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 the Holocene ice wedges in the exposed outcrop on the terrace of Seyakha (Mutnaya) River [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.921683, 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):
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: 70.369725 * Longitude: 68.386909
Minimum DEPTH, sediment/rock: 1 m * Maximum DEPTH, sediment/rock: 1 m
Event(s):
Comment:
Contents of stable isotopes of oxygen (δ¹⁸O), deuterium (δ²Н) and deuterium excess values (dexc) in the Holocene ice wedges in the exposed outcrop on the terrace of Seyakha (Mutnaya) River, Bovanenkovskoye oil and gas condensate field.
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 | Sample ID | Sample ID | Vasil'chuk, Yurij K | |||
| 2 | DEPTH, sediment/rock | Depth sed | m | Vasil'chuk, Yurij K | Geocode – from | |
| 3 | DEPTH, sediment/rock | Depth sed | m | Vasil'chuk, Yurij K | Geocode – to | |
| 4 | δ18O, water | δ18O H2O | ‰ SMOW | Vasil'chuk, Yurij K | Mass spectrometer Finnigan Delta-V | |
| 5 | δ Deuterium, water | δD H2O | ‰ SMOW | Vasil'chuk, Yurij K | Mass spectrometer Finnigan Delta-V | |
| 6 | Deuterium excess | d xs | ‰ | Vasil'chuk, Yurij K | Mass spectrometer Finnigan Delta-V | |
| 7 | Sample comment | Sample comment | Vasil'chuk, Yurij K | Sampling |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
115 data points
Data
| 1 Sample ID | 2 Depth sed [m] (from) | 3 Depth sed [m] (to) | 4 δ18O H2O [‰ SMOW] | 5 δD H2O [‰ SMOW] | 6 d xs [‰] | 7 Sample comment (Sampling) |
|---|---|---|---|---|---|---|
| zh 1 | 1 | 1.1 | -16.43 | -126.4 | 5.04 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 2 | 1 | 1.1 | -17.23 | -130.8 | 7.04 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 3 | 1 | 1.1 | -17.53 | -132.9 | 7.34 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 4 | 1 | 1.1 | -18.14 | -135.1 | 10.02 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 5 | 1 | 1.1 | -17.35 | -126.8 | 12.00 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 6 | 1 | 1.1 | -16.90 | -124.3 | 10.90 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 7 | 1 | 1.1 | -17.49 | -129.7 | 10.22 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 8 | 1 | 1.1 | -17.99 | -118.5 | 25.40 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 10 | 1 | 1.1 | -17.26 | -129.7 | 8.38 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 11 | 1 | 1.1 | -17.00 | -127.2 | 8.80 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 12 | 1 | 1.1 | -16.91 | -129.0 | 6.28 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 13 | 1 | 1.1 | -16.73 | -127.2 | 6.64 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 14 | 1 | 1.1 | -16.99 | -121.0 | 14.92 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 15 | 1 | 1.1 | -17.09 | -124.6 | 12.72 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 16 | 1 | 1.1 | -17.85 | -133.3 | 9.50 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 17 | 1 | 1.1 | -17.82 | -131.5 | 11.06 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 18 | 1 | 1.1 | -18.08 | -133.7 | 10.90 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 19 | 1 | 1.1 | -17.20 | -124.3 | 13.30 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 20 | 1 | 1.1 | -17.14 | -131.1 | 6.02 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 21 | 1 | 1.1 | -17.13 | -122.8 | 14.20 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 22 | 1 | 1.1 | -16.93 | -123.2 | 12.20 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 23 | 1 | 1.1 | -16.91 | -122.8 | 12.50 | Horizontal ice sampling at a depth of 1.0-1.10 m |
| zh 24 | 1 | 1.1 | -14.14 | -101.6 | 11.50 | Horizontal ice sampling at a depth of 1.0-1.10 m |