The Miaogou Formation is a geological formation in Inner Mongolia, north China. While its absolute age is uncertain, it has been estimated to represent Early Cretaceous (around Aptian–Albian) sediments based on the faunal composition. Dinosaur remains are among the fossils that have been recovered from the formation.
History
The primary fossil-producing outcrop of the Miaogou Formation is the Maortu locality, which was discovered in 1959 by a joint expedition of Chinese and Russian paleontologists.[3] Initial reports of the locality's fauna incorrectly assigned the fossils to either the Ulansuhai or Dashuigou formations, but a later discussion corrected this.[4]
Paleoenvironment
Analysis of the formation's geology indicates that it represents a hot, humid environment with large lake systems.[3] The formation's lower member preserves alluvial fan to braided stream deposits, while the upper member preserves meandering stream and lacustrine deposits.[5]
^ abZhang, Shuai; Liu, Lihui; Liu, Qinfu; Zhang, Bingjie; Qiao, Zhichuan; Teppen, Brian J. (February 2021). "Genesis of Palygorskite in the Neogene Baiyanghe Formation in Yangtaiwatan Basin, Northwest China, Based on the Mineralogical Characteristics and Occurrence of Enriched Trace Elements and Ree". Clays and Clay Minerals. 69 (1): 23–37. doi:10.1007/s42860-020-00104-7. ISSN0009-8604.
^Liu, Lihui; Zhang, Shuai; Liu, Qinfu; Liu, Linsong; Deng, Youjun (September 2021). "Palaeoclimate, palaeosalinity and redox conditions control palygorskite claystone formation: an example from the Yangtaiwatan Basin, northwest China". Clay Minerals. 56 (3): 210–221. doi:10.1180/clm.2022.1. ISSN0009-8558.
^Vickaryous, Matthew K; Russell, Anthony P; Currie, Philip J; Zhao, Xi-Jin (2001-12-01). "A new ankylosaurid (Dinosauria: Ankylosauria) from the Lower Cretaceous of China, with comments on ankylosaurian relationships". Canadian Journal of Earth Sciences. 38 (12): 1767–1780. doi:10.1139/e01-051. ISSN0008-4077.