Radioisotopic and biostratigraphic constraints on the classical Middle–Upper Permian succession and tetrapod fauna of the Moscow syneclise, Russia

V.I. Davydov; M.P. Arefiev; V.K. Golubev; E.V. Karasev; M.A. Naumcheva; M.D. Schmitz; V.V. Silantiev; V.V. Zharinova

doi:10.1130/G47172.1

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Research Article| April 29, 2020

Radioisotopic and biostratigraphic constraints on the classical Middle–Upper Permian succession and tetrapod fauna of the Moscow syneclise, Russia

V.I. Davydov;

V.I. Davydov

1

Department of Geosciences, Boise State University, Boise, Idaho 83725, USA

2

Institute of Geology and Petroleum Technology, Kazan Federal University, 18 Kremlyovskaya Street, Kazan, Republic of Tatarstan 420008, Russia

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M.P. Arefiev;

M.P. Arefiev

2

Institute of Geology and Petroleum Technology, Kazan Federal University, 18 Kremlyovskaya Street, Kazan, Republic of Tatarstan 420008, Russia

3

Geological Institute of Russian Academy of Sciences, Pyzhevsky lane 7, Moscow 119017, Russia

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V.K. Golubev;

V.K. Golubev

2

Institute of Geology and Petroleum Technology, Kazan Federal University, 18 Kremlyovskaya Street, Kazan, Republic of Tatarstan 420008, Russia

4

Borissiak Paleontological Institute of the Russian Academy of Sciences, Profsoyuznaya 123, Moscow 117647, Russia

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E.V. Karasev;

E.V. Karasev

2

Institute of Geology and Petroleum Technology, Kazan Federal University, 18 Kremlyovskaya Street, Kazan, Republic of Tatarstan 420008, Russia

4

Borissiak Paleontological Institute of the Russian Academy of Sciences, Profsoyuznaya 123, Moscow 117647, Russia

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M.A. Naumcheva;

M.A. Naumcheva

4

Borissiak Paleontological Institute of the Russian Academy of Sciences, Profsoyuznaya 123, Moscow 117647, Russia

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M.D. Schmitz;

M.D. Schmitz

1

Department of Geosciences, Boise State University, Boise, Idaho 83725, USA

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V.V. Silantiev;

V.V. Silantiev

2

Institute of Geology and Petroleum Technology, Kazan Federal University, 18 Kremlyovskaya Street, Kazan, Republic of Tatarstan 420008, Russia

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V.V. Zharinova

2

Institute of Geology and Petroleum Technology, Kazan Federal University, 18 Kremlyovskaya Street, Kazan, Republic of Tatarstan 420008, Russia

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Author and Article Information

V.I. Davydov

1

Department of Geosciences, Boise State University, Boise, Idaho 83725, USA

2

Institute of Geology and Petroleum Technology, Kazan Federal University, 18 Kremlyovskaya Street, Kazan, Republic of Tatarstan 420008, Russia

M.P. Arefiev

2

Institute of Geology and Petroleum Technology, Kazan Federal University, 18 Kremlyovskaya Street, Kazan, Republic of Tatarstan 420008, Russia

3

Geological Institute of Russian Academy of Sciences, Pyzhevsky lane 7, Moscow 119017, Russia

V.K. Golubev

2

Institute of Geology and Petroleum Technology, Kazan Federal University, 18 Kremlyovskaya Street, Kazan, Republic of Tatarstan 420008, Russia

4

Borissiak Paleontological Institute of the Russian Academy of Sciences, Profsoyuznaya 123, Moscow 117647, Russia

E.V. Karasev

2

Institute of Geology and Petroleum Technology, Kazan Federal University, 18 Kremlyovskaya Street, Kazan, Republic of Tatarstan 420008, Russia

4

Borissiak Paleontological Institute of the Russian Academy of Sciences, Profsoyuznaya 123, Moscow 117647, Russia

M.A. Naumcheva

4

Borissiak Paleontological Institute of the Russian Academy of Sciences, Profsoyuznaya 123, Moscow 117647, Russia

M.D. Schmitz

1

Department of Geosciences, Boise State University, Boise, Idaho 83725, USA

V.V. Silantiev

2

Institute of Geology and Petroleum Technology, Kazan Federal University, 18 Kremlyovskaya Street, Kazan, Republic of Tatarstan 420008, Russia

V.V. Zharinova

2

Institute of Geology and Petroleum Technology, Kazan Federal University, 18 Kremlyovskaya Street, Kazan, Republic of Tatarstan 420008, Russia

Publisher: Geological Society of America

Received: 05 Nov 2019

Revision Received: 28 Feb 2020

Accepted: 08 Mar 2020

First Online: 20 Jul 2023

Online ISSN: 1943-2682

Print ISSN: 0091-7613

Geology (2020) 48 (7): 742–747.

https://doi.org/10.1130/G47172.1

Abstract

The East European Platform and the PreUrals are the regions where the Permian System was first established, but the provincialism of fossils and lack of radioisotopic age control have prevented the use there of the regional Permian subdivisions used outside of the region. We report the first U-Pb zircon chemical abrasion–isotope dilution–thermal ionization mass spectrometry (CA-ID-TIMS) age of 253.95 ± 0.06 Ma for a volcanic tuff from the terrestrial upper part of the lower Vyatkian Regional Stage in the Moscow syneclise (Russia). This age greatly improves the correlation of the East European Platform and the PreUrals with the international geologic time scale, and contributes to our understanding of sedimentation within the Permian-Triassic transition in the studied region. The new radioisotopic age integrated within the regional chronostratigraphic framework reveals the synchrony in extinction of faunas of the Dinocephalian superassemblage in the studied region with that in South Africa.

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Radioisotopic and biostratigraphic constraints on the classical Middle–Upper Permian succession and tetrapod fauna of the Moscow syneclise, Russia

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Radioisotopic and biostratigraphic constraints on the classical Middle–Upper Permian succession and tetrapod fauna of the Moscow syneclise, Russia

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