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Analysis of sediment core from Chukchi Sea reveals that carbon mobilization via permafrost thaw was more than twice as high during the end of the deglaciation (~13 K yr BP) as compared to the late Holocene. https://t.co/9rls1tMndX
Analysis of sediment core from Chukchi Sea reveals that carbon mobilization via permafrost thaw was more than twice as high during the end of the deglaciation (~13 K yr BP) as compared to the late Holocene. https://t.co/9rls1tMndX
Remobilization of old permafrost carbon to Chukchi Sea sediments during the end of the last deglaciation https://t.co/f3qfAzbwND