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First findings of dinocysts in the upper Oligocene Turtas formation in Southern Tyumen oblast (West Siberia). / Kuzmina, O. B.; Shurygin, B. N.

In: Doklady Earth Sciences, Vol. 467, No. 2, 01.04.2016, p. 341-345.

Research output: Contribution to journal › Article › peer-review

Harvard

Kuzmina, OB & Shurygin, BN 2016, 'First findings of dinocysts in the upper Oligocene Turtas formation in Southern Tyumen oblast (West Siberia)', Doklady Earth Sciences, vol. 467, no. 2, pp. 341-345. https://doi.org/10.1134/S1028334X1604019X

APA

Kuzmina, O. B., & Shurygin, B. N. (2016). First findings of dinocysts in the upper Oligocene Turtas formation in Southern Tyumen oblast (West Siberia). Doklady Earth Sciences, 467(2), 341-345. https://doi.org/10.1134/S1028334X1604019X

Vancouver

Kuzmina OB, Shurygin BN. First findings of dinocysts in the upper Oligocene Turtas formation in Southern Tyumen oblast (West Siberia). Doklady Earth Sciences. 2016 Apr 1;467(2):341-345. doi: 10.1134/S1028334X1604019X

Author

Kuzmina, O. B. ; Shurygin, B. N. / First findings of dinocysts in the upper Oligocene Turtas formation in Southern Tyumen oblast (West Siberia). In: Doklady Earth Sciences. 2016 ; Vol. 467, No. 2. pp. 341-345.

BibTeX

@article{54702ff602014be8b07e9f981a81f760,
title = "First findings of dinocysts in the upper Oligocene Turtas formation in Southern Tyumen oblast (West Siberia)",
abstract = "A new occurrence of dinocysts Pseudokomewuia in continental Cenosoic (Oligocene–Miocene) rocks of the West Siberian plain is identified. A complex of palynomorphs with dominant microphytoplankton (dinocysts) was found for the first time in the lacustrine-marsh sediments of the south of Tyumen oblast. The variable composition of the complex with Pseudokomewuia aff. laevigata He and Pseudokomewuia aff. granulata He species is traced upward through the section. The layers that correspond to the maximum abundance of Pseudokomewuia (akme) are distinguished and correlated with sections studied previously, which are located in the Barabinsk lithofacial region. Sediments with dinocysts are compared with sediments of the same age from North America, Northern Europe, and Southern China.",
author = "Kuzmina, {O. B.} and Shurygin, {B. N.}",
year = "2016",
month = apr,
day = "1",
doi = "10.1134/S1028334X1604019X",
language = "English",
volume = "467",
pages = "341--345",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - First findings of dinocysts in the upper Oligocene Turtas formation in Southern Tyumen oblast (West Siberia)

AU - Kuzmina, O. B.

AU - Shurygin, B. N.

PY - 2016/4/1

Y1 - 2016/4/1

N2 - A new occurrence of dinocysts Pseudokomewuia in continental Cenosoic (Oligocene–Miocene) rocks of the West Siberian plain is identified. A complex of palynomorphs with dominant microphytoplankton (dinocysts) was found for the first time in the lacustrine-marsh sediments of the south of Tyumen oblast. The variable composition of the complex with Pseudokomewuia aff. laevigata He and Pseudokomewuia aff. granulata He species is traced upward through the section. The layers that correspond to the maximum abundance of Pseudokomewuia (akme) are distinguished and correlated with sections studied previously, which are located in the Barabinsk lithofacial region. Sediments with dinocysts are compared with sediments of the same age from North America, Northern Europe, and Southern China.

AB - A new occurrence of dinocysts Pseudokomewuia in continental Cenosoic (Oligocene–Miocene) rocks of the West Siberian plain is identified. A complex of palynomorphs with dominant microphytoplankton (dinocysts) was found for the first time in the lacustrine-marsh sediments of the south of Tyumen oblast. The variable composition of the complex with Pseudokomewuia aff. laevigata He and Pseudokomewuia aff. granulata He species is traced upward through the section. The layers that correspond to the maximum abundance of Pseudokomewuia (akme) are distinguished and correlated with sections studied previously, which are located in the Barabinsk lithofacial region. Sediments with dinocysts are compared with sediments of the same age from North America, Northern Europe, and Southern China.

UR - http://www.scopus.com/inward/record.url?scp=84971247522&partnerID=8YFLogxK

U2 - 10.1134/S1028334X1604019X

DO - 10.1134/S1028334X1604019X

M3 - Article

AN - SCOPUS:84971247522

VL - 467

SP - 341

EP - 345

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 25830258