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New data on age and conditions of buried organic-rich sediments formation in the сentral Ob River. / Maksimov, F. E.; Savelieva, L. A.; Laukhin, S. A.; Kuznetsov, V. Yu; Arslanov, Kh A.; Petrov, A. Yu; Grigoriev, V. A.; Levchenko, S. B.

в: Contemporary Problems of Ecology, Том 10, № 4, 01.07.2017, стр. 370-379.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Maksimov, FE, Savelieva, LA, Laukhin, SA, Kuznetsov, VY, Arslanov, KA, Petrov, AY, Grigoriev, VA & Levchenko, SB 2017, 'New data on age and conditions of buried organic-rich sediments formation in the сentral Ob River', Contemporary Problems of Ecology, Том. 10, № 4, стр. 370-379. https://doi.org/10.1134/S1995425517040047

APA

Maksimov, F. E., Savelieva, L. A., Laukhin, S. A., Kuznetsov, V. Y., Arslanov, K. A., Petrov, A. Y., Grigoriev, V. A., & Levchenko, S. B. (2017). New data on age and conditions of buried organic-rich sediments formation in the сentral Ob River. Contemporary Problems of Ecology, 10(4), 370-379. https://doi.org/10.1134/S1995425517040047

Vancouver

Maksimov FE, Savelieva LA, Laukhin SA, Kuznetsov VY, Arslanov KA, Petrov AY и пр. New data on age and conditions of buried organic-rich sediments formation in the сentral Ob River. Contemporary Problems of Ecology. 2017 Июль 1;10(4):370-379. https://doi.org/10.1134/S1995425517040047

Author

Maksimov, F. E. ; Savelieva, L. A. ; Laukhin, S. A. ; Kuznetsov, V. Yu ; Arslanov, Kh A. ; Petrov, A. Yu ; Grigoriev, V. A. ; Levchenko, S. B. / New data on age and conditions of buried organic-rich sediments formation in the сentral Ob River. в: Contemporary Problems of Ecology. 2017 ; Том 10, № 4. стр. 370-379.

BibTeX

@article{152fc1e232be438cb6db794a0ef93b74,
title = "New data on age and conditions of buried organic-rich sediments formation in the сentral Ob River",
abstract = "This article presents the results of a comprehensive geochronological study of gyttja deposits from a section of a terrace above a floodplain located on the right bank of the Ob River near the town of Kolpashevo. According to the 230Th/U dating, the age of the gyttja could be dated in the range of 110–95 kyr. The results of spore–pollen analysis suggest that the gyttja deposit was formed in the period of a wide distribution of middle taiga forest landscapes with the dominance of spruce; the climatic conditions were similar to modern ones. These events probably took place in the interstadial time during MIS-5c or at the end of Kazantsevo interglacial period.",
keywords = "Th/U and С dating, interstadial and interglacial conditions, pollen analysis",
author = "Maksimov, {F. E.} and Savelieva, {L. A.} and Laukhin, {S. A.} and Kuznetsov, {V. Yu} and Arslanov, {Kh A.} and Petrov, {A. Yu} and Grigoriev, {V. A.} and Levchenko, {S. B.}",
year = "2017",
month = jul,
day = "1",
doi = "10.1134/S1995425517040047",
language = "English",
volume = "10",
pages = "370--379",
journal = "Contemporary Problems of Ecology",
issn = "1995-4255",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "4",

}

RIS

TY - JOUR

T1 - New data on age and conditions of buried organic-rich sediments formation in the сentral Ob River

AU - Maksimov, F. E.

AU - Savelieva, L. A.

AU - Laukhin, S. A.

AU - Kuznetsov, V. Yu

AU - Arslanov, Kh A.

AU - Petrov, A. Yu

AU - Grigoriev, V. A.

AU - Levchenko, S. B.

PY - 2017/7/1

Y1 - 2017/7/1

N2 - This article presents the results of a comprehensive geochronological study of gyttja deposits from a section of a terrace above a floodplain located on the right bank of the Ob River near the town of Kolpashevo. According to the 230Th/U dating, the age of the gyttja could be dated in the range of 110–95 kyr. The results of spore–pollen analysis suggest that the gyttja deposit was formed in the period of a wide distribution of middle taiga forest landscapes with the dominance of spruce; the climatic conditions were similar to modern ones. These events probably took place in the interstadial time during MIS-5c or at the end of Kazantsevo interglacial period.

AB - This article presents the results of a comprehensive geochronological study of gyttja deposits from a section of a terrace above a floodplain located on the right bank of the Ob River near the town of Kolpashevo. According to the 230Th/U dating, the age of the gyttja could be dated in the range of 110–95 kyr. The results of spore–pollen analysis suggest that the gyttja deposit was formed in the period of a wide distribution of middle taiga forest landscapes with the dominance of spruce; the climatic conditions were similar to modern ones. These events probably took place in the interstadial time during MIS-5c or at the end of Kazantsevo interglacial period.

KW - Th/U and С dating

KW - interstadial and interglacial conditions

KW - pollen analysis

UR - http://www.scopus.com/inward/record.url?scp=85028034639&partnerID=8YFLogxK

U2 - 10.1134/S1995425517040047

DO - 10.1134/S1995425517040047

M3 - Article

AN - SCOPUS:85028034639

VL - 10

SP - 370

EP - 379

JO - Contemporary Problems of Ecology

JF - Contemporary Problems of Ecology

SN - 1995-4255

IS - 4

ER -

ID: 10241930