Microfacies and foraminifers of the Tulian horizon (the Visean substage, Lower Carboniferous) of the southeast of the East European platform and the Southern Urals
https://doi.org/10.18599/grs.2025.3.26
Abstract
The article presents the characteristics of microfacies and foraminiferal complexes of the Tulian horizon of the Visean substage in sections of the Preduralskaya-106 and Oktyabrskaya-106 boreholes in the Eastern part of the Volga-Ural region and the Sikaza 2 section of the western slope of the Southern Urals. The age of the deposits corresponds to the foraminiferal zone Endothyranopsis compressa – Paraarchaediscus koktjubensis of Russia. Based on the study of the microstructures of carbonate rocks, six microfacies (MF) are distinguished, differing in component composition and textures. Limestones are mainly fine-grained polybioclastic packstones. The main components (grains) are the remains of tubular algae, foraminifers, echinoderms (mainly crinoids), ostracods, brachiopods, rarely bryozoans, as well as calcispheres, peloids and intraclasts. The deposits were formed in the conditions of an open shallow shelf of the ramp type with different hydrodynamics. An analysis of the distribution of microfacies in sections and the relationship of foraminifer complexes with them is given.
Keywords
About the Authors
E. Yu. BashlykovaRussian Federation
Elena Yu. Bashlykova – Junior Researcher
16/2, Karl Marks st., Ufa, 450077, Ufa
E. N. Gorozhanina
Russian Federation
Elena N. Gorozhanina – Cand. Sci. (Geology and Mineralogy), Senior Researcher
16/2, Karl Marks st., Ufa, 450077, Ufa
E. I. Kulagina
Russian Federation
Elena I. Kulagina – Dr. Sci. (Geology and Mineralogy), Chief Researcher
16/2, Karl Marks st., Ufa, 450077, Ufa
References
1. Aleksseev A.S., Nikolaeva S.V., Goreva N.V., Donova N.B., Kossovaya O.L., Kulagina E.I., Kucheva N.A., Kurilenko A.V., Kutygin R.V., Popeko L. I. and Stepanova T.I. (2022). Russian regional Carboniferous stratigraphy. In: Lucas, S. G., Schneider, J. W., Wang, X. and Nikolaeva, S. (eds). The Carboniferous Timescale. Geological Society, London, Special Publications, 512(1), pp. 49–117. https://doi.org/10.1144/sp512-2021-134
2. Bashlykova E.Yu., Kulagina E.I. (2020). Late Viséan Foraminiferal Assemblages of the 106 Oktyabrskaya Borehole, South-East of the East European Platform. Proc. Kazan Golovkinsky Young Scientists’ Stratigraphic Meeting, 2020. Sedimentary Earth Systems: Stratigraphy, Geochronology, Petroleum Resources. October 26-30, Kazan, Russia. Kazan: KPFU, pp. 9–13. http://dx.doi.org/10.26352/E922_KAZAN2020
3. Conil R., Groessens E., Laloux M., Poty E., Tourneur F. (1991). Carboniferous guide foraminifera, corals and conodonts in the FrancoBelgian and Campine basins: their potential for widespread correlation. Cour. Forschungsinst. Senckenberg, 130, pp. 15–30.
4. Cózar P., Vachard D., Izart A., Said I., Somerville I., Rodríguez S., Coronado I., El Houicha M., Ouarhache D. (2020). Lower-middle Viséan transgressive carbonates in Morocco: Palaeobiogeographic insights. Journal of African Earth Sciences, 168, pp. 1–27. http://dx.doi.org/10.1016/j.jafrearsci.2020.103850
5. Dunham R.J. (1962). Classification of carbonate rocks according to depositional texture. Classification of Carbonate Rocks. A Symposium: Am. Assoc. Pet. Geol. Mem. 1. Tulsa; Oklahoma: AAPG, pp. 108–121. https://doi.org/10.1306/M1357
6. Flügel E. (2010). Microfacies of Carbonate Rocks. Berlin: Springer, 984 p. https://doi.org/10.1007/978-3-642-03796-2
7. Fortunatova N.K., Zaitseva E.L., Bushueva M.A., Ermolova T.E., Mikheeva A.I., Stupak A.A., Baranova A.V., Kononova L.I., Mamontov D.A., Kharchenko S.I., Avdeeva A.A., Kanev A.S., Evdokimov N.V., Goncharov E.O., Zorin A.B., Belousov G.A., Gorodkov A.B., Shishkina T.Yu., Volodina A.G., Kholmyanskaya N.Yu., Kravchenko M.S., Afanasyeva M.S., Evdokimova I. (2023). Stratigraphy of the lower Carboniferous of the Volga-Ural subregion (materials for updating the stratigraphic scheme). Moscow: VNIGNI, 288 p. (In Russ.)
8. Gorozhanina E.N. (2010). Types of carbonate platforms of the Southern Urals and the Urals, their connection with oil and gas potential. Geology, minerals and problems of geoecology of Bashkortostan, the Urals and adjacent territories: Proc. 8th Interregional Sci. and Pract. Conf. Ufa, November 17-18. Ufa: Designpoligrafservice, pp. 188–191. (In Russ.)
9. Gorozhanina E.N., Bashlykova E.Yu., Kulagina E.I. (2021). Microfacies of the Tulian Horizon (Visean Stage, Lower Carboniferous) of the Sikaza 2 section (Southern Urals, Russia).
10. Uchenye Zapiski Kazanskogo Universiteta. Seriya Estestvennye Nauki, 163(3), pp. 414–429. (In Russ.) doi: 10.26907/2542-064X.2021.3.414-429
11. Guidebook to the carboniferous sections of the Southern Urals (Bashkiria). (1975). Moscow: Nauka, 183 p. (In Russ.)
12. Guidebook to the Southern Urals. Excursion 047. (1984). Upper Paleozoic of the Southern Urals. 27th International. Geol. Congress. Moscow: Nauka, 136 p. (In Russ.)
13. Guidebook of Excursion for the Paleozoic and Upper Precambrian Sections of the Western slope of the Southern Urals and Preuralian Regions. (1995).
14. Comp. by: V.L. Kozlov, Z.A. Sinitsyna, E.I. KuIagina, V.N. Pazukhin, V.N. Puchkov, N.M. Kochetkova, A.N. Abramova, T.V. Klimenko, N.D. Sergeeva; Ed. by V.N. Puchkov. Ufa, 165 p.
15. Kulagina E.I., Kochetkova N.M., Byvsheva T.V. (1988). On the paleontological characteristics of the Lower-Middle Visean deposits of the Orenburg region. Biostratigraphy of the Devonian and Carboniferous of the Urals. Ufa: BFAN USSR, pp. 42–58. (In Russ.)
16. Kulagina E.I., Klimenko T.V. (2014). Foraminifera complexes of the Upper Visean sublayer of the Cikaza River basin on the Western slope of the Southern Urals. Geologicheskiy sbornik, 11, pp. 48–57. (In Russ.)
17. Kulagina E. (2022). Foraminiferal sequence of the middle-upper Viséan (Mississippian) of the Sikasya River Valley in the South Urals and correlation with the Belgian standard. Paläontologische Gesellschaft, 96(3), pp. 495–516. https://doi.org/10.1007/s12542-021-00556-9
18. Makhlina M.H., Zhulitova V.E. (1984). On the detailed dissection of the Tulian horizon in the strato-region. Izvestiya vuzov. Geologiya i razvedka, 12, pp. 3–11. (In Russ.)
19. Makhlina M.H., Vdovenko M.V., Alekseev A.S., Exsheva T.V., Donakova D.M., Zhulitova V.E., Kononova L.I., Umnova N.M., Shik E.M. (1993). The lower Carboniferous of the Moscow syneclise and Voronezh anteclise. Moscow: Nauka, 221 p. (In Russ.)
20. Postoyalko M. V., Garan I.M. (1972). Fauna of the Pesterkovsky horizon of the lower vise of the western slope of the Middle Urals. Stratigraphy and foraminifera of the Lower Carboniferous of the Urals, 197, pp. 3–19. (In Russ.)
21. Poty E., Devuyst F.-X., Hance L. (2006). Upper Devonian and Mississippian foraminiferal and rugose coral zonations of Belgium and Northern France: a tool for Eurasian correlations. Geological Magazine, 143, pp. 829–857. https://doi.org/10.1017/S0016756806002457
22. Puchkov V.N. (2000). Paleogeodynamics of the Southern and Middle Urals. Ufa: Dauria, 146 p. (In Russ.)
23. Resolutions of the Interdepartmental Stratigraphic Committee and its standing committees. (2008). The state of study of Precambrian and Phanerozoic stratigraphy in Russia. Tasks of further research, is. 38. St. Petersburg: VSEGEI Publishing House, 131 p. (In Russ.)
24. Silantyev V.V., Validov M.F., Miftakhutdinova D.N., Nurgalieva N.G., Korolev E.A., Ganiev B.G., Lutfullin A.A., Shumatbayev K.D., Khabipov R.M., Sudakov V.A., Akhmadullina Yu.A., Golod K.A. Leontiev A.A., Shamsiev R.R., Nikonorova D.A., Krikun S.S., Noikin M.V., Abdullina E.A. (2023). Visean terrigenous sediments of the South Tatar Arch (Volga-Urals oil and gas bearing province) – multifacial filling of the karst surface of the Tournaisian isolated carbonate platform. Georesursy = Georesources, 25(4), pp. 3–28. (In Russ.) https://doi.org/10.18599/grs.2023.4.1
25. Sinitsyna Z.A., Sinitsyn I.I. (1975). Stratigraphy of the Lower carboniferous deposits of the Sikaza river area on the western slope of the Southern Urals. Stratigraphy and geology of the carboniferous of the Southern Urals and the eastern margin of the Russian Platform. Ufa: BFAN USSR, pp. 40–57. (In Russ.)
26. Sinitsyna Z.A. (1975). Section of the lower Carboniferous on the Sikaza river. Guide to the carboniferous sections of the Southern Urals (Bashkiria). VIII International Congress on Stratigraphy and Geology of Carboniferous. Moscow: Nauka, pp. 32–45. (In Russ.)
27. Stratigraphic schemes of the Urals (Precambrian, Paleozoic) (1993). Yekaterinburg: Ural. geol.- filming. expedition, 152 p. (In Russ.)
28. The decision of the Interdepartmental Regional Stratigraphic Meeting on the Middle and Upper Paleozoic of the Russian Platform with regional stratigraphic schemes. Leningrad. 1988 (1990). The carboniferous system. Leningrad: VSEGEI Publishing House, 41 p. (In Russ.)
29. Vdovenko M.V. (2009). The Tulian horizon of the Lower Carboniferous and its analogues in the stratigraphic scheme of Eastern Ukraine. Collection of scientific papers of the Institute of Geological Sciences of Ukraine, pp. 43–50. (In Russ.)
30. Wilson J.L. (1980). The carbonate facies in the geological history. Moscow: Nedra, 463 p. Wright V.P., Vanstone S.D. (2001). Onset of Late Palaeozoic glacioeustasy and the evolving climates of low latitude areas: a synthesis of current understanding. Journal of the Geological Society, 276, pp. 579–582. https://doi.org/10.1144/jgs.158.4.579/
31. Zaitseva E.L., Sakhnenko K.V. (2018). Facies Features of The Distribution Of Late Visean Foraminifera Of The Volga-Ural Region. Proc. XVII All–Russian Micropaleontological Meeting “Modern micropaleontology - problems and prospects”, Kazan, September 24–29, 2018. Moscow: PIN RAS, pp. 44–48. (In Russ.)
32. Zaytseva E.L., and Sakhnenko K.V. (2019). Facial Features of the Distribution of Late Viséan Foraminifers in the Volgа–Ural Region. Paleontological Journal, 53(9), pp. 961–965. https://doi.org/10.1134/S0031030119090193
Review
For citations:
Bashlykova E.Yu., Gorozhanina E.N., Kulagina E.I. Microfacies and foraminifers of the Tulian horizon (the Visean substage, Lower Carboniferous) of the southeast of the East European platform and the Southern Urals. Georesursy = Georesources. 2025;27(3):179-194. (In Russ.) https://doi.org/10.18599/grs.2025.3.26