Porituberoolithus is an oogenus of dinosaur egg found in the late Campanian Oldman Formation and Dinosaur Park Formation of Alberta, the Fossil Forest Member of the Fruitland Formation in New Mexico, the Upper Shale Member of the Aguja Formation in Texas and Cerro del Pueblo Formation (Difunta Group) of Mexico. It was originally described as distinct from the Elongatoolithids on the basis of its ornamentation, but it was listed as a member of that oofamily by Wang et al. 2010.[1][2] It is very similar to Subtiliolithus, but has a thicker shell.[2]
^Q. Wang, X.-L. Wang, Z.-K. Zhao and Y.-G. Jiang. 2010. A new oogenus of Elongatoolithidae from the Upper Cretaceous Chichengshan Formation of Tiantai Basin, Zhejiang Province. Vertebrata PalAsiatica 48(2):111-118
^ abD. K. Zelenitsky, L. V. Hills, and P. J. Currie. (1996). Parataxonomic classification of ornithoid eggshell fragments from the Oldman Formation (Judith River Group; Upper Cretaceous), southern Alberta. Canadian Journal of Earth Sciences 33:1655-1667
Porituberoolithus is an oogenus of dinosaur egg found in the late Campanian Oldman Formation and Dinosaur Park Formation of Alberta, the Fossil Forest...
Continuoolithus, eggs of Hypacrosaurus, Spheroolithus, Prismatoolithus, Porituberoolithus, Tristaguloolithus, and Dispersituberoolithus are also known. Dinosaurian...
to prevent water loss through the eggshell. Tipoolithus resembles Porituberoolithus in its microstructure and thickness, and resembles Subtiliolithus...
Indeterminate cf. Paronychodon cf. P. lacustris Theropoda incertae sedis Porituberoolithus cf. P. warnerensis One eggshell fragment Laid by a theropod Prismatoolithus...
Paraelongatoolithus, Undulatoolithus, and Rodolphoolithus. Also, Porituberoolithus and Continuoolithus are occasionally included in Elongatoolithidae...
as thick as the cone layer. Paraelongatoolithus is very similar to Porituberoolithus, but differs in the ornamentation. Even though the sole Paraelongatoolithus...
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