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Late Vendian Kotlinian Crisis on the East European Platform : Lithogeochemical Indicators of Depositional Environment. / Maslov, A. V.; Grazhdankin, D. V.; Podkovyrov, V. N.

In: Lithology and Mineral Resources, Vol. 54, No. 1, 01.01.2019, p. 1-26.

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Maslov AV, Grazhdankin DV, Podkovyrov VN. Late Vendian Kotlinian Crisis on the East European Platform: Lithogeochemical Indicators of Depositional Environment. Lithology and Mineral Resources. 2019 Jan 1;54(1):1-26. doi: 10.1134/S0024490219010048

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Maslov, A. V. ; Grazhdankin, D. V. ; Podkovyrov, V. N. / Late Vendian Kotlinian Crisis on the East European Platform : Lithogeochemical Indicators of Depositional Environment. In: Lithology and Mineral Resources. 2019 ; Vol. 54, No. 1. pp. 1-26.

BibTeX

@article{1c6ce85dc7f34ec2a4e9b28f026d5332,
title = "Late Vendian Kotlinian Crisis on the East European Platform: Lithogeochemical Indicators of Depositional Environment",
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.",
keywords = "PLANKTONIC COMMUNITY STRUCTURE, CARBON-ISOTOPE EXCURSION, DEEP-SEA SEDIMENTS, DOUSHANTUO FORMATION, DETRITAL ZIRCONS, ORGANIC-MATTER, TRACE FOSSILS, SOUTH CHINA, OCEAN OXYGENATION, MARINE-SEDIMENTS",
author = "Maslov, {A. V.} and Grazhdankin, {D. V.} and Podkovyrov, {V. N.}",
year = "2019",
month = jan,
day = "1",
doi = "10.1134/S0024490219010048",
language = "English",
volume = "54",
pages = "1--26",
journal = "Lithology and Mineral Resources",
issn = "0024-4902",
publisher = "Maik Nauka-Interperiodica Publishing",
number = "1",

}

RIS

TY - JOUR

T1 - Late Vendian Kotlinian Crisis on the East European Platform

T2 - Lithogeochemical Indicators of Depositional Environment

AU - Maslov, A. V.

AU - Grazhdankin, D. V.

AU - Podkovyrov, V. N.

PY - 2019/1/1

Y1 - 2019/1/1

N2 - 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.

AB - 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.

KW - PLANKTONIC COMMUNITY STRUCTURE

KW - CARBON-ISOTOPE EXCURSION

KW - DEEP-SEA SEDIMENTS

KW - DOUSHANTUO FORMATION

KW - DETRITAL ZIRCONS

KW - ORGANIC-MATTER

KW - TRACE FOSSILS

KW - SOUTH CHINA

KW - OCEAN OXYGENATION

KW - MARINE-SEDIMENTS

UR - http://www.scopus.com/inward/record.url?scp=85063946767&partnerID=8YFLogxK

U2 - 10.1134/S0024490219010048

DO - 10.1134/S0024490219010048

M3 - Article

AN - SCOPUS:85063946767

VL - 54

SP - 1

EP - 26

JO - Lithology and Mineral Resources

JF - Lithology and Mineral Resources

SN - 0024-4902

IS - 1

ER -

ID: 25478795