δ¹⁸O in ice wedges, ice lenses and snow from Kular, Yakutia (Russia)

Variations of δ¹⁸О in Late Pleistocene ice wedges, in structure-forming ice and segregated ice lenses, as well as in snow and water of Burguat River were determined. The studied section of the yedoma strata has been exposed in an outcrop of the slope sediments on a gentle slope in the foothills of K...

Full description

Bibliographic Details
Main Authors: Vasil'chuk, Yurij K, Vasil'chuk, Alla Constantinovna
Format: Dataset
Language:English
Published: PANGAEA 2020
Subjects:
DATE/TIME
DEPTH
sediment/rock
Hydrochemistry
Ice wedges
Kular
Kular_2
Late Pleistocene
Location
Northern Yakutia
North Yakutia
Russia
Oxygen isotopes
palaeotemperature
permafrost
Sample comment
Sample ID
trace elements
Treatment
Yedoma
δ18O
water
Ice
wedge*
Yakutia
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.926031
https://doi.org/10.1594/PANGAEA.926031
Description
Summary:Variations of δ¹⁸О in Late Pleistocene ice wedges, in structure-forming ice and segregated ice lenses, as well as in snow and water of Burguat River were determined. The studied section of the yedoma strata has been exposed in an outcrop of the slope sediments on a gentle slope in the foothills of Kular Ridge, nearby Kular Settlement, on the right bank of the Burguat River, 0.5 kilometers from the mouth of the Emis Creek.

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