Late Vendian Kotlinian Crisis on the East European Platform: Lithogeochemical Indicators of Depositional Environment View Full Text


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Article Info

DATE

2019-01

AUTHORS

A. V. Maslov, D. V. Grazhdankin, V. N. Podkovyrov

ABSTRACT

Sharp changes in the biodiversity of fossil organisms in the Upper Vendian of the East European Platform are considered as the manifestation of global crisis immediately prior to the “Cambrian Explosion.” However, they could be caused by local environmental perturbations. Variations of some lithogeochemical indicators of depositional environment (indicators of paleoclimate, exhalation activity, redox settings, and paleobioproductivity) were analyzed in order to establish the possible influence of sedimentary systems on evolutionary processes in the Late Vendian and at the boundary with the Cambrian. The applied algorithm of lithogeochemical studies revealed no significant perturbations in physical properties of the environment on a scale of sedimentary basins. The obtained data suggest that local factors did not affect the evolution of Ediacaran biota on the East European Platform and confirm the global nature of transitions between the Redkinian, Belomorian, and Kotlinian biotas. More... »

PAGES

1-26

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  • Identifiers

    URI

    http://scigraph.springernature.com/pub.10.1134/s0024490219010048

    DOI

    http://dx.doi.org/10.1134/s0024490219010048

    DIMENSIONS

    https://app.dimensions.ai/details/publication/pub.1113204493


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    384 https://www.grid.ac/institutes/grid.426536.0 schema:alternateName Ural Branch of the Russian Academy of Sciences
    385 schema:name Zavaritsky Institute of Geology and Geochemistry, Ural Branch of the Russian Academy of Sciences, ul. Vonsovskogo 15, 620075, Yekaterinburg, Russia
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    387 https://www.grid.ac/institutes/grid.465386.a schema:alternateName Institute of Precambrian Geology and Geochronology
    388 schema:name Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, nab. Makarova 2, 199034, St. Petersburg, Russia
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