The review examines Antarctic sea ice over the last 130,000 years, using modern observations, models and evidence preserved in paleoclimate archives. It considers how sea ice interacts with ocean and atmospheric circulation, ice sheets and ice shelves, marine productivity, and the carbon cycle.

The authors report strong evidence from theory and models that changes in Antarctic sea ice can affect other parts of the Earth system. Paleoclimate records provide examples of sea-ice changes occurring at the same time as changes in ocean circulation, marine productivity and the carbon cycle.