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Deep beneath Antarctica's ice, scientists have drilled 523 meters through solid ice at Crary Ice Rise—and recovered a 228-meter sediment core that spans 23 million years of Earth's climate history. The international SWAIS2C project has achieved what no one has done before: a direct, detailed record of how the West Antarctic Ice Sheet responded to past warming above 2°C. If the West Antarctic Ice Sheet collapses entirely, global sea levels could rise by 4–5 meters. This core could tell us how fast that might happen—and at what temperature thresholds. Key discoveries: The Record: Sediment layers span 23 million years, including periods when global temperatures were significantly higher than 2°C above pre-industrial. Evidence of Open Ocean: Fragments of shells and light-dependent marine organisms suggest the area was once ice-free—implying past collapse of the Ross Ice Shelf and parts of the ice sheet. Diverse Sediments: From fine mud to compact gravel with embedded rocks—indicating shifting environments: ice sheet, open ocean, ice shelf, calving margins. Engineering Feat: Two previous attempts failed. This team drilled deeper than any previous sub-ice sediment core (10m previously; now 200m). Operated 700km from nearest station, in continuous shifts, using hot-water drill and riser pipe. What's Next: Detailed analysis to pinpoint when retreats occurred and what triggered them—critical data for sea-level rise projections. A window into Earth's past—and a warning for its future. Boost your science knowledge with top courses! Explore cutting-edge science on Udemy: https://ecef.pushed.click/das8qbs5 Your support fuels our shorts and videos—thank you!