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Detrital zircon age and biostratigraphic and chemostratigraphic constraints on the Ediacaran–Cambrian transitional interval in the Irkutsk Cis–Sayans Uplift, southwestern Siberian Platform

Published online by Cambridge University Press:  02 December 2020

Vasiliy V. Marusin Open the ORCID record for Vasiliy V. Marusin [Opens in a new window] ,
Alena A. Kolesnikova ,
Boris B. Kochnev ,
Nikolay B. Kuznetsov ,
Boris G. Pokrovsky ,
Tatiana V. Romanyuk ,
Galina A. Karlova ,
Sergey V. Rud’ko ,
Andrey V. Shatsillo  and
Alexander S. Dubenskiy
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Vasiliy V. Marusin*
Affiliation:
Department of Stratigraphy and Sedimentology, Trofimuk Institute of Petroleum Geology and Geophysics of SB RAS, Akademika Koptyuga Prospect 3, Novosibirsk630090, Russia Department of Geology and Geophysics, Novosibirsk State University, Pirogova Street 1, Novosibirsk630090, Russia
Alena A. Kolesnikova
Affiliation:
Geological Institute of RAS, Pyzhevsky Lane 7, Moscow119017, Russia
Boris B. Kochnev
Affiliation:
Department of Stratigraphy and Sedimentology, Trofimuk Institute of Petroleum Geology and Geophysics of SB RAS, Akademika Koptyuga Prospect 3, Novosibirsk630090, Russia Department of Geology and Geophysics, Novosibirsk State University, Pirogova Street 1, Novosibirsk630090, Russia
Nikolay B. Kuznetsov
Affiliation:
Geological Institute of RAS, Pyzhevsky Lane 7, Moscow119017, Russia Institute of the Earth’s Crust of SB RAS, Lermontova Street 128, Irkutsk664033, Russia
Boris G. Pokrovsky
Affiliation:
Geological Institute of RAS, Pyzhevsky Lane 7, Moscow119017, Russia
Tatiana V. Romanyuk
Affiliation:
Schmidt Institute of Physics of the Earth of RAS, Bol’shaya Gruzinskaya Street 10/1, Moscow123995, Russia
Galina A. Karlova
Affiliation:
Department of Stratigraphy and Sedimentology, Trofimuk Institute of Petroleum Geology and Geophysics of SB RAS, Akademika Koptyuga Prospect 3, Novosibirsk630090, Russia
Sergey V. Rud’ko
Affiliation:
Geological Institute of RAS, Pyzhevsky Lane 7, Moscow119017, Russia Institute of the Earth’s Crust of SB RAS, Lermontova Street 128, Irkutsk664033, Russia
Andrey V. Shatsillo
Affiliation:
Institute of the Earth’s Crust of SB RAS, Lermontova Street 128, Irkutsk664033, Russia Schmidt Institute of Physics of the Earth of RAS, Bol’shaya Gruzinskaya Street 10/1, Moscow123995, Russia
Alexander S. Dubenskiy
Affiliation:
Geological Institute of RAS, Pyzhevsky Lane 7, Moscow119017, Russia
Victor S. Sheshukov
Affiliation:
Geological Institute of RAS, Pyzhevsky Lane 7, Moscow119017, Russia
Sergey M. Lyapunov
Affiliation:
Geological Institute of RAS, Pyzhevsky Lane 7, Moscow119017, Russia
*
Author for correspondence: Vasiliy V. Marusin, Email: [email protected]
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Abstract

A number of ecological and geochemical transformations occurred during late Ediacaran and early Cambrian time, the effects of which are difficult to overestimate. However, the strong linkage of biostratigraphic and chemostratigraphic methods with lithofacies makes the localization of the Precambrian–Cambrian boundary and its correlation with lithologically contrasting sections highly debatable. We analyse the taxonomy and stratigraphic distribution of small skeletal fossils and trace fossils, the carbonate carbon and oxygen isotope composition, and U–Pb detrital zircon age in the Ediacaran–Cambrian transitional interval of the Irkutsk Cis–Sayans Uplift (southwestern Siberian Platform). This interval (Moty Group) comprises a transgressive succession with red-coloured alluvial to deltaic siliciclastic deposits (Shaman Formation) and overlying shallow-marine carbonates (Irkut Formation). The lower Irkut Formation hosts sporadic and poorly preserved tubular Cambrotubulus fossils, which are known from both the terminal Ediacaran Period (c. 550–541 Ma) and the Terreneuvian Epoch (541–521 Ma), and typical Fortunian trace fossils, including an index ichnotaxon of the Cambrian boundary Treptichnus pedum. The biostratigraphic and carbonate carbon isotope data and U–Pb concordia ages of 531.1 ± 5.2 Ma (mean weighted, 530.6 ± 5.3 Ma) of the five youngest zircon grains from the lower Irkut Formation indicate that at least the shallow-marine carbonates of the upper Moty Group correspond to the Cambrian Stage 2 (c. 529–521 Ma). In the Irkutsk Cis–Sayans Uplift, the Cambrian Period tentatively began before or during the accumulation of the alluvial to deltaic siliciclastic Khuzhir and Shaman formations, and this crucial divide remained unmarked in the palaeontological and isotopic records.

Keywords

trace fossilssmall skeletal fossilscarbon isotopesdetrital zirconTerreneuviansouth Siberian Platform
Type
Original Article
Information
Geological Magazine , Volume 158 , Issue 7 , July 2021 , pp. 1156 - 1172
Copyright
© The Author(s), 2020. Published by Cambridge University Press

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References

Andersen, T (2005) Detrital zircons as tracers of sedimentary provenance: limiting conditions from statistics and numerical simulation. Chemical Geology 216, 249–70.CrossRefGoogle Scholar
Astashkin, VA, Pegel, TV, Shabanov, YY, Sukhov, SS, Sundukov, VM, Repina, LN, Rozanov, AY and Zhuravlev, AY (1991) The Cambrian System on the Siberian Platform: Correlation Chart and Explanatory notes. Herdon: International Union of Geological Sciences, Publication 27, 133 pp.Google Scholar
Babcock, LE, Peng, S, Zhu, M, Xiao, S and Ahlberg, P (2014) Proposed reassessment of the Cambrian GSSP. Journal of African Earth Sciences 98, 3–10.CrossRefGoogle Scholar
Boggiani, PC, Gaucher, C, Sial, AN, Babinski, M, Simon, CM, Riccomini, C, Ferreira, VP and Fairchild, TR (2010) Chemostratigraphy of the Tamengo Formation (Corumbá Group, Brazil): a contribution to the calibration of the Ediacaran carbon-isotope curve. Precambrian Research 182, 382–401.CrossRefGoogle Scholar
Bowring, SA, Grotzinger, JP, Condon, DJ, Ramezani, J, Newall, MJ and Allen, PA (2007) Geochronologic constraints on the chronostratigraphic framework of the Neoproterozoic Huqf Supergroup, Sultanate of Oman. American Journal of Science 307, 1097–145.CrossRefGoogle Scholar
Brasier, M, Cowie, J and Taylor, M (1994) Decision on the Precambrian–Cambrian boundary stratotype. Episodes 17, 3–9.CrossRefGoogle Scholar
Brasier, MD, Khomentovsky, VV and Corfield, RM (1993) Stable isotopic calibration of the earliest skeletal fossil assemblages in eastern Siberia (Precambrian-Cambrian boundary). Terra Nova 5, 225–32.CrossRefGoogle Scholar
Buatois, LA (2017) Treptichnus pedum and the Ediacaran–Cambrian boundary: significance and caveats. Geological Magazine 155, 174–80.CrossRefGoogle Scholar
Buatois, LA, Almond, J and Germs, GJB (2013) Environmental tolerance and range offset of Treptichnus pedum: implications for the recognition of the Ediacaran-Cambrian boundary. Geology 41, 519–22.CrossRefGoogle Scholar
Buatois, LA, Gingras, MK, MacEachern, J, Mángano, MG, Zonneveld, J-P, Pemberton, SG, Netto, RG and Martin, A (2005) Colonization of brackish-water systems through time: evidence from the trace-fossil record. PALAIOS 20, 321–47.CrossRefGoogle Scholar
Buatois, LA, Mángano, MG, Minter, NJ, Zhou, K, Wisshak, M, Wilson, MA and Olea, RA (2020) Quantifying ecospace utilization and ecosystem engineering during the early Phanerozoic – The role of bioturbation and bioerosion. Science Advances 6, eabb0618.CrossRefGoogle ScholarPubMed
Chechel’, EI (1976) A find of Cyclomedusa in the Ostrov Formation deposits of the Enisey Ridge. Geologiya i Geofizika 17, 118–20 [in Russian].Google Scholar
Dickinson, WR and Gehrels, GE (2009) Use of U–Pb ages of detrital zircons to infer maximum depositional ages of strata: a test against a Colorado Plateau Mesozoic database. Earth and Planetary Science Letters 288, 115–25.CrossRefGoogle Scholar
Elhlou, S, Belousova, E, Griffin, WL, Pearson, NJ and Riley, SY (2006) Trace element and isotopic composition of GJ-red zircon standard by laser ablation. Geochimica et Cosmochimica Acta 70, A158.CrossRefGoogle Scholar
Erwin, DH and Valentine, JW (2013) The Cambrian Explosion: The Construction of Animal Biodiversity. Englewood: Roberts and Company Publishers Inc., 416 pp.Google Scholar
Fisher, RA and Yates, F (1974) Statistical Tables for Biological, Agricultural and Medical Research, 6th Ed. London: Longman, 156 pp.Google Scholar
Friedman, I, O’Neil, J and Cebula, G (1982) Two new carbonate stable isotope standards. Geostandards Newsletter 6, 11–2.CrossRefGoogle Scholar
Gehrels, G (2012) Detrital zircon U–Pb geochronology: current methods and new opportunities. In Tectonics of Sedimentary Basins (eds Busby, C and Azor, A), pp. 47–62. Hoboken, New Jersey: John Wiley & Sons.Google Scholar
Gehrels, GE, Valencia, VA and Ruiz, J (2008) Enhanced precision, accuracy, efficiency, and spatial resolution of U-Pb ages by laser ablation–multicollector-inductively coupled plasma mass spectrometry. Geochemistry, Geophysics, Geosystems 9, Q03017.CrossRefGoogle Scholar
Gladkochub, DP, Donskaya, TV, Stanevich, AM, Pisarevsky, SA, Zhang, S, Motova, ZL, Mazukabzov, AM and Li, H (2019) U–Pb detrital zircon geochronology and provenance of Neoproterozoic sedimentary rocks in southern Siberia: new insights into breakup of Rodinia and opening of Paleo-Asian Ocean. Gondwana Research 65, 1–16.CrossRefGoogle Scholar
Gladkochub, DP, Stanevich, AM, Mazukabzov, AM, Donskaya, TV, Pisarevsky, SA, Nicoll, G, Motova, ZL and Kornilova, TA (2013) Early evolution of the Paleoasian ocean: LA-ICP-MS dating of detrital zircon from Late Precambrian sequences of the southern margin of the Siberian craton. Russian Geology and Geophysics 54, 1150–163.CrossRefGoogle Scholar
Gougeon, RC, Mángano, MG, Buatois, LA, Narbonne, GM and Laing, BA (2018) Early Cambrian origin of the shelf sediment mixed layer. Nature Communications 9, 1909.CrossRefGoogle ScholarPubMed
Grazhdankin, DV, Kontorovich, AE, Kontorovich, VA, Saraev, SV, Filippov, YF, Efimov, AS, Karlova, GA, Kochnev, BB, Nagovitsin, KE, Terleev, AA and Fedyanin, GO (2015) Vendian of the Fore-Yenisei sedimentary basin (southeastern West Siberia). Russian Geology and Geophysics 56, 560–72.CrossRefGoogle Scholar
Grazhdankin, DV, Marusin, VV, Izokh, OP, Karlova, GA, Kochnev, BB, Markov, GE, Nagovitsin, KE, Sarsembaev, Z, Peek, S, Cui, H and Kaufman, AJ (2020) Quo vadis, Tommotian? Geological Magazine 157, 22–34.CrossRefGoogle Scholar
Griffin, WL, Powell, WJ, Pearson, NJ and O’Reilly, SY (2008) GLITTER: Data reduction software for laser ablation ICP-MS. In Laser Ablation ICP-MS in the Earth Sciences: Current Practices and Outstanding Issues (ed. Sylvester, PJ), pp. 308–11. Quebec: Mineralogical Association of Canada, Short Course Series no. 40.Google Scholar
Grotzinger, JP, Bowring, SA, Saylor, BZ and Kaufman, AJ (1995) Biostratigraphic and geochronologic constraints on early animal evolution. Science 270, 598–604.CrossRefGoogle Scholar
Hantsoo, KG, Kaufman, AJ, Cui, H, Plummer, RE and Narbonne, GM (2018) Effects of bioturbation on carbon and sulfur cycling across the Ediacaran-Cambrian transition at the GSSP in Newfoundland, Canada. Canadian Journal of Earth Sciences 55, 1240–52.CrossRefGoogle Scholar
Horstwood, MSA, Košler, J, Gehrels, G, Jackson, SE, McLean, NM, Paton, C, Pearson, NJ, Sircombe, K, Sylvester, P, Vermeesch, P, Bowring, JF, Condon, DJ and Schoene, B (2016) Community-derived standards for LA-ICP-MS U-(Th-)Pb geochronology – uncertainty propagation, age interpretation and data reporting. Geostandards and Geoanalytical Research 40, 311–32.CrossRefGoogle Scholar
Jackson, SE, Pearson, NJ, Griffin, WL and Belousova, EA (2004) The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U–Pb zircon geochronology. Chemical Geology 211, 47–69.CrossRefGoogle Scholar
Jensen, S (1997) Trace fossils from the Lower Cambrian Mickwitzia sandstone, south-central Sweden. Fossils and Strata 42, 110.Google Scholar
Jensen, S (2003) The Proterozoic and earliest Cambrian trace fossil record; patterns, problems and perspectives. Integrative and Comparative Biology 43, 219–28.CrossRefGoogle Scholar
Jensen, S, Saylor, BZ, Gehling, JG and Germs, GJB (2000) Complex trace fossils from the terminal Proterozoic of Namibia. Geology 28, 143–6.2.0.CO;2>CrossRefGoogle Scholar
Kaufman, AJ and Knoll, AH (1995) Neoproterozoic variations in the C-isotopic composition of seawater: stratigraphic and biogeochemical implications. Precambrian Research 72, 27–49.CrossRefGoogle Scholar
Kaufman, AJ, Knoll, AH, Semikhatov, MA, Grotzinger, JP, Jacobsen, SB and Adams, W (1996) Integrated chronostratigraphy of Proterozoic-Cambrian boundary beds in the western Anabar region, northern Siberia. Geological Magazine 133, 509–33.CrossRefGoogle Scholar
Khomentovsky, VV, Faizulin, MS and Karlova, GA (1998a) The Nemakit-Daldynian Stage of Vendian in the southwestern Siberian Platform. Doklady Earth Sciences 363, 1075–7.Google Scholar
Khomentovsky, VV, Fedorov, AB and Karlova, GA (1998b) The Lower Cambrian boundary in inner areas of the north Siberian Platform. Stratigraphy and Geological Correlation 6, 3–9.Google Scholar
Khomentovsky, VV and Karlova, GA (1993) Biostratigraphy of the Vendian-Cambrian beds and the lower Cambrian boundary in Siberia. Geological Magazine 130, 29–45.CrossRefGoogle Scholar
Khomentovsky, VV and Karlova, GA (2002) The boundary between Nemakit-Daldynian and Tommotian Stages (Vendian–Cambrian Systems) of Siberia. Stratigraphy and Geological Correlation 10, 217–38.Google Scholar
Khomentovsky, VV and Karlova, GA (2005) The Tommotian Stage base as the Cambrian lower boundary in Siberia. Stratigraphy and Geological Correlation 13, 21–34.Google Scholar
Khomentovsky, VV, Shenfil’, VY, Yakshin, MS and Butakov, EP (1972) Base Sections of Upper Precambrian and Lower Cambrian Deposits of the Siberian Platform. Nauka: Moscow, 356 pp. [in Russian].Google Scholar
Kochnev, BB and Karlova, GA (2010) New data on biostratigraphy of the Vendian Nemakit-Daldynian Stage in the southern Siberian Platform. Stratigraphy and Geological Correlation 18, 492–504.CrossRefGoogle Scholar
Kochnev, BB, Pokrovsky, BG, Kuznetsov, AB and Marusin, VV (2018) C- and Sr- isotope chemostratigraphy of Vendian-Lower Cambrian carbonates of central Siberian Platform. Russian Geology and Geophysics 59, 585–605.CrossRefGoogle Scholar
Kouchinsky, A, Bengtson, S, Pavlov, V, Runnegar, B, Torssander, P, Young, E and Ziegler, K (2007) Carbon isotope stratigraphy of the Precambrian-Cambrian Sukharikha River section, northwestern Siberian platform. Geological Magazine 144, 609–18.CrossRefGoogle Scholar
Kouchinsky, A, Bengtson, S, Runnegar, B, Skovsted, C, Steiner, M and Vendrasco, M (2012) Chronology of early Cambrian biomineralization. Geological Magazine 149, 221–51.CrossRefGoogle Scholar
Krasnov, VI, Savitsky, VE, Tesakov, YI and Khomentovsky, VV (eds) (1983) Resolution of the USSR Stratigraphic Conference on the Precambrian, Palaeozoic and Quaternary Systems of Central Siberia. Part 1. Upper Precambrian. Lower Palaeozoic. Novosibirsk: SNIIGGiMS, 215 pp. [in Russian].Google Scholar
Landing, E, Geyer, G, Brasier, MD and Bowring, SA (2013) Cambrian evolutionary radiation: context, correlation, and chronostratigraphy – overcoming deficiencies of the first appearance datum (FAD) concept. Earth-Science Reviews 123, 133–72.CrossRefGoogle Scholar
Lenton, TM and Daines, SJ (2018) The effects of marine eukaryote evolution on phosphorus, carbon and oxygen cycling across the Proterozoic–Phanerozoic transition. Emerging Topics in Life Sciences 2, 267–78.Google ScholarPubMed
Letnikova, EF, Kuznetsov, AB, Vishnevskaya, IA, Veshcheva, SV, Proshenkin, AI and Geng, H (2013) The Vendian passive continental margin in the southern Siberian Craton: geochemical and isotopic (Sr, Sm–Nd) evidence and U–Pb dating of detrital zircons by the LA-ICP-MS method. Russian Geology and Geophysics 54, 1177–94.CrossRefGoogle Scholar
Li, D, Ling, H-F, Shields-Zhou, GA, Chen, X, Cremonese, L, Och, L, Thirlwall, M and Manning, CJ (2013) Carbon and strontium isotope evolution of seawater across the Ediacaran-Cambrian transition: Evidence from the Xiaotan section, NE Yunnan, South China. Precambrian Research 225, 128–47.CrossRefGoogle Scholar
Linnemann, U, Ovtcharova, M, Schaltegger, U, Gärtner, A, Hauntmann, M, Geyer, G, Vickers-Rich, P, Rich, T, Plessen, B, Hofmann, M, Zieger, J, Krause, R, Kreisfeld, L and Smith, J (2019) New high-resolution age data from the Ediacaran-Cambrian boundary indicate rapid, ecologically driven onset of the Cambrian explosion. Terra Nova 31, 49–58.CrossRefGoogle Scholar
Liu, AG, Brasier, MD, Bogolepova, OK, Raevskaya, EG and Gubanov, AP (2013) First report of a newly discovered Ediacaran biota from the Irkineeva Uplift, East Siberia. Newsletters on Stratigraphy 46, 95–110.CrossRefGoogle Scholar
Ludwig, KR (2012) User’s Manual for Isoplot Version 3.75–4.15: A Geochronological Toolkit for Microsoft Excel. Berkeley: Berkeley Geochronology Center, Special Publication no. 5, 75 p.Google Scholar
MacNaughton, RB and Narbonne, GM (1999) Evolution and ecology of Neoproterozoic-Lower Cambrian trace fossils, NW Canada. PALAIOS 14, 97–115.CrossRefGoogle Scholar
Maloof, AC, Porter, SM, Moore, JL, Dudás, FӦ, Bowring, SA, Higgins, JA, Fike, DA and Eddy, MP (2010) The earliest Cambrian record of animals and ocean geochemical change. GSA Bulletin 122, 1731–74.CrossRefGoogle Scholar
Mángano, MG and Buatois, LA (2014) Decoupling of body-plan diversification and ecological structuring during the Ediacaran-Cambrian transition: evolutionary and geobiological feedbacks. Proceedings of the Royal Society B 281, 20140038.CrossRefGoogle ScholarPubMed
Mángano, MG and Buatois, LA (2017) The Cambrian revolutions: trace-fossil record, timing, links and geobiological impact. Earth-Science Reviews 173, 96–108.CrossRefGoogle Scholar
Marusin, VV, Kochnev, BB, Karlova, GA and Nagovitsin, KE (2019) Resolving Terreneuvian stratigraphy in subtidal-intertidal carbonates: palaeontological and chemostratigraphical evidence from the Turukhansk Uplift, Siberian Platform. Lethaia 52, 464–85.CrossRefGoogle Scholar
McIlroy, D and Brasier, MD (2016) Ichnological evidence for the Cambrian explosion in the Ediacaran to Cambrian succession of Tanafjord, Finnmark, northern Norway. In Earth System Evolution and Early Life: a Celebration of the Work of Martin Brasier (eds Brasier, AT, McIlroy, D and McLoughlin, N), pp. 351–68. Geological Society of London, Special Publication no. 448.Google Scholar
Melnikov, NV, Yakshin, MS, Shishkin, BB, Efimov, AO, Karlova, GA, Kilina, LI, Konstantinova, LN, Kochnev, BB, Kraevskiy, BG, Melnikov, PN, Nagovitsyn, KE, Postnikov, AA, Ryabkova, LV, Terleev, AA and Khabarov, EM (2005) Stratigraphy of Oil and Gas Basins of Siberia. Riphean and Vendian of Siberian Platform and the Adjacent Folded Belts. Novosibirsk: Academic Publishing House ‘Geo’, 428 pp. [in Russian].Google Scholar
Minter, NJ, Buatois, LA, Mángano, MG, Davies, NS, Gibling, MR, MacNaughton, RB and Labandeira, CC (2017) Early bursts of diversification defined the faunal colonization of land. Nature Ecology & Evolution 1, 0175.CrossRefGoogle Scholar
Minter, NJ, Buatois, LA, Mángano, MG, MacNaughton, RB, Davies, NS and Gibling, MR (2016) The prelude to continental invasion. In The Trace-Fossil Record of Major Evolutionary Events (eds Mángano, MG and Buatois, LA), pp. 157–204. Dordrecht: Springer, Topics in Geobiology no. 39.CrossRefGoogle Scholar
Moczydłowska, M (1991) Acritarch biostratigraphy of the Lower Cambrian and the Precambrian–Cambrian boundary in the southeastern Poland. Fossils and Strata 29, 1–127.Google Scholar
Moczydłowska, M (1998) Cambrian acritarchs from Upper Silesia, Poland: biochronology and tectonic implications. Fossils and Strata 46, 1–121.Google Scholar
Nagovitsin, KE, Rogov, VI, Marusin, VV, Karlova, GA, Kolesnikov, AV, Bykova, NV and Grazhdankin, DV (2015) Revised Neoproterozoic and Terreneuvian stratigraphy of the Lena-Anabar Basin and northwestern slope of the Olenek Uplift, Siberian Platform. Precambrian Research 270, 226–45.CrossRefGoogle Scholar
Nemchin, AA and Cawood, PA (2005) Discordance of the U–Pb system in detrital zircons: Implication for provenance studies of sedimentary rocks. Sedimentary Geology 182, 143–62.CrossRefGoogle Scholar
Nikishin, AM, Romanyuk, TV, Moskovsky, DV, Kuznetsov, NB, Kolesnikova, AA, Dubensky, AS, Sheshukov, VS and Lyapunov, SM (2020) The Upper Triassic strata of the Mountaineous Crimea: the first results of U-Pb dating of detrital zircons. Moscow University Geology Bulletin 2, 18–33.Google Scholar
Pelechaty, SM, Grotzinger, JP, Kashirtsev, VA and Zhernovsky, VP (1996) Chemostratigraphic and sequence stratigraphic constraints on Vendian-Cambrian basin dynamics, northeast Siberian Craton. The Journal of Geology 104, 543–63.CrossRefGoogle Scholar
Peng, S, Babcock, LE and Cooper, RA (2012) The Cambrian Period. In The Geologic Time Scale 2012 (eds Gradstein, FM, Ogg, JG, Schmitz, MD and Ogg, GM), pp. 437–88. Amsterdam: Elsevier.CrossRefGoogle Scholar
Peters, SE and Gaines, RR (2012) Formation of the Great Unconformity as a trigger for the Cambrian explosion. Nature 484, 363–7.CrossRefGoogle ScholarPubMed
Pisarchik, YK (1963) Lithology and Facies of Lower and Middle Cambrian Strata of the Irkutsk Amphitheatre in a Context of their Oil- and Salt-Bearing Capability. Moscow: Gostoptekhizdat, 346 pp. [in Russian].Google Scholar
Pokrovsky, BG, Bujakaite, MI and Kokin, OV (2012) Geochemistry of C, O, and Sr isotopes and chemostratigraphy of Proterozoic rocks in the Northern Yenisei Ridge. Lithology and Mineral Resources 47, 177–99.CrossRefGoogle Scholar
Priyatkina, N, Collins, WJ, Khudoley, AK, Letnikova, EF and Huang, H-Q (2018) The Neoproterozoic evolution of the western Siberian Craton margin: U-Pb-Hf isotopic records of detrital zircons from the Yenisey Ridge and the Prisayan Uplift. Precambrian Research 305, 197–217.CrossRefGoogle Scholar
Romanyuk, TV, Kuznetsov, NB, Belousova, EA, Gorozhanin, VM and Gorozhanina, EN (2018) Paleotectonic and paleogeographic conditions for the accumulation of the Lower Riphean Ai Formation in the Bashkir Uplift (Southern Urals): the Terranechrone® detrital zircon study. Geodynamics & Tectonophysics 9, 1–37 [in Russian with English abstract].CrossRefGoogle Scholar
Rozanov, AYu (1992) Some problems concerning the Precambrian–Cambrian transition and the Cambrian faunal radiation. Journal of the Geological Society, London 149, 593–8.CrossRefGoogle Scholar
Rozanov, AY, Missarzhevsky, VV, Volkova, NA, Voronova, LG, Krylov, IN, Keller, BM, Korolyuk, IK, Lendzion, K, Michniak, R, Pyhova, NG and Sidorov, AD (1969) The Tommotian Stage and the Cambrian Lower Boundary Problem. Moscow: Nauka, 380 pp. [in Russian].Google Scholar
Rozanov, AY, Semikhatov, MA, Sokolov, BS, Fedonkin, MA and Khomentovskii, VV (1997) The decision on the Precambrian–Cambrian boundary stratotype: a breakthrough or misleading action? Stratigraphy and Geological Correlation 5, 19–28.Google Scholar
Shahkarami, S, Buatois, LA, Mángano, MG, Hagadorn, JW and Almond, J (2020) The Ediacaran–Cambrian boundary: evaluating stratigraphic completeness and the Great Unconformity. Precambrian Research 345, 105721.CrossRefGoogle Scholar
Shenfil’, VY (1991) The Late Precambrian of the Siberian Platform. Novosibirsk: Nauka, 184 pp. [in Russian].Google Scholar
Sláma, J, Košler, J, Condon, DJ, Crowley, JL, Gerdes, A, Hanchar, JM, Horstwood, MSA, Morris, GA, Nasdala, L, Norberg, N, Schaltegger, U, Schoene, B, Tubrett, MN and Whitehouse, MJ (2008) Plešovice zircon — A new natural reference material for U–Pb and Hf isotopic microanalysis. Chemical Geology 249, 1–35.CrossRefGoogle Scholar
Smith, EF, Macdonald, FA, Petach, TA, Bold, U and Schrag, DP (2016) Integrated stratigraphic, geochemical, and paleontological late Ediacaran to early Cambrian records from southwestern Mongolia. GSA Bulletin 128, 442–68.CrossRefGoogle Scholar
Sovetov, JK (1977) Upper Precambrian Sandstones of the Southwestern Siberian Platform. Novosibirsk: Nauka, 295 pp. [in Russian].Google Scholar
Sovetov, JK (2002) Vendian foreland basin of the Siberian cratonic margin: Paleopangean accretionary phases. Russian Journal of Earth Sciences 4, 363–87.CrossRefGoogle Scholar
Sovetov, JK (2018) Sedimentology and stratigraphic correlation of Vendian deposits in the southwestern Siberian Craton: major contribution of an exocratonic clastic source to sedimentary systems. Lithosfera 18, 20–45 [in Russian with English abstract].Google Scholar
Sovetov, JK and Jensen, S (2010) Lower Cambrian boundary in the northwestern Siberian Platform: new paleontological and sedimentological data. In Geodynamic Evolution of Lithosphere of the Central Asian Foldbelt (From Ocean to Continent), vol. 2. Irkutsk: Institute of the Earth’s Crust of SB RAS, pp. 87–9 [in Russian].Google Scholar
Sukhov, SS, Shabanov, YY, Pegel, TV, Saraev, SV, Filippov, YF, Korovnikov, IV, Sundukov, VM, Fedorov, AB, Varlamov, AI, Efimov, AS, Kontorovich, VA and Kontorovich, AE (2016) Stratigraphy of Oil and Gas Basins of Siberia. Cambrian of Siberian Platform. Vol. 1 Stratigraphy. Novosibirsk: Trofimuk Institute of Petroleum Geology and Geophysics of SB RAS, 497 pp. [in Russian].Google Scholar
Tsukui, K, Isozaki, Y, Zhu, M, Ramezani, J, Sato, T, Zhang, X and Bowring, SA (2017) High-precision U-Pb temporal constraints on the Early Cambrian diversification of animal life from eastern Yunnan. In Proceedings of JpGU–AGU Joint Meeting 2017, Chiba. Makuhari Messe: Japanese Geoscience Union, BCG09-01.Google Scholar
Vernikovsky, VA, Kazansky, AY, Matushkin, NY, Metelkin, DV and Sovetov, JK (2009) The geodynamic evolution of the folded framing and the western margin of the Siberian craton in the Neoproterozoic: geological, structural, sedimentological, geochronological, and paleomagnetic data. Russian Geology and Geophysics 50, 380–93.CrossRefGoogle Scholar
Vinogradov, VI, Belenitskaya, GA, Bujakaite, MI, Kuleshov, VN, Minaeva, MA and Pokrovskii, BG (2006) Isotopic signatures of deposition and transformation of Lower Cambrian saliferous rocks in the Irkutsk Amphitheatre: Communication 3. Carbon and oxygen isotopic compositions in carbonates. Lithology and Mineral Resources 41, 271–9.CrossRefGoogle Scholar
Walter, MR, Elphinstone, R and Heys, GR (1989) Proterozoic and Early Cambrian trace fossils from the Amadeus and Georgina Basins, central Australia. Alcheringa 13, 209–56.CrossRefGoogle Scholar
Wiedenbeck, M, Allé, P, Corfu, F, Griffin, WL, Meier, M, Oberli, F, von Quadt, A, Roddick, JC and Spiegel, W (1995) Three natural zircon standards for U–Th–Pb, Lu–Hf, trace-element and REE analyses. Geostandards Newsletter 19, 1–23.CrossRefGoogle Scholar
Wiedenbeck, M, Hanchar, JM, Peck, WH, Sylvester, P, Valley, J, Whitehouse, M, Kronz, A, Morishita, Y, Nasdala, L, Fiebig, J, Franchi, I, Girard, J-P, Greenwood, RC, Hinton, R, Kita, N, Mason, PRD, Norman, M, Ogasawara, M, Piccoli, PM, Rhede, D, Satoh, H, Schulz-Dobrick, B, Skår, Ø, Spicuzza, MJ, Terada, K, Tindle, A, Togashi, S, Vennemann, T, Xie, Q and Zheng, Y-F (2004) Further characterisation of the 91500 zircon crystal. Geostandards and Geoanalytical Research 28, 9–39.CrossRefGoogle Scholar
Wood, R, Liu, AG, Bowyer, F, Wilby, PR, Dunn, FS, Kenchington, CG, Cuthill, JFH, Mitchell, EG and Penny, A (2019) Integrated records of environmental change and evolution challenge the Cambrian Explosion. Nature Ecology & Evolution 3, 528–38.CrossRefGoogle ScholarPubMed
Yang, B, Steiner, M, Li, G and Keupp, H (2014) Terreneuvian small shelly faunas of East Yunnan (South China) and their biostratigraphic implications. Palaeogeography, Palaeoclimatology, Palaeoecology 398, 28–58.CrossRefGoogle Scholar
Yao, J, Xiao, S, Yin, L, Li, G and Yuan, X (2005) Basal Cambrian microfossils from the Yurtus and Xishanblaq formations (Tarim, North-West China): Systematic revision and biostratigraphic correlation of Micrhystridium-like acritarchs. Palaeontology 48, 687–708.CrossRefGoogle Scholar
Yuan, H-L, Gao, S, Dai, M-N, Zong, C-L, Günther, D, Fontaine, GH, Liu, X-M and Diwu, C (2008) Simultaneous determinations of U–Pb age, Hf isotopes and trace element compositions of zircon by excimer laser-ablation quadrupole and multiple-collector ICP-MS. Chemical Geology 247, 100–18.CrossRefGoogle Scholar
Zhu, M, Babcock, LE and Peng, S (2006) Advances in Cambrian stratigraphy and paleontology: integrating correlation techniques, paleobiology, taphonomy and paleoenvironmental reconstruction. Palaeoworld 15, 217–22.CrossRefGoogle Scholar
Zhu, M, Yang, A, Yuan, J, Li, G, Zhang, J, Zhao, F, Ahn, S-Y and Miao, L (2018) Cambrian integrative stratigraphy and timescale of China. Science China Earth Sciences 62, 25–60.CrossRefGoogle Scholar
Zhu, M, Zhuravlev, AY, Wood, RA, Zhao, F and Sukhov, SS (2017) A deep root for the Cambrian explosion: implications of new bio and chemostratigraphy from the Siberian Platform. Geology 45, 459–62.CrossRefGoogle Scholar
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