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New paleomagnetic data from Late Neoproterozoic sedimentary successions in Southern Urals, Russia: implications for the Late Neoproterozoic paleogeography of the Iapetan realm

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Abstract

We present the results of paleomagnetic study of Ediacaran sedimentary successions from the Southern Urals. The analysis of the sedimentary rocks of the Krivaya Luka, Kurgashlya and Bakeevo Formations reveal stable mid-temperature and high-temperature remanence components. Mid-temperature components were acquired during Devonian (Bakeevo Formation) and Late Carboniferous–Early Permian remagnetization events. The high-temperature components in Kurgashlya and Bakeevo Formations are interpreted to be primary, because they are supported by a positive conglomerate test (Bakeevo Formation) and magnetostratigraphic pattern (Kurgashlya Formation). The high-temperature component in the Krivaya Luka Formation is interpreted to be a Late Ediacaran overprint. Our new paleomagnetic poles together with some previously published Ediacaran poles from Baltica and Laurentia are used herein to produce a series of paleogeographic reconstructions of the opening of the Iapetus Ocean.

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Acknowledgments

Richard Ernst and an anonymous reviewer, as well as the Guest Editor of this volume Brendan Murphy made valuable comments and suggestions for the paper which improved its clarity essentially and corrections in English are much appreciated. Paleogeographic reconstructions are made with free GPLATES software (http://www.gplates.org/). This is contribution 388 from the ARC Centre of Excellence for Core to Crust Fluid Systems and TIGeR publication # 501. This study funded by grant 14-05-00731 from the Russian Foundation of Basic Research.

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Lubnina, N.V., Pisarevsky, S.A., Puchkov, V.N. et al. New paleomagnetic data from Late Neoproterozoic sedimentary successions in Southern Urals, Russia: implications for the Late Neoproterozoic paleogeography of the Iapetan realm. Int J Earth Sci (Geol Rundsch) 103, 1317–1334 (2014). https://doi.org/10.1007/s00531-014-1013-x

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