Where: Russian Federation (55.7° N, 51.7° E: paleocoordinates 28.4° N, 44.0° E)
• coordinate estimated from map
• outcrop-level geographic resolution
When: Lingula Shale Member (Baitugan Formation), Roadian (272.3 - 268.8 Ma)
• Beds numbered 1-3 from bottom to top; bed 1 is Ufimian, while beds 2 and 3 (which contain most of the fossils) are Lower Kazanian, of the Baitugan Formation (Nurgaliev et al. 2015)
•Overlain by the beds of outcrop S7 (Collection no. 197600)
Environment/lithology: marine; shale
•Package 1 Interval 0.0 - 10.0m Thickness 10.0m
•Reddish-brown, calcareous, irregularly bedded siltstones and shales with interbeds of yellowish-brown polymict sandstones.
•[Lower Kazanian Substage - Baitugan Beds - Lingula Shales Member]
•Package 2 Interval 10.0m - 10.5m Thickness 0.5m
•Thin alternation of grey and red shales.
•Package 3 Interval 10.5 - 21.0m Thickness 10.5m
•Bluish-grey, thinly bedded, plat shales with numerous remains of the inarticulate brachiopod Lingula orientalis, and ostracods. The rock contains bivalves and fish scales." (Nurgaliev et al. 2015)
Size class: macrofossils
Primary reference: D. K. Nurgaliev, V. V. Silantiev, and S. V. Nikolaeva. 2015. Type and reference sections of the Middle and Upper Permian of the Volga and Kama River Regions: A Field Guidebook of XVIII International Congress on Carboniferous and Permian. 1-208 [A. Dunhill/B. Allen/P. Wagner]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 197599: authorized by Alex Dunhill, entered by Bethany Allen on 17.11.2018
Creative Commons license: CC BY (attribution)
Taxonomic list
| Lingulata | |
| Bivalvia | |
|
Pseudobakewellia ceratophagaeformis Noinskyi 1913 oyster | |
|
Schizodus rossicus de Verneuil 1845 clam | |
| Ostracoda | |
|
Cavellina sp. Coryell 1928 ostracod | |
|
Healdianella sp. ostracod | |
| Protohaploxypinus | |