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Biostratigraphy and lithostratigraphy of the Mid-Carboniferous boundary beds in the Muradymovo section (South Urals, Russia)

Published online by Cambridge University Press:  08 October 2013

ELENA KULAGINA ,
SVETLANA NIKOLAEVA ,
VLADIMIR PAZUKHIN  and
NATALIYA KOCHETOVA
ELENA KULAGINA*
Affiliation:
Institute of Geology, Ufa Scientific Centre, Russian Academy of Sciences, Karla Marksa ul.16/2, Ufa 450077, Russia
SVETLANA NIKOLAEVA
Affiliation:
Borissiak Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya ul. 123, Moscow 117997, Russia International Commission on Zoological Nomenclature, Natural History Museum, London SW7 5BD, UK
VLADIMIR PAZUKHIN
Affiliation:
Institute of Geology, Ufa Scientific Centre, Russian Academy of Sciences, Karla Marksa ul.16/2, Ufa 450077, Russia
NATALIYA KOCHETOVA
Affiliation:
Institute of Geology, Ufa Scientific Centre, Russian Academy of Sciences, Karla Marksa ul.16/2, Ufa 450077, Russia
*
†Author for correspondence: kulagina@ufaras.ru
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Abstract

The uninterrupted succession of the Mississippian–Pennsylvanian boundary beds in the Muradymovo section in the South Urals contains diverse fossils and has a high correlative potential. The Muradymovo section is located in the Zilair Megasynclinorium (ZM), which belongs to the West Uralian Subregion and displays carbonate-siliciclastic deep-water facies of the Bukharcha Formation, which is partly Serpukhovian (Kosogorian, Protvian and Yuldybaevian) and partly Bashkirian (Syuranian). In the southern ZM, the lower part of the formation contains argillaceous carbonates with beds of shale and siltstone, subordinate clastic limestones and limestone breccia, while the upper part is mostly limestone with cherty interbeds. In the north of the ZM, the formation mainly consists of limestone. The Muradymovo succession contains no identifiable gaps in the Mid-Carboniferous Boundary (MCB) portion and has a succession of foraminiferal, conodont, ammonoid and ostracod zones. The MCB in this section coincides with the base of the Bogdanovkian and is defined by the entry of Declinognathodus noduliferus. This level falls within the upper part of the foraminiferal Monotaxinoides transitorius Zone, is near the base of the ammonoid Homoceras–Hudsonoceras Genozone and can be correlated worldwide.

Keywords

Mid-Carboniferous boundarybiostratigraphyammonoidsmicrofossilsSouth Urals
Type
Original Articles
Information
Geological Magazine , Volume 151 , Issue 2 , March 2014 , pp. 269 - 298
Copyright
Copyright © Cambridge University Press 2013 

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References

Aizenverg, D. E., Astakhova, T. V., Berchenko, N. E., Brazhnikova, N. E., Vdovenko, M. V., Dunaeva, N. N., Zernetzkaja, N.V., Poletaev, V. J. & Sergeeva, M.T. 1983. Upper Serpukhovian Substage in the Donets Basin (Paleontological characterization). Kiev: Naukova Dumka, 164 pp.Google Scholar
Alvarez-marron, J., Brown, D., Perez-Estaun, A., Puchkov, V. & Gorozhanina, Y. 2000. Accretionary complex structure and kinematics during Paleozoic arc-continent collision in the southern Urals. Tectonophysics 325, 175–91.CrossRefGoogle Scholar
Baesemann, J. F. & Lane, H. R. 1985. Taxonomy and evolution of the genus Rhachistognathus Dunn (Conodonts; Late Mississippian to early middle Pennsylvanian). Courier Forschungsinstitut Senckenberg 74, 93–136.Google Scholar
Bisat, W. S. 1924. The Carboniferous goniatites of the North of England and their zones. Proceedings of the Yorkshire Geological Society 20, 40–124.Google Scholar
Bisat, W. S. 1928. The Carboniferous Goniatite Zones of England and their Continental Equivalents. Heerlen: Congrès de Stratigraphie Carbonifère, 117–33.Google Scholar
Brady, H. B. 1873. On Archaediscus karreri, a new type of Carboniferous foraminifera. The Annals and Magazine of Natural History, Series 4 (12), 286–90.Google Scholar
Brady, H. B. 1876. A Monograph of Carboniferous and Permian Foraminifera (the Genus Fusulina Excepted). London: Palaeontographical Society, 166 pp.Google Scholar
Branson, E. B. & Mehl, M. G. 1941. New and little known Carboniferous conodont genera. Journal of Paleontology 15, 97–106.Google Scholar
Brazhnikova, N. E. & Potievskaja, P. D. 1948. Results of the examination of foraminifers from borehole samples at the western boundary of the Donets Basin (in Ukrainian), Trudy Instituta Geologicheskikh Nauk, v.1, vyp. 2 (Collection of Works in Paleontology and Stratigraphy), 76–103.Google Scholar
Brazhnikova, N. E. & Vdovenko, M. V. 1983. Foraminifers, pp. 42–86. In Verkhneserpukhovskii pod’’yarus Donetskogo basseina (eds Aisenverg, D. E., Astakhova, T. V., Berchenko, O. I., Brazhnikova, N. E., Vdovenko, M. V., Dunaeva, N. N., Zernetzkaya, N. V., Poletaev, V. I. & Sergeeva, M. T.), Akademiya Nauk Ukrainskoi SSR, Institut Geologicheskikh Nauk, Kiev, Naukova Dumka.Google Scholar
Brazhnikova, N. E. & Jarzeva, M. V. 1956. On the evolution of the genus Monotaxis . Voprosy Mikropaleontologii, Akademiya Nauk SSSR, Otdelenie Geologo-Geograficheskikh Nauk, Geologicheskiy Institut 1, 62–8.Google Scholar
Brenckle, P. L. 1991. Foraminiferal division of the Lower Carboniferous/Mississippian in North America. In Intercontinental correlation and division of the Carboniferous System (eds Brenckle, P. L. & Manger, W. L.), 65–78. Courier Forschungsinstitut Senckenberg 130.Google Scholar
Brenckle, P. L. 2005. A Compendium of Upper Devonian-Carboniferous Type Foraminifers from the Former Soviet Union. Cushman Foundation for Foraminiferal Research, Special Publication no. 38, 153 pp.Google Scholar
Brenckle, P. L., Baesemann, J. F., Lane, H. R., West, R. R., Webster, G. D., Langenheim, R. L., Brand, U. & Richards, B. C. 1997. Arrow Canyon, the Mid-Carboniferous boundary stratotype. In PaleoForams 97 Guidebook, pp. 13–32. Post-Conference field trip to the Arrow Canyon Range, southern Nevada, USA. Cushman Foundation for Foraminiferal Research Supplement to Special Publication no. 36, 13–32.Google Scholar
Brenckle, P. L. & Grelecki, C. J. 1993. Type Archaediscacean Foraminifers (Carboniferous) from the Former Soviet Union and Great Britain. Cushman Foundation for Foraminiferal Research, Special Publication no. 30, 59 pp.Google Scholar
Cooper, Ch. L. 1941. Chester ostracodes of Illinois. Illinois State Geological Survey, Report of Investigations III. no. 77, 5–101.Google Scholar
Cordell, R. J. 1952. Ostracodes from the Upper Pennsylvanian of Missouri. Part I: The Family Bairdiidae. Journal of Paleontology 26(1), 74–112.Google Scholar
Durkina, A. V. 1959. Foraminifers of the lower Carboniferous deposits of the Timan-Pechora Province. Trudy Vsesoyuznogo Neftyanogo Nauchno-Issledovatel'skogo Geologo-Razvedochnogo Instituta (VNIGRI), Mikrofauna SSSR, Sbornik 10, Vypusk 155, 132–389.Google Scholar
Ellison, S. P. Jr. & Graves, R. W. Jr. 1941. Lower Pennsylvanian (Dimple Limestone) conodonts of the Marathon region, Texas. Bulletin of the School of Mines and Metallurgy, University of Missouri, Technical Series 14(3), 1–13.Google Scholar
Einor, O. L., Furdui, R. S. & Aleksandrov, V. A. 1973. Syuranian Horizon and the problem of the boundary between the Lower and Middle Carboniferous in the South Urals. In Materialy po geologii, gidrogeologii, geokhimii i geofizike Ukrainy, Belorussii, Armenii, Urala, Kazakhstana i Sibiri. Sbornik nauchnykh rabot 9, pp. 92–102. Kiev: Kiev University.Google Scholar
Gibshman, N. B. & Akhmetshina, L. Z. 1991. Micropaleontologic basis for determination of the Mid-Carboniferous boundary in the North Caspian syneclise, USSR. Courier Forschungsinstitut Senckenberg 130, 273–95.Google Scholar
Ginkel, A. C. van. 2010. Systematics of the Eostaffellidae (Late Paleozoic Foraminifera). Cushman Foundation Foraminiferal Research, Special Publication no. 42, 1–130.Google Scholar
Gorozhanina, Y. N., Kulagina, E. I., Brown, D., Alvarez-Marron, J. & Pazukhin, V. N. 2001. Lithofacial and paleontological characterization of the Lower and Middle Carboniferous of the Kuruil River (South Urals), pp. 130–40. In Geologiya i perspektivy rasshireniya syr’evoi bazy Bashkortostana I sopredelnykh territorii, vol. 1 (Voprosy geologii, geologicheskie pamyatniki, geoekologiya. materially IV respublikanskoi geologicheskoi konferentsii. Ufa: Institute of Geology, Ufa Research Centre, Russian Academy of Science.Google Scholar
Grozdilova, L. P. & Lebedeva, N. S. 1954. Foraminifers of the lower Carboniferous and Bashkirian Stage of the middle Carboniferous of the Kolvo-Vishera region. Trudy Vsesoyuznogo Neftyanogo Nauchno-Issledovatel'skogo Geologo-Razvedochnogo Instituta (VNIGRI), Mikrofauna SSSR, Sbornik 7, Novaya Seriya 81, 4–235.Google Scholar
Gründel, J. 1975. Neue Ostracoden der Healdiacea und Quasillitacea aus dem Dinant der Insel Rugen. Zeitschrift für Geologische Wissenschaften 7, 971–83.Google Scholar
Higgins, A. C. 1975. Conodont zonation of the late Viséan – early Westphalian strata of the south and central Pennines of northern England. Bulletin of the Geological Survey of Great Britain 53, 1–90.Google Scholar
Higgins, A. C. & Bouckaert, J. 1968. Conodont stratigraphy and palaeontology of the Namurian of Belgium. Mémoires pour servir à l’explication des Cartes géologiques et minières de la Belgique 10, 1–64.Google Scholar
Ivanova, R. M. 1970 New species of archaeodiscids from the Viséan of the South Urals. In Materialy po Paleontologii Urala (eds Breiel, M. G. & Papulov, G. N.), pp. 148–51. Institut Geologii i geokhimii, Akademiya nauk SSSR, Uralskii filial, Sverdlovsk.Google Scholar
Ivanova, R. M. 1973. The Bashkirian Stage of the eastern slope of the South Urals. Trudy Instituta Geologii i Geokhimii, Sverdlovsk 82 (Kamennougolnye otlozheniya vostochnogo sklonaYuzhnogo Urala), 87–102.Google Scholar
Ivanova, R. M. & Chuvashov, B. I. 1993. Bashkirian stage of the Sim Depression (western slope of the South Urals). Stratigrafiya. Geologicheskaya Korrelyatsia 1(1), 76–88.Google Scholar
Kamaletdinov, M. A. 1974. Pokrovnye struktury Urala. Moscow: Nauka, 230 pp.Google Scholar
Keller, B. M. 1949. Palaeozoic flysch formation in the Zilair Syncline on the South Urals and similar formations. Trudy Instituta Geologicheskikh Nauk, Akademiya Nauk SSSR; Geologicheskaya Seriya 104(34), 1–164.Google Scholar
Kellett, B. 1933. Ostracodes of the Upper Pennsylvanian and the Lower Permian strata of Kansas: I. The Aparchitidae, Beyrichiidae, Glyptopleuridae, Kloedenellidae, Kirkbyidae and Youngiellidae. Journal of Paleontology 7(1), 59–168.Google Scholar
Khvorova, I. V. 1961. Flysch and Lower Molassa formations of the South Urals. Trudy Geologicheskogo Instituta SSSR 37, 352 pp.Google Scholar
Kochetova, N. N. 2008. Ostracodes in the stratigraphy of the Middle Carboniferous of the South Urals. Novosti paleontologii i stratigrafii 10–11, Prilozhenie k zhurnalu Geologiya i geofizika 49, 137–40.Google Scholar
Kondiajn, O. A., Belyaev, A. A., Melgunov, F. N. & Rumayntseva, N. A. (eds) 2011. Geologiya i poleznye iskopaemye Rossii (Geology and mineral resources of Russia), vol. 1. Western Russia and the Urals. Book 2. The Urals. St Petersburg: All Russia Institute of Geology (VSEGEI), Russian Academy of Sciences, Ministry of Natural Resource and Ecology & Rosnedra, 584 pp.Google Scholar
Kochetova, N. N. 1991. New species of ostracods from the Serpukhovian Stage of the South Urals. In Paleontologiya i stratrigrafiya devona i karbona Yuzhnogo Urala (ed. Maslov, V. A.), pp. 54–63. Bashkirskii Nauchnyi tsentr, Akademiya Nauk SSSR, Ufa.Google Scholar
Kotschetkova, N. M. 1983. Ostrakody srednego karbona Yuzhnogo Urala. Moscow: Nauka, 120 pp.Google Scholar
Krestovnikov, V. N. 1935. On the stratigraphy of the goniatitic Carboniferous of the basin of the Syuran River in the South Urals. Byulleten Moskovskogo Obshchestva Ispytatelei Prirody. Otdel Geologicheskii 13(1), 114–26.Google Scholar
Krestovnikov, V. N. & Theodorovich, G. I. 1936. A new species of the genus Archaediscus from the Carboniferous of the South Urals. Byulleten Moskovskogo Obshchestva Ispytatelei Prirody, Otdelenie Geologii 44, 86–90 (in Russian).Google Scholar
Kulagina, E. I. 1988. Zonal assemblages of foraminifers from the Serpukhovian deposits of the Sakmara-Ik region of the South Urals. Biostratigraphy and Lithology of the Upper Paleozoic of the Urals. Sbornik nauchnykh trudov. Sverdlovsk: Uralskoe otdelenie AN SSSR, 24–35.Google Scholar
Kulagina, E. I. & Pazukhin, V. N. 1986. On biostratigraphy of the Serpukhovian of the Zilair Megasynclinorium. In Dokembrii i paleozoi Yuzhnogo Urala. BFAN SSSR (Bashkirian Branch of the USSR Academy of Sciences), Ufa, 70–79.Google Scholar
Kulagina, E. I. & Pazukhin, V. N., Kochetova, N. N. & Nikolaeva, S. V. 2002. The Mid-Carboniferous boundary in the Muradymovo Section. In Putevoditel geologicheskikh ekskursii po karbonu Urala. Part 1. Yuzno-Uralskaya ekskursiya (ed. Chuvashov, B.I.), pp. 41–8. Yekaterinburg: Institute Geologii i geokhimii Uralian Branch, Russian Academy of Sciences.Google Scholar
Kulagina, E. I., Pazukhin, V. N., Kotschetkova, N. M., Sinitsyna, Z.A. & Kochetova, N. N. 2001. Stratotipicheskie i opornye razrezy bashkirskogo yarusa karbona Yuzhnogo Urala. Ufa: Gilem. 138 pp.Google Scholar
Kulagina, E. I., Pazukhin, V. N., Nikolaeva, S. V. & Kochetova, N. N. 2000. Biozonation of the Syuran Horizon of the Bashkirian Stage in the Southern Urals as indicated by ammonoids, conodonts, foraminifers and ostracodes. Stratigrafiya. Geologicheskaya Korrelyatsiya 8(2), 38–56 (English translation in Stratigraphy and Geological Correlation, 8(2), 137–156).Google Scholar
Kulagina, E. I., Rumjanzeva, Z. S., Pazukhin, V. N. & Kotchetova, N. N. 1992. Granitsa nizhnego i srednego karbona na Yuzhnom Urale i Srednem Tian Shane (The Mid-Carboniferous boundary in the South Urals and Middle Tien Shan). Moscow: Nauka, 112 pp.Google Scholar
Kullmann, J. & Nikolaeva, S. V. 1999. Ammonoid turnover at the Mid-Carboniferopus boundary and the biostratigraphy of the Early Upper Carboniferous. In Iskopaemye Tsefalopody, Noveishie Dostizheniya V Ikh Izuchenii (ed. Rozanov, A.Y. & Shevyrev, A.A.), pp. 169–94. Moscow: Paleontological Institute, Russian Academy of Sciences.Google Scholar
Kullmann, J. & Nikolaeva, S. V. 2002. Mid-Carboniferous Boundary and the global Lower Bashkirian ammonoid biostratigraphy In Carboniferous and Permian of the World (eds Hills, L. V., Henderson, C. M. & Bamber, E. W.), pp. 780–94. Canadian Society of Petroleum Geologists Memoir no. 19.Google Scholar
Laloux, M. 1988. Foraminiferes du Viseen Superieur & du Namurien du bassin franco-belge. Bulletin de la Société Belge de Géologie 96(3), 205–20.Google Scholar
Lane, H. R., Baesemann, J. F., Brenckle, P. L. & West, R. R. 1985. Arrow Canyon, Nevada: A Potential Mid-Carboniferous Boundary Stratotype. In Proceedings of the 10th International Congress of the Carboniferous Stratigraphy and Geology, 4, 429–40. Madrid 1983.Google Scholar
Lane, H. R., Brenckle, P. L., Baesemann, J. F. & Richards, B. C. 1999. The IUGS boundary in the middle of the Carboniferous: Arrow Canyon, Nevada, USA. Episodes 22(4), 272–83.Google Scholar
Lane, H. R. & Manger, W. L. 1985. Toward a boundary in the Middle of the Carboniferous (1975–1985): ten years of progress. Courier Forschungsinstitut Senckenberg 74, 15–34.Google Scholar
Li, X., Shen, G., Wu, X. & Tong, Z. 1987. A proposed boundary stratotype in Jingyan, Eastern Gansu for the Upper and Lower Carboniferous of China. In Carboniferous Boundaries in China (ed. Wang, C. Y.), pp. 69–88. Beijing: Science Press.Google Scholar
Librovitch, L. S. 1947. Goniatitic faunas of the Carboniferous of the USSR and their significance for the stratigraphy of these beds. Byulleten Moskovskogo Obshchestva Ispytatelei Prirody. Otdel Geologicheskii 22(5), 51–68.Google Scholar
Lipina, O. A. 1948. Textulariids of the upper part of the lower Carboniferous of the southern slope of the Moscow Basin. Trudy Instituta Geologicheskii Nauk, Akademiya Nauk SSSR, vypusk 62, Geologicheskaya Seriya 19,196–215.Google Scholar
Malakhova, N. P. 1956. Foraminifera of the limestones of the Shartymka River in the South Urals. Akademiya Nauk SSSR, Ural'skii Filial, Trudy Gorno-Geologicheskovo Instituta, vypusk 24, Sbornik po Voprosam Stratigrafii 3, 72–124.Google Scholar
Manger, W. L. & Saunders, W. B. 1982. An ammonoid-based Middle Carboniferous boundary. In Biostratigraphic Data for a Mid-Carboniferous Boundary. Biennial meeting of Subcommission on Carboniferous Stratigraphy (eds Ramsbottom, W. H. C., Saunders, W. B. & Owens, B.), pp. 95–100. Leeds, 1981.Google Scholar
Manger, W. L., Weyant, M. & Pareyn, C. 1985. Mid-Carboniferous ammonoid biostratigraphy, Bechar Basin, Algeria. Courier Forschungsinstitut Senckenberg 74, 181–96.Google Scholar
Maslo, A. & Vachard, D. 1997. Reappraisal of the Carboniferous eostaffellinids. Revue de Micropaléontologie 40, 39–69.Google Scholar
Mikhailov, A.V. 1935. On the phylogeny of Carboniferous foraminifers. Izvestiya Leningradskogo Geologo-Gidro-geodezicheskogo tresta, 2/3 (7/8), 38–42.Google Scholar
Mizuno, Y. & Ueno, K. 1997. Conodont and foraminiferal faunal changes across the Mid-Carboniferous boundary in the Hina Limestone Group, Southwest Japan. Prace Państwowego Instytutu Geologicznego 47, 189–200.Google Scholar
Nemirovskaya, T. I. & Nigmadganov, I. M. 1993. Some new conodonts from the Mid-Carboniferous boundary deposits of the Middle Asia. Jahrbuch für Geologie B.-A. 136(1), 213–21.Google Scholar
Nemirovskaya, T. I. & Nigmadganov, I. M. 1994.The Mid-Carboniferous Conodont Event, Courier Forschungsinstitut Senckenberg 168, 319–333.Google Scholar
Nemirovskaya, T. I., Perret, M.-F. & Meischner, D. 1994. Lochriea ziegleri and Lochriea senckenbergica—new conodont species from the latest Visean and Serpukhovian in Europe. Courier Forschungsinstitut Senckenberg 168, 311–17.Google Scholar
Nemyrovska, T. I. 1999. Bashkirian conodonts of the Donets Basin. Scripta Geologica 119, 1–115.Google Scholar
Nemyrovska, T. I. 2005. Late Viséan/early Serpukhovian conodont succession from the Triollo section, Palencia (Cantabrian Mountains, Spain). Scripta Geologica 129, 13–89.Google Scholar
Nemyrovska, T. I., Wagner, R. H., Winkler Prins, C. F. & Montanez, I. 2011. Conodont faunas across the Mid-Carboniferous boundary from the Barcaliente Formation at La Lastra (Palentian Zone, Cantabrian Mountains, northwest Spain); geological setting, sedimentological characters and faunal descriptions. Scripta Geologica 143, 127–82.Google Scholar
Nigmadganov, I. M. & Nemirovskaya, T. I. 1992. New species of conodonts from the Mid-Carboniferous boundary beds of the South Tien Shan. Paleontologicheskii Zhurnal 1992(3), 51–6.Google Scholar
Nikolaeva, S. V. 1994. Serpukhovian and Bashkirian Ammonoids of Central Asia. Trudy Paleontologicheskogo Instituta, Rossiskaya Akademiya Nauk 259, 1–143.Google Scholar
Nikolaeva, S. V. 1995 a. Ammonoid biostratigraphy for the proposed Mid-Carboniferous boundary stratotype, Aksu River, South Tien Shan, Central Asia. Annales de Société Géologique de Belgique 116, 265–73.Google Scholar
Nikolaeva, S. V. 1995 b. Ammonoids from the late Lower and early Upper Carboniferous of Central Asia. Courier Forschungsinstitut Senckenberg 179, 107 pp.Google Scholar
Nikolaeva, S. V. 1999. Ammonoids of the Bogdanovsky Horizon (Middle Carboniferous) of the South Urals. Paleontologicheskii Zhurnal 1999(1), 10–18 (English translation in Paleontological Journal 33, 10–18).Google Scholar
Nikolaeva, S. V. & Kullmann, J. 1998. A review of Middle Namurian ammonoid biostratigraphy. Newsletters on Stratigraphy 36, 117–44.Google Scholar
Nikolaeva, S. V. & Nigmadganov, I. M. 1992. Lower-Middle Carboniferous boundary beds in the South Tien Shan. Izvestiya Akademii Nauk SSSR. Seriya Geologicheskaya 36, 117–44.Google Scholar
Orlova, O. & Bensh, F. R. 2004. New foraminiferal taxa from the Lower-Middle-Carboniferous boundary deposits of the Middle Tien Shan. Geologiya i Mineralnye Resursy. Tashkent, Nauchno-prakticheskiy Zhurnal 5, 8–17.Google Scholar
Orlov-Labkovsky, O., Bensh, F. R. & Mikhno, N. M. 2003. Revision of the Carboniferous foraminiferal zonation of the Middle and South Tien Shan, Central Asia. In XV International Congress on Carboniferous and Permian Stratigraphy. Utrecht, The Netherlands, 10–16 August 2003. Abstract (024), pp. 386–9.Google Scholar
Pareyn, C., Saunders, W. B., Manger, W. L. & Lemosquet, Y. 1984. The middle Carboniferous ammonoid succession of the Bechar Basin and adjacent areas, Sud-Oranais, Algeria. In Neuvieme Congres International de Stratigraphie & de Geologie du Carbonifere, Washington and Champaign Urbana 1979, Compte Rendu 2, Biostratigraphy (eds Sutherland, P. K. & Manger, W. L.), pp. 437–42.Google Scholar
Pazukhin, V. N. 1995. Lower Carboniferous conodont-based biostratigraphy of the western slope of the Zilair Megasynclinorium. In Ezhegodnik 1994. Informatsionnnye materialy, pp. 37–8. Ufa: Institute of Geology, Ufa Research Centre, Russian Academy of Sciences.Google Scholar
Pazukhin, V. N. & Gorozhanina, E. N. 2003. Stratigraphy and facies of the Unbetovo Formation of the Middle Carboniferous of the western slope of the Zilair Megasynclinorium on the South Urals. Geologicheskii Sbornik no. 3. Informatsionnnye Materialy, pp. 63–70. Ufa: Institute of Geology, Ufa Research Centre, Russian Academy of Sciences.Google Scholar
Phillips, J. 1846. On the remains of microscopic animals in the rocks of Yorkshire. Proceedings of the Geologic and Polytechnic Society of the West Riding of Yorkshire 2, 274–85.Google Scholar
Ponomareva, G. Y. 2004. On the problem of the Serpukhovian and Bashkirian boundary in the Gostinskii Section. Vestnik Permskogo Universiteta 3, 13–19.Google Scholar
Ponomareva, G. Y. 2010. Zonal divisions at the Viséan-Serpukhovian boundary based on foraminifera in the Malaya Inya section (Western slope of the North Urals). In Stratigraphy and Regional Geology of the East of the Russian Platform and Western Urals. Sbornik nauchnykh trudov, pp. 44–51. Perm: Permskii Gosudarstvennyi Universitet.Google Scholar
Ponomareva, G. Y., Lyadova, R. A., Shcherbakova, M. V., Pazukhin, V. N., Nasedkina, V. A. & Kitaev, P. M. 2002. Serpukhovian-Bashkirian boundary beds in the Gostinskii section. In Stratigrafiya i Paleogeografiya Karbona Evrazii (eds Chuvashov, B.I. & Amon, E.O.), pp. 238–42. Yekaterinburg: Institute Geologii i Geokhimii, Uralian Branch, Russian Academy of Sciences.Google Scholar
Puchkov, V. N. 2002. Paleogeodinamika Yuzhnogo i Srednego Urala (Paleogeodynamics of the South and Central Urals). Ufa: Dauria. 200 pp.Google Scholar
Puchkov, V. N. 2009. Paleozoic evolution of the East European continental margin involved in the Uralide Orogeny. In Mountain Building in the Uralides: Pangea to the Present (eds Brown, D., Juhlin, C. & Puchkov, V.), pp. 9–31. Geophysical Monograph no. 132.Google Scholar
Ramsbottom, W. H. C. & Saunders, W. B. 1985. Evolution and evolutionary biostratigraphy of Carboniferous ammonoids. Journal of Paleontology 59(1), 123–39.Google Scholar
Rauser-Chernousova, D. M. 1948 a. Contributions to the foraminiferal fauna of the Carboniferous deposits of central Kazakhstan. Trudy Instituta Geologicheskii Nauk, Akademiya Nauk SSSR, vypusk 66, Geologicheskaya Seria 21, 1–27.Google Scholar
Rauser-Chernousova, D. M. 1948 b. Some new species of foraminifers from lower Carboniferous deposits of the Moscow Basin. Trudy Instituta Geologicheskikh Nauk, Akademiya Nauk SSSR, vypusk 62, Geologicheskaya Seriya 19, 227–38.Google Scholar
Rauser-Chernousova, D. M., Belyaev, G. & Reitlinger, E. A. 1936. Upper Paleozoic foraminifers of the Pechora region. Trudy Polarnoi Komissii, Akademiya Nauk SSSR 28, 159–232.Google Scholar
Rauser-Chernousova, D. M., Bensh, F. R., Vdovenko, M. V., Gibshman, N. B., Leven, E. Y., Lipina, O. A., Reitlinger, E. A., Solovjeva, M. N. & Chediya, I. O. 1996. Spravochnik po Sistematike Foraminifer Paleozoya (Endothyroida, Fusulinoida) (Reference Book on the Systematic of Palaeozoic Foraminifera (Endothyroida, Fusulinoida)). Moscow: Nauka. 203 pp.Google Scholar
Rauser-Chernousova, D. M., Gryzlova, N. D., Kireeva, D. D., Leontovich, G. E., Safonova, T. P. & Chernova, E. I. 1951. Middle Carboniferous Fusulinids of the Russian Platform and Adjacent Regions, a Handbook and Guide. Akademiya nauk SSSR, Institut Geologischeskikh Nauk, Ministerstvo Neftyanoi Promyshlennosti SSSR, 380 pp.Google Scholar
Reitlinger, E. A. 1949. Smaller foraminifers in the lower part of the middle Carboniferous of the Middle Urals and Kama River area. Izvestiya Akademii Nauk SSSR, Seriya Geologicheskaya 6, 149–64.Google Scholar
Reitlinger, E. A. 1950. Foraminifers from middle Carboniferous deposits in the central part of the Russian Platform (exclusive of the family Fusulinidae). Trudy Instituta Geologicheskikh Nauk, Akademiya Nauk SSSR, Geologicheskaya Seriya 47, no. 126.Google Scholar
Reitlinger, E. A. 1956. The Lasiodiscidae, a new family. Voprosy Mikropaleontologii, Akademiya Nauk SSSR 1, 69–78.Google Scholar
Reitlinger, E. A. 1961. Stratigraphy of the Middle Carboniferous deposits of the Borehole no. 1 Krasnaya Polyana section of the Middle Trans-Volga. Regionalnaya Stratigrafiya SSSR, Geologicheskii Institut Akademiya Nauk SSSR 5, 218–60.Google Scholar
Reitlinger, E. A. 1963. On a single paleontological criterion for the establishment of Lower Carboniferous boundaries based on the foraminiferal fauna (in Russian). Voprosy Mikropaleontologii, Akademiya Nauk SSSR 7, 22–56.Google Scholar
Reitlinger, E. A. 1980. On the boundary between the Bogdanovkian and Krasnopolyanian (foraminifers of the Homoceras Zone). Voprosy Mikroplaeontologii 23, 23–38.Google Scholar
Richards, B. C. 2011. Report of the Task Group to establish a GSSP close to the existing Viséan-Serpukhovian boundary. Newsletter on Carboniferous Stratigraphy 29, 26–9.Google Scholar
Richards, B. C., Lane, H. R. & Brenckle, P. L. 2002. The IUGS Mid-Carboniferous (Mississippian-Pennsylvanian) global boundary stratotype section and point at Arrow Canyon, Nevada, USA. In Carboniferous and Permian of the World (eds Hills, L. V., Henderson, C. M. & Bamber, E. W.), pp. 802–31. Canadian Society of Petroleum Geologists Memoir no. 19.Google Scholar
Riley, N. 1987. Type ammonoids from the Mid-Carboniferous boundary interval in Britain. Courier Forschungsinstitut Senckenberg 98, 25–37.Google Scholar
Riley, N. 1998. Comment on global nomenclature of the Carboniferous Subsystems and the Mid-Carboniferous Boundary GSSP. Newsletters on Carboniferous Stratigraphy 16, 26–8.Google Scholar
Riley, N., Varker, W. J., Owens, B., Higgins, A. C. & Ramsbottom, H. C. 1987. Stonehead Beck, Cowling, North Yorkshire, England: a British proposal for the Mid-Carboniferous boundary stratotype. Courier Forschungsinstitut Senckenberg 98, 159–77.Google Scholar
Robinson, E. 1978. A stratigraphical index of British Ostracoda. Geological Journal Special Issue 8,121–66.Google Scholar
Roundy, P. V. 1926. Conodonts. In Mississippian Formations of San Saba County, Texas (eds Roundy, P. V., Girty, G. H. & Goldman, M. I.), pp. 8–17. United States Geological Survey Professional Paper no. 146.Google Scholar
Rumjanzeva, Z. S. 1970. Stratigraphiya i foraminifery namyurskikh i nizhnebashkirskikh otlozhenii sistemy Chatkalskikh gor. In Biostratigrafiya osadochnykh obrazovanii Uzbekistana (ed. Kuzichkina, Yu. M.), pp. 138–97. Tashkent: Ministerstvo geologii Uzbekskoi SSR, Tashkentskii geologorazvedochnyi Trest “Tashkentgeologia”, Kompleksnaya geologosyemochnaya poiskovaya ekspeditsiya and Leningrad: Nedra, Leningradskoye otdelenie.Google Scholar
Rumjanzeva, Z. S. 1989. Zonal subdivision of the Serpukhov and Bashkirian of the Middle Tien Shan on foraminifers. Byulleten Moskovskogo Obshchestva Ispytatelei Prirody. Otdel Geologicheskii 64(3), 124.Google Scholar
Ruzhencev, V. E. & Bogoslovskaya, M. F. 1971. Namurian stage in the ammonoid evolution. Early Namurian ammonoids. Trudy Paleontologicheskogo Instituta, Akademiya Nauk SSSR 133, 1–382.Google Scholar
Ruzhencev, V. E. & Bogoslovskaya, M. F. 1978. Namurian stage in the ammonoid evolution. Late Namurian ammonoids. Trudy Paleontologicheskogo Instituta, Akademiya Nauk SSSR 167, 1–338.Google Scholar
Shlykova, T. I. 1951. Foraminifera of the Visean and Namurian stages (lower Carboniferous) of the western flank of the Moscow Basin. Trudy Vsesoyuznogo Neftyanogo Nauchno-Issledovatel'skogo Geologo-Razvedochnogo Instituta (VNIGRI), Novaya Seriya 56, 109–78.Google Scholar
Simakov, K.V., Bless, M. J. M., Bouckaert, J., Conil, R., Gagiev, M. H., Kolesov, Ye. V., Onoprienko, Yu. I., Roty, E., Razina, N. P., Shilo, N. A., Smirnova, L. V., Streel, M. & Swennen, R. 1984. Addendum to Upper Fammenian and Tournaisian deposits of the Omolon region (NE-USSR). Natuurhistorisch Museum, Maastricht, p. 1–13.Google Scholar
Sinitsyna, Z. A., Kulagina, E. I. & Klimenko, T. V. 1997. The Viséan Stage of the Western Slope of the South Urals. In Biostratigrafiya i Neftegazonosnost Paleozoya Bashkirskogo Priuraliya. Sbornik Nauchnykh Trudov (ed. Lozin, E.V.), pp. 21–31. Ufa: Bashkirskii nauchno-issledovatelskii i proektnyi institut (BashNIPINeft) no. 93.Google Scholar
Skipp, B. A., Brenckle, P. L., Poletaev, V. I., Nemirovskaya, T. I., Lane, H. R. & Manger, W. L. 1989. The continuing international search for a mid-Carboniferous boundary stratotype: Donets Basin, USSR, 1988. Episodes 12(3), 179–83.Google Scholar
Skompski, S., Alekseev, A., Meischner, D., Nemirovskaya, T., Perret, M.-F. & Varker, W. J. 1995. Conodont distribution across the Viséan/Namurian boundary. Courier Forschungsinstitut Senckenberg 188, 177–209.Google Scholar
Somerville, I.D. 2008. Biostratigraphic zonation and correlation of Mississippian rocks in Western Europe: some case studies in the late Viséan/Serpukhovian. Geological Journal 43, 209–40.Google Scholar
Stepanova, T. I. & Kucheva, N. A. 2006. Section Khudolaz — the stratotypes of horizons of the Lower Carboniferous subregional scheme for the eastern slope of the Urals. Litosfera 1, 45–75.Google Scholar
Thompson, M. L. 1944. Pennsylvanian Morrowan rocks and fusulinids of Kansas. Kansas State Geological Survey, Bulletin 52(7), 409–31.Google Scholar
Titus, A. L. & Manger, W. L. 2001. Mid-Carboniferous Ammonoid Biostratigraphy, Southern Nye County, Nevada: implications of the first North American Homoceras. The Paleontological Society Memoir no. 55 . Supplement to Journal of Paleontology 75(4), 1–31.Google Scholar
Titus, A. L., Webster, G. D., Manger, W. L. & Dewey, C. P. 1997. Biostratigraphic analysis of the Mid-Carboniferous boundary at the South Syncline Ridge, Nevada Test Site, Nevada, United States. Proceedings of the 13th International Congress on the Carboniferous and Permian. Prace Panstwowego Institutu Geologicznego 157, 207–12.Google Scholar
Ulrich, E. O. & Bassler, R. S. 1906. New American Paleozoic Ostracoda. Notes and description of Upper Carboniferous genera and species. Proceedings of the US National Museum 30, no. 1446, p. 146–64.Google Scholar
Vachard, D. & Maslo, A. 1996. Precisions biostratigraphiques & micropaléontologiques sur le Bashkirien d’Ukraine (carbonifère moyen). Revue de Paléobiologie Genève 15(2), 357–83.Google Scholar
Vdovenko, M. V. 1988. Foraminiferal scale of the Lower Carboniferous of the Eastern part of the East-European platform. Doklady Akademii nauk USSR. Otdelenie Geologicheskikh, Khimicheskikh i Biologicheskikh Nauk 9, 10–14.Google Scholar
Vdovenko, M.V., Aizenverg, D. E., Brazhnikova, N. V. & Poletaev, V. J. 1989. Zonal stratigraphic schemes of the Lower Carboniferous of the Donets Basin. Tektonika i Stratigrafiya 30, 52–53.Google Scholar
Vissarionova, A. I. 1948. Primitive fusulinids from the lower Carboniferous of the European part of the USSR. Trudy Instituta Geologicheskikh Nauk, Akademiya Nauk SSSR, vypusk 62, Geologicheskaya Seriya 19, 216–26.Google Scholar
Youngquist, W. L. & Miller, A. K. 1949. Conodonts from the late Mississippian Pella Beds of south central Iowa. Journal of Paleontology 23, 617–22.Google Scholar
Zaitseva, E. L. & Klenina, L. N. 2008. Mid-Carboniferous boundary beds in the Peri-Caspian Basin. Byulleten Moskovskogo Obshchestva Ispytatelei Prirody. Otdel Geologicheskii 83(3), 21–41.Google Scholar