The Xiguayuan Formation is an Early Cretaceous (Barremian ) geologic formation in Hebei Province of China . Fossil ornithopod tracks have been reported from the formation.[ 1] It was deposited in a shallow lacustrine setting and is noted for its hyperpycnite facies.[ 2]
Fossil content
The formation has provided the following fossils:
Ichnofossils
Insects
Bivalves
See also
References
^ Weishampel et al., 2004, pp.517-607
^ Dou et al., 2020
Bibliography
Dou, Luxing; Hou, Jiagen; Song, Suihong; Zhang, Li; Liu, Yuming; Sun, Shuang; Li, Yongqiang; Wang, Xixin; Ren, Ying Tang and Heng Tian, Xiaoxu (2020), "Sedimentary characteristics of hyperpycnites in a shallow lacustrine environment: A case study from the Lower Cretaceous Xiguayuan Formation, Luanping Basin, Northeast China" , Geological Journal , 55 (5): 3344– 3360, Bibcode :2020GeolJ..55.3344D , doi :10.1002/gj.3599 , ISSN 0072-1050
Lockley, M. G.; Matsukawa, M. (1998), "Lower Cretaceous vertebrate tracksites of East Asia. In S. G. Lucas, J. I. Kirkland, and J. W. Estep (eds.), Lower and Middle Cretaceous Terrestrial Ecosystems", New Mexico Museum of Natural History and Science Bulletin , 14 : 135– 142
Weishampel, David B. ; Dodson, Peter ; Osmólska, Halszka (2004), The Dinosauria, 2nd edition , Berkeley: University of California Press, pp. 1– 880, ISBN 0-520-24209-2 , retrieved 2019-02-21