Stable isotopes (δ¹⁸О) in surface water and snowpatches of the northeast coast of Chukotka

The relation of the stable oxygen isotope (δ¹⁸O) was measured in surface water and snowpatches of the northeast coast of Chukotka collected in 1987 and 2017. Data is compiled from Vasil'chuck 1992 (vol.1 & vol.2) and Vasil'chuk et al. 2021.

Bibliographic Details
Main Authors:	Vasil'chuk, Yurij K, Maslakov, Alexey A, Budantseva, Nadine A, Vasil'chuk, Alla Constantinovna, Komova, Nina N
Format:	Dataset
Language:	English
Published:	PANGAEA 2022
Subjects:	Chukotka Russia Chulcheveem_river cryostratigraphy Event label Koolen_creek Latitude of event Lavrentia_bay Lavrentia_lake Lavrentia_Lorino_road Lavrentia_settl_creek Lavrentia_settl_glac Lavrentia_settl_snow1 Lavrentia_settl_snow2 Lavrentia_settl_snow3 Lavrentia_settl_snow4 Location Longitude of event massive ice Mass spectrometer Finnigan Delta-V North-Eastern Chukotka Sample comment Sample ID Sample material SNOW Snow/ice sample Stable isotopes stable isotopes of water Surface water sample SWS δ18O maximum minimum
Online Access:	https://doi.pangaea.de/10.1594/PANGAEA.939629 https://doi.org/10.1594/PANGAEA.939629

Description
Summary:	The relation of the stable oxygen isotope (δ¹⁸O) was measured in surface water and snowpatches of the northeast coast of Chukotka collected in 1987 and 2017. Data is compiled from Vasil'chuck 1992 (vol.1 & vol.2) and Vasil'chuk et al. 2021.