Holocene January paleotemperature of northwestern Siberia reconstructed based on stable isotope ratio of ice wedges

• Published in: Permafrost and Periglacial Processes
• Main Authors: Vasil'chuk, Yurij K., Vasil'chuk, Alla C., Budantseva, Nadine A.
• Other Authors: Russian Foundation for Basic Research
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2022
• Subjects: Ice; permafrost; Permafrost and Periglacial Processes; Thermokarst; wedge*; Siberia
• Online Access: http://dx.doi.org/10.1002/ppp.2177; https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.2177; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/ppp.2177

Abstract Ice wedges are considered as a paleoarchive of winter air temperatures as their stable isotope composition has been widely used to reconstruct winter climatic conditions in the Arctic regions. Ice wedge stable isotope records, obtained in recent decades for many Arctic permafrost areas of Russia and North America, demonstrate a clear shift from lower to higher values between the Late Pleistocene and Holocene (by 5–10‰ for δ 18 O values in some regions of the Russian Arctic), which is widely accepted as evidence of winter air temperature increase. However, the evolution of winter air temperatures during the Holocene is less clear and, according to proxy reconstructions, winter climate trends are not synchronous and may significantly vary throughout the Arctic. In this study, we investigate the stable isotope composition of Holocene syngenetic ice wedges and modern ice veinlets of northwestern Siberia. Radiocarbon dating of enclosing sediments and a few dates of organic material from ice wedges demonstrate that ice wedges grew constantly within the study area during the Holocene though early–mid‐Holocene in northwestern Siberia is often considered as a thermal optimum. In fact, many proxy records indicate an increase of summer air temperatures followed by thermokarst activity, peatland formation, and northward advance of the treeline. According to our data, winter climate conditions in terms of mean air temperature of the coldest winter month (January) did not change significantly during the key Holocene stages, and during the Greenlandian and most of the Northgrippian stages (between 11.4 and 6 cal ka BP) mean January air temperature ( T mJ ) varied between −21 and −30°C, and from the end of the Northgrippian, during the Meghalayan stages of Holocene (5.2–0.9 cal ka BP), T mJ varied between −24 to −28°C. Mean January air temperature during the Holocene was generally 1–2°C lower than the modern one, meanwhile the submeridional direction of T mJ isotherms and eastward decrease of T mJ values in Holocene ...