Reference articles on history, science, culture and more
Encyclopedia

Quantou Formation

Geological formation in Jilin, China

The Quantou Formation is a Cretaceous Period (Mesozoic Era) geologic formation in China. It is primarily Albian in age. It has been explored for its potential as a tight oil reservoir.

Dinosaur remains are among the fossils that have been recovered from the formation.

01Fossil content

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Dinosaurs

Ornithischians

Ornithischians of the Quantou Formation
Genus Species Location Stratigraphic position Material Notes Image
Changchunsaurus C. parvus A thescelosaurid ornithischian
Helioceratops H. brachygnathus A neoceratopsian

Saurischians

Saurischians of the Quantou Formation
Genus Species Location Stratigraphic position Material Notes Image
Dromaeosauridae indet. Indeterminate A large dromaeosaurid theropod
Jiutaisaurus J. xidiensis A titanosauriform sauropod

Mammals

Mammals of the Quantou Formation
Genus Species Location Stratigraphic position Material Notes Image
Gobiconodon G. gongzhulingensis A gobiconodontid eutriconodont
Zhangolestes Z. jilinensis A zalambdalestid eutherian

Oofossils

Oofossils of the Quantou Formation
Genus Species Location Stratigraphic position Material Notes Image
Jilinoolithus J. lamellotestus Likely laid by non-avian maniraptoran theropod
Watch videos about Quantou FormationExplainers and documentaries on YouTube (opens in a new tab)

Sources and credits

This article is adapted from the Wikipedia article Quantou Formation, written by its contributors and licensed under CC BY-SA 4.0. Fathomly has changed the layout, removed citation markers, navigation and maintenance notices, and adjusted punctuation. This adapted version is shared under the same license. For references, see the original article.

Fathomly is not affiliated with or endorsed by the Wikimedia Foundation. Spotted a problem? Tell us.