Historic Antarctic Core Drilling Unveils 23-Million-Year Climate Record, Impacts on Future Sea Levels

February 18, 2026
Historic Antarctic Core Drilling Unveils 23-Million-Year Climate Record, Impacts on Future Sea Levels
  • Researchers used marine microfossils for preliminary dating and plan to apply multiple techniques through a ten-country collaboration to refine the sediment timeline.

  • A multinational team drilled a 228-meter-long sediment core beneath Crary Ice Rise in West Antarctica, the longest ever retrieved from under an ice sheet, revealing a 23-million-year climate record.

  • The expedition ties into broader debates on climate policy, sea-level rise, and ice-sheet stability in a warming world.

  • Samples from the 228-meter core are en route to New Zealand for analysis by researchers across ten countries to determine past temperatures and melting conditions relevant to future sea-level rise.

  • Certain sediment layers contain shells and marine remnants, indicating periods when the region was open ocean and the ice sheet was temporarily absent.

  • The operation involved 29 scientists and support personnel living in tents, with major logistical support from Antarctica New Zealand and the U.S. NSF, reflecting extensive cross-continental cooperation.

  • The expedition site is remote, underscoring the significant logistical and technical challenges of Antarctic drilling and core collection.

  • The core provides a 23-million-year environmental record, including warmer-than-present periods, offering crucial data on how the ice sheet may respond to warming temperatures and thresholds.

  • Preliminary dating suggests the record spans the last 23 million years, capturing warmer global climates and informing predictions about ice-sheet retreat under future warming.

  • The Crary Ice Rise site lies near potential breakup pathways toward the Ross Ice Shelf, about 700 kilometers from the nearest Antarctic station.

  • West Antarctica holds enough ice to raise global sea levels by several meters if melted, and satellite data show accelerating mass loss amid uncertain tipping-point temperatures.

  • Findings ground-truth past open-ocean conditions in the region and inform models of the West Antarctic Ice Sheet’s response to future warming, including potential sea-level contributions.

Summary based on 3 sources


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