δ¹⁸O composition of ice wedges from Ayon Island and paleotemperature reconstructions of the Northern Chukotka
Syngenetic ice wedges have been investigated on Ayon Island. Their isotope composition and the geochemical characteristics of both ice wedges and enclosing sediments have been obtained; four ice-wedge stages have been distinguished. Paleo temperature reconstructions for Ayon Island and adjacent terr...
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Format: | Dataset |
Language: | English |
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PANGAEA
2020
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.915112 https://doi.org/10.1594/PANGAEA.915112 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.915112 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Ayon Island Chaun-Chukotka deuterium heavy oxygen Holocene ice wedge Late Pleistocene Stable isotope |
spellingShingle |
Ayon Island Chaun-Chukotka deuterium heavy oxygen Holocene ice wedge Late Pleistocene Stable isotope Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna δ¹⁸O composition of ice wedges from Ayon Island and paleotemperature reconstructions of the Northern Chukotka |
topic_facet |
Ayon Island Chaun-Chukotka deuterium heavy oxygen Holocene ice wedge Late Pleistocene Stable isotope |
description |
Syngenetic ice wedges have been investigated on Ayon Island. Their isotope composition and the geochemical characteristics of both ice wedges and enclosing sediments have been obtained; four ice-wedge stages have been distinguished. Paleo temperature reconstructions for Ayon Island and adjacent territories of northern Chukotka have been obtained based of these results. Almost identical trends in the distribution of ice-wedge isotope characteristics in the Arctic islands and in the lower reaches of the Kolyma River were observed, as well as differences in the magnitude of isotope oscillations during the transition from the Late Pleistocene to the Holocene compared to ice wedges of the Lower Kolyma region. The sediments have been dated by the radiocarbon (14C) method (Kotov and Ryabchun, 1986). 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, 199). 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). Analysis of major ion chemistry of ice - titration methods (titrimetric methods) are based on determining the quantity of a reagent of known concentration that is required to react completely with the analyte. 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‰. |
format |
Dataset |
author |
Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna |
author_facet |
Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna |
author_sort |
Vasil'chuk, Yurij K |
title |
δ¹⁸O composition of ice wedges from Ayon Island and paleotemperature reconstructions of the Northern Chukotka |
title_short |
δ¹⁸O composition of ice wedges from Ayon Island and paleotemperature reconstructions of the Northern Chukotka |
title_full |
δ¹⁸O composition of ice wedges from Ayon Island and paleotemperature reconstructions of the Northern Chukotka |
title_fullStr |
δ¹⁸O composition of ice wedges from Ayon Island and paleotemperature reconstructions of the Northern Chukotka |
title_full_unstemmed |
δ¹⁸O composition of ice wedges from Ayon Island and paleotemperature reconstructions of the Northern Chukotka |
title_sort |
δ¹⁸o composition of ice wedges from ayon island and paleotemperature reconstructions of the northern chukotka |
publisher |
PANGAEA |
publishDate |
2020 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.915112 https://doi.org/10.1594/PANGAEA.915112 |
op_coverage |
MEDIAN LATITUDE: 70.423306 * MEDIAN LONGITUDE: 166.630004 * SOUTH-BOUND LATITUDE: 65.983300 * WEST-BOUND LONGITUDE: 140.833300 * NORTH-BOUND LATITUDE: 77.100000 * EAST-BOUND LONGITUDE: 179.400000 |
long_lat |
ENVELOPE(161.000,161.000,69.500,69.500) ENVELOPE(170.711,170.711,68.804,68.804) ENVELOPE(167.987,167.987,69.936,69.936) ENVELOPE(140.833300,179.400000,77.100000,65.983300) |
geographic |
Arctic Kolyma Chaun Ayon |
geographic_facet |
Arctic Kolyma Chaun Ayon |
genre |
Arctic Arctic Chukotka kolyma river Permafrost and Periglacial Processes |
genre_facet |
Arctic Arctic Chukotka kolyma river Permafrost and Periglacial Processes |
op_relation |
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 Noveishie otlozheniya i paleogeografiya pleistotsena Chukotki (The Recent Deposits and Paleogeography of the Pleistocene in the Chukotka Peninsula) [in Russian] (1980). Moscow: Nauka Kotov, A N (1997): The features of cryolithogenesis in ablation zone of the Late Pleistocene glaciers [in Russian]. In: Istoriya fundamental'nykh issledovanii kriosfery Zemli v Arktike i Subarktike (History of Basic Studies of the Earth Cryosphere in the Arctic and Subarctic), Novosibirsk: Nauka, 249-259 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. Kotov, A N (1999): Late Pleistocene cryolithogenic sediments and glacier ice in the Ekityki River valley (Northern Chukotka) [in Russian, 1999a]. In: Kompleksnoe issledovanie Chukotki (problemy geologii i biogeografii) (The Integrated Study of Chukotka (Problems in Geology and Biogeography)), Magadan: Kn. Izd., 93-102 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 Schwamborn, Georg; Meyer, Hanno; Fedorov, Grigory B; Schirrmeister, Lutz; Hubberten, Hans-Wolfgang (2006): Ground ice and slope sediments archiving late Quaternary paleoenvironment and paleoclimate signals at the margins of El'gygytgyn Impact Crater, NE Siberia. Quaternary Research, 66(2), 259-272, https://doi.org/10.1016/j.yqres.2006.06.007 Tarakanov, L V; Kaplin, P A; Kursalova, V I (1974): The structure and absolute age of recent sediments of the Valkarai Lowland (northern Chukotka) [in Russian]. Dokl. Akad. Nauk SSSR, 216(5), 1128-1130 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.) Vasil'chuk, Yurij K (2016): Spatio-temporal distribution of mean January air temperature over the Russian Arctic during 30-12 ka BP with high temporal resolution. Arktika i Antarktika (Arctic and Antarctic), 1, 86-103, https://doi.org/10.7256/2453-8922.2016.1.21310 https://doi.pangaea.de/10.1594/PANGAEA.915112 https://doi.org/10.1594/PANGAEA.915112 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.915112 https://doi.org/10.3103/S0145875218010131 https://doi.org/10.1002/ppp.416 https://doi.org/10.1016/j.yqres.2006.06.007 https://doi.org/10.7256/2453-8922.2016.1.21310 |
_version_ |
1766302351658844160 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.915112 2023-05-15T14:28:11+02:00 δ¹⁸O composition of ice wedges from Ayon Island and paleotemperature reconstructions of the Northern Chukotka Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna MEDIAN LATITUDE: 70.423306 * MEDIAN LONGITUDE: 166.630004 * SOUTH-BOUND LATITUDE: 65.983300 * WEST-BOUND LONGITUDE: 140.833300 * NORTH-BOUND LATITUDE: 77.100000 * EAST-BOUND LONGITUDE: 179.400000 2020-04-22 application/zip, 7 datasets https://doi.pangaea.de/10.1594/PANGAEA.915112 https://doi.org/10.1594/PANGAEA.915112 en eng PANGAEA 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 Noveishie otlozheniya i paleogeografiya pleistotsena Chukotki (The Recent Deposits and Paleogeography of the Pleistocene in the Chukotka Peninsula) [in Russian] (1980). Moscow: Nauka Kotov, A N (1997): The features of cryolithogenesis in ablation zone of the Late Pleistocene glaciers [in Russian]. In: Istoriya fundamental'nykh issledovanii kriosfery Zemli v Arktike i Subarktike (History of Basic Studies of the Earth Cryosphere in the Arctic and Subarctic), Novosibirsk: Nauka, 249-259 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. Kotov, A N (1999): Late Pleistocene cryolithogenic sediments and glacier ice in the Ekityki River valley (Northern Chukotka) [in Russian, 1999a]. In: Kompleksnoe issledovanie Chukotki (problemy geologii i biogeografii) (The Integrated Study of Chukotka (Problems in Geology and Biogeography)), Magadan: Kn. Izd., 93-102 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 Schwamborn, Georg; Meyer, Hanno; Fedorov, Grigory B; Schirrmeister, Lutz; Hubberten, Hans-Wolfgang (2006): Ground ice and slope sediments archiving late Quaternary paleoenvironment and paleoclimate signals at the margins of El'gygytgyn Impact Crater, NE Siberia. Quaternary Research, 66(2), 259-272, https://doi.org/10.1016/j.yqres.2006.06.007 Tarakanov, L V; Kaplin, P A; Kursalova, V I (1974): The structure and absolute age of recent sediments of the Valkarai Lowland (northern Chukotka) [in Russian]. Dokl. Akad. Nauk SSSR, 216(5), 1128-1130 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.) Vasil'chuk, Yurij K (2016): Spatio-temporal distribution of mean January air temperature over the Russian Arctic during 30-12 ka BP with high temporal resolution. Arktika i Antarktika (Arctic and Antarctic), 1, 86-103, https://doi.org/10.7256/2453-8922.2016.1.21310 https://doi.pangaea.de/10.1594/PANGAEA.915112 https://doi.org/10.1594/PANGAEA.915112 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Ayon Island Chaun-Chukotka deuterium heavy oxygen Holocene ice wedge Late Pleistocene Stable isotope Dataset 2020 ftpangaea https://doi.org/10.1594/PANGAEA.915112 https://doi.org/10.3103/S0145875218010131 https://doi.org/10.1002/ppp.416 https://doi.org/10.1016/j.yqres.2006.06.007 https://doi.org/10.7256/2453-8922.2016.1.21310 2023-01-20T07:34:32Z Syngenetic ice wedges have been investigated on Ayon Island. Their isotope composition and the geochemical characteristics of both ice wedges and enclosing sediments have been obtained; four ice-wedge stages have been distinguished. Paleo temperature reconstructions for Ayon Island and adjacent territories of northern Chukotka have been obtained based of these results. Almost identical trends in the distribution of ice-wedge isotope characteristics in the Arctic islands and in the lower reaches of the Kolyma River were observed, as well as differences in the magnitude of isotope oscillations during the transition from the Late Pleistocene to the Holocene compared to ice wedges of the Lower Kolyma region. The sediments have been dated by the radiocarbon (14C) method (Kotov and Ryabchun, 1986). 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, 199). 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). Analysis of major ion chemistry of ice - titration methods (titrimetric methods) are based on determining the quantity of a reagent of known concentration that is required to react completely with the analyte. 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‰. Dataset Arctic Arctic Chukotka kolyma river Permafrost and Periglacial Processes PANGAEA - Data Publisher for Earth & Environmental Science Arctic Kolyma ENVELOPE(161.000,161.000,69.500,69.500) Chaun ENVELOPE(170.711,170.711,68.804,68.804) Ayon ENVELOPE(167.987,167.987,69.936,69.936) ENVELOPE(140.833300,179.400000,77.100000,65.983300) |