Vasil'chuk, Yurij K; Maslakov, Alexey A; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Komova, Nina N (2022): Stable isotope composition (δ¹⁸О, δ²H and dexc) of massive ice bodies, Eastern Chukotka [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.939626
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Abstract:
Massive ice (MI) bodies exposed in floodplain and terraces at 7 sites have been studied from 1985 to 2020. In recent research stable oxygen and hydrogen isotope composition of massive ice bodies on the extreme North-Eastern Chukotka (near Lavrentiya settlement and Koolen' lake) have been studied in detail. It was concluded that studied massive ice bodies have intrasedimental origin and most likely are dated back to the Late Pleistocene age. Mean δ18O values range from –18.5 ‰ to –15 ‰ whereas mean δ2H values range from –146‰ to –128 ‰ that is higher than expected for the Late Pleistocene ice bodies in this region, which most likely resulted from isotopic fractionation during freezing of water-saturated sediments in a closed system when forming ice isotopically enriched compared with initial water. The analysis of co-isotope ratios for massive ice shows that initial water is mainly of meteoric origin (precipitation, water of lakes and taliks).
Keyword(s):
Related to:
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
Further details:
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
Vaikmäe, Rein; Vasil'chuk, Yurij K (1991): Oxygen isotope composition of ground ice in the north of Western Siberia, Yakutia and Chukotka [in Russian]. Tallinn: Punning J.-M.K. (ed). Academy of Sciences of Estonia. 70 p.
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; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Maslakov, Alexey A; Chizhova, Julia N (2018): Oxygen Isotope Composition of Holocene Ice Wedges of Eastern Chukotka. Doklady Earth Sciences, 480(2), 758-762, https://doi.org/10.1134/S1028334X18060107
Vasil'chuk, Yurij K; Chizhova, Julia N; Maslakov, Alexey A; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna (2018): OXYGEN AND HYDROGEN ISOTOPE VARIATIONS IN A RECENTLY FORMED MASSIVE ICE AT THE MOUTH OF THE AKKANI RIVER, EASTERN CHUKOTKA. Ice and Snow, 58(1), 78-93, https://doi.org/10.15356/2076-6734-2018-1-78-93
Funding:
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:
Median Latitude: 65.614139 * Median Longitude: -171.086517 * South-bound Latitude: 65.503411 * West-bound Longitude: -171.416060 * North-bound Latitude: 65.983563 * East-bound Longitude: -170.961614
Date/Time Start: 1987-07-01T00:00:00 * Date/Time End: 2020-09-01T00:00:00
Event(s):
MI-1 * Latitude: 65.983563 * Longitude: -170.961614 * Date/Time: 1987-07-01T00:00:00 * Location: Chukotka, Russia * Method/Device: Snow/ice sample (SNOW) * Comment: Date is giving the sampling month
Comment:
For stable isotope analysis, ice was sampled both vertically and horizontally from the ice beds, depending on the outcrop accessibility. Isotope oxygen in MI sampled in 1985-1987 was measured using a G-50 device in the isotope geology laboratory at the Institute of Geology, Tallinn, Estonia (Prof. R. Vaykmäe) and in the isotope hydrology laboratory at the Institute of Water Problems of Russian Academy of Science (Dr. A. Esikov). Control measurements were taken in both laboratories. The massive beds sampled during field studies in 2016-2020 were analyzed in the stable isotope laboratory of the Geography Faculty at Lomonosov Moscow State University (Prof. Yu. Vasil'chuk and Dr. N. Budantseva) using a Finnigan Delta-V Plus mass spectrometer applying equilibration techniques. International water standards (SMOW, GRESP, and SLAP) were used for calibration. Analytical precision was ±0.4‰ for δ18O and ±1‰ for δ2H. All values are presented in δ-notation in per mille (‰) relative to the Vienna Standard Mean Ocean Water (VSMOW).
Parameter(s):
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
85 data points