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Spatio-temporal distribution of mean January air temperature over the Russian Arctic during 30-12 ka BP with high temporal resolution
Vasil'chuk Yurii Kirillovich

Doctor of Geology and Mineralogy

Professor, the department of Geochemistry of Landscapes and Soil Geography, Lomonosov Moscow State University

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

vasilch_geo@mail.ru
Другие публикации этого автора
 

 

Abstract.

The palaeoreconstructions of the mean January temperatures based on the distribution of δ values (oxygen isotope composition) in the Late Pleistocene ice wedges in yedoma dated by radiocarbon are yielded. Verification of the equation linking current data of δ values in modern ice wedges with mean January temperatures has been done. In yedoma of different regions of the Russian Arctic formed 30-12 ka BP made the analysis reliability of radiocarbon ages. It is enabled to set on the time scale the isotopic events with high temporal resolution - with step 2-4 ka. New maps of the mean January palaeotemperatures for the time intervals 30-28, 24-22, 20-18, 16-12 ka BP are created for the Russian Arctic.

Keywords: cryochrone, palaeoreconstructions, Russian Arctic, Pleistocene, mean January temperature, oxygen isotopes, yedoma, ice wedge, radiocarbon, permafrost

DOI:

10.7256/2453-8922.2016.1.21310

Article was received:

15-12-2016


Review date:

10-12-2016


Publish date:

16-01-2017


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

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