Abstract
The activation of modern sedimentation on the shallows of the Laptev Sea, which underwent exclusively erosion in the past, has been revealed. It occurs against the background of rising sea levels. In this activation, the key role of reducing the area of sea ice, cryogenic and hydrodynamic processes, initiated by climate warming, was established. Sedimentation, accompanied by the formation of islands, is confined to positive uplift morphostructures.
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