Where: Jiangsu, China (34.5° N, 117.4° E: paleocoordinates 0.5° S, 149.4° E)
• coordinate stated in text
• small collection-level geographic resolution
When: Redlichia chinensis trilobite zone, Mantou Formation, Series 2 (521.0 - 509.0 Ma)
• "The Mantou Formation ranges from the middle Cambrian Stage 4 to the top of the Wuliuan. This lithostratigraphic unit is characterized by widely distributed siliciclastic deposits in the North China Block." Fossils come from "basal Mantou Formation (Cambrian Stage 4, Series 2)" "All specimens of Vyscystis? spinosa sp. nov. were collected from purple mudstones in the lower part of the Mantou Formation together with numerous hyoliths and trilobites (e.g. Redlichia murakamii). This level occurs in the Redlichia chinensis trilobite Zone, corresponding to the Cambrian Stage 4 in the international global stratigraphic chart "
Environment/lithology: transition zone or lower shoreface; lithified mudstone
Size class: macrofossils
Preservation: mold/impression
Collection methods: Reposited in Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (NIGPAS)
Primary reference: D.Z. Wang, M. Nohejlová, Z.X. Sun, H. Zeng, B. Lefebvre, X.L. Yang, and F.C. Zhao. 2024. First report of lepidocystid echinoderm in the Cambrian of North China: Evolutionary and Palaeobiogeographic implications. Palaeogeography, Palaeoclimatology, Palaeoecology 644:112194 [P. Novack-Gottshall/P. Novack-Gottshall]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 235095: authorized by Phil Novack-Gottshall, entered by Phil Novack-Gottshall on 01.06.2024
Creative Commons license: CC BY (attribution)
Taxonomic list
Trilobita | |
"Redlichia murakamii" = Redlichia (Pteroredlichia) murakamii
"Redlichia murakamii" = Redlichia (Pteroredlichia) murakamii Resser and Endo 1937 trilobite | |
Hyolitha | |
Brachiopoda | |
Brachiopoda indet. Cuvier 1805 | |
Lepidocystoidea | |
Vyscystis ? spinosa Wang et al. 2024 |