Paleotemperatures in the lower Kolyma river, Plakhinskii Yar site
A continuous 15-18 m long sequence of permafrost with ice wedges at the Plakhinskii Yar site (Karetovo yedoma, left side of the Stadukhin Channel, lower Kolyma River) has been studied in terms of structure, stable isotopes, radiocarbon ages, major ion chemistry, and spore-pollen spectra. The obtaine...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.914981 2023-05-15T14:28:07+02:00 Paleotemperatures in the lower Kolyma river, Plakhinskii Yar site Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna LATITUDE: 68.678800 * LONGITUDE: 160.285200 2020-04-21 application/zip, 7 datasets https://doi.pangaea.de/10.1594/PANGAEA.914981 https://doi.org/10.1594/PANGAEA.914981 en eng PANGAEA Vasil'chuk, Yurij K; Vasil'chuk, Alla Constantinovna (2018): Winter air paleotemperatures at 30-12 ka BP in the lower. Kolyma River, Plakhinskii Yar yedoma: evidence from stable isotopes. Earth's Cryosphere, XXII(5), https://doi.org/10.21782/KZ1560-7496-2018-5(3-19) Fukuda, M; Nagaoka, D; Saijyo, K; Nakamura, T; Kunitsky, Victor V (1997): Radiocarbon dating results of organic materials obtained from Siberian permafrost areas. Rep. Inst. Low Temperature Sci., Hokkaido University, Sapporo, 17-28 Konyakhin, M A; Mikhalev, D V; Solomatin, V I (1996): Oxygen Isotope Composition of Ground Ice. Moscow University Press, Moscow (in Russian), 156pp. Nikolaev, Vladimir I; Mikhalev, D V; Romanenko, Fedor A; Brilli, M (2010): Reconstruction of the formation conditions for permafrost in Northeastern Russia from isotope data (example fromreference sections in the lower Kolyma Lowland). Led i Sneg, 50(4), 79-90 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 Vasil'chuk, Yurij K; Vasil'chuk, Alla Constantinovna; van der Plicht, Johannes; Kutschera, V; Rank, D (2001): Radiocarbon dating of the Late Pleistocene ice wedges in the Bison section in the lower reaches of the Kolyma River. Doklady Earth Sciences, 379(5), 589-593 https://doi.pangaea.de/10.1594/PANGAEA.914981 https://doi.org/10.1594/PANGAEA.914981 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY ice wedge Late Pleistocene northeastern Yakutia oxygen isotope permafrost Plakhino site pollen and spores radiocarbon water chemistry Yedoma Dataset 2020 ftpangaea https://doi.org/10.1594/PANGAEA.914981 https://doi.org/10.21782/KZ1560-7496-2018-5(3-19 https://doi.org/10.7256/2453-8922.2016.1.21310 2023-01-20T07:34:32Z A continuous 15-18 m long sequence of permafrost with ice wedges at the Plakhinskii Yar site (Karetovo yedoma, left side of the Stadukhin Channel, lower Kolyma River) has been studied in terms of structure, stable isotopes, radiocarbon ages, major ion chemistry, and spore-pollen spectra. The obtained data allow quantitative estimates of Late Pleistocene permafrost and climate conditions in the area between 30 and 12 ka BP. The study confirms the previous inference that local winters at 30-28 ka BP were much colder than at present. Dataset Arctic Ice kolyma river permafrost wedge* Yakutia PANGAEA - Data Publisher for Earth & Environmental Science Kolyma ENVELOPE(161.000,161.000,69.500,69.500) Yar ENVELOPE(151.300,151.300,70.917,70.917) Plakhino ENVELOPE(86.407,86.407,67.938,67.938) Karetovo ENVELOPE(161.250,161.250,68.783,68.783) ENVELOPE(160.285200,160.285200,68.678800,68.678800) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
ice wedge Late Pleistocene northeastern Yakutia oxygen isotope permafrost Plakhino site pollen and spores radiocarbon water chemistry Yedoma |
spellingShingle |
ice wedge Late Pleistocene northeastern Yakutia oxygen isotope permafrost Plakhino site pollen and spores radiocarbon water chemistry Yedoma Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna Paleotemperatures in the lower Kolyma river, Plakhinskii Yar site |
topic_facet |
ice wedge Late Pleistocene northeastern Yakutia oxygen isotope permafrost Plakhino site pollen and spores radiocarbon water chemistry Yedoma |
description |
A continuous 15-18 m long sequence of permafrost with ice wedges at the Plakhinskii Yar site (Karetovo yedoma, left side of the Stadukhin Channel, lower Kolyma River) has been studied in terms of structure, stable isotopes, radiocarbon ages, major ion chemistry, and spore-pollen spectra. The obtained data allow quantitative estimates of Late Pleistocene permafrost and climate conditions in the area between 30 and 12 ka BP. The study confirms the previous inference that local winters at 30-28 ka BP were much colder than at present. |
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 |
Paleotemperatures in the lower Kolyma river, Plakhinskii Yar site |
title_short |
Paleotemperatures in the lower Kolyma river, Plakhinskii Yar site |
title_full |
Paleotemperatures in the lower Kolyma river, Plakhinskii Yar site |
title_fullStr |
Paleotemperatures in the lower Kolyma river, Plakhinskii Yar site |
title_full_unstemmed |
Paleotemperatures in the lower Kolyma river, Plakhinskii Yar site |
title_sort |
paleotemperatures in the lower kolyma river, plakhinskii yar site |
publisher |
PANGAEA |
publishDate |
2020 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.914981 https://doi.org/10.1594/PANGAEA.914981 |
op_coverage |
LATITUDE: 68.678800 * LONGITUDE: 160.285200 |
long_lat |
ENVELOPE(161.000,161.000,69.500,69.500) ENVELOPE(151.300,151.300,70.917,70.917) ENVELOPE(86.407,86.407,67.938,67.938) ENVELOPE(161.250,161.250,68.783,68.783) ENVELOPE(160.285200,160.285200,68.678800,68.678800) |
geographic |
Kolyma Yar Plakhino Karetovo |
geographic_facet |
Kolyma Yar Plakhino Karetovo |
genre |
Arctic Ice kolyma river permafrost wedge* Yakutia |
genre_facet |
Arctic Ice kolyma river permafrost wedge* Yakutia |
op_relation |
Vasil'chuk, Yurij K; Vasil'chuk, Alla Constantinovna (2018): Winter air paleotemperatures at 30-12 ka BP in the lower. Kolyma River, Plakhinskii Yar yedoma: evidence from stable isotopes. Earth's Cryosphere, XXII(5), https://doi.org/10.21782/KZ1560-7496-2018-5(3-19) Fukuda, M; Nagaoka, D; Saijyo, K; Nakamura, T; Kunitsky, Victor V (1997): Radiocarbon dating results of organic materials obtained from Siberian permafrost areas. Rep. Inst. Low Temperature Sci., Hokkaido University, Sapporo, 17-28 Konyakhin, M A; Mikhalev, D V; Solomatin, V I (1996): Oxygen Isotope Composition of Ground Ice. Moscow University Press, Moscow (in Russian), 156pp. Nikolaev, Vladimir I; Mikhalev, D V; Romanenko, Fedor A; Brilli, M (2010): Reconstruction of the formation conditions for permafrost in Northeastern Russia from isotope data (example fromreference sections in the lower Kolyma Lowland). Led i Sneg, 50(4), 79-90 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 Vasil'chuk, Yurij K; Vasil'chuk, Alla Constantinovna; van der Plicht, Johannes; Kutschera, V; Rank, D (2001): Radiocarbon dating of the Late Pleistocene ice wedges in the Bison section in the lower reaches of the Kolyma River. Doklady Earth Sciences, 379(5), 589-593 https://doi.pangaea.de/10.1594/PANGAEA.914981 https://doi.org/10.1594/PANGAEA.914981 |
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.914981 https://doi.org/10.21782/KZ1560-7496-2018-5(3-19 https://doi.org/10.7256/2453-8922.2016.1.21310 |
_version_ |
1766302256012984320 |