Cairanoolithus

Cairanoolithus eggs are spherical and fairly large, measuring in diameter. Tanaka et al. (2015) noted that the shell had a high rate of water vapor conductance. Therefore, they concluded that Cairanoolithus nests were covered by organic or inorganic material, similar to modern eggs with high vapor conductance. Oospecies Two oospecies of Cairanoolithus have been described: • Cairanoolithus dughii is the type oospecies. At , its eggshell is slightly thicker than that of C. roussetensis. It has slender, partially fused columnar eggshell units. Their outer surface is almost without ornamentation, and the inner surface is covered with hollows once filled by organic cores. C. dughii's eggshell exhibits an angusticanaliculate pore system, i.e. its pores are long, narrow, and straight. • Cairanoolithus roussetensis, which was formerly classified in its own oogenus, Dughioolithus, can be distinguished from C. dughii by its thinner eggshell (measuring thick), its broader eggshell units, and the relative prominence of its ornamentation. Like C. dughii, C. roussetensis typically has an angusticanaliculate pore system, though some specimens have prolatocanaliculate pores, meaning they have variable diameter across their length. Some authors consider the two oospecies to be synonymous. Cousin (2002) argued that the differences between them were due to intraspecific variation or due to taphonomy. He also described several eggshell fragments that possibly belong to an additional distinct oospecies of Cairanoolithus; however these specimens were referred to C. roussetensis by Selles and Galobart (2015). ==Classification==

}} While it was formerly considered a megaloolithid, Cairanoolithus is now considered to belong its own monotypic oofamily, Cairanoolithidae. It belongs to the dinosauroid-spherulitic basic type, a group including sauropod eggs and ornithischian eggs, but paraphyletically excluding theropod eggs. However, numerous characteristics distinguish Cairanoolithus from sauropod eggs (oofamilies Megaloolithidae and Faveoloolithidae), even though they bear superficial similarities in size and shape. Cairanoolithus's columnar eggshell units are quite unlike the fan-shaped ones seen in Megaloolithus, Faveoloolithus, or Fusioolithus. Also, its subdued ornamentation contrasts strongly with the heavily sculpted eggshells of sauropod eggs, and it has a different pore system. Eggs of ornithopods (Spheroolithidae and Ovaloolithidae), on the other hand, show much closer similarity to cairanoolithids in ornamentation and pore system. However, ornithopod eggs are typically much smaller, and the crystal structure of their eggshell units is distinct. , the possible parent of Cairanoolithus'' The cladistic analysis by Sellés and Galobart in 2015 supported an ornithischian parentage. Late Campanian to early Maastrichtian ornithischians from Southwestern Europe are restricted to rhabdodontids and the nodosaurid Struthiosaurus. When Sellés and Galobart analyzed the pelvises of Rhabdodon (the largest known rhabdodontid) and Struthiosaurus, they found that Rhabdodon could not have laid eggs as big as Cairanoolithus. On the other hand, even though Struthiosaurus was relatively small, the unique orientation of its ischia would have easily allowed it to lay eggs as large as a cairanoolithid egg. However, interpreting Cairanoolithus as the eggs of a nodosaur does raise the question of why Cairanoolithus or similar eggs have not been found in areas with a greater nodosaur abundance. == Distribution ==

Cairanoolithus is native to Southwestern Europe, including southern France and northern Iberia. Its fossils date to the late Campanian to early Maastrichtian. and from southern France (in Rousset Village, Roquehautes-Crete du Marbre, the Villeveyrac Basin, and Argelliers-Montamaud). ==Paleoecology==

The Late Cretaceous ecosystems of Europe (which was then an island archipelago) show complex mixing of taxa originating from Africa, Asia, and North America. In Southwestern Europe, Cairanoolithus co-occurs with numerous other types of fossil eggs; Megaloolithus is particularly common, are also present. Dinosaur body fossils are also common, including nodosaurids, rhabdodontids, titanosaurs, dromaeosaurids, basal iguanodontians, hadrosaurids, neoceratosaurians, and coelurosaurs. Other vertebrates include bony fish, squamates, cryptodiran turtles, alligatorids, and mammals. ==History==

The Aix Basin was first excavated for fossils in 1869 by French paleontologist Philippe Matheron. In the 1950s, Raymond Dughi and Francois Sirugue, a pair of French paleontologists working for the Museum d'Histoire Naturelle Aix-en-Provence, extensively studied the basin's fossil eggshells. They divided the eggs they had found into ten different types, but they did not describe them in detail. In the 1970s and 1980s, further work was done by the French paleontologist P. Kerourio and the German paleontologist H. K. Erben. In his 1983 doctoral thesis, M. M. Penner devised one of the early classification schemes for egg fossils. He was the first to recognize the eggs now named Cairanoolithus as a distinct type; under his classification scheme, they were called "Group 2". Following further discoveries in 2001, Géraldine Garcia and Monique Vianey-Liaud synomized the two oogenera. In 2002, French paleontologist R. Cousin took a step further and synonymized the two oospecies. Three years later, Selles and Angel Galobart published a comprehensive reanalysis of Cairanoolithus, in which they formally named the new oofamily, Cairanoolithidae, to contain Cairanaoolithus. Contrary to Cousin's conclusions, Selles and Galobart separated the oospecies C. dughii and C. roussetensis. Also, they demonstrated that Cairanoolithus was not the eggs of an ornithopod or sauropod and conjectured that it could be the eggs of a nodosaur. ==References==