Where: Xinjiang, China (39.7° N, 78.8° E: paleocoordinates 11.6° S, 49.4° E)
• coordinate estimated from map
• local area-level geographic resolution
When: Upper Member (Bachu Formation), Tournaisian (358.9 - 346.7 Ma)
• member-level stratigraphic resolution
Environment/lithology: lithified, argillaceous limestone and lithified limestone
•
•"The Upper member of the Bachu Formation, consisting of bioclastic limestone, is characterized by the apparence of abundant brachiopods and conodonts."
Reposited in the NIGPAS
• In addition to the Nanjing Institue of Geology & Palaeontology, speciens are housed at the Department of Invertebrate Palaeontology, Museum of Victoria (NMVP), Australia.
Primary reference: Z. Q. Chen and G. R. Shi. 1999. Latest Devonian (Famennian) to earliest Carboniferous (Tournaisian) brachiopods from the Bachu Formation of the Tarim Basin, Xinjiang Province, northwest China. Rivista Italiana di Paleontologia e Stratigrafia 105(2):231-250 [N. Heim/N. Heim]more details
Purpose of describing collection: biostratigraphic analysis
PaleoDB collection 58134: authorized by Noel Heim, entered by Noel Heim on 23.01.2006
Creative Commons license: CC BY (attribution)
Taxonomic list
•
•Abundance categories are:
•1 = 1 to 5 specimens
•2 = 5 to 9 specimens
•3 = 10 to 20 specimens
•4 = more than specimens
•**The overlap of categories 1 and 2 is recorded here as it was given in the text.
Rhynchonellata | |
Strophomenata | |
Schuchertella guizhouensis Yang 1964 | |
Conodonta | |
Spathognathodus stabilis conodont | |
"Neoprioniodus barbatus" = Idioprioniodus
"Neoprioniodus barbatus" = Idioprioniodus conodont | |
Bispathodus aculeatus, Siphonodella cf. sulcata, "Polygnathus communis" = Neopolygnathus communis, Polygnathus cf. inornatus
Siphonodella cf. sulcata conodont
"Polygnathus communis" = Neopolygnathus communis Branson and Mehl 1934 conodont Polygnathus communis communis
Polygnathus cf. inornatus conodont | |
"Hindeodella germana" = Ozarkodina
"Hindeodella germana" = Ozarkodina conodont |