Dellapé defined the formation's stratotype in 1981 in the eastern area of the Bajo de Añelo, where the relation between the base and top is clearly exposed. The deposits are mostly clastic, interbedded with banks of limestone and layers of anhydrite, which were defined as continental and shallow marine facies associated with semiarid conditions.
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.
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.
A study of pollen found in outcrops of the middle member of the Allen Formation supported a late Maastrichtian age for these layers.

Fossil content

Dinosaurs

Dinosaur eggs are known from the formation.

Ornithischians

; Ankylosaurs
GenusSpeciesLocationStratigraphic positionMaterialNotesImages
AnkylosauriaIndeterminateArriagada FarmTwo teeth, five osteoderms, and a partial sacrumFossil remains possibly belonging to a parankylosaur distinct from Patagopelta
PatagopeltaP. cristataSalitral Moreno localityLowerTooth, three posterior dorsal vertebrae, caudal vertebrae, two caudal centra, right femur, partial cervical half ring, and osteodermsA possible parankylosaur

; Hadrosaurs
GenusSpeciesLocationStratigraphic positionMaterialNotesImages
BonapartesaurusB. rionegrensisSalitral Moreno and Islas Malvinas.LowerA partial skeleton.A hadrosaur
KelumapusauraK. machiCerro Matadero, Arriagada FarmUpperPartial skull, a cervical vertebrae, several sacrals, sternal rib and sternal plate, and multiple referred specimens found in a bonebedA saurolophine hadrosaur
LapampasaurusL. cholinoiIslas MalvinasLowerElements of the axial and appendicular skeleton of a subadult individualA hadrosaur
WillinakaqeW. salitralensisSalitral Moreno site.LowerA right premaxilla.A saurolophine hadrosaur

Saurischians

;Sauropods
GenusSpeciesLocationStratigraphic positionMaterialNotesImages
AeolosaurusIndeterminateLowerA titanosaur

Bonatitan

B.reigi
LowerBraincases, caudal vertebrae, and several limb elementsA titanosaur
MenucocelsiorM. arriagadaiLowerSeventeen caudal vertebrae and several appendicular bones: a right humerus, a left fibula and some metapodial.A titanosaur
PanamericansaurusP. schroederi"Five tail vertebrata, sacral vertebrae, left humerus and rib fragments"A titanosaur
Pellegrinisaurus?P. powelliLower "Dorsal and caudal vertebrae, partial femur"A titanosaur
RocasaurusR. munioziMiddle"Partial postcranial skeleton"A titanosaur
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------
------