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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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):
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):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | Vasil'chuk, Yurij K | |||
2 | Latitude of event | Latitude | Vasil'chuk, Yurij K | |||
3 | Longitude of event | Longitude | Vasil'chuk, Yurij K | |||
4 | Sample ID | Sample ID | Vasil'chuk, Yurij K | |||
5 | DEPTH, sediment/rock | Depth sed | m | Vasil'chuk, Yurij K | Geocode – from | |
6 | DEPTH, sediment/rock | Depth sed | m | Vasil'chuk, Yurij K | Geocode – to | |
7 | Ice type | Ice type | Vasil'chuk, Yurij K | |||
8 | Sample comment | Sample comment | Vasil'chuk, Yurij K | |||
9 | δ18O, water | δ18O H2O | ‰ SMOW | Vasil'chuk, Yurij K | Mass spectrometer Finnigan Delta-V | |
10 | δ Deuterium, water | δD H2O | ‰ SMOW | Vasil'chuk, Yurij K | Mass spectrometer Finnigan Delta-V | |
11 | Deuterium excess | d xs | ‰ | Vasil'chuk, Yurij K | Mass spectrometer Finnigan Delta-V |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
114 data points