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Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Jessica Yurevna; Vasil'chuk, Alla Constantinovna; Garankina, Ekaterina Vadimovna; Chizhova, Julia Nikolaevna; Shorkunov, Il'ya Germanovich (2020): δ¹⁸O, δ²Н and dexc in Late Pleistocene massive ice and ice wedges and in the Holocene ice wedges from sandy loam under peat deposits in the upper Mordyyakha River [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.921680, In: Vasil'chuk, YK et al. (2020): Isotope-geochemical composition of the massive ice of the Mordyakha and Seyakha (Mutnaya) Rivers interfluve, Central Yamal Peninsula [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.921687

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Keyword(s):
Holocene; Hydrogen isotopes; ice wedge; Late Pleistocene; massive ice; Oxygen isotopes; pollen and spores; Yamal Peninsula
Supplement to:
Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Jessica Yurevna; Vasil'chuk, Alla Constantinovna; Garankina, Ekaterina Vadimovna; Chizhova, Julia Nikolaevna; Shorkunov, Il'ya Germanovich (2018): Isotope-geochemical composition of massive ice beddings on the interfluve of the rivers Mordyakha and Seyakha (Mutnaya), Central Yamal Peninsula. Arktika i Antarktika (Arctic and Antarctic), 1, 50-75, https://doi.org/10.7256/2453-8922.2018.1.25833
Coverage:
Latitude: 68.188333 * Longitude: 68.860833
Minimum DEPTH, sediment/rock: 0.6 m * Maximum DEPTH, sediment/rock: 10.0 m
Event(s):
11-YuV-1 * Latitude: 68.188333 * Longitude: 68.860833 * Penetration: 0.6 * Location: Yamal Peninsula, northwestern Siberia * Method/Device: Sampling by hand (HAND) * Comment: Horizontal Sampling at 0.6 m depth
11-YuV-2 * Latitude: 68.188333 * Longitude: 68.860833 * Location: Yamal Peninsula, northwestern Siberia * Method/Device: Sampling by hand (HAND)
Comment:
Contents of stable isotopes of oxygen (δ¹⁸O), deuterium (δ²Н) and deuterium excess values (dexc) in Late Pleistocene massive ice and ice wedges (11-YuV-2) and in the Holocene ice wedges from sandy loam under peat deposits (11-YuV-1) in the upper Mordyyakha River, 537 km of the Ob-Bovanenkovo railway road.
The ice isotopic composition was determined at the Laboratory of Stable Isotope Geochemistry (Lomonosov Moscow State University) using a Delta-V mass spectrometer with a standard gas bench option. δ¹⁸O measurement implied equilibration of analyzed samples with CO₂ over 24 h, while the δ²H measurement was carried out using a platinum catalytic agent over 40 min. The values are presented in δ‐notation in per mil (‰) relative to the Vienna Standard Mean Ocean Water (VSMOW). For measurements international standards V-SMOW, SLAP and MSU own laboratory standard (snow of the Garabashi glacier) were used. Analytical precision was ±0.1‰ for δ¹⁸О and ±0.6‰ for δ²H.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEventVasil'chuk, Yurij K
2Latitude of eventLatitudeVasil'chuk, Yurij K
3Longitude of eventLongitudeVasil'chuk, Yurij K
4Sample IDSample IDVasil'chuk, Yurij K
5DEPTH, sediment/rockDepth sedmVasil'chuk, Yurij KGeocode – from
6DEPTH, sediment/rockDepth sedmVasil'chuk, Yurij KGeocode – to
7Ice typeIce typeVasil'chuk, Yurij K
8Sample commentSample commentVasil'chuk, Yurij K
9δ18O, waterδ18O H2O‰ SMOWVasil'chuk, Yurij KMass spectrometer Finnigan Delta-V
10δ Deuterium, waterδD H2O‰ SMOWVasil'chuk, Yurij KMass spectrometer Finnigan Delta-V
11Deuterium excessd xsVasil'chuk, Yurij KMass spectrometer Finnigan Delta-V
Size:
114 data points

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