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2. Evolution of a high-latitude sediment drift inside a glacially-carved trough based on high-resolution seismic stratigraphy (Kveithola, NW Barents Sea). (1st September 2016)

3. Evolution of a high-latitude sediment drift inside a glacially-carved trough based on high-resolution seismic stratigraphy (Kveithola, NW Barents Sea). (1st September 2016)

7. Simulated last deglaciation of the Barents Sea Ice Sheet primarily driven by oceanic conditions. (15th June 2020)