Since the beginning of the twentieth century, the global ocean has undergone unprecedented changes caused by global warming (Gillett et al., 2021;Stocker et al., 2013). These changes are notably pronounced in the Arctic region due to polar amplification with major consequences for sea-ice cover and the thermohaline circulation (Cavalieri et al., 1997;Shindell & Faluvegi, 2009). The Arctic Ocean and its marginal seas are characterized by large seasonal sea-ice changes. Melting in summer and sea-ice formation in winter, including coastal polynyas, through the production of cold and saline waters, alter deep-water formation and subsequently the Arctic Ocean circulation (Arrigo, 2014;Cai et al., 2010;Overland & Wang, 2013;Xiao et al., 2013). At the current rate of decline (0.42% year −1 ), the Arctic Ocean may be ice-free in summer season in the next 50 or even 30 years (Comiso, 2012;Wang et al., 2019), which will profoundly impact the global climate and carbon cycle and further accelerate global warming causing damages to the polar ecosystems (Moline et al., 2008). In Arctic marginal seas changes in sea-ice cover and thickness involve different thermodynamic and dynamic factors (Polyakov et al., 2003). In the case of the East Siberian Sea (ESS), land run-off and atmospheric circulation are controlling factors of the sea-ice distribution (Park et al., 2020;Rigor & Wallace, 2004).Our knowledge on natural variability of Arctic sea ice and on-going changes are limited by the lack of long time series observations. Information on past sea-ice distribution can be obtained from micropaleontological fossils (