Аннотация:. Here, we present a new ice-wedge based oxygen isotope record from the Oyogos Yar mainland coast (Northeast Siberian Arctic), based on paired stable-isotope and radiocarbon age spanning the last two millennia. The record confirms the long-term winter warming signal as well as the unprecedented temperature rise in the last decades. This demonstrates that winter warming over the last millennia is a coherent feature in the Northeastern Siberian Arctic, supporting the hypothesis of an insolation-driven seasonal Holocene temperature evolution followed by a strong warming most likely related to anthropogenic forcing.