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Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Chizhova, Julia N; Podborny, Yevgeny; Vasil'chuk, Jessica Yurevna (2021): δ²H, δ¹⁸O and Deuterium excess values in Holocene multistage massive ice near the Sabettayakha River mouth, Yamal Peninsula, northwest Siberia [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.933096

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Abstract:
Holocene massive ground ice near the Sabettayakha River mouth, on the coast of the Gulf of Ob, Yamal Peninsula, northwest Siberia is studied. The multistage massive-ice bodies have thickness up to 5.7 m and occur in Holocene sediments of modern floodplain and the first terrace of the coastal lagoon. Stable isotope analyses revealed that the multistage massive ice bodies formed syngenetically during the freezing of water- saturated sediment, under intensive cryogenic fractionation.
Keyword(s):
Holocene; Ion concentrations; massive ice; pollen and spores; Sabettayakha River; stable isotope data; Yamal Peninsula
Related to:
Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Chizhova, Julia N; Podborny, Yevgeny; Vasil'chuk, Jessica Yurevna (2016): Holocene multistage massive ice, Sabettayakha river mouth, Yamal Peninsula, northwest Siberia. GeoResJ, 9-12, 54-66, https://doi.org/10.1016/j.grj.2016.09.002
Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Chizhova, Julia N; Podborny, Yevgeny; Vasil'chuk, Jessica Yurevna (2021): Depth of massive ice bodies near the Sabettayakha River mouth, Yamal Peninsula, northwest Siberia. PANGAEA, https://doi.org/10.1594/PANGAEA.933097
Further details:
Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Podborny, Yevgenij Ye; Chizhova, Julia Nikolaevna (2016): Multistage Holocene massive ground ice in Northern West Siberia. Earth's Cryosphere, 20(1), 34-45
Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Podborny, Yevgeny; Podborny, Yevgenij Ye; Sullina, A N; Chizhova, Julia Nikolaevna (2015): Multistage Holocene massive ice near the Sabettayaha River mouth, Yamal Peninsula. Earth's Cryosphere, 19(4), 36-47
Vasil'chuk, Yurij K; Podborny, Yevgenij Ye; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Sullina, A N; Chizhova, Julia Nikolaevna (2016): δ18O and δD variations in Holocene massive ice in the Sabettayakha river mouth, northern Yamal Peninsula. Doklady Earth Sciences, 470(2), 1086-1092, https://doi.org/10.1134/S1028334X16100172
Funding:
Russian Foundation for Basic Research, grant/award no. 18-05-60272: Arctic
Russian Science Foundation, grant/award no. 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
Coverage:
Latitude: 71.249246 * Longitude: 72.107585
Event(s):
Sabettayakha_river * Latitude: 71.249246 * Longitude: 72.107585 * Location: Yamal Peninsula, northwestern Siberia * Method/Device: Multiple investigations (MULT)
Comment:
Isotopic analyses were performed in the Stable Isotope Laboratory of the Geographical Department of Lomonosov Moscow State University using a mass spectrometer Finnigan Delta-V with the standard gas -bench option. International standards V-SMOW (Vienna Standard Mean Ocean Water), GISP (Greenland Ice Sheet Precipitation) and SLAP (Standard Light Antarctic Precipitation), as well as the laboratory's own standard -fresh snow of the Cauca- sus glacier Garabashi ( δ¹⁸О= -15.60 ‰ , δ²H = -110.0 ‰ ) were used for the measurements. The precision of the δ¹⁸О and δ²H measurements is 0.1 and 0.6 ‰, respectively.
Data was submitted and proofread by Yurij K Vasil'chuk and Lyubov Bludushkina at the faculty of Geography, department of Geochemistry of Landscapes and Geography of Soils, Lomonosov Moscow State University.
Funding was received from the Russian Science Foundation (Award nr. 19-17-00126, field research), the Russian Foundation for Basic Research (Award nr. 18-05-60272, isotope analysis).
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
333 data points

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