The Dongpo Formation can be found within the North China Craton, currently amongst the oldest known cratons in the world, alongside its southern edge. The formation itself is primarily composed of yellowish-green shale, siltstone, and fine-grained sandstone.[1]
The formation is dominated by macroalgae forms, like Glomulus, alongside tubular forms such as Wutubus and Shaanxilithes. There are also some Ediacaran-type fossils, and some rare trace fossils, all of which has helped to constrain the age of the formation to the terminal Ediacaran, between 550Ma and 538.8Ma.[1]
12345678910111213Wang, Xin; Zhang, Xingliang; Dai, Tao; Liu, Wei; Zhang, Yuan; Li, Luoyang (March 2026). "New occurrence of a postglacial Ediacaran macrofossil assemblage from North China and its evolutionary implication". Precambrian Research. 434: 107992. doi:10.1016/j.precamres.2025.107992.{{cite journal}}: CS1 maint: article number as page number (link)
↑Wang, Xin; Zhang, Xingliang; Liu, Wei (October 2021). "Biostratigraphic constraints on the age of Neoproterozoic glaciation in North China". Journal of Asian Earth Sciences. 219: 104894. doi:10.1016/j.jseaes.2021.104894.{{cite journal}}: CS1 maint: article number as page number (link)
↑Chumakov, N. M. (August 2009). "The Baykonurian glaciohorizon of the Late Vendian". Stratigraphy and Geological Correlation. 17 (4): 373–381. doi:10.1134/S0869593809040029.
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