Glacial and climate history of the last 24 000 years in the Polar Ural Mountains, Arctic Russia, inferred from partly varved lake sediments

• Published in: Boreas
• Main Authors: Regnéll, Carl, Haflidason, Haflidi, Mangerud, Jan, Svendsen, John Inge
• Other Authors: Norges Forskningsråd
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2018
• Subjects: Arctic; glacier; ural mountains
• Online Access: http://dx.doi.org/10.1111/bor.12369; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbor.12369; https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12369; https://onlinelibrary.wiley.com/doi/full-xml/10.1111/bor.12369

We present a well‐dated, high‐resolution and continuous sediment record spanning the last c . 24 000 years from lake Bolshoye Shchuchye located in the Polar Ural Mountains, Arctic Russia. This is the first continuous sediment succession reaching back into the Last Glacial Maximum ( LGM ) ever retrieved from this region. We reconstruct the glacial and climate history in the area since the LGM based on sedimentological and geochemical analysis of a 24‐m‐long sediment core. A robust chronology was established using a combination of AMS 14 C‐dating, the position of the Vedde Ash and varve counting. The varved part of the sediment core spans across the LGM from 24 to 18.7 cal. ka BP . We conclude that the lake basin remained ice‐free throughout the LGM , but that mountain glaciers were present in the lake catchment. A decrease in both glacial varve preservation and sedimentation rate suggests that these glaciers started to retreat c . 18.7 cal. ka BP and had disappeared from the catchment by 14.35 cal. ka BP . There are no indications of glacier regrowth during the Younger Dryas. We infer a distinct climatic amelioration following the onset of the Holocene and an Early to Middle Holocene thermal optimum between 10–5 cal. ka BP . Our results provide a long‐awaited continuous and high‐resolution record of past climate that supplements the existing, more fragmentary data from moraines and exposed strata along river banks and coastal cliffs around the Russian Arctic.