| Naobaogou Formation | |
|---|---|
| Stratigraphic range: | |
| Type | Geological formation |
| Sub-units | Members I-III |
| Underlies | Laowopu Formation |
| Overlies | Shiyewan Formation |
| Thickness | More than 1000 m |
| Lithology | |
| Primary | Siltstone |
| Other | Conglomerate |
| Location | |
| Country | China |
| Extent | Daqing Mountains |
The Naobaogou Formation is a geological formation in the Daqing Mountains of China. It is likely of Lopingian (Late Permian) age. It consists of three rhythms of sediment, labelled members I-III primarily of purple siltstone, but each with a thick basal conglomerate bed. It is notable for its fossil content, producing one of the most diverse Late Permian vertebrate faunas outside Russia and South Africa. [1]
| Genus | Species | Material | Notes | Images |
|---|---|---|---|---|
| Caodeyao [2] | C. liuyufengi | Partial skull, mandible, humerus | A eutherocephalian, closely related to Purlovia. | |
| Daqingshanodon [3] | D. limbus | Skull | Dicynodont | |
| Dicynodontia | Indeterminate | Partial skulls | 5 additional morphotypes in addition to Daqingshanodon and Turfanodon, 2 of which are closely related to the former taxon and 3 or 4 related to Jimusaria. [4] [5] | |
| Elginia [1] | E. wuyongae | Partial skull | Pareiasaur | |
| Euchambersia | E. liuyudongi | Skull and lower jaw | Akidnognathid therocephalian | |
| Gansurhinus [6] [7] | G. naobaogouensis | Relatively complete skeleton of an immature individual | Captorhinid | |
| Jimusaria [8] | J. monanensis | Skulls, cervicals, scapula | Dicynodontoid dicynodont | |
| Jiufengia [9] | J. jiai | Partial skull and postcranial skeleton | Akidnognathid therocephalian | |
| Laosuchus [10] | L. hun | Partial skull and postcranial skeleton | Chroniosuchian | |
| Shiguaignathus [11] | S. wangi | Partial skull | Akidnognathid therocephalian | |
| Turfanodon [5] | T. jiufengensis | Relatively complete skeleton and skulls | Dicynodontoid dicynodont |