Minimal, average, and maximum values of δ¹⁸O in ice wedge of the sections from Mamontova Gora and Syrdakh Lake, Central Yakutia

DOI

The oxygen isotope composition of the Late Pleistocene and Holocene syngenetic ice wedges, exposed at Mamontova Gora and Syrdakh Lake, is determined. In the area of Mamontova Gora, δ¹⁸O is in the range of –24.7 to –30.9‰ for the Late Pleistocene ice wedges, and of –23.2 to –25.9‰ for the Holocene ice wedges. In the area of Syrdakh Lake, δ18O ranges from –29.2 to –32.5‰. Obtained isotope data allowed to reconstruct the average winter air temperatures.

Stable oxygen isotope measurements were conducted in the Stable Isotope Laboratory of Moscow State University using Delta V Plus mass spectrometer.

Identifier
DOI https://doi.org/10.1594/PANGAEA.937734
Related Identifier https://doi.org/10.1134/S1028334X19050283
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.937734
Provenance
Creator Vasil'chuk, Yurij K ORCID logo; Shmelev, Denis; Cherbunina, Mariya Yu; Budantseva, Nadine A; Broushkov, Anatoly V; Vasil'chuk, Alla Constantinovna (ORCID: 0000-0003-1921-030X)
Publisher PANGAEA
Publication Year 2021
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 30 data points
Discipline Earth System Research
Spatial Coverage (130.965W, 62.544S, 133.953E, 62.978N); Sakha Republic, Russia; Syrdakh, Central Yakutia