Stable oxygen isotopes composition (δ¹⁸O) in Late Pleistocene ice wedges and segregated ice in Balyktakh River valley and in Sopochnaya Karga Peninsula

Oxygen isotope ratios in ice wedges were determined on a Finnigan Delta-E mass spectrometer at the Isotope Laboratory of the Institute of Geology of Estonia. Measurement errors of δ¹⁸O are 0.1‰.

Bibliographic Details
Main Authors:	Vasil'chuk, Yurij K, Makeev, V M, Maslakov, Alexey A, Budantseva, Nadine A, Vasil'chuk, Alla Constantinovna
Format:	Dataset
Language:	English
Published:	PANGAEA - Data Publisher for Earth & Environmental Science 2020
Subjects:	Arctic islands Holocene ice complex ice wedge Late Pleistocene oxygen and hydrogen stable isotopes radiocarbon age winter paleotemperature Yedoma Event label Sample ID Location Ice type ELEVATION Distance δ18O, water Mass spectrometer Finnigan Delta-E Arctic Balyktakh Karga
Online Access:	https://dx.doi.org/10.1594/pangaea.915948 https://doi.pangaea.de/10.1594/PANGAEA.915948

Description
Summary:	Oxygen isotope ratios in ice wedges were determined on a Finnigan Delta-E mass spectrometer at the Isotope Laboratory of the Institute of Geology of Estonia. Measurement errors of δ¹⁸O are 0.1‰.