δ18О values in the Late Pleistocene ice wedges, segregated and pore ice in the Zelyony Mys section, right bank in the lower reaches of the Kolyma River and in veinlets on the floodplain

DOI

Isotopic analysis of ice wedges has been performed in the laboratory of the Water Problems Institute of the Russian Academy of Sciences (senior researcher A.D. Esikov) on a Varian Mat 250 mass spectrometer, sample preparation was carried out by the authors within a month after sampling.

Identifier
DOI https://doi.org/10.1594/PANGAEA.944154
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Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.944154
Provenance
Creator Vasil'chuk, Yurij K ORCID logo; Vasil'chuk, Alla Constantinovna (ORCID: 0000-0003-1921-030X)
Publisher PANGAEA
Publication Year 2022
Funding Reference Russian Science Foundation https://doi.org/10.13039/501100006769 Crossref Funder ID 19-17-00126 https://rscf.ru/en/project/19-17-00126/ Verification and validation of Late Pleistocene paleotemperature scenario based on the stable isotope data in syngenetic ice wedges in Siberia using independent paleoclimatic models
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 246 data points
Discipline Earth System Research
Spatial Coverage (161.381 LON, 68.787 LAT); North Yakutia, Russia