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Vasil'chuk, Yurij K; Budantseva, Nadine A; Maslakov, Alexey A; Vasil'chuk, Alla Constantinovna; Vasil'chuk, Jessica Yurevna (2024): Stable isotope (δ18О, δ2H and dexc) minimum, mean, and maximum values for massive ice, Eastern Chukotka [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.971499, In: Vasil'chuk, YK et al. (2024): AMS radiocarbon dating (22-27 cal Ka BP) of massive ice on the coast of Mechigmen and Lavrentia Bays, Eastern Chukotka, and stable isotope (δ18O, δ2H) composition of dated ice [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.971505

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Keyword(s):
AMS; deuterium; Late Pleistocene; massive ice; oxygen isotopes; radiocarbon
Related to:
Budantseva, Nadine A; Maslakov, Alexey A; Vasil'chuk, Alla Constantinovna; Vasil'chuk, Yurij K; Kuzyakin, Lev P (2023): Reconstruction of the mean January air temperature in the Early Holocene on the eastern coast of Chukotka [In Russian]. Ice and Snow, 63(1), 93-103
Budantseva, Nadine A; Maslakov, Alexey A; Vasil'chuk, Yurij K; Baranskaya, Alisa V; Belova, N V; Vasil'chuk, Alla Constantinovna; Romanenko, Fedor A (2020): Winter air temperature in the early and middle Holocene on the eastern coast of Daurkin Peninsula, Chukotka, reconstructed from stable isotopes of ice wedges [In Russian]. Ice and Snow, 60(2), 251-262, https://doi.org/10.31857/S2076673420020038
Vasil'chuk, Alla Constantinovna; Vasil'chuk, Yurij K (2021): Pollen as a potential indicator of the origin of massive ice in northwest Siberia. Permafrost and Periglacial Processes, 32(3), 349-367, https://doi.org/10.1002/ppp.2095
Vasil'chuk, Yurij K; Budantseva, Nadine A; Farquharson, Louise M; Maslakov, Alexey A; Vasil'chuk, Alla Constantinovna; Chizhova, Julia N (2018): Isotopic evidence for Holocene January air temperature variability on the East Chukotka Peninsula. Permafrost and Periglacial Processes, 29(4), 283-297, https://doi.org/10.1002/ppp.1991
Vasil'chuk, Yurij K; Maslakov, Alexey A; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Komova, Nina N (2021): Isotope Signature Of The Massive Ice Bodies On The Northeast Coast Of Chukotka Peninsula. Geography, Environment, Sustainability, 14(4), 9-19, https://doi.org/10.24057/2071-9388-2021-020
References:
Dansgaard, W (1964): Stable isotopes in precipitation. Tellus, 16(4), 436-468, https://doi.org/10.3402/tellusa.v16i4.8993
Funding:
Russian scientific foundation (RSF), grant/award no. 23-17-00082
Coverage:
Median Latitude: 65.528107 * Median Longitude: -171.050889 * South-bound Latitude: 65.507889 * West-bound Longitude: -171.197278 * North-bound Latitude: 65.547500 * East-bound Longitude: -170.973333
Date/Time Start: 2016-09-04T01:30:00 * Date/Time End: 2020-07-30T02:00:00
Event(s):
Akkani  * Latitude: 65.507889 * Longitude: -171.197278 * Date/Time: 2016-09-04T01:30:00 * Location: Chukotka, Russia * Method/Device: Ice corer (IC)
Lavrentia_1  * Latitude: 65.547500 * Longitude: -170.973333 * Date/Time: 2017-08-18T03:00:00 * Location: Chukotka, Russia * Method/Device: Ice corer (IC)
Lavrentia_2  * Latitude: 65.528933 * Longitude: -170.982056 * Date/Time: 2020-07-30T02:00:00 * Location: Chukotka, Russia * Method/Device: Ice corer (IC)
Comment:
Stable oxygen and hydrogen compositions in ice were analyzed in the stable isotope laboratory of the Faculty of Geography at Lomonosov Moscow State University using a Finnigan Delta-V Plus mass spectrometer applying equilibration techniques. The values are presented in δ-notation in per mille (‰) relative to the Vienna Standard Mean Ocean Water (VSMOW). International reference materials (V-SMOW-2, GISP, and SLAP) were used for the calibration. The analytical precision is ±0.1‰ for δ18О and ±0.8‰ for δ2H. Deuterium excess (dexc) was calculated as dexc = δ2H - 8δ18O (Dansgaard 1964). Totally, 84 samples of massive ice were analyzed for stable isotope composition, and organic micro-inclusions for 14C AMS analysis were extracted from 5 samples.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEventVasil'chuk, Yurij K
LocationLocationVasil'chuk, Yurij K
SiteSiteVasil'chuk, Yurij K
Sample IDSample IDVasil'chuk, Yurij K
δ18O, minimumδ18O minVasil'chuk, Yurij KMass-specrometer, Thermo Scientific, Finnigan Delta-V Plus
δ18Oδ18OVasil'chuk, Yurij KMass-specrometer, Thermo Scientific, Finnigan Delta-V PlusMean
δ18O, maximumδ18O maxVasil'chuk, Yurij KMass-specrometer, Thermo Scientific, Finnigan Delta-V Plus
δ Deuterium, minimumδD min‰ SMOWVasil'chuk, Yurij KMass-specrometer, Thermo Scientific, Finnigan Delta-V Plus
δ DeuteriumδD‰ SMOWVasil'chuk, Yurij KMass-specrometer, Thermo Scientific, Finnigan Delta-V PlusMean
10 δ Deuterium, maximumδD max‰ SMOWVasil'chuk, Yurij KMass-specrometer, Thermo Scientific, Finnigan Delta-V Plus
11 Deuterium excess, minimumd xs minVasil'chuk, Yurij KMass-specrometer, Thermo Scientific, Finnigan Delta-V Plus
12 Deuterium excessd xsVasil'chuk, Yurij KMass-specrometer, Thermo Scientific, Finnigan Delta-V PlusMean
13 Deuterium excess, maximumd xs maxVasil'chuk, Yurij KMass-specrometer, Thermo Scientific, Finnigan Delta-V Plus
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
36 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Event

Location

Site

Sample ID

δ18O min []

δ18O []

δ18O max []

δD min [‰ SMOW]

δD [‰ SMOW]
10 
δD max [‰ SMOW]
11 
d xs min []
12 
d xs []
13 
d xs max []
Akkani 2 km southeast from Chulkheveem (Akkani) River mouth and 1 km west from Akkani sea hunters base on the Mechigmen Bay coast. The coast of Mechigmen Bay, Eastern Chukotka, Akkani16-M33-17.88-17.13-16.27-135.8-128.1-121.64.209.0015.80
Lavrentia_1 The coast of Lavrentiya Bay (St. Lawrence Bay), about 3 km south of the Lavrentiya settlement. The coast of Mechigmen Bay, Eastern Chukotka, Lavrentia.17-M26-18.96-16.97-14.84-148.4-131.4-116.3-2.484.5211.02
Lavrentia_2 The coast of Lavrentiya Bay (St. Lawrence Bay), about 5 km south of the Lavrentiya settlement. The coast of Mechigmen Bay, Eastern Chukotka, Lavrentia20-M11-21.30-18.70-16.60-163.9-145.8-123.9-6.504.1014.20