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Stable isotopes of oxygen and hydrogen in Holocene ice wedges on the western coast of Baydarata Bay, at the mouth of the Ngarka-Tambyakha River
Budantseva Nadine Arkad'evna

PhD in Geography

Senior Scientific Associate, the department of Geography, M. V. Lomonosov Moscow State University 

119992, Russia, g. Moscow, ul. Leninskie Gory, 1, stroenie 19

nadin.budanceva@mail.ru
Другие публикации этого автора
 

 
Belova Natal'ya Gennadievna

PhD in Geography

Scientific Associate, the faculty of Geography, Laboratory of Geoecology of the North, M. V. Lomonosov Moscow State University

119991, Russia, g. Moscow, ul. Leninskie Gory, 1, of. Zh10

nataliya-belova@yandex.ru
Vasil'chuk Alla Constantinovna

Doctor of Geography

Leading Scientific Associate, the faculty of Geography, Laboratory of Geoecology of the North, M. V. Lomonosov Moscow State University

119991, Russia, g. Moscow, ul. Leninskie Gory, 1, of. Zh10

alla-vasilch@yandex.ru
Vasil'chuk Yurii Kirillovich

Doctor of Geology and Mineralogy

Professor, the department of Geochemistry of Landscapes and Geography of Soils, M. V. Lomonosov Moscow State University

119991, Russia, g. Moscow, ul. Leninskie Gory, 1, of. 2009

vasilch_geo@mail.ru

Abstract.

The object of this study is the ice wedges of Holocene age on the western coast of the Baydarata Bay, at the mouth of the Ngarka-Tambyakha River. In the coastal cliff structure of the thin polygonal peatland have been studied. The peatland is located in the upper part of the terrace 8-17 m high. The peat is underlain by gray icy loam with layered-lenticular cryogenic structure. Ice wedges revealed at the depth 0.8 m. Their width was 1.5-2 m, and outcropped height about 1.15 m high. One representative ice wedge was sampled across horizontal axis in the upper part, 9 samples were analyzed on a mass spectrometer, the oxygen isotope and hydrogen isotope composition of ice wedges was obtained. The main conclusions are: harsh winter air temperature in the area in Holocene varied between –16 and –19° С, which is about 10°С warmer compared to Late Pleistocene and were close to modern ones. Obtained results complement sparse information on Holocene winter air temperature for the Baydarata Bay coast.

Keywords: Baydarata Bay, Ngarka-Tambyakha, radiocarbon, Holocene, hydrogen isotopes, oxygen isotopes, modern ice vein, ice wedge, peatland, Arctic

DOI:

10.7256/2453-8922.2018.1.25857

Article was received:

31-03-2018


Review date:

31-03-2018


Publish date:

07-04-2018


This article written in Russian. You can find full text of article in Russian here .

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