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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ftdatacite:10.1594/pangaea.914981 2023-05-15T16:36:53+02:00 Paleotemperatures in the lower Kolyma river, Plakhinskii Yar site Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna 2020 application/zip https://dx.doi.org/10.1594/pangaea.914981 https://doi.pangaea.de/10.1594/PANGAEA.914981 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://dx.doi.org/10.21782/kz1560-7496-2018-5(3-19) https://dx.doi.org/10.7256/2453-8922.2016.1.21310 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY ice wedge Late Pleistocene northeastern Yakutia oxygen isotope permafrost Plakhino site pollen and spores radiocarbon water chemistry Yedoma Collection of Datasets article Collection 2020 ftdatacite 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 2022-02-09T13:19:56Z 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. : Data was submitted and proofread by Yurij K Vasil'chuk and Lyubov Bludushkina at the faculty of Geography, department of Geochemistry of Landscapes and Geography of Soils, Lomonosov Moscow State University. Article in Journal/Newspaper Ice kolyma river permafrost wedge* Yakutia DataCite Metadata Store (German National Library of Science and Technology) Karetovo ENVELOPE(161.250,161.250,68.783,68.783) Kolyma ENVELOPE(161.000,161.000,69.500,69.500) Plakhino ENVELOPE(86.407,86.407,67.938,67.938) Yar ENVELOPE(151.300,151.300,70.917,70.917) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
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. : Data was submitted and proofread by Yurij K Vasil'chuk and Lyubov Bludushkina at the faculty of Geography, department of Geochemistry of Landscapes and Geography of Soils, Lomonosov Moscow State University. |
format |
Article in Journal/Newspaper |
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 - Data Publisher for Earth & Environmental Science |
publishDate |
2020 |
url |
https://dx.doi.org/10.1594/pangaea.914981 https://doi.pangaea.de/10.1594/PANGAEA.914981 |
long_lat |
ENVELOPE(161.250,161.250,68.783,68.783) ENVELOPE(161.000,161.000,69.500,69.500) ENVELOPE(86.407,86.407,67.938,67.938) ENVELOPE(151.300,151.300,70.917,70.917) |
geographic |
Karetovo Kolyma Plakhino Yar |
geographic_facet |
Karetovo Kolyma Plakhino Yar |
genre |
Ice kolyma river permafrost wedge* Yakutia |
genre_facet |
Ice kolyma river permafrost wedge* Yakutia |
op_relation |
https://dx.doi.org/10.21782/kz1560-7496-2018-5(3-19) https://dx.doi.org/10.7256/2453-8922.2016.1.21310 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
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 |
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