Comparison of average δ¹⁸O values in syngenetic Late Pleistocene and Holocene ice wedges of Siberia

DOI

Average δ¹⁸O values in syngenetic ice wedges of Siberia are investigated.The oxygen isotope composition in the Late Pleistocene ice wedges change from the west to the east by 8–10 ‰: δ¹⁸O values vary in Western Siberia from –19 to –25 ‰, in Northern Yakutia from –30 to –35 ‰, in the north of Chukotka from –28 to –33 ‰, in the south of Chukotka from –23 to –29 ‰.

Stable isotope analyses were made at the isotope laboratory of the Institute of Water Problems RAS (Dr. A.Yesikov) using a Finnigan MAT 250 mass spectrometer, analytical precision was ±0.6‰ and at the Tallinn Institute of Geology (Prof. R. Vaikmäe), analytical precision was ±0.4‰.

Identifier
DOI https://doi.org/10.1594/PANGAEA.939402
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.939402
Provenance
Creator Vasil'chuk, Yurij K
Publisher PANGAEA - Data Publisher for Earth & Environmental Science
Publication Year 2022
Funding Reference Russian Science Foundation, 19 17 00126
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Representation
Language English
Resource Type Dataset
Format text/tab-separated-values
Size 108 data points
Discipline Earth System Research
Spatial Coverage (72.560W, 62.255S, 171.259E, 75.450N); Chukotka, Russia; Bykovsky Peninsula, Siberia; Krasnoyarsk, Russia; North Yakutia, Russia; Sakha Republic, Russia; Magadan, Russia; Yamal Peninsula, northwestern Siberia