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Vasil'chuk, Yurij K; Vasil'chuk, Alla Constantinovna (2020): δ¹⁸O in the ice veinlets of modern syngenetic ice wedges on Ayon Island, northern Chukotka, neighboring islands of eastern Arctic of Russia [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.915109, In: Vasil'chuk, YK; Vasil'chuk, AC (2020): δ¹⁸O composition of ice wedges from Ayon Island and paleotemperature reconstructions of the Northern Chukotka [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.915112

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Keyword(s):
Ayon Island; Chaun-Chukotka; deuterium; heavy oxygen; Holocene; ice wedge; Late Pleistocene; Stable isotope
Related to:
Vasil'chuk, Yurij K; Vasil'chuk, Alla Constantinovna (2018): The Oxygen Isotope Composition of Ice Wedges of Ayon Island and Paleotemperature Reconstructions of the Late Pleistocene and Holocene of the Northern Chukotka. Moscow University Geology Bulletin, 73(1), 87-99, https://doi.org/10.3103/S0145875218010131
Further details:
Kotov, A N (1998): Alas and ice complexes of the deposits in northwest Chukotka (the East Siberian Sea coast) [in Russian]. Kriosfera Zemli, 2(1), 11-18
Kotov, A N (1999): Cryolithogenic sediments in Wrangell Island [in Russian, 1999b]. In: Kompleksnoe issledovanie Chukotki (problemy geologii i biogeografii) (The Integrated Study of Chukotka) (Problems in Geology and Biogeography)), Magadan: Kn. Izd.
Meyer, Hanno; Dereviagin, Alexander Yu; Siegert, Christine; Schirrmeister, Lutz; Hubberten, Hans-Wolfgang (2002): Palaeoclimate reconstruction on Big Lyakhovsky Island, North Siberia - Hydrogen and oxygen isotopes in ice wedges. Permafrost and Periglacial Processes, 13, 91-105, https://doi.org/10.1002/ppp.416
Vasil'chuk, Alla Constantinovna (2007): Palynology and Chronology of Polygonal Ice Wedge Complexes in the Russian Permafrost Area [in Russian]. Moscow University Press, Moscow, 488 pp.
Vasil'chuk, Yurij K (1989): Correlation of oxygen isotope composition of ice wedges with mean winter and mean January air temperature [in Russian]. Conference Paper: Isotopes in the Hydrosphere. Extended abstracts of the 3rd All-Union USSR Symposium., At Kaunas. Moscow: Publishing House of the Institute of Water Problems of the USSR Academy of Sciences
Vasil'chuk, Yurij K (1989): The formation conditions of Late Pleistocene and Holocene wedge ice of Chukotka (isotope - cryolithochronological analysis). Dokl. Akad. Nauk SSSR, 309(4), 920-924
Vasil'chuk, Yurij K (1991): Reconstruction of the paleoclimate of the Late Pleistocene and Holocene on the basis of isotope studies of subsurface ice and waters of the permafrost zone. Water Resources, 17(6), 640–647
Vasil'chuk, Yurij K (1992): Oxygen Isotope Composition of Ground Ice (Application to Paleogeocryological Reconstructions) [in Russian]. Theor. Probl. Dept., RAS, Moscow University, Research Institute of Engineering for Construction (PNIIIS), Moscow (Volume 1, 420 pp., Volume 2, 264 pp.)
Coverage:
Median Latitude: 71.640562 * Median Longitude: 159.796344 * South-bound Latitude: 65.983300 * West-bound Longitude: 140.833300 * North-bound Latitude: 77.100000 * East-bound Longitude: 179.400000
Event(s):
Amguema_River * Latitude: 67.050000 * Longitude: 178.883300 * Location: Chukotka, Russia
Ayon_Island * Latitude: 69.784675 * Longitude: 168.656655 * Location: Chukotka, Russia
Bolshoy_Lyakhovsky_Island_south * Latitude: 73.333300 * Longitude: 141.666700 * Location: Chukotka, Russia
Comment:
Values of δ18O in the ice veinlets of modern syngenetic ice wedges on Ayon Island, in northern Chukotka and on the neighboring islands of Eastern Arctic of Russia, according to (Vasil'chuk, 1992) with additions. Winter mean (twint.mean) and January (tJ) air temperature values were calculated using equation: tJ = 1.5 δ18Opiw (±3 °C), twint.mean = δ18Opiw (±2 °C). by the technique of Yu. Vasil'chuk (1989, 1991). Mean annual ground temperatures were calculated using reconstructions of mean summer temperature by the technique of A. Vasil'chuk [2007] and of mean winter temperature by the technique of Yu. Vasil'chuk (1989). Isotopic analyses were performed at the Institute of Water Problems, RAS and at the Institute of Geology, the city of Tallinn. Oxygen isotope measurements of ice wedge were carried out in the isotope laboratory of the Institute of Geology of Estonia (Prof. R. Vaikmae) using a Finnigan Delta-E mass spectrometer. Analytical precision was ±0.4‰ and in the isotope laboratory of the Institute of Water Problems RAS (Dr. A.Yesikov) using a Finnigan MAT 250 mass spectrometer. Analytical precision was ±0.6‰.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEventVasil'chuk, Yurij K
2LATITUDELatitudeVasil'chuk, Yurij KGeocode
3LONGITUDELongitudeVasil'chuk, Yurij KGeocode
4Ice typeIce typeVasil'chuk, Yurij K
5δ18O, waterδ18O H2O‰ SMOWVasil'chuk, Yurij K
6Total annual freezing indexTAFIVasil'chuk, Yurij KCalculated, see Comment∑ twint, [°C/day ]
7Temperature, mean winterT win°CVasil'chuk, Yurij KCalculated, see Commentaverage
8Temperature, air, JanuaryT air (1)°CVasil'chuk, Yurij KCalculated, see Commentaverage
9Temperature, ground, annual meanMAGT°CVasil'chuk, Yurij KCalculated, see Commentaverage annual temperature (snow and vegetation cover is removed)
10Reference/sourceReferenceVasil'chuk, Yurij K
Size:
99 data points

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