Stable oxygen and hydrogen isotope compositions of the Messoyakha-1 and Pestsovoe pingo ice cores, Northwest Siberia
Two large pingos from ice cores of different origin in the continuous permafrost zone of northwest Siberia, the Messoyaha-1 pingo (10.5 m in height) and the Pestsovoe pingo (17 m in height), have been studied. Obtained distribution of stable oxygen and hydrogen isotopes in pingo ice cores allowed to...
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Language: | English |
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PANGAEA
2022
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.939382 https://doi.org/10.1594/PANGAEA.939382 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.939382 |
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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 |
Delta-V continuous flow isotope ratio mass spectrometer (CF-IRMS) with GasBench DEPTH sediment/rock Deuterium excess Event label hydrogen isotope ice-core Latitude of event Location Longitude of event Messoyakha-1 Northwest Siberia Oxygen isotopes Pestsovoe Pingo Sample comment Sample type Yamal-Nenets Russia δ18O δ Deuterium |
spellingShingle |
Delta-V continuous flow isotope ratio mass spectrometer (CF-IRMS) with GasBench DEPTH sediment/rock Deuterium excess Event label hydrogen isotope ice-core Latitude of event Location Longitude of event Messoyakha-1 Northwest Siberia Oxygen isotopes Pestsovoe Pingo Sample comment Sample type Yamal-Nenets Russia δ18O δ Deuterium Vasil'chuk, Yurij K Chizhova, Julia N Budantseva, Nadine A Kurchatova, Anna Rogov, Victor V Vasil'chuk, Alla Constantinovna Stable oxygen and hydrogen isotope compositions of the Messoyakha-1 and Pestsovoe pingo ice cores, Northwest Siberia |
topic_facet |
Delta-V continuous flow isotope ratio mass spectrometer (CF-IRMS) with GasBench DEPTH sediment/rock Deuterium excess Event label hydrogen isotope ice-core Latitude of event Location Longitude of event Messoyakha-1 Northwest Siberia Oxygen isotopes Pestsovoe Pingo Sample comment Sample type Yamal-Nenets Russia δ18O δ Deuterium |
description |
Two large pingos from ice cores of different origin in the continuous permafrost zone of northwest Siberia, the Messoyaha-1 pingo (10.5 m in height) and the Pestsovoe pingo (17 m in height), have been studied. Obtained distribution of stable oxygen and hydrogen isotopes in pingo ice cores allowed to understand the ice core formation. Ice formation was estimated according to the Rayleigh fractionation in a closed-system versus an open-system framework. For the Pestsovoe pingo the decrease in δ¹⁸O values with corresponding increase in dexc with depth indicates a closed system upon freezing of the lake talik from the top down. For the Messoyakha-1 pingo, the values of δ¹⁸O and δ²Н showed a weak tendency to decrease with depth, with values of dexc varying randomly. Ice that was segregated in the overlying and underlying sediments had similar values of δ¹⁸O and δ²Н and a low slope. Isotopically nonequilibrium ice formation was established for ice which had been segregated in a closed system and for ice cores formed in an open to semiclosed system. The vacuum mechanism of water suction from the surrounding lake or lake talik may have played a significant role during the formation of the upper ice core of the Messoyakha-1 pingo and its additional growth. |
format |
Dataset |
author |
Vasil'chuk, Yurij K Chizhova, Julia N Budantseva, Nadine A Kurchatova, Anna Rogov, Victor V Vasil'chuk, Alla Constantinovna |
author_facet |
Vasil'chuk, Yurij K Chizhova, Julia N Budantseva, Nadine A Kurchatova, Anna Rogov, Victor V Vasil'chuk, Alla Constantinovna |
author_sort |
Vasil'chuk, Yurij K |
title |
Stable oxygen and hydrogen isotope compositions of the Messoyakha-1 and Pestsovoe pingo ice cores, Northwest Siberia |
title_short |
Stable oxygen and hydrogen isotope compositions of the Messoyakha-1 and Pestsovoe pingo ice cores, Northwest Siberia |
title_full |
Stable oxygen and hydrogen isotope compositions of the Messoyakha-1 and Pestsovoe pingo ice cores, Northwest Siberia |
title_fullStr |
Stable oxygen and hydrogen isotope compositions of the Messoyakha-1 and Pestsovoe pingo ice cores, Northwest Siberia |
title_full_unstemmed |
Stable oxygen and hydrogen isotope compositions of the Messoyakha-1 and Pestsovoe pingo ice cores, Northwest Siberia |
title_sort |
stable oxygen and hydrogen isotope compositions of the messoyakha-1 and pestsovoe pingo ice cores, northwest siberia |
publisher |
PANGAEA |
publishDate |
2022 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.939382 https://doi.org/10.1594/PANGAEA.939382 |
op_coverage |
MEDIAN LATITUDE: 67.341821 * MEDIAN LONGITUDE: 78.217024 * SOUTH-BOUND LATITUDE: 66.174753 * WEST-BOUND LONGITUDE: 76.435992 * NORTH-BOUND LATITUDE: 68.508889 * EAST-BOUND LONGITUDE: 79.998056 * DATE/TIME START: 2013-10-01T00:00:00 * DATE/TIME END: 2017-11-30T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.5 m * MAXIMUM DEPTH, sediment/rock: 32.5 m |
long_lat |
ENVELOPE(146.601,146.601,59.667,59.667) ENVELOPE(76.435992,79.998056,68.508889,66.174753) |
geographic |
Talik |
geographic_facet |
Talik |
genre |
Ice ice core nenets permafrost Permafrost and Periglacial Processes Siberia |
genre_facet |
Ice ice core nenets permafrost Permafrost and Periglacial Processes Siberia |
op_relation |
Vasil'chuk, Yurij K; Chizhova, Julia N; Budantseva, Nadine A; Kurchatova, Anna; Rogov, Victor V; Vasil'chuk, Alla Constantinovna (2021): Stable oxygen and hydrogen isotope compositions of the Messoyakha and Pestsovoe pingos in northwest Siberia as markers of ice core formation. Permafrost and Periglacial Processes, 32(4), 558-571, https://doi.org/10.1002/ppp.2122 Chizhova, Julia Nikolaevna; Vasil'chuk, Yurij K (2018): Use of stable water isotopes to identify stages of the pingo ice core formation. Ice and Snow, 58(4), 507-523, https://doi.org/10.15356/2076-6734-2018-4-507-523 Vasil'chuk, Yurij K; Budantseva, Nadine A (2010): Radiocarbon dating of the pingo of the Pestsovoye gas field in the north of West Siberia. Engineering Geology, 2, 16-23 Vasil'chuk, Yurij K; Budantseva, Nadine A; Rogov, Victor V; Chizhova, Julia Nikolaevna (2019): Variations of Stable Oxygen and Hydrogen Isotopes in the Ice Core of the Pingo (Southern Part of Gydan Peninsula). Doklady Earth Sciences, 488(1), 1137-1141, https://doi.org/10.1134/S1028334X19090319 Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Rogov, Victor V; Podborny, Yevgenij Ye; Chizhova, Julia Nikolaevna (2017): New data on variations of stable isotopes in the pingo ice core in the southern part of the Tazovsky Peninsula. Doklady Earth Sciences, 472(2), 200-204, https://doi.org/10.1134/S1028334X17020064 Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Yoshikawa, K; Podborny, Yevgenij Ye; Chizhova, Julia Nikolaevna (2014): Isotope composition of pingo ice core in the Yevo-Yakha River valley, north-west Siberia. Earth's Cryosphere, 4(18), 41-51 Vasil'chuk, Yurij K; Lawson, D E; Yoshikawa, Kenji; Budantseva, Nadine A; Chizhova, Julia N; Podborny, Yevgenij Ye; Vasil'chuk, Alla Constantinovna (2016): Stable isotopes in the closed-system Weather Pingo, Alaska and Pestsovoye Pingo, northwestern Siberia. Cold Regions Science and Technology, 128, 13-21, https://doi.org/10.1016/j.coldregions.2016.05.001 https://doi.pangaea.de/10.1594/PANGAEA.939382 https://doi.org/10.1594/PANGAEA.939382 |
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.939382 https://doi.org/10.1002/ppp.2122 https://doi.org/10.15356/2076-6734-2018-4-507-523 https://doi.org/10.1134/S1028334X19090319 https://doi.org/10.1134/S1028334X17020064 https://doi.org/10.1016/j.coldregions.2 |
_version_ |
1766027697308303360 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.939382 2023-05-15T16:37:24+02:00 Stable oxygen and hydrogen isotope compositions of the Messoyakha-1 and Pestsovoe pingo ice cores, Northwest Siberia Vasil'chuk, Yurij K Chizhova, Julia N Budantseva, Nadine A Kurchatova, Anna Rogov, Victor V Vasil'chuk, Alla Constantinovna MEDIAN LATITUDE: 67.341821 * MEDIAN LONGITUDE: 78.217024 * SOUTH-BOUND LATITUDE: 66.174753 * WEST-BOUND LONGITUDE: 76.435992 * NORTH-BOUND LATITUDE: 68.508889 * EAST-BOUND LONGITUDE: 79.998056 * DATE/TIME START: 2013-10-01T00:00:00 * DATE/TIME END: 2017-11-30T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.5 m * MAXIMUM DEPTH, sediment/rock: 32.5 m 2022-01-10 text/tab-separated-values, 516 data points https://doi.pangaea.de/10.1594/PANGAEA.939382 https://doi.org/10.1594/PANGAEA.939382 en eng PANGAEA Vasil'chuk, Yurij K; Chizhova, Julia N; Budantseva, Nadine A; Kurchatova, Anna; Rogov, Victor V; Vasil'chuk, Alla Constantinovna (2021): Stable oxygen and hydrogen isotope compositions of the Messoyakha and Pestsovoe pingos in northwest Siberia as markers of ice core formation. Permafrost and Periglacial Processes, 32(4), 558-571, https://doi.org/10.1002/ppp.2122 Chizhova, Julia Nikolaevna; Vasil'chuk, Yurij K (2018): Use of stable water isotopes to identify stages of the pingo ice core formation. Ice and Snow, 58(4), 507-523, https://doi.org/10.15356/2076-6734-2018-4-507-523 Vasil'chuk, Yurij K; Budantseva, Nadine A (2010): Radiocarbon dating of the pingo of the Pestsovoye gas field in the north of West Siberia. Engineering Geology, 2, 16-23 Vasil'chuk, Yurij K; Budantseva, Nadine A; Rogov, Victor V; Chizhova, Julia Nikolaevna (2019): Variations of Stable Oxygen and Hydrogen Isotopes in the Ice Core of the Pingo (Southern Part of Gydan Peninsula). Doklady Earth Sciences, 488(1), 1137-1141, https://doi.org/10.1134/S1028334X19090319 Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Rogov, Victor V; Podborny, Yevgenij Ye; Chizhova, Julia Nikolaevna (2017): New data on variations of stable isotopes in the pingo ice core in the southern part of the Tazovsky Peninsula. Doklady Earth Sciences, 472(2), 200-204, https://doi.org/10.1134/S1028334X17020064 Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Yoshikawa, K; Podborny, Yevgenij Ye; Chizhova, Julia Nikolaevna (2014): Isotope composition of pingo ice core in the Yevo-Yakha River valley, north-west Siberia. Earth's Cryosphere, 4(18), 41-51 Vasil'chuk, Yurij K; Lawson, D E; Yoshikawa, Kenji; Budantseva, Nadine A; Chizhova, Julia N; Podborny, Yevgenij Ye; Vasil'chuk, Alla Constantinovna (2016): Stable isotopes in the closed-system Weather Pingo, Alaska and Pestsovoye Pingo, northwestern Siberia. Cold Regions Science and Technology, 128, 13-21, https://doi.org/10.1016/j.coldregions.2016.05.001 https://doi.pangaea.de/10.1594/PANGAEA.939382 https://doi.org/10.1594/PANGAEA.939382 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Delta-V continuous flow isotope ratio mass spectrometer (CF-IRMS) with GasBench DEPTH sediment/rock Deuterium excess Event label hydrogen isotope ice-core Latitude of event Location Longitude of event Messoyakha-1 Northwest Siberia Oxygen isotopes Pestsovoe Pingo Sample comment Sample type Yamal-Nenets Russia δ18O δ Deuterium Dataset 2022 ftpangaea https://doi.org/10.1594/PANGAEA.939382 https://doi.org/10.1002/ppp.2122 https://doi.org/10.15356/2076-6734-2018-4-507-523 https://doi.org/10.1134/S1028334X19090319 https://doi.org/10.1134/S1028334X17020064 https://doi.org/10.1016/j.coldregions.2 2023-01-20T09:15:37Z Two large pingos from ice cores of different origin in the continuous permafrost zone of northwest Siberia, the Messoyaha-1 pingo (10.5 m in height) and the Pestsovoe pingo (17 m in height), have been studied. Obtained distribution of stable oxygen and hydrogen isotopes in pingo ice cores allowed to understand the ice core formation. Ice formation was estimated according to the Rayleigh fractionation in a closed-system versus an open-system framework. For the Pestsovoe pingo the decrease in δ¹⁸O values with corresponding increase in dexc with depth indicates a closed system upon freezing of the lake talik from the top down. For the Messoyakha-1 pingo, the values of δ¹⁸O and δ²Н showed a weak tendency to decrease with depth, with values of dexc varying randomly. Ice that was segregated in the overlying and underlying sediments had similar values of δ¹⁸O and δ²Н and a low slope. Isotopically nonequilibrium ice formation was established for ice which had been segregated in a closed system and for ice cores formed in an open to semiclosed system. The vacuum mechanism of water suction from the surrounding lake or lake talik may have played a significant role during the formation of the upper ice core of the Messoyakha-1 pingo and its additional growth. Dataset Ice ice core nenets permafrost Permafrost and Periglacial Processes Siberia PANGAEA - Data Publisher for Earth & Environmental Science Talik ENVELOPE(146.601,146.601,59.667,59.667) ENVELOPE(76.435992,79.998056,68.508889,66.174753) |