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[dinosaur] Eggshells reveal dinosaur diversity in Willow Creek Formation from latest Cretaceous of Alberta

Ben Creisler

A new paper:

Darla K. Zelenitsky, François Therrien, Kohei Tanaka, Philip John Currie & Christopher L. DeBuhr (2016)
Latest Cretaceous eggshell assemblage from the Willow Creek Formation (upper Maastrichtian-lower Paleocene) of Alberta, Canada reveals higher dinosaur diversity than represented by skeletal remains.
Canadian Journal of Earth Sciences (advance online publication)
doi: 10.1139/cjes-2016-0080

The Willow Creek Formation (upper Maastrichtian-lower Paleocene) of southwestern Alberta is a poorly fossiliferous formation that preserves a low end-Cretaceous dinosaur diversity compared to most correlative terrestrial deposits in the North American Western Interior. Although only three dinosaur taxa are known from skeletal remains (Tyrannosaurus rex, Hadrosauridae indet., and Leptoceratopsidae indet.), study of hundreds of dinosaur eggshells recovered from several sites in the formation reveals the presence of a more diverse dinosaur assemblage. Morphological and histological analyses of the eggshells indicate the presence of at least seven dinosaur ootaxa (Continuoolithus, Montanoolithus, Porituberoolithus, Prismatoolithusspp., Spheroolithus spp.). These ootaxa are referable to at least two ornithopod and five small theropod species, likely including dromaeosaurids, oviraptorosaurs, and troodontids. When considering the taxonomic affinity of eggshells and skeletal remains, the present study triples the known dinosaur diversity of the Willow Creek Formation, increasing the number of dinosaurs from three to at least nine species. Probable ornithopod eggshells comprise most of the eggshells preserved, although small theropods were likely an important component of the Willow Creek ecosystem as most ootaxa can be ascribed to these dinosaurs. Although fossil bones are rarely found in the Willow Creek Formation, fossil eggshells are common compared to most other dinosaur-bearing formations in Alberta. The caliche-bearing deposits, indicative of arid to semi-arid conditions, typical of the formation were likely conducive to the preservation of calcareous eggshells.