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Significance The seas are rising as the planet warms, and reconstructions of past sea level provide critical insight into the sensitivity of ice sheets to warmer temperatures. Past sea level is reconstructed from the geologic record by measuring the elevations of fossilized marine sediments and coral reefs. However, the elevations of these features also record local uplift or subsidence due to the growth and decay of ice sheets since the time of deposition. We compare observations of paleo sea level across the Bahamian archipelago with a range of Earth deformation models to revise estimates of the last interglacial global mean sea level. Our results suggest that polar ice sheets may be less sensitive to high-latitude warming than previously thought.

Sea-level trends across The Bahamas constrain peak last interglacial ice melt