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Statements

Subject Item
dbr:List_of_paleognath_species
dbo:wikiPageWikiLink
dbr:Continuoolithus
Subject Item
dbr:Continuoolithus
rdfs:label
Continuoolithus
rdfs:comment
Continuoolithus is an oogenus (fossil egg genus) of dinosaur egg found in the late Cretaceous of North America. It is most commonly known from the late Campanian of Alberta and Montana, but specimens have also been found dating to the older Santonian and the younger Maastrichtian. It was laid by an unknown type of theropod. These small eggs (measuring 77–123 mm (3.0–4.8 in) long) are similar to the eggs of oviraptorid dinosaurs (oofamily Elongatoolithidae), but have a distinctive type of ornamentation.
foaf:depiction
n12:Dinosaur_park_formation_fauna.png
dcterms:subject
dbc:Oldman_fauna dbc:Dinosaur_Park_fauna dbc:Egg_fossils dbc:Campanian_genera dbc:Dinosaur_reproduction dbc:Paleontology_in_Alberta dbc:Paleontology_in_Montana dbc:Prehistoric_theropods dbc:Maastrichtian_genus_extinctions dbc:Fossil_parataxa_described_in_1996 dbc:Late_Cretaceous_dinosaurs_of_North_America dbc:Milk_River_Formation dbc:Santonian_genus_first_appearances
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dbr:Troodontid dbc:Oldman_fauna dbr:Dromaeosaur dbr:Campanian dbr:Dinosaur_reproduction dbc:Egg_fossils dbr:Troodon dbr:Paleognathous dbr:Krokolithes dbr:Turtle dbr:Timeline_of_egg_fossil_research dbr:Tristaguloolithus dbr:Western_Interior_Seaway dbr:Montana dbr:Willow_Creek_Formation dbr:Lizard dbr:Caenagnathid dbr:Overbank dbr:Crocodylian dbr:Elongatoolithidae dbr:Maiasaura dbr:Floodplain dbr:Shell_membrane dbr:Tyrannosaurid dbr:Tubercuoolithus dbr:Dinosaur_Park_Formation dbr:Montanoolithus dbc:Campanian_genera dbr:Reticuoolithus dbr:Quetzalcoatlus dbr:Ornithischian dbr:Albertosaurus dbr:Porituberoolithus dbr:Sturgeon dbr:North_Horn_Formation dbr:Utah dbc:Dinosaur_reproduction dbc:Prehistoric_theropods dbc:Paleontology_in_Montana dbr:Macroelongatoolithus dbc:Maastrichtian_genus_extinctions dbr:Paralic dbr:Spheruprismatoolithus dbc:Paleontology_in_Alberta dbr:Bird dbr:Oviducts dbr:New_Mexico dbr:Thescelosaur dbr:Orodromeus dbr:Ankylosaur dbr:Belly_River_Group dbr:Hypacrosaurus dbr:Spheroolithus dbr:Champsosaurus dbr:Oogenus dbr:Prismatoolithidae dbr:Elongatoolithid dbr:Ankylosaurid dbr:Betty_Quinn dbr:Alluvial dbr:Palaios n16:Dinosaur_park_formation_fauna.png dbr:Multituberculate dbr:Triprismatoolithus dbr:Species dbr:Ceratopsid dbr:Milk_River_Formation dbr:Dinosaur_egg dbr:Pterodactyloid dbr:Pterosaur dbr:Ceratopsian dbr:Oldman_Formation dbr:Darla_Zelenitsky dbr:Montana_State_University dbr:Santonian dbr:Alberta dbc:Fossil_parataxa_described_in_1996 dbc:Late_Cretaceous_dinosaurs_of_North_America dbr:Jack_Horner_(paleontologist) dbr:Archosaur dbr:Cretaceous dbc:Santonian_genus_first_appearances dbr:Dispersituberoolithus dbr:Cf. dbr:Ornithomimid dbr:Ichnite dbr:Theropod dbr:Oviraptorid dbr:Incertae_sedis dbr:Prismatoolithus dbr:List_of_dinosaur_oogenera dbr:Fruitland_Formation dbr:Pachycephalosaur dbr:Aguja_Formation dbr:Cartilaginous dbr:Maastrichtian dbr:Karl_Hirsch dbr:Hadrosaur dbc:Milk_River_Formation dbr:Hadrosaurid dbr:North_America dbc:Dinosaur_Park_fauna dbr:Mammal
owl:sameAs
freebase:m.0g5t6sd wikidata:Q5165433 n15:4iNDP yago-res:Continuoolithus
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dbt:Palaeognathae dbt:Reflist dbt:'s dbt:Extinct dbt:Oobox dbt:Short_description dbt:Fossil_range dbt:Portal dbt:Taxonbar dbt:Convert
dbo:thumbnail
n12:Dinosaur_park_formation_fauna.png?width=300
dbp:authority
Zelenitsky, Hills & Currie, 1996
dbp:subdivision
* C. canadensis (Zelenitsky, Hills & Currie, 1996)
dbp:subdivisionRanks
Oospecies
dbp:synonyms
Spongioolithus hirschi (Bray 1999)
dbp:taxon
Continuoolithus
dbo:abstract
Continuoolithus is an oogenus (fossil egg genus) of dinosaur egg found in the late Cretaceous of North America. It is most commonly known from the late Campanian of Alberta and Montana, but specimens have also been found dating to the older Santonian and the younger Maastrichtian. It was laid by an unknown type of theropod. These small eggs (measuring 77–123 mm (3.0–4.8 in) long) are similar to the eggs of oviraptorid dinosaurs (oofamily Elongatoolithidae), but have a distinctive type of ornamentation. Continuoolithus nests would have been incubated under vegetation and sediment, unlike nests of Troodon and oviraptorids, which were incubated by brooding adults. Adaptations in the eggshell, such as high porosity and prominent ornamentation, would have helped the embryo breathe while buried. One fossil egg contains a tiny embryonic skeleton at an exceptionally young stage of development (perhaps eight to ten days old) showing the earliest stages of bone development.
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