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Lower Paleozoic Deposits in the Transition Zone between the Carbonate Platform and Black Shale Basin (Eastern Taimyr)

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Abstract

Sedimentological features of the Upper Cambrian–Middle Ordovician rocks exposed in eastern Taimyr in the Faddey Gulf area are discussed. The studied sections belong to the transitional facies zone located between the carbonate platform (Siberian Platform continuation) in the south and a relatively deep-water basin in the north. The studied deposits compose a genetically coherent sequence formed in the distal zone of the siliciclastic–carbonate ramp at a depth exceeding the storm wave base. The lower (Upper Cambrian–lowermost Ordovician) part of the sequence is represented by limestones, dolomitized carbonate siltstones, and sandstones with shale layers. The upper (Lower–Middle Ordovician) part of the studied interval is dominated by shales with thin layers of carbonate siltstones. The carbonate detritus was sourced from a shallow-water shelf located south of the studied sections. The siliciclastic admixture in carbonate siltstones and sandstones was sourced from an island in the northern part of the modern Siberian Platform. The sandy material was transported by storm bottom currents; the fine-grained particles, by surface currents and winds as particulates and suspension clouds in the bottom water. Carbonate sandstones with the typical turbidite sedimentary structures, common in the lower part of the section, were deposited by turbidity currents initiated by storms. At that time, a prominent break likely existed in the ramp profile. The predominant NE orientation of flute casts indicates the alongslope (or along the trough axis) transport of material by bottom currents. The ramp topography was leveled in the second half of the Early Ordovician and in the Middle Ordovician.

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REFERENCES

  1. Amy, L.A., Talling, P.J., Peakall, J., et al., Bed geometry used to test recognition criteria of turbidites and (sandy) debrites, Sediment. Geol., 2005, vol. 179, pp. 163–174.

    Article  Google Scholar 

  2. Argnani, A. and Lucchi, F.R., Tertiary siliciclastic turbidite systems of the Northern Apennines, in Anatomy of an Orogen: the Apennines and Adjacent Mediterranean Basins, Vai, G.B. and Martini, I.P., Eds., Dordrecht: Springer, 2001, pp. 327–349.

    Google Scholar 

  3. Atlas paleozoiskoi fauny Taimyra (Atlas of Paleozoic Fauna in Taimyr), St. Petersburg: Kartfabr. VSEGEI, 2003, ch. 1 (Brachiopods, ostracods, and conodonts).

  4. Bagaeva, A.A., Mozoleva, I.N., and Borisenkov, K.V., New stratigraphic subdivision in the Lenivka–Klyuevka structural-formation zone in Taimyr, in Litologiya osadochnykh kompleksov Evrazii i shel’fovykh oblastei (Lithology of Sedimentary Complexes in Eurasia and Shelf Zones), Kazan: KazanUniv., 2019, pp. 28–29.

  5. Basilici, G., Vieira de Luca P.H., and Poire, D.G., Hummocky cross-lamination-like structures and combined-flow ripples in the Punta Negra Formation (Lower-Middle Devonian, Argentine Precordillera): A turbiditic deep-water or storm-dominated prodelta inner-shelf system?, Sediment. Geol., 2012, vol. 267–268, pp. 73–92.

    Article  Google Scholar 

  6. Bezzubtsev, V.V., Geological structure and mineral resources in the Taimyr fold zone, in Otchet Taimyrskoi opytno-proizvodstvennoi partii po rezul’tatam aerofotogeologicheskogo kartirovaniya masshtaba 1 : 200 000 Taimyrskoi skladchatoi oblasti v 1972–1979 gg (Report of the Taimyr Experimental-Industrial Team Based on Results of the Aerophotogeologcial Mapping (Scale 1 : 200 000) in the Taimyr Fold Zone in 1972–1979), Krasnoyarsk, 1979.

  7. Bezzubtsev, V.V., Zalyaleev, R.Sh., Goncharov, Yu.I., and Sakovich, A.B., Geologicheskaya karta Gornogo Taimyra. Masshtab 1 : 500 000 (Geological Map of the Taimyr Mountains. Scale 1 : 500 000), Krasnoyarsk, 1983.

  8. Bezzubtsev, V.V., Zalyaleev, R.Sh., and Sakovich, A.B., Geologicheskaya karta Gornogo Taimyra. Masshtab 1 : 500 000. Ob"yasnitel’naya zapiska (Geological Map of the Taimyr Mountains. Scale 1 : 500 000. Explanatory Note), Bezzubtsev, V.V., Ed., Krasnoyarsk, 1986. Bobrov, V.N., Bardeeva, M.A., Kleikova, N.I., Lyapina, G.G., and Yan, G.Kh., Legenda Olenekskoi serii listov Gosudarstvennoi geologicheskoi karty Rossiiskoi Federatsii masshtaba 1 : 200 000. Ob"yasnitel’naya zapiska (Legend for the Olenek Sheet Series of the State Geological Map of the Russian Federation. Scale 1 : 200 000. Explanatory Note), Moscow: Aerogeologiya, 2000.

  9. Chaudhuri, A.K., Climbing ripple structure and associated storm-lamination from a Proterozoic carbonate platform succession: their environmental and petrogenetic significance, J. Earth Syst. Sci., 2005, vol. 114, no. 3, pp. 199–209.

    Article  Google Scholar 

  10. Dott, R.H. and Bourgeois, G., Hummocky stratification: significance of its variable bedding sequences, Geology, 1982, vol. 93, pp. 663–680.

    Google Scholar 

  11. Flügel, E., Microfacies of carbonate rocks: analysis, interpretation and application. Springer, 2010, pp. 564–566.

    Book  Google Scholar 

  12. Guensburg, T.E., Phylogenetic implications of the oldest crinoids, J. Paleontol., 2012, vol. 86.

  13. Hequette, A. and Hill, P.R., Storm-generated currents and offshore sediment transport on a sandy shoreface, Tibjak Beach, Canadian Beaufort Sea, Mar. Geol., 1993, vol. 113, pp. 283–304.

    Article  Google Scholar 

  14. Kaban’kov, V.Ya., Sobolevskaya, R.F., and Proskurnin, V.F., Late Cambrian–Early Paleozoic Evolution Stage of the Novaya Zemlya–Taimyr–Severnaya Zemlya Thrust Fold System, in Prirodnye Resursy Taimyra (Natural Resources of Taimyr), 2003, no. 1, pp. 210–228.

  15. Kachurina, N.V., Makar’ev, A.A., Makar’eva, E.M., et al., Gosudarstvennaya geologicheskaya karta Rossiiskoi Federatsii. Masshtab 1 : 1 000 000. List T-45-48 – m. Chelyuskin. Ob"yasnitel’naya zapiska (State Map of The Russian Federation. Scale 1 : 1 000 000. Sheet T-45-48 (Cape Chelyuskin). Explanatory Note), St. Petersburg: Kartfabr. VSEGEI, 2012.

  16. Kanygin, A.V., Yadrenkina, A.G., Timokhin, A.V., et al., Stratigrafiya neftegazonosnykh basseinov Sibiri. Ordovik Sibirskoi platformy (Stratigraphy of Petroliferous Basins in Siberia: Ordovician of the Siberian Platform), Novosibirsk: Geo, 2007.

  17. Kanygin, A., Dronov, A., Timokhin, A., and Gonta, T., Depositional sequences and palaeoceanographic change in the Ordovician of the Siberian Craton, Palaeogeogr. Palaeoclimatol. Palaeoecol., 2010, vol. 296, no. 3/4, pp. 285–296.

    Article  Google Scholar 

  18. Kuzmichev, A.B., Danukalova, M.K., Proskurnin, V.F., et al., The pre-Vendian (640-610 Ma) granite magmatism in the Central Taimyr fold belt: the final stage of the Neoproterozoic evolution of the Siberian paleocontinent active margin, Geodynam. Tectonoph., 2019, vol. 10, no. 4, pp. 841–861.

    Article  Google Scholar 

  19. Makar’ev, A.A. and Makar’eva, E.M., Gosudarstvennaya geologicheskaya karta Rossiiskoi Federatsii masshtaba 1 : 1 000 000. List T-45-48 (m. Chelyuskin) (State Geological Map of the Russian Federation. Scale 1 : 1 000 000. Sheet T-45-48 (Cape Chelyuskin), St. Petersburg: PMGRE, 2011.

  20. Markovskii, V.A., Shneider, G.V., Proskurnin, V.F., et al., Gosudarstvennaya geologicheskaya karta Rossiiskoi Federatsii (novaya seriya). Masshtab 1 : 1 000 000. List T-48-50 (o. Bol’shevik) (State Geological Map of the Russian Federation. Scale 1 : 1 000 000. Sheet T-48-50 (Bol’shevik Island), St. Petersburg: Kartfabrika VSEGEI, 2003.

  21. Mutti, E. and Ricci Lucchi, F., Turbidites of the northern Apennines: introduction to facies analysis, Int. Geol. Rev., 1978, vol. 20, no. 2, pp. 125–166.

    Article  Google Scholar 

  22. Obut, A.M. and Sobolevskaya, R.F., Graptolity ordovika Taimyra (Ordovician Graptolites in Taimyr), Moscow: Nauka, 1964.

  23. Pease, V. and Scott, R.A., Crustal affinities in the Arctic Uralides, northern Russia: significance of detrital zircon ages from Neoproterozoic and Palaeozoic sediments in Novaya Zemlya and Taimyr, J. Geol. Soc. London, 2009, vol. 166, pp. 517–527.

    Article  Google Scholar 

  24. Pomar, L., Types of carbonate platforms: a genetic approach, Basin Research, 2001, vol. 13, pp. 313–334.

    Article  Google Scholar 

  25. Sarkar, S., Banerjee, S., Chakraborty, S., and Bose, K.B., Shelf storm flow dynamics: insight from the Mesoproterozoic Rampur Shale, central India, Sediment. Geol., 2002, vol. 147, pp. 89–104.

    Article  Google Scholar 

  26. Sobolevskaya, R.F., Atlas paleozoiskoi fauny Taimyra (Atlas of Paleozoic Fauna in Taimyr), St. Petersburg: VNIIOkeangeologiya, 2011, vol. 221, part 2 (Ordovician and Silurian Graptolites).

  27. Sobolevskaya, R.F. and Kaban’kov, V.Ya., Stratigrafiya kembriiskikh otlozhenii Gornogo Taimyra (Stratigraphy of Cambrian Rocks in the Taimyr Mountains), St. Petersburg: VNIIOkeangeologiya, 2014, vol. 228.

  28. Sobolevskaya, R.F., Sobolev, H.H., and Matveev, V.P., New Ordovician and Silurian Subdivisions in Taimyr, in Stratigrafiya i paleontologiya Rossiiskoi Arktiki, (Stratigraphy and Paleontology in the Russian Arctic), Bondarev, V.I., Ed., St. Petersburg: VNIIOkeangeologiya, 1997.

  29. Stepanov, G.I., Uspenskaya, I.B., Tarutin, O.A., et al., Geological Structure and Mineral Resources between the Zhdanov, Faddey, and Pregradnaya Rivers, in Otchet o rezul’tatakh geologicheskoi s"emki i poiskov masshtaba 1 : 200 000 v tsentral’noi chasti lista T-48-XXXIV, XXXV, XXXVI, provedennoi otryadom № 2 Taimyrskoi partii letom 1964 g (Report on Results of the Geological Mapping and Prospecting (Scale 1 : 200 000, Sheets T-48-XXXIV–T-48-XXXVI) by Group 2 of the Taimyr Geological Team in 1964), Leningrad: NIIGA, 1965.

  30. Sukhov, S.S., Shabanov, Yu.Ya., Pegel’, T.V., et al., Stratigrafiya neftegazonosnykh basseinov Sibiri. Kembrii Sibirskoi platformy (Stratigraphy of Petroliferous Basins in Siberia: Cambrian of the Siberian Platform), Novosibirsk: INGG SO RAN, 2016, vol. 1 (Stratigraphy).

  31. Uflyand, A.K., Natapov, L.M., Lopatin, V.M., et al., The tectonic nature of Taimyr, Geotektonika, 1991, no. 6, pp. 76–93.

  32. Vernikovsky, V.A., Geodinamicheskaya evolyutsiya Taimyrskoi skladchatoi oblasti (Geodynamic Evolution of the Taimyr Fold Zone), Novosibirsk: SO RAN, 1996.

  33. Williams, M., Siveter, D.J., Salas, M.J., et al., The earliest ostracods: the geological evidence, Senckenberg. Lethaea, 2008, vol. 88, pp. 11–21.

    Article  Google Scholar 

  34. Yancey, T.E., Controls on carbonate and siliciclastic sediment deposition on a mixed carbonate–siliciclastic shelf (Pennsylvanian Eastern Shelf of north Texas), in Sedimentary Modeling: Computer Simulations and Methods for Improved Parameter Definition, Franseen, E.K., Watney, W.L., C.G. St., Kendall, C., and Ross, W., Eds. Kansas Geol. Surv. Bull., 1991, vol. 233, pp. 263–272.

  35. Zonenshain, L.P., Kuz’min, M.I., and Natapov, L.M., Tektonika litosfernykh plit territorii SSSR (Tectonics of Lithospheric Plates in the Soviet Union), Moscow: Nedra, 1990, part 2.

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ACKNOWLEDGMENTS

The authors are grateful to V.F. Proskurin and other colleagues from the Division of Regional Geology and Mineral Resources in Eastern Russia, Karpinsky Russian Geological Research Institute (VSEGEI), for assisting the organization and accomplishment of field works.

Funding

This work was supported by the Russian Foundation for Basic Research (project no. 19-05-00926). Studies by M.K. Danukalova and A.B. Kuzmichev were accomplished in accordance with research plans of Geological Institute, Russian Academy of Sciences.

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Authors and Affiliations

  1. Geological Institute, Russian Academy of Sciences, 119017, Moscow, Russia

    M. K. Danukalova & A. B. Kuzmichev

  2. Karpinsky Russian Geological Research Institute, 199106, St. Petersburg, Russia

    A. A. Bagaeva & T. Yu. Tolmacheva

Authors
  1. M. K. Danukalova
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  2. A. B. Kuzmichev
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  3. A. A. Bagaeva
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  4. T. Yu. Tolmacheva
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Correspondence to M. K. Danukalova.

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Translated by D. Sakya

In the present paper, term “carbonate platform” is used sensu lato (Pomar, 2001).

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Danukalova, M.K., Kuzmichev, A.B., Bagaeva, A.A. et al. Lower Paleozoic Deposits in the Transition Zone between the Carbonate Platform and Black Shale Basin (Eastern Taimyr). Lithol Miner Resour 57, 44–61 (2022). https://doi.org/10.1134/S0024490222010035

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