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Conodonts and ostracodes from the late Tournaisian bathyal sequence of the Polar Urals

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Języki publikacji
EN
Abstrakty
EN
Early Carboniferous (late Tournaisian) conodonts, recovered from siliceous shales and silicites of the Nyan-Vorga Formation within the Lemva tectonic belt of the Polar Urals (Russia), include the biostratigraphically important taxa Siphonodella lanei, Gnathodus typicus, Dollymae hassi, and Scaliognathus anchoralis, marking the following conodont zones of the upper Tournaisian: crenulata, typicus, and anchoralis. Associated species include representatives of genera Siphonodella, Polygnathus, Pseudopolygnathus, Dollymae, Gnathodus, Kladognathus, and Idioprioniodus. These conodont faunas provide the first biostratigraphically constrained correlations between bathyal deposits of the Lemva Allochthone in the Polar Urals and the “standard” conodont zonation. Ostracodes found in the silicite of the typicus Zone are represented by Sagittibythere ? sp. and Tricornina (Bohemia) sp. The ostracodes are reported from the bathyal deposits of Urals for a first time. The traces of the global Mid-Aikuanian Event are recognized in the upper part of the Tournaisian bathyal succession. This event led to turnover in conodont associations and is followed by increasing in conodont diversity.
Wydawca
Rocznik
Strony
48--58
Opis fizyczny
Bibliogr. 24 poz., rys., tab.
Twórcy
  • N.P.Yushkin Institute of Geology Komi SC UrB RAS, 54 Pervomayskaya St., Syktyvkar, Russia
  • N.P.Yushkin Institute of Geology Komi SC UrB RAS, 54 Pervomayskaya St., Syktyvkar, Russia
Bibliografia
  • Bischoff G. (1957) Die Conodonten-Stratigraphie des rheno-herzynischen Unterkarbons mit Berücksichtigung der Wocklumeria-Stufe und der Devon/Karbon-Grenze. Abhandlungen des Hessischen Landesamtes fur Bodenforschung zu Weisbaden 19: 164.
  • Butler M. (1973) Lower Carboniferous conodont faunas from the Eastern Mendips, England. Palaeontology 16, 3: 477-517.
  • Dreesen R., Sadberg C.A., Ziegler W. (1986) Review of Late Devonian and Early Carboniferous conodont biostratigraphy and biofacies models as applied to the Ardenne shelf. Annales de la Societe geologique de Belgique 109: 27-42.
  • Eremenko N.M., Zhuravlev A.V. (2013) Lithological and genetic typization of the middle Palaeozoic deep-water deposits. Osadochnye basseyny, sedimentationnye i postsedimentationnye processy v geologicheskoy istorii. Materials of VII All-Russian lithological meeting (Novosibirsk, 28-31 Oct. 2013). Vol. I: 290-294.
  • Harris A.G. & Sweet W.C. (1989) Mechanical and chemical techniques for separating microfossils from rock. Sediment and residue matrix. [In:] Paleotechniques (ed. R.M. Feldmann, R.E. Chapman & J.T. Hannibal). Paleontol. Soc. Spec. Publ., 4: 70-86.
  • Ji Q. (1987) Early Carboniferous conodonts from Jianghua County of Hunan Province and their stratigraphic value - with a discussion on the Mid-Aikuanian Event. Bulletin of the Institute of Geology, Chinese Academy of Geological Science. 16: 115-141.
  • Kalvoda J. (1994) The conodont extinction at the Middle-Upper Tournaisian boundary. Geolines. 1: 12-15.
  • Lane H.R., Sandberg C.A., Ziegler W. (1980) Taxonomy and phylogeny of some Lower Carboniferous conodonts and preliminary standard post-Siphonodella zonation. Geologica et Palaeontologica. 14: 117-164.
  • Lethiers F., Feist R. (199l) Ostracodes, stratigraphie et bathymrtrie du passage Devonien-Carbonif'ere au Viseen inferieur en Montagne Noire (France). Geobios 24: 71-104.
  • Puchkov V. (2002) Paleozoic evolution of the East European continental margin involved into the Urals. [In:] Mountain Building in the Uralides: Pangea to the Present (ed. D. Brown, C. Juhlin, V. Puchkov). AGU Geophysical Monograph Series, 132: 9-32.
  • Puchkov V.N. (2010) Geology of the Urals and Cis-Urals (actual problems of stratigraphy, tectonics, geodynamics and metallogeny). Design Poligraph Service, Ufa. 280 pp. [in Russian].
  • Saltzman M.R., Groessens E., Zhuravlev A.V. (2004) Carbon cycle models based on extreme changes in δ13C: an example from the lower Mississippian. Paleogeography, Paleoclimatology, Paleoecology 213: 359-377.
  • Sandberg C.A., Gutschick R.C. (1984) Distribution, microfacics and source rock potential of Mississippian Delle Phosphatic Member of Woodman Formation and equivalents, Utah and adjacent States. [In:] Hydrocarbon source rocks of the Greater Rocky Mountain region (ed. J. Woodward, F.F. Meissner & J.L. Clayton). Denver, Colorado, Rocky Mountain Association of Geologists, 135-178.
  • Schornikov E. I., Michailova E. D. (1990) Ostracodes Bythocytheridae at early stage of development. Comparative morphology, paleoecology and evolutionary pathways. Nauka Publishers, Moscow. 278 pp. [in Russian].
  • Scotese C.R. (2016) PALEOMAP PaleoAtlas for GPlates and the PaleoDataPlotter program. Geological Society of America Abstracts with Programs 48, 5. DOI: 10.1130/abs/2016NC-275387.
  • Thompson T.L., & Fellows L.D. (1970) Stratigraphy and conodont biostratigraphy of Kinderhookian and Osagean (Lower Mississippian) rocks of southwestern Missouri and the adjacent area. Missouri Geological Survey - Report of Investigation 45: 1-263.
  • Tian S. & Coen M. (2005) Conodont evolution and stratotype sign of carboniferous Tournaisian-Visean boundary in South China. Science in China Ser. D, Earth Sciences 48, 12: 2131-2141.
  • Varker W.J. & Sevastopulo G.D. (1985) The Carboniferous System: Part. 1 - Conodonts of the Dinantian Subsystem from Great Britain and Ireland. [In:] A stratigraphical index of conodonts (ed. A.C. Higgins & R.L. Austin). British Micropalaeontological Society Series, 167-209.
  • Yao L.; Qie W.; Luo G.; Liu J.; Algeo T. J.; Bai X.; Yang B. & Wang X. (2015) The TICE event: Perturbation of carbon-nitrogen cycles during the mid-Tournaisian (Early Carboniferous) greenhouse-icehouse transition. Chemical Geology 401: 1 - 14. DOI: 10.1016/j.chemgeo.2015.02.021
  • Yudin V.V. (1994) Orogenez Severa Urala i Pay-Khoya. Nauka Publishers, Ekaterinburg. 286 pp. [in Russian].
  • Zhuravlev A.V. (2003) Upper Devonian - Lower Carboniferous conodonts of the north-east of European part of Russia. VSEGEI Publ., St. Petersburg. 85 pp. [in Russian].
  • Zhuravlev A.V., Gerasimova A.I. (2016a) Sequence composition and conodonts of the Kara Formation (Lower Carboniferous) of the Amderma Distirict of the Northern Pay-Khoy. Vestnik IG Komi SC UB RAS 1: 3-10. DOI: 10.19110/2221-1381-2016-1-3-10 [in Russian].
  • Zhuravlev A.V., Gerasimova A.I. (2016b) XMT micropalaeontological study of the silicites. Vestnik IG Komi SC UB RAS 3: 26-32. DOI: 10.19110/2221-1381-2016-3-26-32
  • Ziegler W., Lane H.R. (1987) Cycles in conodont evolution from Devonian to mid-Carboniferous. [In:] Palaeobiology of conodonts (ed. R.J. Aldridge). 147-163.
Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-58f8adec-aa88-4e86-988b-b49f53ad9dd6
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