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Reconstruction of the natural environment and level of Lake Taymyr in the Late Pleistosene and Holocene according to terrace deposit studies. / Kostromina, Natalia ; Fedorov, Grigory ; Savelieva, Larisa .

EGU General Assembly 2018: Geophysical Research Abstracts. European Geosciences Union, 2018. EGU2018-18402.

Research output: Chapter in Book/Report/Conference proceeding › Conference abstracts › Research

Harvard

Kostromina, N, Fedorov, G & Savelieva, L 2018, Reconstruction of the natural environment and level of Lake Taymyr in the Late Pleistosene and Holocene according to terrace deposit studies. in EGU General Assembly 2018: Geophysical Research Abstracts., EGU2018-18402, European Geosciences Union, European Geosciences Union General Assembly 2018, Вена, Austria, 7/04/18.

APA

Kostromina, N., Fedorov, G., & Savelieva, L. (2018). Reconstruction of the natural environment and level of Lake Taymyr in the Late Pleistosene and Holocene according to terrace deposit studies. In EGU General Assembly 2018: Geophysical Research Abstracts [ EGU2018-18402] European Geosciences Union.

Vancouver

Kostromina N, Fedorov G, Savelieva L. Reconstruction of the natural environment and level of Lake Taymyr in the Late Pleistosene and Holocene according to terrace deposit studies. In EGU General Assembly 2018: Geophysical Research Abstracts. European Geosciences Union. 2018. EGU2018-18402

Author

Kostromina, Natalia ; Fedorov, Grigory ; Savelieva, Larisa . / Reconstruction of the natural environment and level of Lake Taymyr in the Late Pleistosene and Holocene according to terrace deposit studies. EGU General Assembly 2018: Geophysical Research Abstracts. European Geosciences Union, 2018.

BibTeX

@inbook{0e8018b2c7a143858e662c1a113efbac,
title = "Reconstruction of the natural environment and level of Lake Taymyr in the Late Pleistosene and Holocene according to terrace deposit studies",
abstract = "This article adduces records, which were obtained during campaign at summer of 2016, in the framework of thePLOT project. The area of research took place in north part of Lake Taymyr. We present data from two laketerraces. How the research shows, the relative elevations of terraces are about 8-10 m and 22-25 m above the lake.On the basis of currently available results of pollen analysis and total organic carbon analysis, it is possible toconclude, that 8-10 m terrace has Holocene age (6,5-5 ka). The pollen data shows the sediments of 8-10 m terraceformed during two periods. The first period was warmer then modern. The second period was close to currentconditions. Available results of 22-25 m terrace allow us to conclude only that it is older than the Holocene",
author = "Natalia Kostromina and Grigory Fedorov and Larisa Savelieva",
year = "2018",
language = "English",
booktitle = "EGU General Assembly 2018",
publisher = "European Geosciences Union",
address = "Germany",
note = " European Geosciences Union General Assembly 2018, EGU2018 ; Conference date: 07-04-2018 Through 12-04-2018",
url = "https://www.egu2018.eu/",

}

RIS

TY - CHAP

T1 - Reconstruction of the natural environment and level of Lake Taymyr in the Late Pleistosene and Holocene according to terrace deposit studies

AU - Kostromina, Natalia

AU - Fedorov, Grigory

AU - Savelieva, Larisa

N1 - Conference code: 18

PY - 2018

Y1 - 2018

N2 - This article adduces records, which were obtained during campaign at summer of 2016, in the framework of thePLOT project. The area of research took place in north part of Lake Taymyr. We present data from two laketerraces. How the research shows, the relative elevations of terraces are about 8-10 m and 22-25 m above the lake.On the basis of currently available results of pollen analysis and total organic carbon analysis, it is possible toconclude, that 8-10 m terrace has Holocene age (6,5-5 ka). The pollen data shows the sediments of 8-10 m terraceformed during two periods. The first period was warmer then modern. The second period was close to currentconditions. Available results of 22-25 m terrace allow us to conclude only that it is older than the Holocene

AB - This article adduces records, which were obtained during campaign at summer of 2016, in the framework of thePLOT project. The area of research took place in north part of Lake Taymyr. We present data from two laketerraces. How the research shows, the relative elevations of terraces are about 8-10 m and 22-25 m above the lake.On the basis of currently available results of pollen analysis and total organic carbon analysis, it is possible toconclude, that 8-10 m terrace has Holocene age (6,5-5 ka). The pollen data shows the sediments of 8-10 m terraceformed during two periods. The first period was warmer then modern. The second period was close to currentconditions. Available results of 22-25 m terrace allow us to conclude only that it is older than the Holocene

UR - https://www.egusphere.net/conferences/EGU2018/SSP/

UR - https://meetingorganizer.copernicus.org/EGU2018/EGU2018-18402.pdf

M3 - Conference abstracts

BT - EGU General Assembly 2018

PB - European Geosciences Union

T2 - European Geosciences Union General Assembly 2018

Y2 - 7 April 2018 through 12 April 2018

ER -

ID: 77220383