Where: Guizhou, China (27.5° N, 108.2° E: paleocoordinates 7.8° N, 125.8° E)
• coordinate based on political unit
• basin-level geographic resolution
When: Xiangshuyuan Formation, Llandovery (443.4 - 433.4 Ma)
• The lowest bed of the formation, about 2 m thick. Beds overlie Lungmachi Formation, with graptolitic fauna, and are overlain by coral-brachiopod-rich sequence of Xiangshuyuan Formation.
• bed-level stratigraphic resolution
Environment/lithology: marine; limestone and calcareous mudstone
Primary reference: Y. Wang, A. J. Boucot, J.Y. Rong and X.C. Yang. 1987. Community paleoecology as a geologic tool: the Chinese Ashgillian-Eifelian (latest Ordovician through early Middle Devonian) as an example. Geological Society of America Special Paper 211:1-100 [M. Foote/M. Foote/M. Foote]more details
Purpose of describing collection: paleoecologic analysis
PaleoDB collection 25869: authorized by Michael Foote, entered by Michael Foote on 26.09.2002
Creative Commons license: CC BY (attribution)
Taxonomic list
Rhynchonellata | |
Zygospiraella sp. Nikiforova 1961 | |
Eospirifer sp. Schuchert 1913 | |
Stromatoporoidea | |
| |
Anthozoa | |
| |
Brachyelasma sp. Lang et al. 1940 horn coral |