Paleotemperatures in the lower Kolyma river, Plakhinskii Yar site

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Autores principales: Vasil'chuk, Yurij K, Vasil'chuk, Alla Constantinovna
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2020
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author Vasil'chuk, Yurij K
Vasil'chuk, Alla Constantinovna
author_facet Vasil'chuk, Yurij K
Vasil'chuk, Alla Constantinovna
collection Datos científicos de ciencias marinas y ambientales
contents 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 Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_914981
institution PANGAEA
language en
publishDate 2020
publisher PANGAEA
record_format pangaea
spellingShingle Paleotemperatures in the lower Kolyma river, Plakhinskii Yar site
Vasil'chuk, Yurij K
Vasil'chuk, Alla Constantinovna
ice wedge; Late Pleistocene; northeastern Yakutia; oxygen isotope; Permafrost; Plakhino site; pollen and spores; Radiocarbon; water chemistry; Yedoma
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.
title Paleotemperatures in the lower Kolyma river, Plakhinskii Yar site
topic ice wedge; Late Pleistocene; northeastern Yakutia; oxygen isotope; Permafrost; Plakhino site; pollen and spores; Radiocarbon; water chemistry; Yedoma
url https://doi.org/10.1594/PANGAEA.914981